cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.784594
title: Radiosonde PS79/33487 during POLARSTERN cruise ANT-XXVIII/5 on 2012-04-16 10:58h

description: Height of tropopause 10083 m, precipitable water content 1.6121 cm
DOI: 10.1594/pangaea.784595
title: Radiosonde PS79/33488 during POLARSTERN cruise ANT-XXVIII/5 on 2012-04-17 10:53h

description: Height of tropopause 10887 m, precipitable water content 1.3030 cm
DOI: 10.1594/pangaea.784596
title: Radiosonde PS79/33489 during POLARSTERN cruise ANT-XXVIII/5 on 2012-04-18 10:59h

description: Height of tropopause 11509 m, precipitable water content 1.5731 cm
DOI: 10.1594/pangaea.784597
title: Radiosonde PS79/33490 during POLARSTERN cruise ANT-XXVIII/5 on 2012-04-19 10:51h

description: Height of tropopause 17120 m, precipitable water content 2.3006 cm
DOI: 10.1594/pangaea.784598
title: Radiosonde PS79/33491 during POLARSTERN cruise ANT-XXVIII/5 on 2012-04-20 10:52h

description: Height of tropopause 16365 m, precipitable water content 2.2384 cm
DOI: 10.1594/pangaea.784599
title: Radiosonde PS79/33492 during POLARSTERN cruise ANT-XXVIII/5 on 2012-04-21 10:50h

description: Height of tropopause 15257 m, precipitable water content 3.1318 cm
DOI: 10.1594/pangaea.784600
title: Radiosonde PS79/33493 during POLARSTERN cruise ANT-XXVIII/5 on 2012-04-22 10:59h

description: Height of tropopause 16158 m, precipitable water content 3.0094 cm
DOI: 10.1594/pangaea.784602
title: Radiosonde PS79/33494 during POLARSTERN cruise ANT-XXVIII/5 on 2012-04-23 10:50h

description: Height of tropopause 16514 m, precipitable water content 2.4337 cm
DOI: 10.1594/pangaea.784603
title: Radiosonde PS79/33495 during POLARSTERN cruise ANT-XXVIII/5 on 2012-04-24 10:56h

description: Height of tropopause 16103 m, precipitable water content 2.9253 cm
DOI: 10.1594/pangaea.784604
title: Radiosonde PS79/33496 during POLARSTERN cruise ANT-XXVIII/5 on 2012-04-25 10:51h

description: Height of tropopause 18012 m, precipitable water content 2.9737 cm
DOI: 10.1594/pangaea.784605
title: Radiosonde PS79/33497 during POLARSTERN cruise ANT-XXVIII/5 on 2012-04-26 10:52h

description: Height of tropopause 17180 m, precipitable water content 4.2146 cm
DOI: 10.1594/pangaea.784606
title: Radiosonde PS79/33498 during POLARSTERN cruise ANT-XXVIII/5 on 2012-04-27 10:50h

description: Height of tropopause 17014 m, precipitable water content 3.9486 cm
DOI: 10.1594/pangaea.784612
title: Radiosonde PS79/33504 during POLARSTERN cruise ANT-XXVIII/5 on 2012-05-03 11:15h

description: Height of tropopause 17169 m, precipitable water content 2.3139 cm
DOI: 10.1594/pangaea.784613
title: Radiosonde PS79/33505 during POLARSTERN cruise ANT-XXVIII/5 on 2012-05-04 10:54h

description: Height of tropopause 13490 m, precipitable water content 1.2311 cm
DOI: 10.1594/pangaea.784614
title: Radiosonde PS79/33506 during POLARSTERN cruise ANT-XXVIII/5 on 2012-05-05 10:55h

description: Height of tropopause 13768 m, precipitable water content 1.5272 cm
DOI: 10.1594/pangaea.784621
title: Radiosonde PS79/33512 during POLARSTERN cruise ANT-XXVIII/3 on 2012-02-16 11:02h

description: Height of tropopause 10688 m, precipitable water content 2.3573 cm
DOI: 10.1594/pangaea.784622
title: Radiosonde PS79/33513 during POLARSTERN cruise ANT-XXVIII/3 on 2012-02-17 10:59h

description: Height of tropopause 8691 m, precipitable water content 0.7556 cm
DOI: 10.1594/pangaea.784623
title: Radiosonde PS79/33514 during POLARSTERN cruise ANT-XXVIII/3 on 2012-02-18 11:01h

description: Height of tropopause 7634 m, precipitable water content 1.4487 cm
DOI: 10.1594/pangaea.784624
title: Radiosonde PS79/33515 during POLARSTERN cruise ANT-XXVIII/3 on 2012-02-19 11:01h

description: Height of tropopause 7187 m, precipitable water content 0.8359 cm
DOI: 10.1594/pangaea.784625
title: Radiosonde PS79/33516 during POLARSTERN cruise ANT-XXVIII/3 on 2012-02-20 10:59h

description: Height of tropopause 9756 m, precipitable water content 1.2154 cm
DOI: 10.1594/pangaea.784626
title: Radiosonde PS79/33517 during POLARSTERN cruise ANT-XXVIII/3 on 2012-02-21 10:59h

description: Height of tropopause 9511 m, precipitable water content 0.7040 cm
DOI: 10.1594/pangaea.784628
title: Radiosonde PS79/33518 during POLARSTERN cruise ANT-XXVIII/3 on 2012-02-22 11:00h

description: Height of tropopause 7918 m, precipitable water content 0.5734 cm
DOI: 10.1594/pangaea.784629
title: Radiosonde PS79/33519 during POLARSTERN cruise ANT-XXVIII/3 on 2012-02-23 10:58h

description: Precipitable water content 0.5145 cm
DOI: 10.1594/pangaea.784630
title: Radiosonde PS79/33520 during POLARSTERN cruise ANT-XXVIII/3 on 2012-02-24 11:00h

description: Height of tropopause 7055 m, precipitable water content 0.7887 cm
DOI: 10.1594/pangaea.784631
title: Radiosonde PS79/33521 during POLARSTERN cruise ANT-XXVIII/3 on 2012-02-25 10:59h

description: Height of tropopause 8107 m, precipitable water content 0.8069 cm
DOI: 10.1594/pangaea.784632
title: Radiosonde PS79/33522 during POLARSTERN cruise ANT-XXVIII/3 on 2012-02-26 11:04h

description: Height of tropopause 10439 m, precipitable water content 0.7625 cm
DOI: 10.1594/pangaea.784633
title: Radiosonde PS79/33523 during POLARSTERN cruise ANT-XXVIII/3 on 2012-02-27 10:59h

description: Height of tropopause 11814 m, precipitable water content 1.1838 cm
DOI: 10.1594/pangaea.784634
title: Radiosonde PS79/33524 during POLARSTERN cruise ANT-XXVIII/3 on 2012-02-28 10:59h

description: Height of tropopause 9616 m, precipitable water content 1.7969 cm
DOI: 10.1594/pangaea.784635
title: Radiosonde PS79/33525 during POLARSTERN cruise ANT-XXVIII/3 on 2012-02-29 10:58h

description: Height of tropopause 9473 m, precipitable water content 0.7476 cm
DOI: 10.1594/pangaea.784636
title: Radiosonde PS79/33526 during POLARSTERN cruise ANT-XXVIII/3 on 2012-03-01 11:00h

description: Height of tropopause 10704 m, precipitable water content 0.9593 cm
DOI: 10.1594/pangaea.784637
title: Radiosonde PS79/33527 during POLARSTERN cruise ANT-XXVIII/3 on 2012-03-02 10:57h

description: Height of tropopause 11275 m, precipitable water content 1.0373 cm
DOI: 10.1594/pangaea.784639
title: Radiosonde PS79/33528 during POLARSTERN cruise ANT-XXVIII/3 on 2012-03-03 11:00h

description: Height of tropopause 10982 m, precipitable water content 1.2410 cm
DOI: 10.1594/pangaea.784640
title: Radiosonde PS79/33529 during POLARSTERN cruise ANT-XXVIII/3 on 2012-03-04 10:59h

description: Height of tropopause 11045 m, precipitable water content 1.6879 cm
DOI: 10.1594/pangaea.784641
title: Radiosonde PS79/33530 during POLARSTERN cruise ANT-XXVIII/3 on 2012-03-05 10:59h

description: Height of tropopause 12224 m, precipitable water content 1.6087 cm
DOI: 10.1594/pangaea.783905
title: Continuous meteorological surface measurement during POLARSTERN cruise ANT-XXVII/4
DOI: 10.1594/pangaea.784642
title: Radiosonde PS79/33531 during POLARSTERN cruise ANT-XXVIII/3 on 2012-03-06 10:58h

description: Height of tropopause 7077 m, precipitable water content 1.3318 cm
DOI: 10.1594/pangaea.784452
title: Continuous meteorological surface measurement during POLARSTERN cruise ANT-XXVIII/1
DOI: 10.1594/pangaea.784979
title: (Table 1) Population density and biomass of the foraminifer Rupertina, and grain size of cores from the Norwegian continental slope

description: Rupertina stabilis occupies a depth restricted biotope of suspension feeding animals situated at the Norwegian continental margin. It extends from the Voring plateau northwards for at least 200 - 300 km, in depths between 600 and 800 m. This slope position is known for relatively strong bottom currents and shifting watermass boundaries. - The species is attached to hard substrates, mainly stones or hydroid stalks and obviously prefers an elevated position. It is building a permanent cyst of sponge spicules and debris at the apertural region. The spicules are used to support a pseudopodial network similar to that described from Halyphysema (LIPPS 1983). It is believed to serve as a filter apparatus. - A review of known occurences in the Atlantic is given, suggesting a temperature adaption of the species ranging from 0°C to a maximum of 8°C. Specimens were successfully cultured for about 2-3 weeks.
description: Biomass was originally given in µg/10 cm**2 and was recalculated to g/m**2 by dividing by 1000.
description: Supplement to: Lutze, Gerhard F; Altenbach, Alexander V (1988): Rupertina stabilis (WALLICH), a highly adapted, suspension feeding foraminifer. Meyniana, 40, 55-69
DOI: 10.1594/pangaea.784453
title: Continuous meteorological surface measurement during POLARSTERN cruise ANT-XXVIII/2
DOI: 10.1594/pangaea.784454
title: Continuous meteorological surface measurement during POLARSTERN cruise ANT-XXVIII/3
DOI: 10.1594/pangaea.784456
title: Continuous meteorological surface measurement during POLARSTERN cruise ANT-XXVIII/5
DOI: 10.1594/pangaea.785401
title: (Table 5) Geochemistry of ODP Site 131-808 muds and mudstones

description: Sediment depth is given in mbsf. Analyses recalculated to include loss on ignition (LOI).
DOI: 10.1594/pangaea.785410
title: (Table 7) Rare earth elements of ODP Site 131-808 muds and mudstones

description: Sediment depth is given in mbsf. Analyses recalculated to include loss on ignition (LOI).
DOI: 10.1594/pangaea.784117
title: Hopanol data from GeoB3918-2
DOI: 10.1594/pangaea.785120
title: (Table 2) CT scan measurements of ODP Site 131-808

description: X-ray computed tomography (CT) is a promising tool that yields data useful for understanding the fine-scale density structure of partly lithified and tectonically deformed sediments. We conducted 21 CT scans of ODP Leg 131 sediments, including whole-round cores and thin-section chips, obtained from the toe of the Nankai accretionary prism. The samples range from highly deformed pieces from the frontal thrust and décollement to homogeneous and essentially undeformed sediments above the frontal thrust and beneath the décollement. In the CT images, kink-like deformation bands and faults are recognized as obvious bright seams, bands, or stripes with relatively high linear attenuation coefficients. The differences in linear attenuation coefficients relative to the matrix range from 0.021 cm**2/g (kink-like deformation band) to 0.038 cm**2/g (fault). These data suggest a 0.10 g/cm**3 to 0.18 g/cm**3 increase in bulk density within the deformation structures, and they appear to be 13% and 33% more compacted than the nondeformed matrix, respectively. In contrast to the samples from the frontal thrust zone, CT images of the décollement sample exhibit relatively homogeneous textures. The attenuation coefficient of the sample of the décollement indicates bulk density and porosity values of 2.45 g/cm**3 and 18%, respectively. The sample, hence, is approximately 50% more compacted than the sediment outside the décollement zone.
description: Supplement to: Soh, Wonn; Byrne, Timothy; Taira, Asahiko; Kono, Atsushi (1993): Computed tomography (CT) scan image analysis of Site 808 cores: structural and physical property implications. In: Hill, IA; Taira, A; Firth, JV; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 131, 135-140
DOI: 10.1594/pangaea.785131
title: Sedimentation rates on the Yermak Plateau during different oxygen isotope stages

description: Three cores of bottom sediments sampled from the Yermak Plateau are scrutinized. Age model based on AMS 14C dating and oxygen isotope stratigraphy (OIS) is presented for the reference core PS 2837. Hypothetical stratigraphic models for cores PS 2834 and PS 2859 are based on lithostratigraphic analyses. Detailed layer-by-layer descriptions of all studied sections are given based on grain size distribution and contents of CaCO3, Corg, and heavy minerals.
description: Supplement to: Levitan, Mikhail A; Musatov, Evgeny E; Burtman, M V (2002): History of Sedimentation on the Yermak Plateau during the Recent 190 ka: Communication 1. Lithology and Mineralogy of Middle Pleistocene–Holocene Sediments. Lithology and Mineral Resources, 37(6), 481-492
DOI: 10.1594/pangaea.785139
title: (Table 1) Sedimentation rates and accumulation rates of Upper Pleistocene and Holocene bottom sediments from the Sea of Okhotsk and silica accumulation rates in these sediments
DOI: 10.1594/pangaea.785140
title: (Table 2) Physical properties of Holocene and Upper Pleistocene bottom sediments from the Sea of Okhotsk
DOI: 10.1594/pangaea.785141
title: (Table 3) Mineral composition of clay fraction from bottom sediments of the Sea of Okhotsk

description: &gt;0 = traces; + = kaolinite is inferred from resolution of reflection doublets of chlorite (004) and kaolinite (002) in diffractograms; empty digital cells = questionable data.
DOI: 10.1594/pangaea.785044
title: (Table 1) Clay mineralogy for hemipelagic mud samples of ODP Site 131-808
DOI: 10.1594/pangaea.785144
title: (Table 4) Chemical composition of bottom sediments from the Sea of Okhotsk
DOI: 10.1594/pangaea.785045
title: (Table 2) Clay mineralogy for turbidite matrix samples of ODP Site 131-808
DOI: 10.1594/pangaea.785057
title: (Table 1) Current ripples from the trench outer slope, ODP Hole 131-808C

description: The Ocean Drilling Program Leg 131, which drilled in the Nankai Trough in the western Pacific Ocean, has shown for the first time that turbidity currents are deflected and reflected against the trench slopes, such that in the trench outer slope there is a predominant pattern of currents, carrying terrigenous sediments, apparently coming from the open-ocean Shikoku Basin directly toward the trench landward-slope. The purpose of this paper is to summarize the evidence for flow rebound at ODP Leg 131 Site 808, and to show that these results have important implications for the interpretation of paleocurrents in ancient linear turbidite systems.
description: Supplement to: Pickering, Kevin T; Underwood, Michael B; Taira, Asahiko (1993): Open-ocean to trench turbidity-current flow in the Nankai Trough: flow collapse and flow reflection. In: Hill, IA; Taira, A; Firth, JV; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 131, 35-43
DOI: 10.1594/pangaea.785817
title: Sea ice draft measured by upward looking sonar at mooring site AWI231-3

description: Lograte: 4 min. The data identification flags (columns 6 & 8) stand for: 1=ice, 2=thin ice/open water, 0=water, empty cells=rejected/erroneous data. Depth was calculated by: (p_uls-p_atm)/(rho * g), where p_uls is the measured water pressure, p_atm is the atmospheric pressure from ECMWF (http://www.ecmwf.int) reanalysis, rho is 1027 kg/m**3, and g is the latitude-dependent acceleration of gravity.
DOI: 10.1594/pangaea.785818
title: Sea ice draft measured by upward looking sonar at mooring site AWI231-4

description: Lograte: 4 min. The data identification flags (columns 6 & 8) stand for: 1=ice, 2=thin ice/open water, 0=water, empty cells=rejected/erroneous data. Depth was calculated by: (p_uls-p_atm)/(rho * g), where p_uls is the measured water pressure, p_atm is the atmospheric pressure from ECMWF (http://www.ecmwf.int) reanalysis, rho is 1027 kg/m**3, and g is the latitude-dependent acceleration of gravity.
DOI: 10.1594/pangaea.785819
title: Sea ice draft measured by upward looking sonar at mooring site AWI231-6

description: Lograte: 1 min. Time gaps: No values recorded by the ULS. The data identification flags (columns 6 & 8) stand for: 1=ice, 2=thin ice/open water, 0=water, empty cells=rejected/erroneous data. Depth was calculated by: (p_uls-p_atm)/(rho * g), where p_uls is the measured water pressure, p_atm is the atmospheric pressure from ECMWF (http://www.ecmwf.int) reanalysis, rho is 1027 kg/m**3, and g is the latitude-dependent acceleration of gravity.
DOI: 10.1594/pangaea.785820
title: Sea ice draft measured by upward looking sonar at mooring site AWI231-7

description: Lograte: 2 min. Time gaps: No values recorded by the ULS. The data identification flags (columns 6 & 8) stand for: 1=ice, 2=thin ice/open water, 0=water, empty cells=rejected/erroneous data. Depth was calculated by: (p_uls-p_atm)/(rho * g), where p_uls is the measured water pressure, p_atm is the atmospheric pressure from ECMWF (http://www.ecmwf.int) reanalysis, rho is 1027 kg/m**3, and g is the latitude-dependent acceleration of gravity.
DOI: 10.1594/pangaea.785821
title: Sea ice draft measured by upward looking sonar at mooring site AWI232-1

description: Lograte: 15 min. The data identification flags (columns 6 & 8) stand for: 1=ice, 2=thin ice/open water, 0=water, empty cells=rejected/erroneous data. Depth was calculated by: (p_uls-p_atm)/(rho * g), where p_uls is the measured water pressure, p_atm is the atmospheric pressure from ECMWF (http://www.ecmwf.int) reanalysis, rho is 1027 kg/m**3, and g is the latitude-dependent acceleration of gravity.
DOI: 10.1594/pangaea.785822
title: Sea ice draft measured by upward looking sonar at mooring site AWI232-4

description: Lograte: 4 min. Time gaps: No values recorded by the ULS. The data identification flags (columns 6 & 8) stand for: 1=ice, 2=thin ice/open water, 0=water, empty cells=rejected/erroneous data. Depth was calculated by: (p_uls-p_atm)/(rho * g), where p_uls is the measured water pressure, p_atm is the atmospheric pressure from ECMWF (http://www.ecmwf.int) reanalysis, rho is 1027 kg/m**3, and g is the latitude-dependent acceleration of gravity.
DOI: 10.1594/pangaea.785823
title: Sea ice draft measured by upward looking sonar at mooring site AWI232-5

description: Lograte: 4 min. Time gaps: No values recorded by the ULS. The data identification flags (columns 6 & 8) stand for: 1=ice, 2=thin ice/open water, 0=water, empty cells=rejected/erroneous data. Depth was calculated by: (p_uls-p_atm)/(rho * g), where p_uls is the measured water pressure, p_atm is the atmospheric pressure from ECMWF (http://www.ecmwf.int) reanalysis, rho is 1027 kg/m**3, and g is the latitude-dependent acceleration of gravity.
DOI: 10.1594/pangaea.785824
title: Sea ice draft measured by upward looking sonar at mooring site AWI232-6

description: Lograte: 4 min. The data identification flags (columns 6 & 8) stand for: 1=ice, 2=thin ice/open water, 0=water, empty cells=rejected/erroneous data. Depth was calculated by: (p_uls-p_atm)/(rho * g), where p_uls is the measured water pressure, p_atm is the atmospheric pressure from ECMWF (http://www.ecmwf.int) reanalysis, rho is 1027 kg/m**3, and g is the latitude-dependent acceleration of gravity.
DOI: 10.1594/pangaea.785825
title: Sea ice draft measured by upward looking sonar at mooring site AWI232-8

description: Lograte: 2 min. Time gaps: No values recorded by the ULS. The data identification flags (columns 6 & 8) stand for: 1=ice, 2=thin ice/open water, 0=water, empty cells=rejected/erroneous data. Depth was calculated by: (p_uls-p_atm)/(rho * g), where p_uls is the measured water pressure, p_atm is the atmospheric pressure from ECMWF (http://www.ecmwf.int) reanalysis, rho is 1027 kg/m**3, and g is the latitude-dependent acceleration of gravity.
DOI: 10.1594/pangaea.785826
title: Sea ice draft measured by upward looking sonar at mooring site AWI233-2

description: Lograte: 3 min. The data identification flags (columns 6 & 8) stand for: 1=ice, 2=thin ice/open water, 0=water, empty cells=rejected/erroneous data. Depth was calculated by: (p_uls-p_atm)/(rho * g), where p_uls is the measured water pressure, p_atm is the atmospheric pressure from ECMWF (http://www.ecmwf.int) reanalysis, rho is 1027 kg/m**3, and g is the latitude-dependent acceleration of gravity.
DOI: 10.1594/pangaea.785827
title: Sea ice draft measured by upward looking sonar at mooring site AWI233-6

description: Lograte: 4 min. The data identification flags (columns 6 & 8) stand for: 1=ice, 2=thin ice/open water, 0=water, empty cells=rejected/erroneous data. Depth was calculated by: (p_uls-p_atm)/(rho * g), where p_uls is the measured water pressure, p_atm is the atmospheric pressure from ECMWF (http://www.ecmwf.int) reanalysis, rho is 1027 kg/m**3, and g is the latitude-dependent acceleration of gravity.
DOI: 10.1594/pangaea.785673
title: Bacteriohopanepolyol data of sediment core GeoB3918-2
DOI: 10.1594/pangaea.785797
title: Sea ice draft measured by upward looking sonar at mooring site AWI207-2

description: Lograte: 8 min. The data identification flags (columns 6 & 8) stand for: 1=ice, 2=thin ice/open water, 0=water, empty cells=rejected/erroneous data. Depth was calculated by: (p_uls-p_atm)/(rho * g), where p_uls is the measured water pressure, p_atm is the atmospheric pressure from ECMWF (http://www.ecmwf.int) reanalysis, rho is 1027 kg/m**3, and g is the latitude-dependent acceleration of gravity.
DOI: 10.1594/pangaea.785798
title: Sea ice draft measured by upward looking sonar at mooring site AWI207-4

description: Lograte: 15 min. The data identification flags (columns 6 & 8) stand for: 1=ice, 2=thin ice/open water, 0=water, empty cells=rejected/erroneous data. Depth was calculated by: (p_uls-p_atm)/(rho * g), where p_uls is the measured water pressure, p_atm is the atmospheric pressure from ECMWF (http://www.ecmwf.int) reanalysis, rho is 1027 kg/m**3, and g is the latitude-dependent acceleration of gravity.
DOI: 10.1594/pangaea.785799
title: Sea ice draft measured by upward looking sonar at mooring site AWI207-6

description: Lograte: 3 min. Time gaps: No values recorded by the ULS. The data identification flags (columns 6 & 8) stand for: 1=ice, 2=thin ice/open water, 0=water, empty cells=rejected/erroneous data. Depth was calculated by: (p_uls-p_atm)/(rho * g), where p_uls is the measured water pressure, p_atm is the atmospheric pressure from ECMWF (http://www.ecmwf.int) reanalysis, rho is 1027 kg/m**3, and g is the latitude-dependent acceleration of gravity.
DOI: 10.1594/pangaea.785800
title: Sea ice draft measured by upward looking sonar at mooring site AWI208-3

description: Lograte: 4 min. The data identification flags (columns 6 & 8) stand for: 1=ice, 2=thin ice/open water, 0=water, empty cells=rejected/erroneous data. Depth was calculated by: (p_uls-p_atm)/(rho * g), where p_uls is the measured water pressure, p_atm is the atmospheric pressure from ECMWF (http://www.ecmwf.int) reanalysis, rho is 1027 kg/m**3, and g is the latitude-dependent acceleration of gravity.
DOI: 10.1594/pangaea.785801
title: Sea ice draft measured by upward looking sonar at mooring site AWI209-3

description: Lograte: 4 min. The data identification flags (columns 6 & 8) stand for: 1=ice, 2=thin ice/open water, 0=water, empty cells=rejected/erroneous data. Depth was calculated by: (p_uls-p_atm)/(rho * g), where p_uls is the measured water pressure, p_atm is the atmospheric pressure from ECMWF (http://www.ecmwf.int) reanalysis, rho is 1027 kg/m**3, and g is the latitude-dependent acceleration of gravity.
DOI: 10.1594/pangaea.785802
title: Sea ice draft measured by upward looking sonar at mooring site AWI210-2

description: Lograte: 8 min. The data identification flags (columns 6 & 8) stand for: 1=ice, 2=thin ice/open water, 0=water, empty cells=rejected/erroneous data. Depth was calculated by: (p_uls-p_atm)/(rho * g), where p_uls is the measured water pressure, p_atm is the atmospheric pressure from ECMWF (http://www.ecmwf.int) reanalysis, rho is 1027 kg/m**3, and g is the latitude-dependent acceleration of gravity.
DOI: 10.1594/pangaea.785803
title: Sea ice draft measured by upward looking sonar at mooring site AWI212-2

description: Lograte: 8 min. The data identification flags (columns 6 & 8) stand for: 1=ice, 2=thin ice/open water, 0=water, empty cells=rejected/erroneous data. Depth was calculated by: (p_uls-p_atm)/(rho * g), where p_uls is the measured water pressure, p_atm is the atmospheric pressure from ECMWF (http://www.ecmwf.int) reanalysis, rho is 1027 kg/m**3, and g is the latitude-dependent acceleration of gravity.