cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.17897/q8rg-km16
title: GeoBasis Disko - Hydrology - RE-1-Multisensor

description: Automatic monitoring of river water properties in Røde Elv (RE) was carried out at this position in 2013. A multisensor (YSI 6820 V2-2) was deployed in the river early in the runoff season and removed late in the runoff season. Data were logged every 10 minutes. The time stamp refer to UTC-3. The multisensor was located at the eastern side of Røde Elv just south of the bridge. However it turned out that the river was influenced by tidal fluctuations at this position. To avoid tidal impact the set-up was moved to a location farther upstream in 2014 (see RE-2). To see data from the present position see: Multisensor. Hydrology:Hydrology GeoBasis Disko:The GeoBasis monitoring programme focuses on selected abiotic characteristics in order to describe the state of Greenlandic terrestrial environments and their potential feedback effects in a changing climate. Monitored plot data is up-scaled to a landscape level and is used to improve ecosystem models to be able to quantify these feedback mechanisms. The GeoBasis programme provides an active response to recommendations in international assessments such as ACIA and SWIPA; and is continuously being adapted based on AMAP and other international founded recommendations. Furthermore, the GeoBasis programme is directly involved in several international networks and research projects (e.g. the Circumpolar Active Layer Monitoring (CALM) programme, the Nordic Centre of Excellence DEFROST, the Danish Centre of Excellence CENPERM, the EU-projects PAGE21 and INTERACT, and the Arctic Research Centre at Aarhus University). The GeoBasis programme is divided into a number of sub-groups, including:
DOI: 10.17897/2hnr-jf30
title: GeoBasis Disko - Hydrology - RE-2-Multisensor

description: Automatic monitoring of river water properties in Røde Elv (RE) was carried out at this position in 2014. A multisensor (YSI 6820 V2-2) was deployed in the river early in the runoff season and removed late in the runoff season. Data were logged every 10 minutes. The time stamp refer to UTC-3. A large flood damaged the set-up in August 2014 and therefore several parameters ends in August. It also turned out that the position was not suitable as the main stream was located at the opposite river bank during periods with low water level. To see data from the present position see: Multisensor Hydrology:Hydrology GeoBasis Disko:The GeoBasis monitoring programme focuses on selected abiotic characteristics in order to describe the state of Greenlandic terrestrial environments and their potential feedback effects in a changing climate. Monitored plot data is up-scaled to a landscape level and is used to improve ecosystem models to be able to quantify these feedback mechanisms. The GeoBasis programme provides an active response to recommendations in international assessments such as ACIA and SWIPA; and is continuously being adapted based on AMAP and other international founded recommendations. Furthermore, the GeoBasis programme is directly involved in several international networks and research projects (e.g. the Circumpolar Active Layer Monitoring (CALM) programme, the Nordic Centre of Excellence DEFROST, the Danish Centre of Excellence CENPERM, the EU-projects PAGE21 and INTERACT, and the Arctic Research Centre at Aarhus University). The GeoBasis programme is divided into a number of sub-groups, including:
DOI: 10.17897/m97q-h023
title: GeoBasis Disko - Hydrology - RE-Multisensor

description: Automatic monitoring of river water properties in Røde Elv (RE) has been carried out at the present position since 2015. A multisensor are deployed in the river early in the runoff season and removed late in the runoff season (before freeze-in). The time stamp refer to UTC-3. Data are logged either by 10 min, 15 min, or 30 min interval. Hydrology:Hydrology GeoBasis Disko:The GeoBasis monitoring programme focuses on selected abiotic characteristics in order to describe the state of Greenlandic terrestrial environments and their potential feedback effects in a changing climate. Monitored plot data is up-scaled to a landscape level and is used to improve ecosystem models to be able to quantify these feedback mechanisms. The GeoBasis programme provides an active response to recommendations in international assessments such as ACIA and SWIPA; and is continuously being adapted based on AMAP and other international founded recommendations. Furthermore, the GeoBasis programme is directly involved in several international networks and research projects (e.g. the Circumpolar Active Layer Monitoring (CALM) programme, the Nordic Centre of Excellence DEFROST, the Danish Centre of Excellence CENPERM, the EU-projects PAGE21 and INTERACT, and the Arctic Research Centre at Aarhus University). The GeoBasis programme is divided into a number of sub-groups, including:
DOI: 10.17897/zjk8-0b45
title: GeoBasis Disko - Hydrology - RiverWaterChemistry

description: Water samples are collected manually in Røde Elv near the location of the automatic monitoring set-up (RE-436-2: 69.25362, -53.49823). In situ measurements of water temperature and water conductivity are carried out when water is sampled. In 2013 and 2014, water from Røde Elv was sampled at locations where the multisensor was mounted/installed at that time. In 2013 the position was RE-1: 69.25277, -53.49916. In 2014 the position was RE-2: 69.256835, -53.498346. Occasionally, water is sampled from tributaries to Røde Elv and other streams in the area. The timestamp refer to UTC-3. More data from Røde Elv are found under Hydrology (WaterDischarge, SuspendedSediment, Multisensor). Hydrology:Hydrology GeoBasis Disko:The GeoBasis monitoring programme focuses on selected abiotic characteristics in order to describe the state of Greenlandic terrestrial environments and their potential feedback effects in a changing climate. Monitored plot data is up-scaled to a landscape level and is used to improve ecosystem models to be able to quantify these feedback mechanisms. The GeoBasis programme provides an active response to recommendations in international assessments such as ACIA and SWIPA; and is continuously being adapted based on AMAP and other international founded recommendations. Furthermore, the GeoBasis programme is directly involved in several international networks and research projects (e.g. the Circumpolar Active Layer Monitoring (CALM) programme, the Nordic Centre of Excellence DEFROST, the Danish Centre of Excellence CENPERM, the EU-projects PAGE21 and INTERACT, and the Arctic Research Centre at Aarhus University). The GeoBasis programme is divided into a number of sub-groups, including:
DOI: 10.17897/cd5v-zs56
title: GeoBasis Disko - Hydrology - SuspendedSediment

description: Water samples are collected manually in the river Røde Elv (RE) near the location of the automatic monitoring set-up (RE-436-2: 69.25362, -53.49823). A depth-integrating sampler (US DH-48) is used for water sampling. In 2013 and 2014, water from Røde Elv was sampled at locations where the multisensor was installed at that time. In 2013 the position was RE-1: 69.25277, -53.49916. In 2014 the position was RE-2: 69.256835, -53.498346. Occasionally, we sample water from tributaries to Røde Elv. The timestamp refer to West Greenland Standard Time (UTC-3). Find more data from Røde Elv under Hydrology (WaterDischarge, RiverWaterChemistry, Multisensor). Hydrology:Hydrology GeoBasis Disko:The GeoBasis monitoring programme focuses on selected abiotic characteristics in order to describe the state of Greenlandic terrestrial environments and their potential feedback effects in a changing climate. Monitored plot data is up-scaled to a landscape level and is used to improve ecosystem models to be able to quantify these feedback mechanisms. The GeoBasis programme provides an active response to recommendations in international assessments such as ACIA and SWIPA; and is continuously being adapted based on AMAP and other international founded recommendations. Furthermore, the GeoBasis programme is directly involved in several international networks and research projects (e.g. the Circumpolar Active Layer Monitoring (CALM) programme, the Nordic Centre of Excellence DEFROST, the Danish Centre of Excellence CENPERM, the EU-projects PAGE21 and INTERACT, and the Arctic Research Centre at Aarhus University). The GeoBasis programme is divided into a number of sub-groups, including:
DOI: 10.17897/jm30-jc87
title: GeoBasis Disko - Hydrology - WaterDischarge

description: Water discharge in Røde Elv (RE) is based on water level registrations and a relation between measured discharge (Q) and water level (h). The Q/h relation is made in close collaboration with Asiaq, Greenland Survey. The timestamp of the calculated discharge data refer to UTC-3. Data was calculated for every 10 minutes up to 2017. From 2017 onwards the time step was 15 minutes. Data cover the main runoff season. However, the start and the end of the annual time series refer to the time when the automatic sensors were deployed and removed from the water. For a better estimation of the break-up and freeze-in period, please contact the GeoBasisDisko data manager. The drainage basin of this Røde Elv site is approximately 100 km2 and varies in elevation from 0-800 m above sea level. Find more data about river water in Røde Elv under Hydrology (RiverWaterChemistry, SuspendedSediment, and Multisensor). Hydrology:Hydrology GeoBasis Disko:The GeoBasis monitoring programme focuses on selected abiotic characteristics in order to describe the state of Greenlandic terrestrial environments and their potential feedback effects in a changing climate. Monitored plot data is up-scaled to a landscape level and is used to improve ecosystem models to be able to quantify these feedback mechanisms. The GeoBasis programme provides an active response to recommendations in international assessments such as ACIA and SWIPA; and is continuously being adapted based on AMAP and other international founded recommendations. Furthermore, the GeoBasis programme is directly involved in several international networks and research projects (e.g. the Circumpolar Active Layer Monitoring (CALM) programme, the Nordic Centre of Excellence DEFROST, the Danish Centre of Excellence CENPERM, the EU-projects PAGE21 and INTERACT, and the Arctic Research Centre at Aarhus University). The GeoBasis programme is divided into a number of sub-groups, including:
DOI: 10.17897/svr0-1574
title: GeoBasis Disko - Ice - AS-SeaIceCover

description: Visual observations of sea ice cover in the near shore Disko Bay area. Observations are performed on a daily basis from the scientific leader´s house at Arctic Station. Looking South. These observations were initiated 1 January 1991. Ice:Ice GeoBasis Disko:The GeoBasis monitoring programme focuses on selected abiotic characteristics in order to describe the state of Greenlandic terrestrial environments and their potential feedback effects in a changing climate. Monitored plot data is up-scaled to a landscape level and is used to improve ecosystem models to be able to quantify these feedback mechanisms. The GeoBasis programme provides an active response to recommendations in international assessments such as ACIA and SWIPA; and is continuously being adapted based on AMAP and other international founded recommendations. Furthermore, the GeoBasis programme is directly involved in several international networks and research projects (e.g. the Circumpolar Active Layer Monitoring (CALM) programme, the Nordic Centre of Excellence DEFROST, the Danish Centre of Excellence CENPERM, the EU-projects PAGE21 and INTERACT, and the Arctic Research Centre at Aarhus University). The GeoBasis programme is divided into a number of sub-groups, including:
DOI: 10.17897/njtx-6m44
title: GeoBasis Disko - Meteorology - AS-CloudCover

description: Visual observations of cloud cover are performed three times a day (7:00, 12:00, and 17:00) from just outside Arctic Station. These observations were initiated in June 1993. Meteorology:Meteorology GeoBasis Disko:The GeoBasis monitoring programme focuses on selected abiotic characteristics in order to describe the state of Greenlandic terrestrial environments and their potential feedback effects in a changing climate. Monitored plot data is up-scaled to a landscape level and is used to improve ecosystem models to be able to quantify these feedback mechanisms. The GeoBasis programme provides an active response to recommendations in international assessments such as ACIA and SWIPA; and is continuously being adapted based on AMAP and other international founded recommendations. Furthermore, the GeoBasis programme is directly involved in several international networks and research projects (e.g. the Circumpolar Active Layer Monitoring (CALM) programme, the Nordic Centre of Excellence DEFROST, the Danish Centre of Excellence CENPERM, the EU-projects PAGE21 and INTERACT, and the Arctic Research Centre at Aarhus University). The GeoBasis programme is divided into a number of sub-groups, including:
DOI: 10.17897/a22w-9z72
title: GeoBasis Disko - Meteorology - AWS1-Meteorology

description: The automatic weather station AWS1 was installed in October 1990 and removed in 2018. We included the main parameters from this station in the GEM database as most parameters are continued at the GeoBasis automatic weather station (AWS2). AWS1 time stamp refer to UTC-3. The automatic weather station was installed at the scientific leader´s house approximately 25 meter above sea level and 300 m from the coast. Wind (speed and direction) and Air temperature were measured at a 9.5 meter high mast. Liquid precipitation were measured at a 2 meter high separate mast. All parameters were logged by 30 minutes interval. Data were monitored and stored by AANDERAA instruments and datalogger. Find more information about the AWS1 station on: http://img.kb.dk/tidsskriftdk/pdf/gto/gto_0095-PDF/gto_0095_72093.pdf. Due to a datalogger failure, average wind speed data was not available until 26 May 1994. The wind speed measurements ends by 31 December 2012. The relative humidity measurements ends by 16 November 2012. The station had a breakdown in July 2002 and remained unstable until October 2004. During that period, the main parameters were gap-filled with data from nearby stations. Find ground temperatures measured at AWS1 under Soil (AWS1-GroundTemperature). Find data from AWS2 under Meteorolgy, Soil, and Snow. Meteorology:Meteorology GeoBasis Disko:The GeoBasis monitoring programme focuses on selected abiotic characteristics in order to describe the state of Greenlandic terrestrial environments and their potential feedback effects in a changing climate. Monitored plot data is up-scaled to a landscape level and is used to improve ecosystem models to be able to quantify these feedback mechanisms. The GeoBasis programme provides an active response to recommendations in international assessments such as ACIA and SWIPA; and is continuously being adapted based on AMAP and other international founded recommendations. Furthermore, the GeoBasis programme is directly involved in several international networks and research projects (e.g. the Circumpolar Active Layer Monitoring (CALM) programme, the Nordic Centre of Excellence DEFROST, the Danish Centre of Excellence CENPERM, the EU-projects PAGE21 and INTERACT, and the Arctic Research Centre at Aarhus University). The GeoBasis programme is divided into a number of sub-groups, including:
DOI: 10.17897/cszt-f010
title: GeoBasis Disko - Meteorology - AWS2-Meteorology

description: The automatic weather station AWS2 was installed in August 2012 in Østerlien just 100 meter east of Arctic Station. The station is located approximately 25 meter above sea level in a gentle south sloping area covered by low vegetation/dwarf shrubs. The time stamp refer to UTC-3. The station consist of a 3 meter high mast with an east west pointing cross beam where sensors are mounted, and a 2 meter high mast where gasfluxes (CO2) are measured using eddy covariance technique. Soil parameters are measured in profiles and boreholes adjacent to the two masts. The AWS2-Meteorology file holds the following parameters (Shortwave radiation in and out, Longwave radiation in and out, Air temperature, Relative humidity, Wind speed, Wind direction, PAR, Air pressure and Albedo). Find gasflux data under FluxMonitoring (EC1-GasFlux). Find soil data from AWS2 under Soil (AWS2-GroundTemperatureP1 and P2, AWS2-SoilMoisture, AWS2-SoilTemperature, AWS2-SurfaceTemperature, AWS2-SoilHeatFlux). Find snow data from AWS2 under Snow (AWS2-SnowDepth, AWS2-SnowTemperature). All data are logged by 30-minute intervals. There is a gap in data from 10 September 2022 to 15 September 2022 due to service and maintenance of the station. There is also a gap from 23 April 2023 to 13 May 2023 due to a failure in the data communication. Meteorology:Meteorology GeoBasis Disko:The GeoBasis monitoring programme focuses on selected abiotic characteristics in order to describe the state of Greenlandic terrestrial environments and their potential feedback effects in a changing climate. Monitored plot data is up-scaled to a landscape level and is used to improve ecosystem models to be able to quantify these feedback mechanisms. The GeoBasis programme provides an active response to recommendations in international assessments such as ACIA and SWIPA; and is continuously being adapted based on AMAP and other international founded recommendations. Furthermore, the GeoBasis programme is directly involved in several international networks and research projects (e.g. the Circumpolar Active Layer Monitoring (CALM) programme, the Nordic Centre of Excellence DEFROST, the Danish Centre of Excellence CENPERM, the EU-projects PAGE21 and INTERACT, and the Arctic Research Centre at Aarhus University). The GeoBasis programme is divided into a number of sub-groups, including:
DOI: 10.17897/fegk-0632
title: GeoBasis Disko - Meteorology - AWS3-Meteorology

description: The automatic weather station AWS3 was installed in July 2013. It is located in the southern part of Blæsedalen (90 meter above sea level) in an open gently rolling area. It is a relatively dry location. A thin layer of soil with low heath vegetation/dwarf shrubs covers the bedrock. The time stamp refer to UTC-3. The AWS3-Meteorology file holds the following parameters (Air temperature, Relative humidity, Wind (speed and direction) Liquid precipitation and PAR). The rain gauge was installed in August 2014. Find more data from AWS3 under Soil (AWS3-SoilMoisture, AWS3-SoilTemperature). Soil temperatures are only available after July 2018. All data are logged by 30-minute intervals. Meteorology:Meteorology GeoBasis Disko:The GeoBasis monitoring programme focuses on selected abiotic characteristics in order to describe the state of Greenlandic terrestrial environments and their potential feedback effects in a changing climate. Monitored plot data is up-scaled to a landscape level and is used to improve ecosystem models to be able to quantify these feedback mechanisms. The GeoBasis programme provides an active response to recommendations in international assessments such as ACIA and SWIPA; and is continuously being adapted based on AMAP and other international founded recommendations. Furthermore, the GeoBasis programme is directly involved in several international networks and research projects (e.g. the Circumpolar Active Layer Monitoring (CALM) programme, the Nordic Centre of Excellence DEFROST, the Danish Centre of Excellence CENPERM, the EU-projects PAGE21 and INTERACT, and the Arctic Research Centre at Aarhus University). The GeoBasis programme is divided into a number of sub-groups, including:
DOI: 10.25625/kxuo3g/rvlcmp
title: final_result.txt
DOI: 10.25625/kxuo3g/y9comx
title: results_1s_reversed.pkl
DOI: 10.25625/kxuo3g/3jewne
title: amplitude_002.mat
DOI: 10.25625/kxuo3g/ctqqhw
title: amplitude_007.mat
DOI: 10.25625/kxuo3g/kpcjcs
title: amplitude_001.mat
DOI: 10.25625/kxuo3g/mnpkoq
title: amplitude_004.mat
DOI: 10.25625/kxuo3g/ukhxyw
title: amplitude_008.mat
DOI: 10.25625/kxuo3g/4mbjud
title: active.txt
DOI: 10.25625/kxuo3g/9mdxvg
title: amplitude_005.mat
DOI: 10.25625/kxuo3g/usir8c
title: amplitude_010.mat
DOI: 10.25625/kxuo3g/8rmgkl
title: amplitude_009.mat
DOI: 10.25625/kxuo3g/dhp29x
title: amplitude_006.mat
DOI: 10.25625/kxuo3g/hysilb
title: amplitude_000.mat
DOI: 10.25625/kxuo3g/i0m9ch
title: amplitude_003.mat
DOI: 10.25625/kxuo3g/jq3ip4
title: results_tau0p01.pkl
DOI: 10.25625/kxuo3g/8cizki
title: combined_new.pkl
DOI: 10.25625/kxuo3g/dm63to
title: passive_new.pkl
DOI: 10.25625/kxuo3g/ive3sk
title: results_1s.pkl
DOI: 10.25625/kxuo3g/wlspng
title: Force_Dissi.pkl
DOI: 10.25625/kxuo3g/e7b1vp
title: results_passive.txt
DOI: 10.25625/kxuo3g/h6trfn
title: amplitude_001.mat
DOI: 10.25625/kxuo3g/hys767
title: amplitude_002.mat
DOI: 10.25625/kxuo3g/jabdwm
title: amplitude_001_mbr.pkl
DOI: 10.25625/kxuo3g/jmztsd
title: amplitude_000_mbr.pkl
DOI: 10.25625/kxuo3g/1rr5yd
title: results_msd.pkl
DOI: 10.25625/kxuo3g/8rclyj
title: amplitude_000.mat
DOI: 10.25625/kxuo3g/j5zg0l
title: amplitude_002_mbr.pkl
DOI: 10.25625/kxuo3g/xegeob
title: results_tau0p0006.pkl
DOI: 10.25625/kxuo3g/zlrvrd
title: results_tau0p002.pkl
DOI: 10.25625/kxuo3g/2t6p4z
title: results_tau0p0006_reversed.pkl
DOI: 10.25625/kxuo3g/l5w9g5
title: results_1s_reversed.pkl
DOI: 10.25625/kxuo3g/mrclwr
title: results_tau0p0001.pkl
DOI: 10.25625/kxuo3g/wx6ik2
title: final_result.txt
DOI: 10.25625/kxuo3g/4gyy53
title: active_new.pkl
DOI: 10.25625/kxuo3g/bmdj8f
title: amplitude_001.mat
DOI: 10.25625/kxuo3g/f66jyl
title: amplitude_008.mat
DOI: 10.25625/kxuo3g/k640lv
title: amplitude_002.mat
DOI: 10.25625/kxuo3g/ewviro
title: amplitude_004.mat
DOI: 10.25625/kxuo3g/od8fqo
title: amplitude_007.mat
DOI: 10.25625/kxuo3g/predmo
title: amplitude_005.mat
DOI: 10.25625/kxuo3g/shtmb9
title: active.txt
DOI: 10.6084/m9.figshare.26304718.v5
title: Datasets by figure

description: These are the source data corresponding to the preprint in the same project.
DOI: 10.25625/kxuo3g/gv6o4k
title: amplitude_006.mat
DOI: 10.25625/kxuo3g/is3mly
title: amplitude_010.mat
DOI: 10.25625/kxuo3g/kah5co
title: amplitude_000.mat
DOI: 10.25625/kxuo3g/nyqmmj
title: amplitude_009.mat
DOI: 10.25625/kxuo3g/oh3lhf
title: amplitude_003.mat
DOI: 10.25625/kxuo3g/7ijeas
title: combined_new.pkl
DOI: 10.25625/kxuo3g/hizeck
title: results_1s.pkl
DOI: 10.25625/kxuo3g/sg3jug
title: Force_Dissi.pkl
DOI: 10.25625/kxuo3g/ugxnss
title: results_tau0p01.pkl
DOI: 10.25625/kxuo3g/wvzdlx
title: passive_new.pkl
DOI: 10.25625/kxuo3g/gdfb7e
title: amplitude_002.mat
DOI: 10.25625/kxuo3g/n56ica
title: amplitude_001_mbr.pkl
DOI: 10.25625/kxuo3g/u7mlzw
title: results_passive.txt
DOI: 10.25625/kxuo3g/wlhxwn
title: amplitude_001.mat
DOI: 10.25625/kxuo3g/9vw0it
title: results_msd.pkl
DOI: 10.25625/kxuo3g/a7n3my
title: amplitude_002_mbr.pkl
DOI: 10.25625/kxuo3g/mhj34d
title: results_tau0p002.pkl
DOI: 10.25625/kxuo3g/o9llto
title: results_tau0p0006.pkl
DOI: 10.25625/kxuo3g/p393nl
title: results_tau0p0006_reversed.pkl
DOI: 10.25625/kxuo3g/1ayxud
title: active_new.pkl
DOI: 10.25625/kxuo3g/ii5pcj
title: final_result.txt
DOI: 10.25625/kxuo3g/j3wczt
title: amplitude_002.mat
DOI: 10.25625/kxuo3g/r0af4s
title: results_1s_reversed.pkl
DOI: 10.25625/kxuo3g/uzrhat
title: results_tau0p0001.pkl
DOI: 10.25625/kxuo3g/7scng9
title: amplitude_008.mat
DOI: 10.25625/kxuo3g/bwmkzg
title: amplitude_001.mat
DOI: 10.25625/kxuo3g/nddrzh
title: amplitude_007.mat
DOI: 10.25625/kxuo3g/zjlbpn
title: amplitude_004.mat
DOI: 10.25625/kxuo3g/5emfki
title: amplitude_010.mat
DOI: 10.25625/kxuo3g/it9lmh
title: active.txt
DOI: 10.25625/kxuo3g/t5gaff
title: amplitude_009.mat
DOI: 10.25625/kxuo3g/wkodfq
title: amplitude_005.mat
DOI: 10.25625/kxuo3g/jgsp5s
title: results_tau0p01.pkl
DOI: 10.25625/kxuo3g/ljvbsv
title: amplitude_006.mat
DOI: 10.25625/kxuo3g/pcesv7
title: Force_Dissi.pkl
DOI: 10.25625/kxuo3g/qsnyvh
title: amplitude_003.mat
DOI: 10.25625/kxuo3g/x3uwpv
title: amplitude_000.mat
DOI: 10.25625/kxuo3g/bwbnrh
title: amplitude_001_mbr.pkl
DOI: 10.25625/kxuo3g/dkvrxk
title: results_1s.pkl
DOI: 10.25625/kxuo3g/hi2i93
title: combined_new.pkl
DOI: 10.25625/kxuo3g/kjctn5
title: passive_new.pkl