cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.856994
title: (Table 2, page 158) Characteristics of manganese nodule assemblages from box grabs and free-fall grabs from the SEDIPERU areas A1 and A2, SONNE cruise SO79

description: In the nodule field of the Peru Basin, situated south of the zone of high bioproductivity, a relatively high flux of biogenic matter explains a distinct redox boundary at about 10 cm depth separating very soft oxic surface sediments from stiffer suboxic sediments. Maximum abundance (50 kg/m**2) of diagenetic nodules is found near the calcite compensation depth (CCD), currently at 4250 m. There, the accretion rate of nodules is much higher (100 mm/Ma) than on ridges (5 mm/Ma). Highest accretion rates are found at the bottom of large nodules that repeatedly sink to a level immediately above the redox boundary. There, distinct diagenetic growth conditions prevail and layers of dense laminated Mn oxide of very pure todorokite are formed. The layering of nodules is mainly the result of organisms moving nodules within the oxic surface sediment from diagenetic to hydrogenetic environments. The frequency of such movements is much higher than that of climatic changes. Two types of nodule burial occur in the Peru Basin. Large nodules are less easily moved by organisms and become buried. Consequently, buried nodules generally are larger than surface nodules. This type of burial predominates in basins. At ridges where smaller nodules prevail, burial is mainly controlled by statistical selection where some nodules are not moved up by organisms.
description: Nodule density and mass abundance was deduced from nodules retrieved by box corer (KG) of 0.25 m**2 or free-fall grab (BG) of 0.133 m**2 impacts.From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
description: Supplement to: von Stackelberg, Ulrich (1997): Growth history of manganese nodules and crusts of the Peru Basin. In: Nicholson, K., Hein, J.R., Bühn, B., Dasgupta, P. (Eds.), Manganese Mineralization: Geochemistry and Mineralogy of Terrestrial and Marine Deposits, Geological Society, London, Special Publications, 119(1), 153-176
DOI: 10.1594/pangaea.856995
title: (Table 8.4, Page 220-223) Chemical composition of different growth structures of manganese nodules, SONNE cruise SO79

description: In the nodule field of the Peru Basin, situated south of the zone of high bioproductivity, a relatively high flux of biogenic matter explains a distinct redox boundary at about 10 cm depth separating very soft oxic surface sediments from stiffer suboxic sediments. Maximum abundance (50 kg/m**2) of diagenetic nodules is found near the calcite compensation depth (CCD), currently at 4250 m. There, the accretion rate of nodules is much higher (100 mm/Ma) than on ridges (5 mm/Ma). Highest accretion rates are found at the bottom of large nodules that repeatedly sink to a level immediately above the redox boundary. There, distinct diagenetic growth conditions prevail and layers of dense laminated Mn oxide of very pure todorokite are formed. The layering of nodules is mainly the result of organisms moving nodules within the oxic surface sediment from diagenetic to hydrogenetic environments. The frequency of such movements is much higher than that of climatic changes. Two types of nodule burial occur in the Peru Basin. Large nodules are less easily moved by organisms and become buried. Consequently, buried nodules generally are larger than surface nodules. This type of burial predominates in basins. At ridges where smaller nodules prevail, burial is mainly controlled by statistical selection where some nodules are not moved up by organisms.
description: From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
description: Supplement to: von Stackelberg, Ulrich (2000): Manganese nodules of the Peru Basin (Chapter 8). In: Cronan, D.S. (Ed.), Handbook of Marine Mineral Deposits. CRC Press, Boca Raton, Florida, USA, 197-238
DOI: 10.1594/pangaea.857858
title: Swath sonar bathymetry during POLARSTERN cruise PS88.1 (ANT-XXX/1.1) with links to multibeam raw data files

description: Contact mailto:infobathy@awi.de for data access.
DOI: 10.1594/pangaea.857749
title: (Table 1) Sampling locations, water depth, and physical and chemical properties of surface sediment samples
DOI: 10.1594/pangaea.857859
title: Swath sonar bathymetry during POLARSTERN cruise PS88.2 (ANT-XXX/1.2) with links to multibeam raw data files

description: Contact mailto:infobathy@awi.de for data access.
DOI: 10.1594/pangaea.857751
title: Hydrochemistry of water samples during METEOR cruise M90

description: WOCE Quality Flags
DOI: 10.1594/pangaea.857753
title: (Table 3) Mg/Ca, Sr/Ca and Calcium isotope ratios of benthonic foraminifers

description: a: Number of replicate analyses 2 if not stated otherwise.*: Denotes samples analysed ones and application of the average 2 SD.c: Analytical precision is better 0.3% for Sr, Mg and Ca determination by ICP-MS.
DOI: 10.1594/pangaea.857759
title: (Table 4) Mg/Ca and Sr/Ca ratios of benthonic foraminifer tests

description: Samples derived from surface sediments (0-1 or 0-0.5 cm) except Cassidulina laevigata from core GA II32 XX, which was selected from 4 to 6 cm sediment depth.Data marked with italic numbers are excluded from the calculated temperature dependencies listed in Table 5.a: Calcium isotope compositions of species displayed in this table are reported in Gussone and Filipsson (2010).b: Analytical precision is better 0.3% for Sr, Mg and Ca determination by ICP-MS.
DOI: 10.1594/pangaea.857760
title: Nitrous oxide from water samples during METEOR cruise M90
DOI: 10.1594/pangaea.858532
title: Continuous meteorological surface measurement during POLARSTERN cruise ANT-XXIX/7
DOI: 10.1594/pangaea.858552
title: Inorganic geochemistry of pore water measured on sediment core PS78/206-3
DOI: 10.1594/pangaea.858553
title: Solid phase element geochemistry measured on sediment core PS78/206-3
DOI: 10.1594/pangaea.858554
title: Inorganic geochemistry of pore water measured on sediment core PS78/220-7
DOI: 10.1594/pangaea.858555
title: Solid phase element geochemistry measured on sediment core PS78/220-7
DOI: 10.1594/pangaea.858556
title: Inorganic geochemistry of pore water measured on sediment core PS78/237-3
DOI: 10.1594/pangaea.858557
title: Solid phase element geochemistry measured on sediment core PS78/237-3
DOI: 10.1594/pangaea.858558
title: Inorganic geochemistry of pore water measured on sediment core PS78/248-6
DOI: 10.1594/pangaea.858560
title: Solid phase element geochemistry measured on sediment core PS78/248-6
DOI: 10.1594/pangaea.858585
title: Sea-ice concentration and under-ice water parameters from the Eurasian central Arctic Ocean during August-September 2012
DOI: 10.1594/pangaea.858586
title: Under-ice fauna from the Eurasian central Arctic Ocean during August-September 2012
DOI: 10.1594/pangaea.858590
title: (Supplement Table S1) Measurement results of δ¹⁸O and Mg/Ca of sediment core GeoB10042-1
DOI: 10.1594/pangaea.858591
title: (Supplement Table S1) Measurement results of Ti/Ca of sediment core GeoB10042-1
DOI: 10.1594/pangaea.858594
title: (Supplement Table S2) Measurement results of δ¹⁸O and Mg/Ca of sediment core GeoB10043-3
DOI: 10.1594/pangaea.858595
title: (Supplement Table S2) Measurement results of Ti/Ca of sediment core GeoB10043-3
DOI: 10.1594/pangaea.858623
title: (Table 1) Sample locations, salinity and sea surface temperatures (SST) annual averages for the upper 10m from World Ocean Atlas 1998
DOI: 10.1594/pangaea.857265
title: (Table III) Age determination of east equatorial Pacific sediments
DOI: 10.1594/pangaea.858627
title: (Table 3) Coretop foraminifer results
DOI: 10.1594/pangaea.857317
title: (Fig. 3a) Stable oxygen isotope ratios of benthic foraminifera of sediment core MD95-2036
DOI: 10.1594/pangaea.857329
title: (Fig. 3b) Stable oxygen isotope ratios of planktonic foraminifera of sediment core MD95-2036
DOI: 10.1594/pangaea.857337
title: (Fig. 3c) Summer SST reconstruction for sediment core MD95-2036
DOI: 10.1594/pangaea.858070
title: Physical oceanography during METEOR cruise M92

description: Data from this cruise has been calibrated together with the data from the following cruise M93 which used the same CTD sensors. Oxygen has been calibrated by combining conventional Winkler titrations from M92 and M93 and data from a Unisense Stox sensor that is capable of measuring very low oxygen values. Oxygen values below 0 come either from very strong vertical gradient which results in an overshoot by a filter of the manufacturer, or are within the noise level of the instrument of about 1 mumol/kg. Such values hould be regarded as very very close to 0. Conductivity/Salinity measurements near the surface frequently suffered from biological matter. Use near surface values with caution.Fluorescence and Turbidity data still contain deck offsets. Use with cautionnc_uncertainty_p = 2.000000nc_uncertainty_t = 0.002000nc_uncertainty_s = 0.002000nc_uncertainty_o = 1.000000
DOI: 10.1594/pangaea.858789
title: Total (dissolved + particulate) U-238 and Th-234 specific activities in seawater during POLARSTERN cruise ARK-XXVII/3
DOI: 10.1594/pangaea.858795
title: Particulate Th-234, Pb-210, Po-210, organic carbon and organic nitrogen concentrations (particles &gt;53 µm) during POLARSTERN cruise ARK-XXVII/3
DOI: 10.1594/pangaea.858187
title: Methane concentration of sediment core M92_0017-1
DOI: 10.1594/pangaea.858863
title: Station list and links to master tracks in different resolutions of POLARSTERN cruise ARK-IX/4, Tromsø - Bremerhaven, 1993-08-06 - 1993-10-06
DOI: 10.1594/pangaea.858188
title: Methane concentration of sediment core M92_0036-1
DOI: 10.1594/pangaea.858189
title: Methane concentration of sediment core M92_0055-1
DOI: 10.1594/pangaea.858190
title: Methane concentration of sediment core M92_0086-1
DOI: 10.1594/pangaea.858191
title: Methane concentration of sediment core M92_0107-1
DOI: 10.1594/pangaea.858192
title: Methane concentration of sediment core M92_0155-1
DOI: 10.1594/pangaea.858202
title: Radiosonde profiles during METEOR cruise M91

description: radiosonde (type: RS92-SGP)
DOI: 10.1594/pangaea.858210
title: Weathering characteristics and lithology of samples from the Rauer Group, Antarctica, obtained in February/March 2007, and conducted with field support of POLARSTERN cruise ANT-XXIII/9

description: The presence of glacial sediments across the Rauer Group indicates that the East Antarctic ice sheet formerly covered the entire archipelago and has since retreated at least 15 km from its maximum extent. The degree of weathering of these glacial sediments suggests that ice retreat from this maximum position occurred sometime during the latter half of the last glacial cycle. Following this phase of retreat, the ice sheet margin has not expanded more than ~1 km seaward of its present position. This pattern of ice sheet change matches that recorded in Vestfold Hills, providing further evidence that the diminutive Marine Isotope Stage 2 ice sheet advance in the nearby Larsemann Hills may have been influenced by local factors rather than a regional ice-sheet response to climate and sea-level change.
description: Supplement to: White, Duanne A; Bennike, Ole; Berg, Sonja; Harley, S; Fink, David; Kiernan, Kevin W; McConnell, Anne; Wagner, Bernd (2009): Geomorphology and glacial history of Rauer Group, East Antarctica. Quaternary Research, 72(1), 80-90
DOI: 10.1594/pangaea.857949
title: Nutrients from underway water samples during METEOR cruise M90

description: WOCE Quality Flags
DOI: 10.1594/pangaea.858004
title: Swath sonar bathymetry during POLARSTERN cruise PS83 (ANT-XXIX/10) with links to multibeam raw data files

description: Contact mailto:infobathy@awi.de for data access.
DOI: 10.1594/pangaea.858865
title: Station list and links to master tracks in different resolutions of POLARSTERN cruise ARK-XI/1, Bremerhaven - Tromsø, 1995-07-07 - 1995-09-20
DOI: 10.1594/pangaea.858869
title: Station list and links to master tracks in different resolutions of POLARSTERN cruise ARK-XV/3, Tromsø - Bremerhaven, 1999-09-08 - 1999-10-14
DOI: 10.1594/pangaea.858870
title: Station list and links to master tracks in different resolutions of POLARSTERN cruise ANT-XVII/2, Cape Town - Cape Town, 2000-01-07 - 2000-03-15
DOI: 10.1594/pangaea.858241
title: Supplementary Table 1b. Nd and Sr isotope ratios in core GeoB3603-2
DOI: 10.1594/pangaea.858871
title: Station list and links to master tracks in different resolutions of POLARSTERN cruise ARK-XVI/1, Bremerhaven - Longyearbyen, 2000-06-30 - 2000-07-30
DOI: 10.1594/pangaea.858879
title: Continuous thermosalinograph oceanography along POLARSTERN cruise track PS85 (ARK-XXVIII/2)

description: Version 2, 2016-10-20
DOI: 10.1594/pangaea.858252
title: Methane concentration of sediment core M92_0254-1
DOI: 10.1594/pangaea.858253
title: Methane concentration of sediment core M92_0268-1
DOI: 10.1594/pangaea.858259
title: Fidelity bias in mollusk assemblages from coastal lagoons of Southern Brazil

description: The South America southern coast exhibits many outcrops with abundant shell beds, from the Pleistocene through the Recent. How much biological information is preserved within these shell beds? Or, what is the actual probability a living community has to leave a fossil record corresponding to these shell deposits? Although ecological and biogeographical aspects might had been pointed, considering these temporal scales, up to the moment there is no taphonomically-oriented studies available. Quantitative comparisons between living (LAs), death (DAs) and fossil assemblages (FAs) are important not only in strictly taphonomic studies, but have grown a leading tool for conservation paleobiology analysis. Comparing LAs, DAs and FAs from estuaries and lagoons in the Rio Grande do Sul Coastal Plain makes possible to quantitatively understand the nature and quantity of biological information preserved in fossil associations in Holocene lagoon facies. As already noted by several authors, spatial scale parts the analysis, but we detected that the FAs refl ects live ones, rather than dead ones, as previously not realized. The results herein obtained illustrates that species present in DA are not as good preserved in recent (Holocene) fossil record as originally thought. Strictly lagoon species are most prone to leave fossil record. The authors consider that the fi delity pattern here observed for estuarine mollusks to be driven by (i) high temporal and spatial variability in the LAs, (ii) spatial mixing in the DA and (iii) differential preservation of shells, due to long residence times in the taphonomically active zone.
description: Supplement to: Ritter, Matias do Nascimento; Erthal, Fernando (2013): Fidelity bias in mollusk assemblages from coastal lagoons of Southern Brazil. Revista Brasileira de Paleontologia, 16(2), 225-236
DOI: 10.1594/pangaea.858881
title: Continuous thermosalinograph oceanography along POLARSTERN cruise track PS87 (ARK-XXVIII/4)

description: Version 2, 2016-10-20
DOI: 10.1594/pangaea.858882
title: Continuous thermosalinograph oceanography along POLARSTERN cruise track PS88.1 (ANT-XXX/1.1)

description: Version 2, 2016-10-20
DOI: 10.1594/pangaea.858883
title: Continuous thermosalinograph oceanography along POLARSTERN cruise track PS88.2 (ANT-XXX/1.2)

description: Version 2, 2016-10-20
DOI: 10.1594/pangaea.858884
title: Continuous thermosalinograph oceanography along POLARSTERN cruise track PS89 (ANT-XXX/2)

description: Version 2, 2016-10-20
DOI: 10.1594/pangaea.858885
title: Continuous thermosalinograph oceanography along POLARSTERN cruise track PS90 (ANT-XXX/3)

description: Version 2, 2016-10-20
DOI: 10.1594/pangaea.858492
title: (Table 2) Integrated values of heterotrophic picoplankton and primary production (euphotic zone) in the Antarctic polar frontal region during POLARSTERN cruise ANT-XIII/2
DOI: 10.1594/pangaea.858493
title: (Table 2) Integrated values of heterotrophic picoplankton and primary production (euphotic zone) in the Antarctic polar frontal region during POLARSTERN cruise ANT-XVI/3
DOI: 10.1594/pangaea.859019
title: Station list and links to master tracks in different resolutions of POLARSTERN cruise PS95.1 (ANT-XXXI/1.1), Bremerhaven - Las Palmas, 2015-10-29 - 2015-11-08
DOI: 10.1594/pangaea.859020
title: Station list and links to master tracks in different resolutions of POLARSTERN cruise PS95.2 (ANT-XXXI/1.2), Las Palmas - Cape Town, 2015-11-09 - 2015-12-01
DOI: 10.1594/pangaea.859918
title: Raw data of continuous VM-ADCP (vessel-mounted Acoustic Doppler Current Profiler) profile during POLARSTERN cruise PS94 (ARK-XXIX/3)
DOI: 10.1594/pangaea.859021
title: Station list and links to master tracks in different resolutions of POLARSTERN cruise PS96 (ANT-XXXI/2 FROSN), Cape Town - Punta Arenas, 2015-12-06 - 2016-02-14
DOI: 10.1594/pangaea.859676
title: Continuous thermosalinograph oceanography along HEINCKE cruise track HE302/1
DOI: 10.1594/pangaea.859677
title: Continuous thermosalinograph oceanography along HEINCKE cruise track HE302/2
DOI: 10.1594/pangaea.859919
title: Raw data of continuous VM-ADCP (vessel-mounted Acoustic Doppler Current Profiler) profile during POLARSTERN cruise PS95 (ANT-XXXI/1)
DOI: 10.1594/pangaea.859920
title: Raw data of continuous VM-ADCP (vessel-mounted Acoustic Doppler Current Profiler) profile during POLARSTERN cruise PS96 (ANT-XXXI/2 FROSN)
DOI: 10.1594/pangaea.859559
title: Physical oceanography measured on water bottle samples during POLARSTERN cruise PS94 (ARK-XXIX/3)
DOI: 10.1594/pangaea.859560
title: Physical oceanography measured with ultra clean CTD/Water sampler-system during POLARSTERN cruise PS94 (ARK-XXIX/3)
DOI: 10.1594/pangaea.859561
title: Physical oceanography measured on water bottle samples with ultra clean CTD/Water sampler-system during POLARSTERN cruise PS94 (ARK-XXIX/3)
DOI: 10.1594/pangaea.861388
title: Physical oceanography during SONNE cruise SO243

description: nc_uncertainty_p = 2.000000nc_uncertainty_t = 0.002000nc_uncertainty_s = 0.002000nc_uncertainty_o = 1.500000The oxygen calibration for this cruise is non-standard as it makes use of the knowledge that O2 concentrations in the core of the OMZ are very close to 0. Winkler titrations can not measure such low concentrations. Tritrations lower than 4 mumol/l have thus been replaced by 0. The resulting calibrations delivers CTD O2 concentrations close to 0 in the core of the OMZ. Profile 26 is somewhat peculiar as it shows some pronounced density inversions. Please use with caution.Fluorescence data still contain deck offsets. Use with caution
DOI: 10.1594/pangaea.861415
title: Bulk sediment and diatom silica carbon isotope composition of sediment profile Co1010
DOI: 10.1594/pangaea.861416
title: Bulk sediment and diatom silica carbon isotope composition of sediment profile Co1011
DOI: 10.1594/pangaea.861417
title: Bulk sediment and diatom silica carbon isotope composition of sediment profile Co1014
DOI: 10.1594/pangaea.861441
title: Continuous meteorological surface measurement during POLARSTERN cruise PS96 (ANT-XXXI/2 FROSN)
DOI: 10.1594/pangaea.861443
title: Continuous meteorological surface measurement during POLARSTERN cruise PS98 (ANT-XXXI/4)
DOI: 10.1594/pangaea.861444
title: Radiosonde PS96/38583 during POLARSTERN cruise PS96 (ANT-XXXI/2) on 2015-12-07 10:59h

description: Precipitable water content 1.8775 cm
DOI: 10.1594/pangaea.861445
title: Radiosonde PS96/38584 during POLARSTERN cruise PS96 (ANT-XXXI/2) on 2015-12-08 11:03h

description: Height of tropopause 11719 m, precipitable water content 1.8456 cm
DOI: 10.1594/pangaea.861446
title: Radiosonde PS96/38585 during POLARSTERN cruise PS96 (ANT-XXXI/2) on 2015-12-09 10:51h

description: Height of tropopause 13255 m, precipitable water content 2.7552 cm
DOI: 10.1594/pangaea.861447
title: Radiosonde PS96/38586 during POLARSTERN cruise PS96 (ANT-XXXI/2) on 2015-12-10 11:11h

description: Height of tropopause 11916 m, precipitable water content 0.9248 cm
DOI: 10.1594/pangaea.861448
title: Radiosonde PS96/38587 during POLARSTERN cruise PS96 (ANT-XXXI/2) on 2015-12-11 10:56h

description: Height of tropopause 10808 m, precipitable water content 1.2892 cm
DOI: 10.1594/pangaea.861449
title: Radiosonde PS96/38588 during POLARSTERN cruise PS96 (ANT-XXXI/2) on 2015-12-12 10:54h

description: Height of tropopause 7105 m, precipitable water content 1.0228 cm
DOI: 10.1594/pangaea.861450
title: Radiosonde PS96/38589 during POLARSTERN cruise PS96 (ANT-XXXI/2) on 2015-12-13 10:57h

description: Height of tropopause 8863 m, precipitable water content 0.9737 cm
DOI: 10.1594/pangaea.861451
title: Radiosonde PS96/38590 during POLARSTERN cruise PS96 (ANT-XXXI/2) on 2015-12-14 07:00h

description: Height of tropopause 9579 m, precipitable water content 0.7392 cm
DOI: 10.1594/pangaea.861452
title: Radiosonde PS96/38591 during POLARSTERN cruise PS96 (ANT-XXXI/2) on 2015-12-14 11:00h

description: Height of tropopause 9900 m, precipitable water content 0.6372 cm
DOI: 10.1594/pangaea.861453
title: Radiosonde PS96/38592 during POLARSTERN cruise PS96 (ANT-XXXI/2) on 2015-12-14 16:57h

description: Height of tropopause 9859 m, precipitable water content 0.8387 cm
DOI: 10.1594/pangaea.861454
title: Radiosonde PS96/38593 during POLARSTERN cruise PS96 (ANT-XXXI/2) on 2015-12-15 06:56h

description: Height of tropopause 9905 m, precipitable water content 0.6278 cm
DOI: 10.1594/pangaea.861455
title: Radiosonde PS96/38594 during POLARSTERN cruise PS96 (ANT-XXXI/2) on 2015-12-15 10:56h

description: Height of tropopause 10009 m, precipitable water content 0.5973 cm
DOI: 10.1594/pangaea.861456
title: Radiosonde PS96/38595 during POLARSTERN cruise PS96 (ANT-XXXI/2) on 2015-12-15 17:15h

description: Height of tropopause 9509 m, precipitable water content 0.6224 cm
DOI: 10.1594/pangaea.861457
title: Radiosonde PS96/38596 during POLARSTERN cruise PS96 (ANT-XXXI/2) on 2015-12-16 06:59h

description: Height of tropopause 9909 m, precipitable water content 0.4960 cm
DOI: 10.1594/pangaea.861458
title: Radiosonde PS96/38597 during POLARSTERN cruise PS96 (ANT-XXXI/2) on 2015-12-16 11:01h

description: Height of tropopause 10099 m, precipitable water content 0.5040 cm
DOI: 10.1594/pangaea.861459
title: Radiosonde PS96/38598 during POLARSTERN cruise PS96 (ANT-XXXI/2) on 2015-12-16 17:08h

description: Height of tropopause 10275 m, precipitable water content 0.4922 cm
DOI: 10.1594/pangaea.861460
title: Radiosonde PS96/38599 during POLARSTERN cruise PS96 (ANT-XXXI/2) on 2015-12-17 06:51h

description: Height of tropopause 10841 m, precipitable water content 0.4392 cm
DOI: 10.1594/pangaea.861461
title: Radiosonde PS96/38600 during POLARSTERN cruise PS96 (ANT-XXXI/2) on 2015-12-18 06:51h

description: Height of tropopause 9691 m, precipitable water content 0.4309 cm