cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.927167
title: Light intensity time series from 16 locations in Lovns Bredning, Limfjorden, Denmark, at 3 m above seabed, 1-March-2017

description: Field studies were conducted in two different areas of the Limfjorden, in Lovns Bredning (26th February to 4th March 2017) and in Løgstør Bredning (6-10th March 2017). In each sampling area, 16 fixed-position moorings were deployed in two circular sensor arrays around a mussel dredging area to investigate possible effects of dredging related sediment plumes (Pastor et al, 2020). The inner array (stations 1 - 8) had a diameter of 200 m and the outer array (stations 9 - 16) was set up with a diameter of 600 m. Integrated temperature and light loggers (HOBO Pendant Temperature/Light 64K Data Logger) were mounted on each mooring in the two circular arrays at three different water depths (0.5, 1.5 and 3.0 m above seabed). The 48 loggers (3 depths and 16 stations) were deployed in each area over a period of four days and light intensity time series were collected with a sampling interval of 30 seconds. Five loggers in the Lovns area did not provide any data due to technical problems (two near-surface loggers and three loggers at 1.5 m above the seabed). However, only one bottom logger at Løgstør Bredning failed to provide data. Each time series was filtered using a 3-minute moving average for removing the largest outliers, but retaining sharp changes in light intensity associated with short-lived sediment plumes caused by experimental mussel dredging.
DOI: 10.1594/pangaea.694971
title: Concentrations of chlorophyll-alpha in water of the Ionian Sea at Station SEPT-2000-IRI34

description: Samples from 2 l of sea water were filtered through polycarbonate Millipore filters. The filters were kept deep frozen and analyzed according to Holm-Hansen et al. (Holm-Hansen, O., Lorenzen, C.J., Holmes, R.W., Strickland, J.D.H. 1965. Fluorometric determination of chlorophyll. Journal du Conseil Permanent International Pour l'Exploration de la Mer 30, 3-15).
DOI: 10.1594/pangaea.707727
title: Other measurements at 30 m from station Payerne (2007-11)
DOI: 10.1594/pangaea.927127
title: Light intensity time series from 16 locations in Løgstør Bredning, Limfjorden, Denmark, at 0.5 m above seabed, 7-March-2017

description: Field studies were conducted in two different areas of the Limfjorden, in Lovns Bredning (26th February to 4th March 2017) and in Løgstør Bredning (6-10th March 2017). In each sampling area, 16 fixed-position moorings were deployed in two circular sensor arrays around a mussel dredging area to investigate possible effects of dredging related sediment plumes (Pastor et al, 2020). The inner array (stations 1 - 8) had a diameter of 200 m and the outer array (stations 9 - 16) was set up with a diameter of 600 m. Integrated temperature and light loggers (HOBO Pendant Temperature/Light 64K Data Logger) were mounted on each mooring in the two circular arrays at three different water depths (0.5, 1.5 and 3.0 m above seabed). The 48 loggers (3 depths and 16 stations) were deployed in each area over a period of four days and light intensity time series were collected with a sampling interval of 30 seconds. Five loggers in the Lovns area did not provide any data due to technical problems (two near-surface loggers and three loggers at 1.5 m above the seabed). However, only one bottom logger at Løgstør Bredning failed to provide data. Each time series was filtered using a 3-minute moving average for removing the largest outliers, but retaining sharp changes in light intensity associated with short-lived sediment plumes caused by experimental mussel dredging.
DOI: 10.1594/pangaea.927169
title: Light intensity time series from 16 locations in Lovns Bredning, Limfjorden, Denmark, at 3 m above seabed, 2-March-2017

description: Field studies were conducted in two different areas of the Limfjorden, in Lovns Bredning (26th February to 4th March 2017) and in Løgstør Bredning (6-10th March 2017). In each sampling area, 16 fixed-position moorings were deployed in two circular sensor arrays around a mussel dredging area to investigate possible effects of dredging related sediment plumes (Pastor et al, 2020). The inner array (stations 1 - 8) had a diameter of 200 m and the outer array (stations 9 - 16) was set up with a diameter of 600 m. Integrated temperature and light loggers (HOBO Pendant Temperature/Light 64K Data Logger) were mounted on each mooring in the two circular arrays at three different water depths (0.5, 1.5 and 3.0 m above seabed). The 48 loggers (3 depths and 16 stations) were deployed in each area over a period of four days and light intensity time series were collected with a sampling interval of 30 seconds. Five loggers in the Lovns area did not provide any data due to technical problems (two near-surface loggers and three loggers at 1.5 m above the seabed). However, only one bottom logger at Løgstør Bredning failed to provide data. Each time series was filtered using a 3-minute moving average for removing the largest outliers, but retaining sharp changes in light intensity associated with short-lived sediment plumes caused by experimental mussel dredging.
DOI: 10.1594/pangaea.921607
title: Fig.10. Average relative spacing

description: # = 1: Sand# = 2: Silt# = 3: Clay
DOI: 10.1594/pangaea.927170
title: Light intensity time series from 16 locations in Lovns Bredning, Limfjorden, Denmark, at 3 m above seabed, 28-February-2017

description: Field studies were conducted in two different areas of the Limfjorden, in Lovns Bredning (26th February to 4th March 2017) and in Løgstør Bredning (6-10th March 2017). In each sampling area, 16 fixed-position moorings were deployed in two circular sensor arrays around a mussel dredging area to investigate possible effects of dredging related sediment plumes (Pastor et al, 2020). The inner array (stations 1 - 8) had a diameter of 200 m and the outer array (stations 9 - 16) was set up with a diameter of 600 m. Integrated temperature and light loggers (HOBO Pendant Temperature/Light 64K Data Logger) were mounted on each mooring in the two circular arrays at three different water depths (0.5, 1.5 and 3.0 m above seabed). The 48 loggers (3 depths and 16 stations) were deployed in each area over a period of four days and light intensity time series were collected with a sampling interval of 30 seconds. Five loggers in the Lovns area did not provide any data due to technical problems (two near-surface loggers and three loggers at 1.5 m above the seabed). However, only one bottom logger at Løgstør Bredning failed to provide data. Each time series was filtered using a 3-minute moving average for removing the largest outliers, but retaining sharp changes in light intensity associated with short-lived sediment plumes caused by experimental mussel dredging.
DOI: 10.1594/pangaea.921239
title: Fig. 4. Penetration path projections
DOI: 10.1594/pangaea.927176
title: Water current velocity time series from Løgstør Bredning, Limfjorden, Denmark, 7-9 March 2017

description: A 600 kHz ADCP (RDI Workhorse Sentinel) was deployed at each site (station 1 at the Lovns Bredning mooring, station 3 at the Løgstør Bredning mooring) in a bottom-mounted, upward-looking configuration. 30-second ensembles of 3D velocity components were collected along with corresponding records of beam correlation and error velocity. Each vertical profile had a bin size of 0.5 m and the first bin was at 1.59 m above the bottom (blanking distance: 0.88 m). The velocity data time series at each bin were filtered using a 30 minute moving average.
DOI: 10.1594/pangaea.927177
title: Water current velocity time series from Lovns Bredning, Limfjorden, Denmark, 7-9 March 2017

description: A 600 kHz ADCP (RDI Workhorse Sentinel) was deployed at each site (station 1 at the Lovns Bredning mooring, station 3 at the Løgstør Bredning mooring) in a bottom-mounted, upward-looking configuration. 30-second ensembles of 3D velocity components were collected along with corresponding records of beam correlation and error velocity. Each vertical profile had a bin size of 0.5 m and the first bin was at 1.59 m above the bottom (blanking distance: 0.88 m). The velocity data time series at each bin were filtered using a 30 minute moving average.
DOI: 10.1594/pangaea.903445
title: Ultra-violet measurements from station Izaña (2019-06)
DOI: 10.1594/pangaea.664249
title: Oceanography at CTD/bottle station IFREMER_1090
DOI: 10.1594/pangaea.921256
title: Fig. 3. Stratigraphy and soil properties of test field
DOI: 10.1594/pangaea.494714
title: Physical oceanography during cruise K9029_1976
DOI: 10.1594/pangaea.664351
title: Oceanography at CTD/bottle station IFREMER_1192
DOI: 10.1594/pangaea.927140
title: Light intensity time series from 16 locations in Løgstør Bredning, Limfjorden, Denmark, at 3 m above seabed, 9-March-2017

description: Field studies were conducted in two different areas of the Limfjorden, in Lovns Bredning (26th February to 4th March 2017) and in Løgstør Bredning (6-10th March 2017). In each sampling area, 16 fixed-position moorings were deployed in two circular sensor arrays around a mussel dredging area to investigate possible effects of dredging related sediment plumes (Pastor et al, 2020). The inner array (stations 1 - 8) had a diameter of 200 m and the outer array (stations 9 - 16) was set up with a diameter of 600 m. Integrated temperature and light loggers (HOBO Pendant Temperature/Light 64K Data Logger) were mounted on each mooring in the two circular arrays at three different water depths (0.5, 1.5 and 3.0 m above seabed). The 48 loggers (3 depths and 16 stations) were deployed in each area over a period of four days and light intensity time series were collected with a sampling interval of 30 seconds. Five loggers in the Lovns area did not provide any data due to technical problems (two near-surface loggers and three loggers at 1.5 m above the seabed). However, only one bottom logger at Løgstør Bredning failed to provide data. Each time series was filtered using a 3-minute moving average for removing the largest outliers, but retaining sharp changes in light intensity associated with short-lived sediment plumes caused by experimental mussel dredging.
DOI: 10.1594/pangaea.880691
title: Expanded measurements from station Lindenberg (2013-02)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.668811
title: Basic measurements of radiation at station Carpentras (1996-09)
DOI: 10.1594/pangaea.927142
title: Light intensity time series from 16 locations in Lovns Bredning, Limfjorden, Denmark, at 0.5 m above seabed, 1-March-2017

description: Field studies were conducted in two different areas of the Limfjorden, in Lovns Bredning (26th February to 4th March 2017) and in Løgstør Bredning (6-10th March 2017). In each sampling area, 16 fixed-position moorings were deployed in two circular sensor arrays around a mussel dredging area to investigate possible effects of dredging related sediment plumes (Pastor et al, 2020). The inner array (stations 1 - 8) had a diameter of 200 m and the outer array (stations 9 - 16) was set up with a diameter of 600 m. Integrated temperature and light loggers (HOBO Pendant Temperature/Light 64K Data Logger) were mounted on each mooring in the two circular arrays at three different water depths (0.5, 1.5 and 3.0 m above seabed). The 48 loggers (3 depths and 16 stations) were deployed in each area over a period of four days and light intensity time series were collected with a sampling interval of 30 seconds. Five loggers in the Lovns area did not provide any data due to technical problems (two near-surface loggers and three loggers at 1.5 m above the seabed). However, only one bottom logger at Løgstør Bredning failed to provide data. Each time series was filtered using a 3-minute moving average for removing the largest outliers, but retaining sharp changes in light intensity associated with short-lived sediment plumes caused by experimental mussel dredging.
DOI: 10.1594/pangaea.870138
title: Links to master tracks in different resolutions from POLAR 2 flight EPICA_IX_04
DOI: 10.1594/pangaea.927147
title: Light intensity time series from 16 locations in Lovns Bredning, Limfjorden, Denmark, at 0.5 m above seabed, 2-March-2017

description: Field studies were conducted in two different areas of the Limfjorden, in Lovns Bredning (26th February to 4th March 2017) and in Løgstør Bredning (6-10th March 2017). In each sampling area, 16 fixed-position moorings were deployed in two circular sensor arrays around a mussel dredging area to investigate possible effects of dredging related sediment plumes (Pastor et al, 2020). The inner array (stations 1 - 8) had a diameter of 200 m and the outer array (stations 9 - 16) was set up with a diameter of 600 m. Integrated temperature and light loggers (HOBO Pendant Temperature/Light 64K Data Logger) were mounted on each mooring in the two circular arrays at three different water depths (0.5, 1.5 and 3.0 m above seabed). The 48 loggers (3 depths and 16 stations) were deployed in each area over a period of four days and light intensity time series were collected with a sampling interval of 30 seconds. Five loggers in the Lovns area did not provide any data due to technical problems (two near-surface loggers and three loggers at 1.5 m above the seabed). However, only one bottom logger at Løgstør Bredning failed to provide data. Each time series was filtered using a 3-minute moving average for removing the largest outliers, but retaining sharp changes in light intensity associated with short-lived sediment plumes caused by experimental mussel dredging.
DOI: 10.1594/pangaea.498175
title: Physical oceanography from BT during cruise U58XX02054B_1984
DOI: 10.1594/pangaea.916125
title: Fig. 12. The average confidence interval
DOI: 10.1594/pangaea.499056
title: Physical oceanography from BT during cruise U90X008243B_1977
DOI: 10.1594/pangaea.830941
title: Satellite-based lake surface water temperatures from Lake_Starnberg, 1989-2013

description: Lake Surface Water Temperature (LSWT) has been extracted from a 3x3 pixel array at the center of the lake. See "Event(s)" for Lake/pixel co-ordinates.
DOI: 10.1594/pangaea.926828
title: Walker Lane GPS Rates

description: The interseismic motion of GPS stations in a tectonically active, diffuse, strike-slip shear zone provide constraints on the overall deformation budget that can be compared to the summation of geologically-estimated fault slip rates to understand regional strain accommodation. The Walker Lane GPS velocities in this dataset represent a subset of GPS stations included in the Nevada Geodetic Laboratory MIDAS velocity solution (Blewitt et al., 2016, 2018; accessible at http://geodesy.unr.edu/velocities/midas.NA12.txt, last accessed 11/19/2020) . This dataset includes velocities for all GPS stations located between 34° N – 43° N latitude and 114° W – 123° W longitude with time series longer than 2.5 years from the semi-continuous MAGNET network operated by the Nevada Geodetic Laboratory (Blewitt et al., 2009) and neighboring continuous GPS stations. The MIDAS velocities are calculated using daily position data collected through August 2019 presented in the NA12 reference frame (Blewitt et al., 2013) , and corrected for the postseismic effects of historic ruptures in and surrounding the Walker Lane. The MIDAS algorithm is a median trend estimator that mitigates both seasonality and step discontinuities in the times series (Blewitt et al., 2016). The resulting velocities are insensitive to the coseismic and postseismic effects of earthquakes that occurred after the midpoint of the time series (Blewitt et al., 2016) , such as the July 2019 Ridgecrest, CA M w 6.4 and 7.1 sequence, but must be corrected for the post-seismic effects of earthquakes that occurred prior to the middle of time series, such as the historic surface rupturing earthquakes in Central Nevada Seismic Belt and the 1993 Landers M w 7.3, and 1999 Hector Mine M w 7.0 events. We apply the viscoelastic postseismic relaxation correction from Bormann et al. (2013) that was developed using the method of Hammond et al. (2010) and the preferred western Basin and Range lower crust (10 20.5 Pa-s) and upper mantle (10 19 Pa-s) viscosity model of Hammond et al. (2009).When using this dataset, please also cite Blewitt et al (2018) as the authors of the original MIDAS NA12 reference frame velocity solution is the basis for our postseismic corrected Walker Lane velocities: Blewitt, G., Hammond, W.C., Kreemer, C., 2018. Harnessing the GPS Data Explosion for Interdisciplinary Science. Eos. https://doi.org/10.1029/2018EO104623.
DOI: 10.1594/pangaea.611071
title: Vertical distribution of siphonophores at station M26_NET003 in the upwelling area off NW Africa (Table 1-7)
DOI: 10.1594/pangaea.771539
title: (Table 9.1.3) Abundance of microorganisms in foulings on rocks of the Axial Seamount, Juan de Fuca Ridge
DOI: 10.1594/pangaea.688647
title: Primary production of carbon from three subfractions at bottle station SEPT-1999-K3

description: Photosynthetic productivity was measured according to the in situ 14C method. Fractionation was carried out by filtration through polycarbonate Millipore filters having porosities 0.2 (total stock), 1.2 and 3.0 µm. (Steemann-Nielsen, E., 1952. The use of radioactive carbon (14C) for measuring organic production in the sea. Journal du Conseil Permanent International pour l' Exploration de la Mer 18, 117-140.)
DOI: 10.1594/pangaea.688648
title: Primary production of carbon from three subfractions at bottle station SEPT-1999-K5

description: Photosynthetic productivity was measured according to the in situ 14C method. Fractionation was carried out by filtration through polycarbonate Millipore filters having porosities 0.2 (total stock), 1.2 and 3.0 µm. (Steemann-Nielsen, E., 1952. The use of radioactive carbon (14C) for measuring organic production in the sea. Journal du Conseil Permanent International pour l' Exploration de la Mer 18, 117-140.)
DOI: 10.1594/pangaea.779089
title: Core-section summary from IODP Hole 317-U1354C
DOI: 10.1594/pangaea.674375
title: Radiosonde measurements from Neumayer Station (1994-03)
DOI: 10.1594/pangaea.467143
title: Physical oceanography measured off Santa Rosa island in 2004, Pisco, Peru
DOI: 10.1594/pangaea.495582
title: Water temperature MBT profiles from cruise U7426245M_1954
DOI: 10.1594/pangaea.779096
title: Carbonate analysis from IODP Hole 317-U1354C

description: Geocode = Top depth CSF-A (m).Introduction to shipboard organic geochemistry on the JOIDES Resolution; ODP Technical Note 30: http://www-odp.tamu.edu/publications/tnotes/tn30/TNOTE_30.PDF
DOI: 10.1594/pangaea.916192
title: Selected tie point of cone penetration tests from Bremen, Northern Germany

description: TieP_#: selected tie point for test S# [m]#: number of test
DOI: 10.1594/pangaea.779115
title: (Table 2) Chemical composition of volcanites from the Sea of Okhotsk
DOI: 10.1594/pangaea.808577
title: Code and readme of a MATLAB-based graphical user interface program for computing functionals of the geopotential

description: We present a novel graphical user interface program GrafLab (GRAvity Field LABoratory) for spherical harmonic synthesis (SHS) created in MATLAB®. This program allows to comfortably compute 38 various functionals of the geopotential up to ultra-high degrees and orders of spherical harmonic expansion. For the most difficult part of the SHS, namely the evaluation of the fully normalized associated Legendre functions (fnALFs), we used three different approaches according to required maximum degree: (i) the standard forward column method (up to maximum degree 1800, in some cases up to degree 2190); (ii) the modified forward column method combined with Horner's scheme (up to maximum degree 2700); (iii) the extended-range arithmetic (up to an arbitrary maximum degree). For the maximum degree 2190, the SHS with fnALFs evaluated using the extended-range arithmetic approach takes only approximately 2-3 times longer than its standard arithmetic counterpart, i.e. the standard forward column method. In the GrafLab, the functionals of the geopotential can be evaluated on a regular grid or point-wise, while the input coordinates can either be read from a data file or entered manually. For the computation on a regular grid we decided to apply the lumped coefficients approach due to significant time-efficiency of this method. Furthermore, if a full variance-covariance matrix of spherical harmonic coefficients is available, it is possible to compute the commission errors of the functionals. When computing on a regular grid, the output functionals or their commission errors may be depicted on a map using automatically selected cartographic projection.
description: Supplement to: Bucha, Blazej; Janak, Juraj (2013): A MATLAB-based graphical user interface program for computing functionals of the geopotential up to ultra-high degrees and orders. Computers & Geosciences, 56, 186-196
DOI: 10.1594/pangaea.812667
title: (Table 5) Lifestyle preference of Arctic indigenous peoples by gender and country
DOI: 10.1594/pangaea.816909
title: Physical oceanography during John P. Tully cruise IOS_96-01
DOI: 10.1594/pangaea.779100
title: Gamma ray attenuation bulk density from IODP Hole 317-U1354C

description: Geocode = Depth CSF-A (m).Gamma-Ray densiometry principles and system implementation notes; Technical Note 26 Chapter 3: http://www-odp.tamu.edu/publications/tnotes/tn26/CHAP3.PDF
DOI: 10.1594/pangaea.870169
title: Links to master tracks in different resolutions from POLAR 2 flight EPICA_IX_33
DOI: 10.1594/pangaea.706907
title: (Page LVI) Salinity of surface water at station Godthaab

description: Position uncertain
DOI: 10.1594/pangaea.870056
title: Links to master tracks in different resolutions from POLAR 2 flight EMAGE-V_06
DOI: 10.1594/pangaea.870106
title: Links to master tracks in different resolutions from POLAR 2 flight EPICA_III_16
DOI: 10.1594/pangaea.812681
title: (Table 16) Arctic indigenous people of age 15 and above experiencing problems with alcohol or drugs in home today and victims of (other than sexual) assaults during last 12 months
DOI: 10.1594/pangaea.872268
title: Links to master tracks in different resolutions from POLAR 2 flight EPICA_I_01
DOI: 10.1594/pangaea.870108
title: Links to master tracks in different resolutions from POLAR 2 flight EPICA_III_18
DOI: 10.1594/pangaea.774928
title: Continuous meteorological observations at Neumayer station (1996-02)
DOI: 10.1594/pangaea.870333
title: Links to master tracks in different resolutions from POLAR 6 flight WEGAS_1112302201
DOI: 10.1594/pangaea.779102
title: Interstitial water analysis from IODP Hole 317-U1354C

description: Geocode = Top depth CSF-A (m)Chemical methods for interstitial water analysis aboard JOIDES Resolution; ODP Technical Note 15: http://www-odp.tamu.edu/publications/tnotes/tn15/technote15.pdfAnalysis of major and trace elements in rocks, sediments, and interstitial waters by ICP-AES; ODP Technical Note 29 : http://www-odp.tamu.edu/publications/tnotes/tn29/TNOTE_29.PDFIntroduction to shipboard organic geochemistry on the JOIDES Resolution; ODP Technical Note 30: http://www-odp.tamu.edu/publications/tnotes/tn30/TNOTE_30.PDF
DOI: 10.1594/pangaea.870209
title: Links to master tracks in different resolutions from POLAR 2 flight EPICA_VII_26
DOI: 10.1594/pangaea.870233
title: Links to master tracks in different resolutions from POLAR 2 flight EPICA_VIII_20
DOI: 10.1594/pangaea.870235
title: Links to master tracks in different resolutions from POLAR 2 flight EPICA_VIII_22
DOI: 10.1594/pangaea.694787
title: Temperature and salinity in the water column of the Ionian Sea at Station SEPT-2000-IRI33

description: The 911plus set has been used. It consists of the 9plus underwater CTD unit and the 11plus V2 deck unit. It has high resolution sampling (24 Hz), pump-controlled T-C ducted flow, up to 10500 meter (15,000 psia) depth capability, maximum auxiliary sensor flexibility, and modem channel for water sampling control. The 911plus set has eight 12-bit A/D channels and supports redundant C&T sensors or custom auxiliary digital inputs.
DOI: 10.1594/pangaea.870135
title: Links to master tracks in different resolutions from POLAR 2 flight EPICA_IX_01