IASC Workshop on the dynamics andmass budget of Arctic glaciers

Abstracts and program
Network on Arctic Glaciology annual meeting &IASC cross-cutting activity on “Glacier-ocean interactions
and their impact on Arctic marine ecosystems”
28-30 January 2020, Obergurgl, Austria
Organised by:
Thorben Dunse, Ward van Pelt, Jakob Abermann and Michael Kuhn

Network on Arctic Glaciology

Cover photo: Pancake ice and bergy bits from surging Tunabreen mix at the headof Tempelfjorden in Svalbard. (Photo: T. Dunse)

ISBN: 978-90-393-7337-8

Participants of the 2020 IASC workshop on Arctic Glaciology in Obergurgl, Austria.
(Photo: T. Dunse)Contents
Preface . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

3

Programme . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

4

Posters . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

8Participants . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

9Minutes of the cross-cutting discussion . . . . . . . . . . . . . . . . . . . . .

11

Introduction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

11

Extended discussion about today’s talks . . . . . . . . . . . . . . . . . . . . . .

11

Key knowledge gaps and how to address? . . . . . . . . . . . . . . . . . . . . .

11

Follow-up/suggestions for new cross-cutting activities? . . . . . . . . . . . . .

12

Minutes of the IASC-NAG open forum meeting . . . . . . . . . . . . . . . .

13

Abstracts . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

16

Arctic land ice regional albedo products from Sentinel-3 . . . . . . . . . . . .

16

Multi-year observations of calving activity and front geometry of two marine terminating outlet glaciers . . . . . . . . . . . . . . . . . . . . . . . . . . . .

17First results from new automated instruments measuring snow water equivalent (SWE) and position/ elevation/ tilt/ rotation on the Greenland Ice
Sheet in the INTAROS project . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 18
Calculating ice volume changes of a small icefield within the CanadianHigh Arctic using Structure from Motion . . . . . . . . . . . . . . . . . . . . . . .

19

Local climate of Zachary glacier, North East Greenland . . . . . . . . . . . . .

20

Predicting Runoff from Ungauged Partially Glaciated Basins in South West
Greenland . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

21

Estimating the contribution of trace metal contaminants from Devon Ice
Cap, NU to the Ocean (2005-2015) . . . . . . . . . . . . . . . . . . . . . . . . . .

22The effect of debris cover and frontal ablation on projections of glaciermass change in Alaska using the Python Glacier Evolution Model (PyGEM)

23

Reinterpreting the surge of Good Friday Glacier, Axel Heiberg Island, Canadian Arctic . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

24

Fjord stratification controls surface emergence of glacial plumes . . . . . .

25

Impact of frontal ablation on the ice thickness estimation of marine-terminating
glaciers in Alaska . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 26
Recent increase in marine ablation of Svalbard glaciers . . . . . . . . . . . .

27

Understanding ice-ocean interactions with detailed observations of terminus behavior . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

28

An icestream margin as seen with high resolution radar . . . . . . . . . . . .

29

On current changes of the Greenland Runoff Limit . . . . . . . . . . . . . . . .

30

The potential of the Wegener Greenland expedition material for modern
glaciological research . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

31

1

5 Years of Arctic Land Ice Velocity and Discharge observed by Sentinel-1 .

32

Albedo of the Cryosphere from Sentinel-3 . . . . . . . . . . . . . . . . . . . . .

33

Decadal scale ice velocity change in the interior of the Greenland Ice Sheet 34
Investigating spatiotemporal patterns in Greenland glacier terminus changes
using automated edge detection in satellite images . . . . . . . . . . . . . . . 35
Glacier retreat in Sørkapp Land, Spitsbergen, from 1961 to 2010 based on
aerial photographs . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

36

Changes in snow cover structure on Hansbreen from repeated radio-echosounding . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

37

Greenland liquid water runoff from 1979 through 2017 . . . . . . . . . . . . .

38

Mapping glacier extent in Norway using Sentinel-2 . . . . . . . . . . . . . . .

39

Causes and patterns of tidewater glacier retreat in the Canadian Arctic . .

40

Snow Cover Reflection Properties on Hansbreen (South Spitsbergen) basedon radio-echo sounding . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

41

How oceanic melt controls tidewater glacier evolution . . . . . . . . . . . . .

42

Patterns and mechanisms of flood release from glacier dammed Donjek
Lake, Yukon . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

43Comprehensive ocean observations in Inglefield Bredning, Northwestern
Greenland . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

44

Synoptic conditions and atmospheric moisture pathways associated withvirga and precipitation over coastal Adélie Land, Antarctica . . . . . . . . . .

45

Hydrological processes in firn at the runoff limit on the Greenland Ice Sheet 46
Land-ice mass imbalance across the Arctic driven by atmosphere andocean forcing . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

48

Basal conditions of Kongsvegen at the onset of surge - revealed using
seismic vibroseis surveys . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

49

IPCC’s Special Report on the Oceans and the Cryosphere in a Warming
Climate - Key messages for the Arctic . . . . . . . . . . . . . . . . . . . . . . . .

50

Short-term ice speed variations near the calving front of Bowdoin Glacier,northwestern Greenland . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

51

The uncertainty of average precipitation forcing . . . . . . . . . . . . . . . . .

52

Future climatic mass balance, snow conditions and runoff in Svalbard . . .

53

Photos to Elevations: a photogrammetry pipeline . . . . . . . . . . . . . . . .

54

Preface
This year’s IASC Workshop on the Dynamics and Mass Budget of Arctic Glaciers &the IASC Network on Arctic Glaciology Annual Meeting took place at the University Centre Obergurgl, in Obergurgl, Austria, 28-30 January 2020. The workshop
hosted a cross-cutting activity on "Glacier-ocean interactions and their impact on
Arctic marine ecosystems" and attracted 41 participants representing 14 countries. The workshop was jointly sponsored by the IASC Cryosphere and Marine
Working Groups, involved in the cross-cutting activity. This also allowed for travel
support of twelve early-career scientists.
Two-and-a half days of scientific sessions with oral presentations and posters
addressed a variety of topics related to glacier mass balance, dynamics andglacier-ocean interactions. Across the Arctic, glacier mass budget and dynamics strongly correlate with air temperature. The influence of oceanic forcing on
tidewater-glacier dynamics and frontal ablation varies with region and appears tobe less important in Arctic Canada (Copland et al.) than in Greenland (Catania etal.). In her keynote talk, Ginny Catania demonstrated that the strong heterogeneity in dynamic response of tidewater glaciers in Greenland is linked to bedrock
topography. Advances in satellite remote sensing facilitate monitoring of glacierflow across the Arctic at high temporal and spatial resolution (Wuite et al.). Several talks highlighted the importance of subglacial discharge plumes for marine
primary production in glacier fjords (e.g. Kanna et al.). However, plumes have
only a positive effect on marine productivity, if they reach surface waters. Thisdepends on discharge volume and depth, but also fjord stratification (De Andrés).
A better understanding of water masses and fjord circulation is thus needed whenassessing impacts of glacier runoff on marine ecosystems. Timeseries of glacier
freshwater runoff in both solid and liquid form are now becoming available for various Arctic regions (e.g. Wuite et al., Mankoff et al. and Van Pelt et al.). Statisticalmodelling helps to enhance the performance of climatic mass balance models andimproved uncertainty assessments of model parameters and climatic input data
(e.g. Rounce et al. and Zolles et al.).
During the open forum meeting, Ward van Pelt was elected new chairman of the
IASC Network on Arctic Glaciology. He will be supported by Wesley van Wychen
as new vice-chair. I wish the new team best of luck with upcoming network activities. Finally, I would like to thank all participants for their contributions to theworkshop. I hope we all meet again at the next workshop and annual meetingin Poland (2021), followed by workshops in Japan in 2022, and again, Obergurgl,
Austria in 2023.

Sogndal, Norway – February 20203

Programme
The meeting takes place at the University Centre in Obergurgl, Austria, 28 - 30
January, 2020.

Monday 27 January
ARRIVAL
19:00 - 21:00

DinnerPlease inform the University Center if you arrive late and whish
dinner after 21:00

Tuesday 28 January
08:30 - 09:00

Registration: pick up your name badge and copy of program.
Please upload your presentations for the morning session.

09:00 - 09:10

WelcomeSession I:

Remote sensing (part I)

Convener:

Tobias Zolles

09:10 - 09:30

5 Years of Arctic Land Ice Velocity and Discharge observed by
Sentinel-1 Jan Wuite, Thomas Nagler, Markus Hetzenecker,
Ludivine Libert, Lars Keuris, Helmut Rott

09:30 - 09:50

Calculating ice volume changes of a small icefield within the
Canadian High Arctic using Structure from Motion Braden
Smeda, Dorota Medrzycka, Luke Copland, Laura Thomson

09:50 - 10:10

Albedo of the Cryosphere from Sentinel-3 Jason Box, Baptiste
Vandecrux, Alex Kokhanovsky, Adrien Wehrlé, Kenneth Mankoff

10:10 - 10:40

Coffee break

Session II:

Calving & Frontal ablation

Convener:

Julia Liu

10:40 - 11:00

Multi-year observations of calving activity and front geometry of
two marine terminating outlet glaciers Andrea Walter, Martin
P. Lüthi, Martin Funk, Andreas Vieli

11:00 - 11:20

Recent increase in marine ablation of Svalbard glaciers Geir
Moholdt, Jack Kohler, Ashley Morris, Josephine Maton, Alex
Gardner, Johannes Fürst

11:20 - 11:40

How oceanic melt controls tidewater glacier evolution Martin
Lüthi, Rémy Mercenier, Andreas Vieli411:40 - 12:00

The effect of debris cover and frontal ablation on projections ofglacier mass change in Alaska using the Python Glacier
Evolution Model (PyGEM) David Rounce, Regine Hock

12:00 - 15:45

Lunch & ski break

15:45 - 16:15

Coffee break

16:15 - 17:00

Poster introductions(1-2 slides and max. 2 minutes per person)

Convener:

Jakob Abermann

17:00 - 18:30

Poster session

19:00 - 20:30

DinnerWednesday 29 January
Session III:

Cross-cutting session (part I)

Convener:

Thorben Dunse

09:00 - 09:30[Keynote] Understanding ice-ocean interactions with detailed
observations of terminus behavior Ginny Catania, Mason Fried,
Denis Felikson, Leigh Stearns

09:30 - 09:50

Fjord stratification controls surface emergence of glacial plumes
Eva De Andrés, Donald A. Slater, Fiamma Straneo, Jaime
Otero, Sarah Das, Francisco Navarro

09:50 - 10:10

Greenland liquid water runoff from 1979 through 2017 Ken
Mankoff, Andreas Ahlstrøm, Xavier Fettweis, Brice Noël10:10 - 10:30

Coffee break

Session IV:

Cross-cutting session (part II)

Convener:

Shin Sugiyama

10:30 - 10:50

Causes and patterns of tidewater glacier retreat in the Canadian
Arctic Luke Copland, Alison Cook, Brice Noel, Chris Stokes,
Michael Bentley, Martin Sharp, Robert Bingham, Michiel van den
Broeke

10:50 - 11:10

Comprehensive ocean observations in Inglefield Bredning,Northwestern Greenland Naoya Kanna, Shin Sugiyama, Takuto
Ando, Izumi Asaji, Yefan Wang, Yuta Sakuragi

11:10 - 11:30

Land-ice mass imbalance across the Arctic driven byatmosphere and ocean forcing Noel Gourmelen, Paul Tepes,
Michel Tsamados, Pete Nienow, Andrew Shepherd, Flora
Weissgerber

11:30 - 12:00

Cross-cutting discussion

12:00 - 15:30

Lunch & ski break

15:30 - 16:00

Coffee break

Session V:

Glacier dynamics

Convener:

Will Kochitzky

16:00 - 16:20

Reinterpreting the surge of Good Friday Glacier, Axel Heiberg
Island, Canadian Arctic Dorota Medrzycka, Luke Copland,
Wesley Van Wychen, David Burgess

16:20 - 16:40

Decadal scale ice velocity change in the interior of theGreenland Ice Sheet Josh Williams, Noel Gourmelen, Pete
Nienow

16:40 - 17:00

Short-term ice speed variations near the calving front of
Bowdoin Glacier, northwestern Greenland Shin Sugiyama,
Shun Tsutaki, Daiki Sakakibara, Izumi Asaji

17:00 - 17:10

Short break

17:10 - 18:30

IASC Network on Arctic Glaciology – Open forum meeting

19:00 - 20:30

DinnerThursday 30 January
Session VI:

Glacier mass budget

Convener:

Danielle Hallé

09:00 - 09:20

The uncertainty of average precipitation forcing Tobias Zolles,
Andreas Born

09:20 - 09:40

IPCC’s Special Report on the Oceans and the Cryosphere in a
Warming Climate - Key messages for the Arctic Regine Hock

09:40 - 10:00

Future climatic mass balance, snow conditions and runoff in
Svalbard Ward van Pelt, Thomas Schuler, Veijo Pohjola

10:00 - 10:20

Snow Cover Reflection Properties on Hansbreen (South
Spitsbergen) based on radio-echo sounding Mariusz Grabiec,
Barbara Barzycka, Michał Laska, Dariusz Ignatiuk, Kamil
Kachniarz

10:20 - 10:50

Coffee break

Session VII:

Remote sensing (part II)

Convener:

Nicole Clerx

10:50 - 11:10

Mapping glacier extent in Norway using Sentinel-2 Liss Marie
Andreassen, Teodor Nagy

11:10 - 11:30

Investigating spatiotemporal patterns in Greenland glacierterminus changes using automated edge detection in satellite
images Julia Liu, Ellyn Enderlin, Andre Khalil

11:30 - 11:50

Photos to Elevations: a photogrammetry pipeline Will
Kochtitzky, Dorota Medrzycka, Braden Smeda, Brittany Main,
Moya Painter, Luke Copland, Alex Culley, Warwick Vincent,
Christine Dow

11:50

Final words
followed by lunch / skiing / side events / early departure

19:00 - 20:30

DinnerPosters• Arctic land ice regional albedo products from Sentinel-3, Adrien Wehrlé,
Jason E. Box, Baptiste Vandecrux, Ken D. Mankoff• First results from new automated instruments measuring snow waterequivalent (SWE) and position/ elevation/ tilt/ rotation on the Greenland Ice
Sheet in the INTAROS project, Andreas P. Ahlstrøm, Robert S. Fausto,
Michele Citterio, Roberta Pirazzini, Teijo Arponen, Jason E. Box• Local climate of Zachary glacier, North East Greenland, Carleen Reijmer, S.A.
Khan, E.J. Rignot, M.R. van de Broeke• Predicting Runoff from Ungauged Partially Glaciated Basins in South West
Greenland, Danielle Hallé, Irina Rogozhina, Signe Hillerup Larsen, Andreas
Ahlstrøm• Estimating the contribution of trace metal contaminants from Devon Ice Cap,NU to the Ocean (2005-2015), David Burgess, James Zheng, Wesley van
Wychen• Impact of frontal ablation on the ice thickness estimation ofmarine-terminating glaciers in Alaska, Fabien Maussion, Beatriz Recinos,
Ben Marzeion• An icestream margin as seen with high resolution radar, Heinrich Miller,
Daniel Steinhage, Daniela Jansen, Veit Helm, Dorthe Dahl Jensen, Yan Jie,
Prasad Gogineni• On current changes of the Greenland Runoff Limit, Horst Machguth• The potential of the Wegener Greenland expedition material for modern
glaciological research, Jakob Abermann, Wolfgang Schöner• Glacier retreat in Sørkapp Land, Spitsbergen, from 1961 to 2010 based on
aerial photographs, Justyna Dudek• Changes in snow cover structure on Hansbreen from repeated radio-echosounding, Kamil Kachniarz, Mariusz Grabiec, Michał Laska, Bartłomiej Luks
• Patterns and mechanisms of flood release from glacier dammed Donjek Lake,
Yukon, Moya Painter, William Kochtitzky, Luke Copland, Christine Dow• Synoptic conditions and atmospheric moisture pathways associated with virga
and precipitation over coastal Adélie Land, Antarctica, Nicolas Jullien,
Etienne Vignon, Michael Sprenger, Franziska Aemisegger, Alexis Berne• Hydrological processes in firn at the runoff limit on the Greenland Ice Sheet,
Nicole Clerx, Horst Machguth, Andrew Tedstone• Basal conditions of Kongsvegen at the onset of surge - revealed using seismic
vibroseis surveys, Anja Diez, Emma C. Smith, Olaf Eisen, Coen Hofstede, Jack
Kohler8

Participants
1. Adrien Wehrlé* (Adrien.Wehrle [at] etu.univ-grenoble-alpes.fr)
GEUS, Denmark
2. Andrea Walter (andrea.walter [at] geo.uzh.ch)
University of Zurich & ETH Zurich, Switzerland
3. Andreas P. Ahlstrøm (apa [at] geus.dk)
GEUS, Denmark
4. Braden Smeda (bsmed045 [at] uottawa.ca)
University of Ottawa, Canada
5. Carleen Reijmer (c.h.tijm-reijmer [at] uu.nl)
Utrecht University, The Netherlands
6. Danielle Hallé* (daniehal [at] stud.ntnu.no)Norwegian University of Science and Technology (NTNU), Norway
7. David Burgess (david.burgess [at] canada.ca)
Geological Survey of Canada
8. David Rounce (drounce [at] alaska.edu)
University of Alaska Fairbanks
9. Dorota Medrzycka (dorota.medrzycka [at] uottawa.ca)
University of Ottawa, Canada
10. Eva De Andrés* (eva.deandres [at] upm.es)
Universidad Politécnica de Madrid, Spain
11. Fabien Maussion (fabien.maussion [at] uibk.ac.at)University of Innsbruck, Austria
12. Geir Moholdt (moholdt [at] npolar.no)
Norwegian Polar Institute, Norway
13. Ginny Catania (gcatania [at] ig.utexas.edu)
The University of Texas, USA
14. Heinrich Miller (Heinrich.Miller [at] awi.de)
Alfred Wegener Institut, Germany
15. Horst Machguth (horst.machguth [at] unifr.ch)
University of Fribourg, Switzerland
16. Jakob Abermann (jakob.abermann [at] uni-graz.at)University of Graz, Austria
17. Jan Wuite (jan.wuite [at] enveo.at)
ENVEO, Austria
18. Jason Box (jeb [at] geus.dk)
GEUS, Denmark
19. Jon Ove Hagen (joh [at] geo.uio.no)
University of Oslo, Norway
20. Josh Williams* (j.j.williams-4 [at] sms.ed.ac.uk)
University of Edinburgh, UK
21. Julia Liu* (jukesliu [at] u.boisestate.edu)
Boise State University, USA
22. Justyna Dudek* (justyna_dudek [at] wp.pl)9

Jagiellonian University, Poland
23. Kamil Kachniarz (kachniarz.kamil [at] gmail.com)
University of Silesia, Centre for Polar Studies, Poland
24. Ken Mankoff (kdm [at] geus.dk)
GEUS, Denmark
25. Liss Marie Andreassen (lma [at] nve.no)
NVE, Norway
26. Luke Copland (luke.copland [at] uottawa.ca)
University of Ottawa, Canada
27. Mariusz Grabiec (mariusz.grabiec [at] us.edu.pl)
University of Silesia, Centre for Polar Studies, Poland
28. Martin Lüthi (martin.luethi [at] geo.uzh.ch)
University of Zurich, Switzerland
29. Michael Kuhn (michael.kuhn [at] uibk.ac.at)University of Innsbruck, Austria
30. Moya Painter (MPAIN046 [at] uottawa.ca)
University of Ottawa, Canada
31. Naoya Kanna (kanna [at] arc.hokudai.ac.jp)
Hokkaido University, Japan
32. Nicolas Jullien* (nicolas.jullien [at] unifr.ch)
University of Fribourg, Switzerland
33. Nicole Clerx* (nicole.clerx [at] unifr.ch)
University of Fribourg, Switzerland
34. Noel Gourmelen (noel.gourmelen [at] ed.ac.uk)
University of Edinburgh, UK
35. Olaf Eisen (oeisen [at] awi.de)
AWI, Germany
36. Regine Hock (rehock [at] alaska.edu)
University of Alaska Fairbanks, USA
37. Shin Sugiyama (sugishin [at] lowtem.hokudai.ac.jp)
Hokkaido University, Japan
38. Thorben Dunse (thorben.dunse [at] hvl.no)
Western Norway University of Applied Sciences, Norway
39. Tobias Zolles* (tobias.zolles [at] uib.no)
University of Bergen & Bjerknes Centre for Climate Research, Norway
40. Ward van Pelt (ward.van.pelt [at] geo.uu.se)
Uppsala University, Sweden
41. Will Kochtitzky* (will.kochtitzky [at] uottawa.ca)
University of Ottawa, Canada
Young scientists receiving IASC travel support are marked *.

Minutes of the cross-cutting discussion
Moderator: Thorben Dunse
Minutes: Adrien Wehrlé and Nicolas Jullien, with additions by Carleen Reijmer

Introduction
Thorben Dunse presents the cross-cutting activity, led by the Cryosphere Working Group (Network on Arctic Glaciology) and the Marine Working Group. It aims tobring together experts within glaciology, oceanography and marine biology/ecology.
The two main objectives of the activity are:
• Glacier-ocean interactions: physical and bio-geochemical processes at tidewater glacier margins• Marine pro-glacial ecosystems and their response to glacier processes andglacier change in a warming climate
The activity follows up the previous cross-cutting activity "The importanceof Arctic glaciers for the Arctic marine ecosystem" (two workshops in 2018 and2019).

Extended discussion about today’s talks
In relation to Ginny Catania’s presentation, Jason Box raises the need to identify key glaciers to study. Better bed maps are needed, especially to study key
glaciers. Long term observations are also needed. Martin Lüthi discusses theimportance to understand which glaciers will change soon to monitor them before the beginning of the change. Olaf Eisen mentions the quality problem of
ice-thickness products. Often only profile lines are surveyed, but grids are generally preferable over single lines, as those may miss out overdeepenings. Icesheet
bedrock maps like "Bedmachine" are not reliable everywhere, because of limited survey data. Several people mention that also the bathymetry in front ofglaciers is often unknown, a knowledge gap which needs to be addressed by future projects.

Key knowledge gaps and how to address?
Thorben Dunse refers to a slide by Lorenz Meire presented during last year’s
cross-cutting discussion: "What we need from glaciologists". It contained thefollowing points:

11• Total freshwater flux to individual fjords (both ice and liquid runoff)• Daily runoff estimates for individual catchments• In-situ discharge observations• Volume of subglacial discharge• Data on large events/lakes
Thorben Dunse adds "sediment fluxes and biogeochemical composition of
glacial freshwater discharge" to the list of variables that glaciologists may provide
to marine ecologists. He points out that the first two points with regards to estimating glacier freshwater discharge in form of both meltwater runoff and frontal
ablation, were addressed in many presentations at this workshop.
As previously mentioned, the need for better bedrock/ice thickness maps andbathymetry is highlighted, as well as ice-dynamic modelling, to improve estimatesof frontal ablation.
The need for oceanographic information when assessing ice-ocean interactions
were highlighted in Eva De Andres’ talk, with respect to understanding subglacial
discharge-plume dynamics and whether or not they reach the sea surface. Ginny
Catania suggests future studies coupling field measurements and modelling withremote sensing.
Andreas P. Ahlstrøm touches on glacial sediment fluxes. There are not thatmany requests at the moment but it could become important. GEUS monitores the
Watson river near Kangerlussuaq, Greenland. Jakob Abermann underlines that
the Zackenberg site in Greenland has some data on sediment fluxes. It is notedthat satellite derived ocean-color provides information on the surface extent of
sediment plumes.

Follow-up/suggestions for new cross-cutting activities?
Thorben Dunse reports on the legacy from cross-cutting activity "The importance of Arctic glaciers for the Arctic marine ecosystem" (two workshops in 2018and 2019). A review article has been submitted to The Cryosphere, entitled "Howdoes glacier discharge affect marine biogeochemistry and primary production in
the Arctic" by Mark Hopwood et al., 2019 (https://doi.org/10.5194/tc-2019-136).
Thorben presents key figure 9 of the paper, summarizing direct and indirect effects on how glaciers may fertilize marine ecosystems and the associated spatial
scale at which these processes operate.
Concerning new cross-cutting activities, Regine Hock suggests the topic ofatmosphere-glaciers interactions. This suggestions finds broad support. A groupis formed that will work on a proposal and establish contact with the Atmosphere
Working Group of IASC, including Ward van Pelt, Regine Hock, Carleen Reijmer,
Tobias Zolles and Jason Box.

Minutes of the IASC-NAG open forum
meeting
Chair: Thorben Dunse
Minutes: Danielle Hallé and Nicolas Jullien
Invited to attend: all participants of the workshop.
Agenda
1.
2.
3.
4.
5.
6.

Introduction to IASC, IASC-CWG and NAG
Election of new chair/co-chair
Network Activities and funding opportunities
Upcoming annual meetings
Book of extended abstracts
Anything else?

Ad. 1
Thorben Dunse presents an overview of the International Arctic Science Committee (IASC) and its 5 working groups. IASC is a non-governmental organization
promoting all aspects of Arctic research. IASC provides no research funding, but
supports workshops that stimulate research activity and knowledge exchange.
During the past years, interdisciplinary work is particularly encouraged, by support of cross-cutting activities. These are endorsed by at least 2 WGs, and ideallybridge between social and human and natural sciences. Networks operate within
the framework of the working groups and have a specific research focus. The Network on Arctic Glaciology is a program of the Cryosphere WG and formed out of
the Working Group on Arctic Glaciology (1994-2011). The organizational structure
consists of a chair (Thorben Dunse, since 2016) and vice-chair (Ward van Pelt,
since 2019) and 18 national contacts.
Ad. 2
Prior to the meeting Thorben Dunse informed all national contacts about thenomination of Ward van Pelt, Uppsala University, Sweden, as the new chair.
Ward served as vice-chair since 2019. There was only positive response to thissuggestion, if any.
• Any objections among the audience or other candidate suggestions?
agree with Ward van Pelt as the new chairman.

All• For vice-chair position: one suggestion to swap the vice chair and chair positions.
• Open to suggestions: suggestions to have more diversity for the position,
within gender and geographical diversity.
• Luke Copland suggested Regine Hock as Vice-chair. Regine nominates
Shin Sugiyama. Shin nominates Regine.

13• How much time does it involve? Setting up cross cutting activities and setting
up meeting, proposal writing.
• Everyone agrees to have North American vice chair, potentially Laura Thompson or Wesley van Wychen: positive reaction to this suggestion. Inform
potential candiates by email.
• Final decision next morning: Wesley van Wychen, University of Waterloo,
Canada, is willing to serve as vice chair. The nomination is accepted by theaudience.
Update of national correspondents: There is a 2-year rule stating thatin case of no participation in the network for 2 years, then the national correspondent should be updated. The audience went through the list of the nationalcorrespondents. The following changes were decided/considered:• Austria: Jakob Abermann takes over after Michael Kuhn
• Canada: Martin Sharp retired. Luke Copland new national contact.
• Germany: Olaf Eisen takes over after Heinz Miller.
• Sweden: Ask Per Holmlund to double-check his continued interest to be national contact.
• UK: potential change; Pete Nienow is mentioned as potential candidate• Greenlandic position? Greenland is a not a member country. Kirsty Langley
is mentioned as potential candidate.
Ad. 3• Proposals of special activities offer funding opportunities.
• Higher chance of funding for cross-cutting activities, involving at least 2 IASC
working groups.
• Very good to have funding for ECS. Previous years were able to cover all
expenses but this year was only partial cover.
• Current call for proposals has deadline 1st of March 2020. Next annual meeting is covered by the funding period.
• Suggestions for follow-up and new cross cutting activities:• Regine Hock suggests moving to atmosphere–ice interactions, incl. for example effects of rain on glacier dynamics.
• Any suggestion for whom to contact: contact working group chair and circulate a list of topics; Steven Arnold from UK is chair of the Atmosphere Working
Group.
• Are there any volunteers to write a short proposal to circulate to the working
group? Regine Hock, Carleen Tijm-Reijmer, Tobias Zolles and Jason
Box agree to write proposal together with Ward van Pelt. They will startwith brainstorming now or tomorrow.

Ad. 4
Suggestions for the next annual meeting are Poland, Japan or North America.
Mariusz Grabiec presents options for Poland and suggests Szczryk, close to
Krakow and Katowice. Mariusz and his Polish colleagues have offered to hostthe meeting for the last two years and are willing to organize the meeting in
2021 or 2022. The offer finds very positive response among the audience andso it is agreed that Poland will host the meeting in 2021. Shin Sugiyama andLuke Copland briefly introduce options for Japan and Canada. A vote among theaudience decides in favour of Japan, as host of the 2022 workshop. The workshop
will likely take place in Niseko, Hokkaido. Obergurgl is booked for the end ofJanuary 2023.
Ad. 5• A book of abstracts, including program, participant list and minutes from boththe open forum meeting and XC discussion will be published on the IASC-NAG
website.
• Suggestion to keep publishing abstract and programme book, but to drop
extended abstract. Fine for everyone.
• Participants are encouraged to submit updates and/or corrections of theirabstract (these may inlcude a figure). Any updates should be send to Wardvan Pelt until 07.02.2020.
Ad. 6• Reminder to form a task group to work on proposal for cross-cutting activity.

Abstracts
Arctic land ice regional albedo products from Sentinel3
Adrien Wehrlé1 , Jason E. Box1 , Baptiste Vandecrux1 , Ken D. Mankoff1
1 GEUS, Denmark

Keywords: ice albedo, Sentinel-3
For much of the pre-melt and melt season, sunlight absorption can be the dominant
melt energy source for snow and ice on land, glaciers, seas, and lakes. The Copernicus
ESA Sentinel-3 A and B platforms host two sensors with optical bands: the Ocean Land
Color Instrument (OLCI) and the Sea and Land Surface Temperature Radiometer (SLSTR).
These data enable production of snow/ice albedo for areas of limited terrain complexity.
Algorithms to retrieve snow and ice albedo are after the SICE project using the GitHub
repository https://github.com/mankoff/SICE. The goal is to produce a 3 year daily 1
km albedo product for seven glacierized areas: Greenland, Arctic Canada, Russian High
Arctic (Frans Josef Land, Novaja Zemlja, Severnaya Zemlya), Iceland and Svalbard. Processing is made using the PolarTEP system and the CREODIAS real-time big data repository. Regional examples are given, starting with Greenland and Iceland and on to otherregions in this pan-Arctic albedo assessment.

16

Multi-year observations of calving activity and front geometry of two marine terminating outlet glaciersAndrea Walter1,2 , Martin P. Lüthi1 , Martin Funk2 , Andreas Vieli1
1 University of Zurich, Switzerland
2 ETH Zurich, Switzerland

Keywords: Calving, multi-year observations
By using a terrestrial radar interferometer, pressure sensors and a time-lapse camera we observed two outlet glaciers in West- and Nordwest-Greenland over six and two
years, respectively. The two glaciers are characterised by different geometries and velocity fields. The resulting very detailed dataset provides us new insights on the calving
process and the changes in front geometry. With the time-lapse camera alone, all calving
events of different sizes and styles can be detected but the volume cannot be quantified. The pressure sensors and the terrestrial radar interferometer are limited to detect
calving events of a minimum size. However, the terrestrial radar interferometer allows
us to quantify the volumes of aerial calving events and calving waves measured with thepressure sensors enable us to distinguish between aerial and subaquatic events. We findthat the calving style and size as well as the front geometry is mainly controlled by the
bed topography and the presence of a subglacial discharge plume. The location of theplume can change from year to year, which leads also to changes in the calving pattern.
Calving style and pattern as well as glacier velocity patterns and geometry changes are
additionally compared with environmental conditions such as the temperature and thepresence of ice-mélange in the proglacial fjord.

First results from new automated instruments measuring snow water equivalent (SWE) and position/ elevation/ tilt/ rotation on the Greenland Ice Sheet in the
INTAROS projectAndreas P. Ahlstrøm1 , Robert S. Fausto1 , Michele Citterio1 , Roberta Pirazzini2 , Teijo
Arponen2 , Jason E. Box1
1 GEUS, Denmark
2 FMI, Finland

Keywords: instruments, Greenland ice sheet, observations, weather stations
The monitoring of the Greenland Ice Sheet carried out in PROMICE includes in-situ observations from more than 20 automatic weather and mass balance stations situated on
the ice, mainly in the ablation zone. These stations gather and transmit data in a highly
challenging physical environment, with stations experiencing up to 9 m of ice melting
per year, several metres of snowfall with subsequent compaction, temperatures below-40 degrees C, several months of complete darkness, ferocious Piteraq winds known todestroy entire villages in Southeast Greenland and potential destructive visits from polar bears and Arctic foxes. As we can only visit the remote stations every few years,
instrumental development has to pay primary attention to structural robustness, power
supply and data transmission economy, besides from instrument performance. Yet, thefast changes in the Arctic environment requires new or improved instrumentation, as newparameters needs to be observed, such as rain on the ice sheet. Here we present thefirst results from experimental deployment on the Greenland Ice Sheet of the SnowFox
instrument from HydroInnova, designed to measure the water equivalent of the overlying
snow (SWE) through the attenuation of cosmic-ray neutrons. The sensor records neutron
events over a regular interval and to derive SWE, the raw neutron counting rate of thesensor must be corrected for variations in barometric pressure and solar activity. We will
also present the concepts of a new GNSS instrument developed to improve the determination of position and elevation of the station as it moves with the flowing and melting
ice, as well as our development of instrument characterization facilities and tilt/rotation
instruments to improve the quality of short- and longwave radiation observations.

Calculating ice volume changes of a small icefield within
the Canadian High Arctic using Structure from Motion
Braden Smeda1 , Dorota Medrzycka1 , Luke Copland1 , Laura Thomson2
1 University of Ottawa, Canada
2 Queen’s University, Canada

Keywords: Glaciology, Mass Balance, Photogrammetry, Remote Sensing
There has been a marked increase in melt season length over the past two decades
on glaciers and ice caps within Canada’s Queen Elizabeth Islands (QEI). Prior to the year
2000 (1958-1995) land ice was in a state of slightly negative mass balance (-11.9 +/- 11.5
Gt yr−1 ), but recent GRACE measurements suggest that mass losses between 2003 and2015 averaged -33 +/- 5 Gt yr−1 . These losses have mainly been attributed to meltwaterrunoff, which makes the QEI one of the largest recent contributors to sea level rise outsideof the ice sheets. Despite these losses, there is a paucity of information concerning how
a warming climate is affecting small (<1 km2 ) ice bodies, which are considered sensitive
indicators of change due to their short response time.
In this study we describe the use of historical and contemporary aerial photographs,
high-resolution optical satellite imagery, and ground penetrating radar (GPR) surveys todetermine the area and volume changes of Adams Icefield within Expedition Fiord (Axel
Heiberg Island) over the past six decades. Historical (1959) and contemporary (2019)
digital elevation models (DEMs) were created via aerial photo surveys using Structurefrom Motion photogrammetry. The DEMs were accurately co-registered by combining
direct measurements of camera positions using an aircraft-mounted dual-frequency GPS
system, and multiple ground control points situated around the study region. Volume
changes derived from DEM differencing were validated using 36 years of in-situ massbalance measurements from Baby Glacier (an ice body within Adams Icefield) collectedintermittently between 1959 and 2019, together with 2014 and 2019 GPR surveys. The
results from this study indicate that small ice masses are rapidly declining within the QEI,and support future projections of the life expectancy of these small ice bodies.

Local climate of Zachary glacier, North East Greenland
Carleen Reijmer1 , S.A. Khan2 , E.J. Rignot3 , M.R. van de Broeke1
1 Institute for Marine and Atmospheric Research Utrecht, Utrecht University, The Netherlands
2 Technical University of Denmark, Kgs. Lyngby, Denmark
3 University of California Irvine, Irvine, CA, United States

Keywords: Weather stations, Greenland, in situ, climate
In August 2016, two automatic weather stations (AWS) were placed on Zachariae ice
stream, North East Greenland. They were installed in support of a project investigating
the surface mass balance, ice velocity and calving conditions of Zachariae ice stream.
The stations are full energy balance stations, i.e. they measure all parameters (air temperature, wind speed, relative humidity, air pressure, and short and long wave incoming
and outgoing radiation) necessary to derive the full surface energy balance. In addition,
the stations are equipped with a sonic height ranger in combination with a draw wire tomeasure snow accumulation and ice melt, respectively, and a GPS to monitor glacier velocity. These stations provide insight in the local climate of north east Greenland, a region
for which only limited in situ data is available.
The AWS were located initially at ∼145 m a.s.l., about 13 km from the glacier front(S22), and at ∼535 m a.s.l., about 35 km from the glacier front (S23). Both are moving
reasonably fast (0.5 – 1.5 km/yr) towards the front, which has an impact on observed
variables mainly since station elevation decreases, although changing (surrounding) topography might impact wind and radiation observations. First results show that both sites
exhibit a strong katabatic signature, with directional constancies around 0.9, and windspeeds in winter being twice as strong as in summer. Temperature difference between
the sites reflect the height difference, and is smaller in summer due to the melting surface impacting the near surface temperature. The lapse rate increases from ∼0.5◦ C/100
m in summer to ∼0.7◦ C/100 m in the other seasons. The lower station, S23, is located in
the ablation zone and has experienced on average 2.1 m ice melt over the past 3 years.
At the higher station the mass budget appears to be in balance over this period.

Figure: Site S23 at installation in August 2016 (left) and in August 2017 (right). Instruments aremarked in the left image.

Predicting Runoff from Ungauged Partially Glaciated Basinsin South West Greenland
Danielle Hallé1 , Irina Rogozhina1 , Signe Hillerup Larsen2 , Andreas Ahlstrøm2
1 Norwegian University of Science and Technology (NTNU), Norway
2 Geological Survey of Denmark and Greenland (GEUS), Denmark

Keywords: downscaling, glacier meltwater runoff, Greenland glaciers and ice caps
As meltwater runoff increases from local glaciers and ice caps in Greenland it motivates the need to have better quantification of runoff to improve understanding for
better estimates of global sea level rise and gauging the potential for natural resource
exploitation. 12% of the world’s glaciers and ice caps are contained around the periphery of Greenland and the vast majority lie in partially glaciated basins that are ungauged
and without weather stations. Thereby, resulting in a gap of data available for calculating runoff and leaving climate models as the key for best estimates and predictions.
Currently, calculating meltwater runoff with coarse resolution general circulation models
or even regional climate models do not capture the intricacies of the terrain in a partially glaciated basin and can create large potential for error. This study will present thestrengths and shortcomings of several climate models by comparing them with in situ
observations with a focus on the disparities of the models across Greenland. With the aim
to more accurately calculate and predict runoff. Downscaling will be applied as a tool tobetter resolve 2m temperature and precipitation in partially glaciated basins. Temperature will be downscaled according to the lapse rate and dynamical downscaling will beapplied for precipitation data. The established method for the predicted runoff will beapplied to catchments in Greenland that are of interest in hydropower development anddrinking water exports.

Estimating the contribution of trace metal contaminantsfrom Devon Ice Cap, NU to the Ocean (2005-2015)
David Burgess1 , James Zheng1 , Wesley van Wychen2
1 Geological Survey of Canada, Canada
2 University of Waterloo, Canada

Keywords: Glacier, metals, melt, calving
Natural and anthropogenic contaminants that accumulate in glaciers and ice caps arehighly susceptible to re-mobilization through melting, run-off, and ice dynamics. Intense
melting of Arctic glaciers and ice caps since the mid-2000’s has significantly increased
the volume of glacier meltwater released from ice caps and tidewater glaciers implying
a strong potential for increases in the mass of contaminants at point locations where
glacier meltwater and/or glacier ice is discharged directly into the ocean. Through combined knowledge of the concentration of contaminants in the ice, firn, and snow of Devon
Ice Cap (DIC) found in ice core studies, and the rates of surface melting and iceberg calving fluxes from the major drainage basins of the DIC, we provide a first-order estimateof the amount of trace metals (Pb, Cd and Sb) discharged to the ocean. Ice and meltwater fluxes are modeled for the period 2005-2015 using a combination of output fromthe Regional Atmospheric Climate Model (RACMO) 2.3 and annual in-situ glacier measurements. Rates of iceberg calving derived in previous studies are used to estimate glacierice flux discharged from main tidewater glaciers draining the DIC. Of particular concern
are contaminants deposited since the industrial revolution, which have been stored inhigh elevation firn as they are particularly vulnerable to remobilization due to upwardmigration of the long-term equilibrium line altitude (ELA). Results from this work provide
a first order estimation of the total mass of trace metals removed from the DIC over the
past 15 years, into the local marine ecosystems and eventually to Oceans.

The effect of debris cover and frontal ablation on projections of glacier mass change in Alaska using the Python
Glacier Evolution Model (PyGEM)
David Rounce1 , Zoe Screwvala1 , Regine Hock1
1 University of Alaska Fairbanks, USA

Keywords: debris, frontal ablation, alaska
Glaciers in Alaska are one of the largest contributors to present-day sea level rise andare projected to continue to be a major contributor in the future as well. Understanding the response of these glaciers to future climate forcing is therefore important for all
coastal communities. Alaska is unique in that it has a large mixture of tidewater, laketerminating, clean-ice, and debris-covered glaciers. This makes Alaska an excellent study
area to investigate how frontal ablation and debris cover affect projections of glacier masschange. Given these processes are poorly accounted for in existing global glacier evolution models, there is a critical need to advance how we account for these processes. In
this study, we apply a new method to estimate the debris thickness of debris-covered
glaciers in Alaska. These debris thickness estimates are used to develop a new module in
the Python Glacier Evolution Model (PyGEM) that explicitly accounts for the effects of debris cover. Projections of glacier mass change from 2000-2100 for an ensemble of generalcirculation models (GCMs) and representative concentration pathways (RCPs) are used toquantify how debris cover and frontal ablation affect glacier mass loss and Alaska’s contribution to sea level rise.

Reinterpreting the surge of Good Friday Glacier, Axel
Heiberg Island, Canadian Arctic
Dorota Medrzycka1 , Luke Copland1 , Wesley Van Wychen2 , David Burgess3
1 University of Ottawa, Canada
2 University of Waterloo, Canada
3 Geological Survey of Canada, Canada

Keywords: Glacier surging, Ice dynamics, Arctic Canada
Previous studies suggested that Good Friday Glacier (78◦ 33’N, 91◦ 30’W), a marineterminating outlet glacier in southwestern Axel Heiberg Island (Canadian Arctic), may
have been actively surging in the 1950-60s, 1990s, and again in 2000-15. However, thelength and characteristics of the active phase(s) remained poorly constrained due to thelack of observations between studies.
Based on previous reports extending back to 1948, and a uniquely long (nearly 60
years) dataset of remotely sensed data, this study is the first to reconstruct the evolutionof (what is known as) a surge-type glacier in the Canadian Arctic. We report a sustainedadvance of ∼9 km spanning the last seven decades, which corresponds to the longest
advance ever observed in the Canadian Arctic, and contrasts with the regional trend ofaccelerated mass loss and glacier retreat over this period. Potential mechanisms forthis asynchronous behaviour include a delayed response to past mass balance conditions
and/or dynamic instabilities.
The evolution of ice motion and glacier geometry patterns in the terminus region
throughout the advance underlines the role of bedrock features, including topographic
highs and overdeepenings, in modulating ice motion. We suggest that what has previously been interpreted as the start of a surge in the 1950s, may instead have been alocalised response to small-scale perturbations in bedrock topography. At this point there
is insufficient evidence to attribute the seven decades of uninterrupted advance to glacier
surging in the classic sense of the term.

Fjord stratification controls surface emergence of glacial
plumesEva De Andrés1 , Donald A. Slater2 , Fiamma Straneo2 , Jaime Otero1 , Sarah Das3 , Francisco Navarro1
1 Universidad Politécnica de Madrid
2 Scripps Institution of Oceanography (CA, USA)
3 Woods Hole Oceanographic Institution (MA, USA)

Keywords: Glacier-fjord interactions, fjord freshening, subglacial discharge plumes, nutrient upwelling
Meltwater and sediment-laden plumes at tidewater glaciers, resulting from the localized subglacial discharge of surface melt, influence submarine melting of the glacier andthe delivery of nutrients to the fjord’s surface waters. It is usually assumed that increased
subglacial discharge will promote the surfacing of these plumes. Here, at a west Greenland tidewater glacier, we investigate the counterintuitive observation of a non-surfacing
plume in July 2012 (a year of record surface melting) compared to the surfacing of theplume in July 2013 (an average melt year). We combine oceanographic observations,
subglacial discharge estimates and an idealized plume model to explain the observed
plumes’ behavior and evaluate the relative impact of fjord stratification and subglacial
discharge on plume dynamics. We find that increased fjord stratification prevented theplume from surfacing in 2012, show that the fjord was more stratified in 2012 due toincreased freshwater content, and speculate that this arose from an accumulation of ice
sheet surface meltwater in the fjord in this record melt year. By developing theoreticalscalings, we show in general that fjord stratification exerts a dominant control on plumevertical extent (and thus surface expression), so that studies using plume surface expression as a means of diagnosing variability in glacial processes should account for possible
changes in stratification. We introduce the idea that despite projections of increased
surface melting over Greenland, the appearance of plumes at the fjord surface could in
the future become less common if the increased freshwater acts to stratify fjords aroundthe ice sheet. We discuss the implications of our findings for nutrient fluxes, trapping of
atmospheric CO2 and the properties of water exported from Greenland’s fjords.

Impact of frontal ablation on the ice thickness estimation of marine-terminating glaciers in Alaska
Fabien Maussion1 , Beatriz Recinos2 , Ben Marzeion2
1 Department of Atmospheric and Cryospheric Sciences, University of Innsbruck, Austria
2 Institute of Geography, Climate Lab, University of Bremen, Bremen, Germany

Keywords: tidewater glaciers volume inversion
Frontal ablation is a major component of the mass budget of calving glaciers, strongly
affecting their dynamics. Most global-scale ice volume estimates to date still suffer fromconsiderable uncertainties related to (i) the implemented frontal ablation parameterization or (ii) not accounting for frontal ablation at all in the glacier model. To improve
estimates of the ice thickness distribution of glaciers, it is thus important to identify andtest low-cost and robust parameterizations of this process. By implementing such parameterization into the ice thickness estimation module of the Open Global Glacier Model(OGGM), we conduct a first assessment of the impact of accounting for frontal ablation on
the estimate of ice stored in glaciers in Alaska. We find that inversion methods based on
mass conservation systematically underestimate the mass turnover and, therefore, thethickness of tidewater glaciers when neglecting frontal ablation. This underestimation
can amount to up to 19% on a regional scale and up to 30% for individual glaciers. Our
sensitivity studies also show that differences in thickness between accounting for and notaccounting for frontal ablation occur mainly at the lower parts of the glacier, both aboveand below sea level. This indicates that not accounting for frontal ablation will have an
impact on the estimate of the glaciers’ potential contribution to sea-level rise.

Recent increase in marine ablation of Svalbard glaciers
Geir Moholdt1 , Jack Kohler1 , Ashley Morris1 , Josephine Maton1 , Alex Gardner2 , Johannes
Fürst3
1 Norwegian Polar Institute, Norway
2 NASA-JPL, USA
3 University of Erlangen, Germany

Keywords: calving, glacier, marine, Svalbard
Frontal ablation of tidewater glaciers represents a significant but poorly quantified partof the overall mass budget of Arctic glaciers, as well as an important source of calved ice
and freshwater for marine ecosystems. Here, we will present a detailed analysis of frontal
ablation for all Svalbard’s 200 tidewater glaciers for the period 2013-2018. We accountfor annual changes in frontal position, surface velocity and ice thickness, and separate
mass losses into components of glacier retreat and ice discharge. The actual physicalprocesses of ice melting and calving at the fronts could not be separated. The results
show that ice discharge dominates the total frontal ablation, but that the contribution fromfrontal retreat is more variable from year to year, with a closer link to climate conditions.
About half of the total frontal ablation is related to a handful of glaciers that are surging.
For both surging and non-surging glaciers, we find a marked increase in frontal ablation
between the years 2014-2015 and 2016-2018. We will discuss potential drivers for thissudden change in context of recent atmospheric and oceanic conditions in the Barents
region.

Understanding ice-ocean interactions with detailed observations of terminus behavior
Ginny Catania1 , Mason Fried1 , Denis Felikson2 , Leigh Stearns3
1 University of Texas, Austin, USA
2 NASA, USA
3 Univ. Kansas, USA

Keywords: glacier terminus; ice-ocean interactions;
The terminus region of marine-terminating outlet glaciers represents the regions where
the ice sheet, ocean, and atmosphere all act together through a suite of processes to impact glacier behavior. Several mechanisms have been identified that can cause terminus
retreat, however the long-term impact to glacier dynamics has not been well understood.
In part, this is because not all glaciers behave the same after a terminus perturbation;some glaciers undergo significant retreat and thinning and others do not. In this talk I
explore the role that fjord and glacier topography plays on the dynamic response of outlet glaciers to terminus perturbations by examining the topography both at the glacierterminus, and inland, where it can impact how thinning spreads into the ice sheet interior.
This reveals that topography plays an important role in controlling the total sea-level risefrom marine-terminating glaciers over the next century and we identify smaller glaciersthat have a high potential to contribute to sea-level rise because their topography willallow thinning to spread far inland. Additionally, heterogeneous patterns of glacier geometry around the Greenland Ice Sheet are to a large degree responsible for the observed,
modern heterogeneity in glacier dynamics.

An icestream margin as seen with high resolution radar
Daniela Jansen1 , Daniel Steinhage1 , Heinrich Miller1 , Veit Helm1 , Steven Franke1 , Olaf
Eisen1,2 , Dorthe Dahl Jensen3,4 , Yan Jie5 , Charles O’Neill5 , Prasad Gogineni5
1 Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research, Germany
2 Department of Geoscience, University of Bremen, Germany
3 Niels Bohr Institute, University of Copenhagen
4 Center for Earth Observation Science, University of Manitoba, Canada
5 Remote Sensing Center, University of Alabama, USA

Keywords: Ice stream, radar
In connection with the East Grip ice core drilling project airborne and groundbased
multichannel radar systems were used to look in detail at the internal structures insideand outside of the Northeast Greenland Icestream. While the icestream margins surface
expression is just delineated by slight depressions their internal structures are characterized by rather complicated multifold elements. These features hopefully can be used tobetter characterize the dynamics inherent in icestream systems.

On current changes of the Greenland Runoff Limit
Horst Machguth1
1 Department of Geosciences, University of Fribourg, Switzerland

Keywords: Greenland, firn, hydrology, mass balance
Meltwater running off the flanks of the Greenland Ice Sheet contributes roughly 60%
to its current mass loss, the rest being due to calving. Only meltwater originating frombelow the elevation of the runoff limit leaves the ice sheet, contributing to mass loss; melt
at higher elevations refreezes in the porous firn and does not drive mass loss. Therefore,
any shift in the runoff limit modifies mass loss and subsequent sea level rise contribution.
Here we use Landsat and AVHRR satellite imagery to map the visible runoff limit along
the K-Transect, south-west Greenland. Our analysis covers the time period 1985 to present
and includes the time of direct mass balance measurements along the K-Transect (1990 topresent). Based on the available satellite imagery, we determine for each melt season the
maximum elevation of the visible runoff limit. Comparing the latter to in situ measured
equilibrium line elevation (ELA), we observe that the two parameters fluctuate in parallel
until roughly the year 2002. Subsequently, they appear decoupled, with maximum visible
runoff limit increasing linearly from year to year while ELA continues to fluctuate strongly.
We interpret this loss in synchronisation in the context of changing firn properties. We
postulate that the decoupling of visible runoff limit and ELA is a direct result of a strong
increase of ice content in the near-surface firn. Continuous ice horizons have formed
which nowadays force meltwater to run off. Earlier, when visible runoff limit and ELA
where still synced, meltwater could percolate into porous firn and refreeze. The observedchange in surface hydrology has the potential to increase mass loss along the K-Transect.

The potential of the Wegener Greenland expedition material for modern glaciological research
Jakob Abermann1 , Wolfgang Schöner1
1 Graz University, Austria

Keywords: historical glacier changes; geodetic balance; Greenland
Alfred Wegener contributed extraordinarily to early days of scientific explorations inGreenland. Involved in three expeditions, we present unique historical data that is stored
at Graz University, where Wegener filled his last academic position until his tragic deathin Greenland in 1930. As a first step, we compare the snow and firn densitiy data thathave been collected during the 1912/13 traverse with the recent comprehensive compilation by (Fausto and others, 2018). Furthermore, we focus on the interesting 1929/1930
expedition during which pioneering interdisciplinary approaches have been performed.
Coincidentally, this expedition was carried out during a very warm period that was in factcomparable to recent years (Chylek and others, 2006; Abermann and others, 2017). We
compare melt rates from the years 1929/1930 obtained at Qaamarujuup in West Greenland (Machguth and others, 2016) with geodetically derived thickness changes since the1980s and hypothesize on the different drivers for these changes since the strong masschange during the Wegener expedition occurred during a time with significantly lower
Greenhouse gas levels than today. We discuss overall volume changes by orthorectifying
historical map material and present a potential research avenue to work on process-based
quantification of the drivers for the observed changes, back in the 1930s and today.

5 Years of Arctic Land Ice Velocity and Discharge observed by Sentinel-1
Jan Wuite1 , Thomas Nagler1 , Markus Hetzenecker1 , Ludivine Libert1 , Lars Keuris1 , Helmut Rott1
1 ENVEO, Austria

Keywords: Ice Velocity, Discharge, Sentinel-1, SAR
Recent years have seen major advancements in satellite Earth observation of polar
land ice. Among the most notable are the developments facilitated by the Copernicus
Sentinel program, including the Sentinel-1 SAR mission. The Sentinel-1 constellation,with a dedicated polar acquisition scheme, has provided the opportunity to derive iceflow velocity of Arctic glaciers and ice sheets at an unprecedented scale and temporal
sampling. In Greenland, a continuous observational record of the margins since October
2014, augmented by dedicated annual ice sheet wide mapping campaigns, enabled theoperational monitoring of key climate variables like ice velocity and glacier discharge. In
2019 six additional tracks have been added to the regular acquisition scheme, covering
now also the slow-moving interior of the Greenland Ice Sheet, opening up new opportunities for interferometric applications and permitting to derive monthly ice sheet wide
velocity maps. Based on repeat pass Sentinel-1 SAR data, acquired in IWS mode, we havegenerated a dense archive of ice velocity maps of the polar regions covering the entire
mission duration, now spanning well over 5 years. Including the latest observational data,
we present ice velocity maps of Greenland and other Arctic ice caps, focusing on time series of ice flow fluctuations of major outlet glaciers. The ice velocity maps, complemented
by ice thickness data derived from RES, form the basis for studying ice dynamics anddischarge fluctuations and trends at sub-monthly to multi-annual time scales. Our results
reveal a complex and versatile pattern of ice flow and discharge. This presentation highlights some of the latest developments and results of Sentinel-1 ice flow mapping in the
Arctic, emphasizing the importance of long-term comprehensive monitoring of the polar
ice masses. This is essential for understanding and predicting their response to climaticchanges.

Albedo of the Cryosphere from Sentinel-3
Jason Box1 , Baptiste Vandecrux1 , Alex Kokhanovsky1 , Adrien Wehrlé1 , Kenneth Mankoff1
1 GEUS, Denmark

Keywords: albedo
For much of the pre-melt and melt season, sunlight absorption can be the dominant
melt energy source for snow and ice on land, glaciers, sea, and lakes. Snow and ice
melt feedbacks play a role in Arctic amplification of climate warming. The Copernicus
ESA Sentinel-3 A and B platforms host two sensors with optical bands: the Ocean Land
Colour Instrument (OLCI) and the Sea and Land Surface Temperature Radiometer (SLSTR).
We show OLCI and SLSTR data can be used to produce optical products (chiefly albedo
but also snow surface grain diameter and specific surface area) at high accuracy. This
presentation presents algorithms, validation, products and a near realtime processing
chain. The albedo product used in data assimilation efforts will be presented. Albedo, anessential climate variable (ECV) along with snow cover (also designated an ECV) may be
unified now that the Sentinel-3 mission carries the torch after a very impressive and long
(20 year) performance of the NASA MODIS sensor. The overlap with MODIS now spanning
three years means we can bridge snow albedo to provide a climate scale measurementof snow albedo, a unified ECV.

Decadal scale ice velocity change in the interior of theGreenland Ice Sheet
Josh Williams1 , Noel Gourmelen1 , Pete Nienow1
1 University of Edinburgh, UK

Keywords: Greenland Interior Ice Velocity
Observations of ice dynamical change in the interior of the Greenland Ice Sheet, at distances > 100km from the ice-margin, are sparse, exhibiting very low spatial and temporal
resolution (i.e. Sole et al., 2013; Doyle et al., 2014; Van de Wal et al., 2015). As such, thebehaviour of interior Greenland ice represents a significant unknown in our understandingof the likely response of the ice sheet to oceanic and atmospheric forcing. The observation of a 2.2% increase in ice velocity over a three year period at a location 140 km fromthe ice margin in South West Greenland (Doyle et al., 2014) has been inferred to suggestthat the ice sheet interior has undergone persistent flow acceleration. It remains unclear,
however, whether this observation is representative of wider trends across the ice sheet.
Here, we investigate changes in ice motion within Greenland’s interior by utilising recent satellite-derived ice velocities covering the period 2013-2018 (Gardner et al., 2019)
in conjunction with GPS velocities collected every 30km along the 2000m elevation contour during the mid-1990s (Thomas et al., 2000). Previous observations from the late1990s/early-2000s through to late-2000s/early-2010s have revealed significant speed-ups
at many of Greenland’s tidewater glaciers (i.e. Bevan et al., 2012; Murray et al., 2015),
in contrast to widespread deceleration within the ablation zone of the South West landterminating margin (i.e. Tedstone et al., 2015; Van de Wal et al., 2015; Stevens et al.,2016). The recent availability of satellite data enables us to compare annual ice velocities
from the period 2013-2018 to those collected at GPS stations in the mid-1990s, thereby
enabling us to detect any long-term changes in ice-sheet wide inland ice motion during aperiod of potentially significant dynamic change.

Investigating spatiotemporal patterns in Greenland glacierterminus changes using automated edge detection insatellite images
Julia Liu1 , Ellyn Enderlin1 , Andre Khalil2
1 Boise State University, USA
2 University of Maine, USA

Keywords: automated glacier mapping
The glaciers peripheral to the Greenland Ice Sheet are estimated to have lost 38
Gt/yr from 2003-2009, making them the second largest contributor to glacier mass loss
outside of the ice sheets (Gardner et al. 2013). The difference between total mass loss
estimates and modeled surface mass balance anomalies over this time period suggeststhat mass loss due to increased ice discharge is on the order of 10-20 Gt/yr but there
have not been any ice discharge estimates to confirm this value. To address this gap
in knowledge, we investigate changes at these peripheral glaciers’ termini. In order toefficiently map terminus position changes for hundreds of glaciers, we developed an automated image analysis method adapted from a program used previously in biomedical
and other applied science image analyses. The adapted 2D Wavelet Transform Modulus
Maxima (WTMM) segmentation method places edge detection lines along regions with thegreatest gradient in intensity in the image, such as the contrast between glacier ice andwater or glacier ice and sea ice. We demonstrate that the method is capable of mapping
glacier terminus position changes over a wide range of image conditions with a 1-pixel
uncertainty. Here we use the automated terminus delineations from this method to generate time series of glacier terminus position for 10 sample glaciers over the Landsat-8
record (2013-present). With these time series, we are able to resolve sub-seasonal to annual temporal patterns as well as regional patterns in terminus position change for these
glaciers. Future work will focus on applying the method to the full Landsat record and fullset of peripheral glaciers in order to investigate longer-term trends in glacier retreat.

Glacier retreat in Sørkapp Land, Spitsbergen, from 1961
to 2010 based on aerial photographs
Justyna Dudek1
1 Institute of Geography and Spatial Management, Jagiellonian University, Poland

Keywords: Geodetic mass balance, DEM extraction from aerial photos, Sørkapp Land,
Spitsergen
Intensification of climate change in the polar regions translates into evolution and dynamics of the entire environment, including glacier systems. The visible effect of glacier
response to the contemporary warming is their negative mass balance and frontal recession. This phenomenon is particularly pronounced in southern Svalbard, where glaciers
are losing mass at an accelerating pace. This work presents changes in the geometry of
glaciers located in Sørkapp Land, the southern peninsula of Spitsbergen, over the periodof 1961 to 2010. A baseline dataset for this investigation consisted of aerial photographs,
captured by Norwegian Polar Institute in summer seasons of 1961, 1990 and 2010 and
two consecutive scenes of Landsat 5 TM acquired in the summer of 1990. Using bothscanned analog and digital photographs, as well as digital maps and digital elevation
models derived from their processing, changes in glacier extent and thickness have beenassessed in the following periods: 1961-1990, 1990-2010 and 1961-2010. Results showthat the area occupied by glaciers of Sørkapp Land decreased in the years 1961-2010 by
130 km2 , i.e. by slightly over 15%. The rate of glacier area change varied over time andamounted to 2 km2 /yr in the period 1961-1990 and speeded up to 4 km2 / yr after 1990.
This process was accompanied by glacier surface lowering at an average rate of 1-2 m/yr.

Changes in snow cover structure on Hansbreen fromrepeated radio-echo sounding
Kamil Kachniarz1 , Mariusz Grabiec1 , Michał Laska1 , Bartłomiej Luks2
1 University of Silesia, Centre for Polar Studies, Katowice, Poland
2 Institute of Geophysics, Polish Academy of Sciences, Centre for Polar Studies, Warsaw, Poland

Keywords:
Snow cover plays a key role in the functioning of glacial system. Thermal conductivity
up to 20 times lower than the ice and the albedo reaching 90% make the snow coveran efficient insulator. Furthermore, the snow layer is a freshwater reservoir that initiates
supraglacial, englacial and subglacial drainage. Climate change in particularly sensitive
Arctic area is manifested by general warming, more frequent winter thaws and shorter
snow cover duration. The main purpose of the work is to determine the structure of snow
cover on the glacier and its inter-seasonal variability based on repeated high-frequency
radio-echo sounding. Field studies were carried out on Hansbreen, southwestern Spitsbergen, at the end of the 2018 and 2019 accumulation seasons. With simultaneous usageof two antennas of different frequencies: 800 MHz and 1.6 GHz, the snow cover stratification and their spatiotemporal changes were carried out. Based on the wavelet analysis
up to 17 layers within snow cover were determined, and validated based on properties
derived from manual snow pits analysis. The abilities of recognition the boundaries withinsnow cover depends on both snow properties and the vertical resolution of the antennas
used. Obtained results were combined with meteorological data from automatic weather
stations, installed on Hansbreen and at the Polish Polar Station in Hornsund, referring tosequences of thaws and refreezing that favour formation of the melt-freeze crusts withinsnow layers. The above data contribute to determination of the snow metamorphisms
rate.

Greenland liquid water runoff from 1979 through 2017
Ken Mankoff1 , Andreas Ahlstrøm1 , Xavier Fettweis2 , Brice Noël3
1 GEUS, Denmark
2 Université de Liège, Belgium
3 Utrecht University, The Netherlands

Keywords: Hydrology, Runoff
We present a new data set capturing high spatial and temporal liquid water flux into
Greenland fjords and coastal seas. Freshwater runoff from the ice and land impacts glacier
dynamics, subglacial discharge plumes, marine terminating glacier frontal melt, fjord
properties (water dynamics, sediment load and deposition, marine biology, ice formation), and a variety of other properties near the ice, tundra, and coastal seas.
We use ERA forced regional models (MAR and RACMO) based runoff at 1 km spatial
and daily temporal resolution from 1979 through 2017. Model outputs are routed througha 90 m digital elevation model to determine where the water flows. Runoff is routed fromthe ice sheet to the ice margin and from the ice sheet and land to the coast, where basin
outlets accumulate upstream runoff and deliver it to the fjord.

Mapping glacier extent in Norway using Sentinel-2
Liss Marie Andreassen1 , Teodor Nagy1
1 Section for Glaciers, Ice and Snow, NVE, Norway

Keywords: glacier, mapping, sentinel,
The previous complete inventory of glaciers in mainland Norway is based on Landsat
imagery (30m) from the period 1999-2006. Here we present first results on a new mapping of glacier extent in Norway using Sentinel-2 imagery of 10 (20) m resolution from2018 (North Norway) and 2019 (South Norway). The results are compared with independent validation data such as aerial imagery of 0.25 m resolution and Pleiades satellite
imagery of 0.5-2 m resolution.

Causes and patterns of tidewater glacier retreat in the
Canadian Arctic
Luke Copland1 , Alison Cook1 , Brice Noel2 , Chris Stokes3 , Michael Bentley3 , Martin Sharp4 ,Robert Bingham5 , Michiel van den Broeke2
1 University of Ottawa, Canada
2 Utrecht University, The Netherlands
3 Durham University, UK
4 University of Alberta, Canada
5 University of Edinburgh, UK

Keywords: Tidewater glacier; Canadian Arctic; Ocean warming; Surface melt
The Canadian Arctic Archipelago (CAA) contains >300 tidewater-terminating glaciers,
but little is known about long-term changes in their frontal positions. Here, we examinechanges in glacier terminus positions since the 1950s and investigate the relative influence of oceanic versus atmospheric temperatures in accounting for these. Over 94% of
tidewater glaciers in the CAA retreated between 1958 and 2015, with a region-wide trendof gradual retreat before ∼2000, followed by a 5x increase in retreat rates up to 2015.
Retreat patterns show no correlation with changes in ocean temperature, but strong correlations with changes in surface melt. This suggests that increased atmospheric temperature has been the primary driver of recent rapid tidewater glacier frontal retreat in thisregion.

Snow Cover Reflection Properties on Hansbreen (South
Spitsbergen) based on radio-echo sounding
Mariusz Grabiec1 , Barbara Barzycka1 , Michał Laska1 , Dariusz Ignatiuk1,2 , Kamil Kachniarz1
1 University of Silesia, Centre for Polar Studies, Poland
2 SIOS Knowledge Centre, Norway

Keywords: GPR, snow density, Internal Reflection Power (IRP)
Monitoring of the snow cover properties on Hansbreen (S Spitsbergen) using Ground
Penetrating Radar (GPR) is one of the longest and the most comprehensive on Svalbard.
Snow depth is frequently the only feature derived from shallow radio-echo sounding. In
this study radiophysical properties of the snow cover have been analysed. The reflection
properties of the snow cover are the result of the complex snowpack characteristics likesize and shape of grain conglomerates, presence of hard layers, snow hardness, etc. The
snow density represents complex physical nature of snow cover and its variation in vertical profile fits well with the distribution of maximum absolute reflection amplitude with acorrelation coefficient of 0.82 at specific traces. The reflection power from the snowpackcolumn can be expressed as Internal Reflection Power (IRP) factor which represents theaverage reflected power and can be considered as index of bulk snow density. The IRP index generally decreases with elevation and increasing snow depth, and corresponds wellto similar relations with bulk snow density derived from numerous snow pits at Hansbreen
in 2008 - 2018. At lower elevations bulk snow density is generally higher due to complex
processes such as more frequent winter thaws and winter rains leading to formation of
hard layers. The same snow structures increase the reflection power. Application the
IRP index as the bulk snow density factor can efficiently improve winter mass balancecalculations.

How oceanic melt controls tidewater glacier evolution
Martin Lüthi1 , Rémy Mercenier1 , Andreas Vieli1
1 Geographical Institute, University of Zurich, Switzerland

Keywords: calving, oceanic melt, tidewater glacier, dynamics
The recent rapid retreat of many Greenland outlet glaciers has been attributed toincreased oceanic melt, but the relationship between oceanic melt and iceberg calving
remains poorly understood. We employed a transient finite-element model that simulates
oceanic melt and ice break-off at the terminus. The response of an idealized tidewater
glacier to various submarine melt rates and seasonal variations is investigated. Our modeling shows that without any oceanic melt, the rate of volume loss at the front is higher
than for intermediate melt rates. Only very high melt rates lead to increasing volume
losses. These results highlight the complex interplay between oceanic melt and calving and question the general assumption that increased submarine melt leads to higher
calving fluxes and hence enhanced retreat. Models for tidewater glacier evolution should
therefore consider calving and oceanic melt as tightly coupled processes rather than as
simple, additive parametrizations.

Patterns and mechanisms of flood release from glacierdammed Donjek Lake, Yukon
Moya Painter1 , William Kochtitzky1 , Luke Copland1 , Christine Dow2
1 Department of Geography, Environment and Geomatics, University of Ottawa, Canada
2 Department of Geography & Environmental Management, University of Waterloo, Canada

Keywords: GLOF, Yukon, remote sensing, glaciology
Donjek Glacier, located in the St Elias Mountains, Yukon, is a surge-type glacier witha repeat surge interval of approximately 12 years since the 1930s. Donjek River runs
perpendicular to the terminus of the glacier from its headwaters on the Kluane Glacierand surrounding ice bodies. Past surges have regularly caused the terminus to advanceand block the river, leading to the formation of an ice-dammed lake. The lake has drained
catastrophically several times over the past 3 decades, resulting in risks and damage todownstream infrastructure.
Surges and subsequent retreat of the glacier terminus have caused Donjek River tomove between several channels in the past depending on the position of the ice andnearby landforms. Analysis of historical satellite imagery since 1990 indicates threemechanisms by which the lake or river will drain depending on the ice extent and timesince the last surge: 1) subglacially under the glacier terminus, 2) subaerially througha canyon cut through the terminus of the glacier or 3) ice-marginally past the terminus.
Subglacial and subaerial drainage of the lake can lead to a catastrophic release and downstream flooding. Analysis of the patterns and timing of these drainage events provides abetter understanding of the interplay between glacier dynamics and the mechanisms offlood release, and how these will evolve in the future.

Comprehensive ocean observations in Inglefield Bredning, Northwestern Greenland
Naoya Kanna1 , Shin Sugiyama2 , Takuto Ando1 , Izumi Asaji3 , Yefan Wang3 , Yuta Sakuragi3
1 Arctic Research Center, Hokkaido University, Japan
2 Institute of Low Temperature Science, Hokkaido University, Japan
3 Graduate School of Environmental Science, Hokkaido University, Japan

Keywords:
Glacial fjords in Greenland are characterized by high productivity, which has been
attributed to meltwater discharge from glaciers. Previous our studies in northwestern
Greenland have revealed the importance of meltwater discharge from a marine-terminating
glacier on the biogeochemical processes in a fjord (Kanna et al., 2018; Naito et al., 2019;
Nishizawa et al., 2019). Marine-terminating glaciers in our study region have been retreating (Sakakibara and Sugiyama, 2018). Changes of the glaciers are possibly affecting
marine ecosystems in the surrounding ocean. Despite increased interest in the impact of
meltwater discharge on marine ecosystems in northwestern Greenland, it remains challenging to observe glacial fjords comprehensively. In the summer 2019, we conductedcomprehensive observations of water properties, sedimentation processes and marine
production in Inglefield Bredning, a 100 km long fjord system in northwestern Greenland.
As a part of a Japanese glacier and ocean research project in Qaanaaq region, Inglefield
Bredning has been studied since 2018. About ten marine-terminating glaciers are flowing
into Inglefield Gulf, which terminate at depths from several ten to over 600 m. In order toclarify the influence of meltwater discharge on water properties and marine productivity,
we conducted boat-based ocean measurements using a conductivity-temperature-depth
profiler near the glaciers (Tracy, Heilprin, Farquhar and Melville glaciers) including ocean
depth measurements. Seawater was collected from several depths to analyze macronutrients, trace metals (e.g., iron), organic carbon and phytoplankton assemblages using
an acid-cleaned Niskin-X water sampler. Zooplankton samples were also collected witha single-NORPAC net (mesh size 335 µm) through two water columns of 50 and 100 m
depths. Sea floor sediments were also collected near the terminus of Heilprin glacierusing an Ekman-Birge grab sampler to clarify sedimentation process of minerals and organic matters. Additionally, we conducted boat-based marine mammals surveys and hydrophone recording near the glacier termini to know how many and what kind of marine
mammals utilize this fjord. In this contribution, we present details of the field activity inthis summer.

Synoptic conditions and atmospheric moisture pathways
associated with virga and precipitation over coastal AdélieLand, Antarctica
Nicolas Jullien1 , Etienne Vignon2 , Michael Sprenger3 , Franziska Aemisegger3 , Alexis
Berne2
1 Department of Geosciences, University of Fribourg, Fribourg, Switzerland
2 Environmental Remote Sensing Laboratory (LTE), Switzerland
3 ETH Zürich, Switzerland

Keywords: Air parcel backtrajectories, radar measurements, synoptic circulation, lowlevel sublimation
Over polar regions, a large fraction of moisture coming from oceans is brought by extratropical cyclones and their associated fronts. Meanwhile, the edges of the Antarctic
and Greenland ice sheets experience katabatic winds. The coastal regions of Antarctica
often experience low-level sublimation of precipitation due to katabatic wind bringing dry
air from the interior’s Plateau, reducing the amount of precipitation that reaches the surface. We investigate the synoptic conditions and the atmospheric transport pathways ofmoisture that lead to virga - when precipitation is completely sublimated - or actual surface precipitation at Dumont d’Urville (DDU) station, coastal Adélie Land, Antarctica. We
combine ground-based radar measurements with Lagrangian back-trajectories and Eulerian diagnostics of extratropical cyclone and front identification based on ERA5 reanalysis
to improve our understanding about virga and surface precipitation. Precipitating systems are often associated with warm fronts. Virga periods - corresponding to 36% of
the precipitating events - often precede and sometimes follow surface precipitation periods. Cyclone positioning, warm front progress and back-trajectories of the precipitating
air parcels show different signatures for each of the three periods. Analysis of moistureatmospheric transport pathways shows the following characteristics: precipitation falling
above DDU during virga happening before surface precipitation periods have an oceanic
origin farther away (30 degrees more to the west) from Adélie Land than the one thatprecipitates down to the ground surface. It is further shown that moisture uptakes occur closer to the coast when sea-ice extent is minimum, and further north when sea-ice
extent is maximum.

Hydrological processes in firn at the runoff limit on theGreenland Ice Sheet
Nicole Clerx1 , Horst Machguth1 , Andrew Tedstone2 , Nicolas Jullien1
1 University of Fribourg, Switzerland
2 University of Bristol, UK

Keywords: Greenland; firn; hydrology; mass balance
The Greenland ice sheet loses mass at an accelerating rate. The majority of current
mass loss is due to surface melt running off into the ocean. The runoff limit is the highest
elevation from which meltwater finds its way off the ice sheet in one melt season. The
location of the runoff limit plays an important role in the mass balance of the Greenland
Ice Sheet. Recent findings have shown that widespread ice slabs have developed on theGreenland ice sheet close to the runoff limit (Fig. 1), impeding meltwater from percolation
and refreezing, and hence accelerating surface runoff.
Hydrological processes like meltwater percolation and refreezing in snow have beenstudied extensively, but existing research is generally focused on vertical percolation
rather than lateral runoff. Compared to snow science, the hydrology of the ice sheet firn
area has received less attention. In situ measurements of firn hydrology affecting thelocation and evolution of the runoff limit in time and space are scarce.

Figure 1. a) 45 km radar profile along the 2013 core transect at KANU (1849 m a.s.l.), close to therunoff limit. Blue indicates ice and cyan to red indicates lower density firn. Arrows visualize
hypothesized pathways of surface melt. b) Hypsography of the ice sheet surface along the radartransect (elevation in meters above the EGM2008 ellipsoid). Modified after Machguth et al. (2016),
Nat. Clim. Change).

In 2020, we will carry out fieldwork in spring and summer on the Greenland ice sheet,close to the current runoff limit. Aim of the fieldwork is to measure the firn hydrology
parameters required for quantifying vertical and lateral meltwater flow and their influenceon the runoff limit. In spring, firn stratigraphy and permeability will be measured andfirn stations will be installed to track changes in liquid water presence in the firn andsnow layer throughout the melt season. We will use the ROSA (Rain On Snow Appliance)
to measure in situ hydrological properties of firn. Summer fieldwork will be carried out
during the melt season and focus on measuring surface meltwater flow as well as lateralmeltwater flow inside the firn. Here we present the ROSA (Fig. 2), a portable lysimeter
originally designed for measuring hydrological processes during rain-on-snow events. We

Figure 2. The rain on snow appliance (ROSA). Items related to the water circulation are in blue,
other parts are highlighted in green. Hoses between discharge measurement, main and secondarytank are only visualised with arrows.

have adapted and upgraded the device to be able to carry out hydrological measurementsof firn properties and changes herein due to meltwater percolation on the Greenland ice
sheet.

Land-ice mass imbalance across the Arctic driven byatmosphere and ocean forcing
Noel Gourmelen1 , Paul Tepes1 , Michel Tsamados1 , Pete Nienow1 , Andrew Shepherd1 ,Flora Weissgerber1
1 School of geosciences, University of Edinburgh, UK

Keywords: Glaciers and ice caps, Mass balance, Geodetic
Arctic glaciers and ice caps (AGIC) accounted for 35% of global sea-level rise since theearly 2010s, are key players in the local freshwater budget, impact thermohaline forcing
in the North Atlantic. They store 40% of the global GIC ice volume, equating to 144
mm of sea level equivalent, and their losses are currently increasing as atmospheric andoceanic forcing intensify and as Arctic sea ice cover shrinks. Furthermore, the dynamic
response of land ice to climate forcing constitutes the main uncertainty in global sea
level projections for the next century. To address this knowledge gap, observations of
the relative contribution of both surface mass balance (SMB) and ice dynamics (D) tothe total losses are necessary, an information which is currently lacking at the Arctic
scale. Estimating GIC mass budgets for the entire Arctic region from satellite altimetry
is challenging because satellite ground track spacing and footprints of modern altimetry
sensors are coarse compared with the small size of GICs, their steep slopes and complex
topography. Within the European Space Agency Mountain Glacier and Ice Caps project,
we exploit globally a novel method to extract elevation from full waveform analysis of
the CryoSat interferometric radar altimeter. High-definition so-called swath processing of
CryoSat-2 radar altimetry data allow us to quantify ice losses across the Arctic and outsideof Greenland between 2010 and 2017, and to partition loss between surface and dynamic
processes. We find that while changes in meteorology are responsible for 87% of AGIC ice
loss, dynamic imbalance is increasing in the Barents and Kara Seas where it now accounts
for 43% of total ice loss, locally exceeding fresh water volume from receding sea-ice. Thispattern suggests that profuse warm Atlantic water incursions, or Atlantification, of thesector has a major impact on the loss of Arctic land ice, and that this effect should beconsidered in global sea level projections. Our results draw attention to the importanceof quantifying ocean warming in the Arctic to improve regional climate projections and to
reduce uncertainty in the parametrisation of future-generation climate models.

Basal conditions of Kongsvegen at the onset of surge revealed using seismic vibroseis surveys
Emma C. Smith1 , Anja Diez2,∗ , Olaf Eisen1,3 , Coen Hofstede1 , Jack Kohler2
1 Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Germany
2 Norwegian Polar Institute, Tromsø, Norway
3 Department of Geosciences, University of Bremen, Bremen, Germany∗ Now at: SINTEF Digital, Trondheim, Norway

Keywords: Svalbard, basal properties, active seismics
Kongsvegen is a well-studied surge-type glacier in the Kongsfjord area of northwest
Svalbard. Long-term monitoring has shown that the ice surface velocity has been increasing for the past 4 years; presenting a unique opportunity to study the internal ice
structure, basal conditions and thermal regime that play a crucial role in initiating glacier
surges. In April 2019, three-component seismic vibroseis surveys were conducted at twosites on the glacier, using a small Electrodynamic Vibrator source (ElViS). Site 1 is in theablation area and site 2 near the equilibrium line, where the greatest increase in icesurface velocity has been observed.
Initial analysis indicates the conditions at the two sites are significantly different. At
site 1 the ice is around 220 m thick, sitting on a relatively flat and uniform bed, withno clear change in the bed reflection along the profile. There is a horizontally layered
sediment package ∼60 m thick underlaying the bed. The ice column shows no internallayering. By contrast at site 2 (Fig. 1), where the ice is around 390 m thick, there is much
more complex internal ice structure. Clear internal ice reflections are visible between
150-250 m depth – where we expect a transition from cold to temperate ice. Further
reflections in the 100 m above the bed indicate there could be shearing or sedimententrainment in this area. Below the bed, cross-cutting layers are clearly visible and the
bed reflection itself shows changing reflection polarity – suggesting water or very wet
sediment is present in some areas. This suggests ice movement by basal sliding andshearing is likely.

IPCC’s Special Report on the Oceans and the Cryospherein a Warming Climate - Key messages for the Arctic
Regine Hock1
1 University of Alaska Fairbanks, USA

Keywords: climate change, cryosphere, Arctic, glaciers
XXX

Short-term ice speed variations near the calving frontof Bowdoin Glacier, northwestern Greenland
Shin Sugiyama1 , Shun Tsutaki2 , Daiki Sakakibara3 , Izumi Asaji1
1 Institute of Low Temperature Science, Hokkaido University, Japan
2 National Institute of Polar Research, Japan
3 Arctic Research Center, Hokkaido University, Japan

Keywords: ice speed, tidewater glacier, Greenland, GPS
Ice flow speed near the glacier front controls discharge from tidewater glaciers. Onceaccelerated, increase in discharge leads to rapid glacier mass loss, as recently observed inGreenlandic and other Arctic tidewater glaciers. Ice dynamics near the front of a tidewater glacier is sensitive to basal and ocean perturbations, because relatively small driving
stress is balanced by stresses acting at the bed and the front. To forecast the response of
tidewater glaciers to climate and ocean changes, it is crucial to understand mechanisms
driving ice speed variations. Nevertheless, high frequency ice speed data are sparse near
the front of tidewater glaciers because in-situ measurements are technically difficult. To
investigate short-term ice speed variations of a tidewater glacier, we operated GPS receivers within about 4 km from the front of Bowdoin Glacier in northwestern Greenland.
Three dual frequency GPS receivers were mounted on aluminum poles drilled into the ice,and operated continuously for several weeks in July 2013-2017 and 2019. Total durationof the measurements over the six summer seasons was about 13 weeks. GPS data werepost processed with reference data recorded nearby the glacier to obtain ice displacement every 15 min with an accuracy of several millimeters. Ice speed showed complex
high frequency variations, which were associated with melt, tides and rain. For example,
lowermost GPS station at several hundred meters from the calving front (1.6 m a−1 ) accelerated by 70% during an intensive melt period in July 2016. Speed was tidally modulated
for most of the time, and its amplitude in 2015 was up to 30%. Heavy rain storm ( 5mm h−1 ) triggered short-lived speed up events in July 2013 and 2014. Our observations
indicated that tidewater glacier dynamics is susceptible to meltwater and ocean forcing
at the basal and frontal boundaries.

The uncertainty of average precipitation forcing
Tobias Zolles1,2 , Andreas Born2
1 Department of Earth Science, University of Bergen, Bergen, Norway
2 Bjerknes Centre for Climate Research, Bergen, Norway

Keywords: Energy balance, Greenland Ice Sheet, modeling, climatology
Although climate undergoes natural variability, it is a common practice that simulations of past ice sheets use climatological instead of transient forcing . We test thesensitivity of the surface mass balance (SMB) of the Greenland ice sheet with the energy balance model BESSI. An ensemble of climate forcings with average values of temperature, precipitation, long and short-wave radiation, and dew point is generated andcompared with the fully transient simulation. This is furthermore compared to daily climatological forcing as well as individual components of the forcing as averages. The
climatological forcing leads to an almost 50% larger SMB. Reordering the forcing years ina synthetic transient simulation has a negligible effect of 2% on average Greenland-wide
surface mass balance. Mixed forcings of all but one forcing variable transient and thelast one climatological and vice versa revealed that the biggest driver for the much larger
SMB in the climatological case is the precipitation followed by temperature. To further
investigate the effect of averaging precipitation, which changes its nature from eventbased to continuous, alternative climatological forcing were created. To retain the event(storm) based nature of precipitation, monthly climatologies were used instead and the
sub-monthly variability taken from one of the original transient members. Additionally,
synthetic regular sub-monthly frequencies of precipitation were used as another calculation method. By using monthly averages with natural sub-monthly the SMB error of theclimatological forcing can be reduced to below 20%. We conclude that forcing energybalance models with climatological forcings creates a substantial error in the SMB, which
can mainly be attributed to the precipitation forcing. As long as the amplitude of theintra-annual variability is known, the order of the years has only a marginal impact on theGreenland wide SMB.

Future climatic mass balance, snow conditions and runoff
in Svalbard
Ward van Pelt1 , Thomas Schuler2 , Veijo Pohjola1
1 Uppsala University, Sweden
2 Oslo University, Norway

Keywords:
In a recent modelling experiment, we have generated a long-term (1957–2018) distributed dataset of climatic mass balance for the glaciers, snow conditions, and runoff
across Svalbard (Van Pelt et al. 2019). Following up on this experiment, we now use
the same model to make future projections under RCP4.5 and RCP8.5 scenarios for 20192060. Future meteorological input for the model is constructed from a combination of 1)
long-term trends in Arctic CORDEX regional climate model output, and 2) short-term pastvariability extracted from a downscaled ECMWF reanalysis product (NORA10). 3-Hourly
output is generated for both glacier- and land-covered parts of Svalbard at a 1x1-km spatial resolution and for two emission scenarios (RCP4.5 and RCP8.5). For the RCP4.5 scenario, results indicate an accelerated decrease of the climatic mass balance from close tozero in recent decades to about -1.5 m w.e. a−1 in 2050-2060 (-2.0 m w.e. a−1 for RCP8.5),
primarily due to expansion of ablation zones. By the end of the simulation period, duringsome years the ELA extends above the maximum elevation of all glaciers in Svalbard. Firn
degradation causes complete firn removal in southern Svalbard and strong retreat in thenorthern parts. Despite shrinking firn zones, increased winter rainfall and melt cause therefreezing trend to be close to zero. As a result of ablation zone expansion, runoff fromglaciers is found to about triple between 2019 and 2060. Comparing the seasonal snow
season duration during the periods 1957-2018 and 2019-2060 reveals largest changes incoastal regions across Svalbard, and most pronounced in the south, with snow arriving up
to two months later in autumn and disappearing up to two months earlier in spring.

Photos to Elevations: a photogrammetry pipelineWill Kochtitzky1 , Dorota Medrzycka1 , Braden Smeda1 , Brittany Main1 , Moya Painter1 ,Luke Copland1 , Alex Culley2 , Warwick Vincent2 , Christine Dow3
1 University of Ottawa, Canada
2 Université Laval, Canada
3 University of Waterloo, Canada

Keywords: elevation change; photogrammetry; Canada; remote sensing
Elevation measurements are fundamental to observing glacier dynamics and massbalance. However, high resolution (<1 m) and accurate elevation measurements arestill rare for glaciers worldwide. Here, we present a semi-automated pipeline to create high resolution orthomosaic images and digital elevation models (DEM) from aerial
photographs. We do this using a Nikon D850 SLR camera attached to a high-precision
GPS mounted on a fixed wing aircraft or helicopter. We wrote custom software in R andPython to determine the precise positions of the photos based on the GPS record, which isprocessed using PPP methods from Natural Resources Canada. We then use high performance supercomputing to process the data using Agisoft Metashape-Pro. We are able toproduce DEMs and orthographic mosaics at a scale of 10 cm - 1 m for tens of square kilometers from hundreds to thousands of photos at once. Here, we showcase examples fromthe Canadian Arctic and Yukon St. Elias Mountains and show that airborne photo surveys
can be an effective tool to rapidly measure the elevation of Earth features at landscapescales with sub-meter level precision. This data can be applied to measure the mass balance of glaciers with annual surveys, and can shine new light on glacier dynamics. Thesemethods can help provide substantial new insights into many different Earth processes,
including ice-ocean interactions.