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  • PANGAEA  (13)
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Keywords
Years
  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Timmermann, Ralph; Le Brocq, Anne M; Deen, Tara J; Domack, Eugene W; Dutrieux, Pierre; Galton-Fenzi, Ben; Hellmer, Hartmut H; Humbert, Angelika; Jansen, Daniela; Jenkins, Adrian; Lambrecht, Astrid; Makinson, Keith; Niederjasper, Fred; Nitsche, Frank-Oliver; Nøst, Ole Anders; Smedsrud, Lars Henrik; Smith, Walter (2010): A consistent dataset of Antarctic ice sheet topography, cavity geometry, and global bathymetry. Earth System Science Data, 2(2), 261-273, https://doi.org/10.5194/essd-2-261-2010
    Publication Date: 2023-03-16
    Description: Sub-ice shelf circulation and freezing/melting rates in ocean general circulation models depend critically on an accurate and consistent representation of cavity geometry. Existing global or pan-Antarctic data sets have turned out to contain various inconsistencies and inaccuracies. The goal of this work is to compile independent regional fields into a global data set. We use the S-2004 global 1-minute bathymetry as the backbone and add an improved version of the BEDMAP topography for an area that roughly coincides with the Antarctic continental shelf. Locations of the merging line have been carefully adjusted in order to get the best out of each data set. High-resolution gridded data for upper and lower ice surface topography and cavity geometry of the Amery, Fimbul, Filchner-Ronne, Larsen C and George VI Ice Shelves, and for Pine Island Glacier have been carefully merged into the ambient ice and ocean topographies. Multibeam survey data for bathymetry in the former Larsen B cavity and the southeastern Bellingshausen Sea have been obtained from the data centers of Alfred Wegener Institute (AWI), British Antarctic Survey (BAS) and Lamont-Doherty Earth Observatory (LDEO), gridded, and again carefully merged into the existing bathymetry map. The global 1-minute dataset (RTopo-1 Version 1.0.5) has been split into two NetCDF files. The first contains digital maps for global bedrock topography, ice bottom topography, and surface elevation. The second contains the auxiliary maps for data sources and the surface type mask. A regional subset that covers all variables for the region south of 50 deg S is also available in NetCDF format. Datasets for the locations of grounding and coast lines are provided in ASCII format.
    Keywords: AWI_OceDyn; Comment; File format; File size; ice2sea; Ocean Dynamics @ AWI; RTopo; RTopo-1; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
    Location Call Number Expected Availability
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  • 2
    Publication Date: 2023-03-17
    Keywords: ATOS2; ATOS2/20-1; ATOS2/22-1; ATOS2/23-1; ATOS2/24-1; ATOS2/26-1; ATOS2/28-1; ATOS2/29-1; ATOS2/30-1; ATOS2/31-1; ATOS2/33-1; ATOS2/85-1; ATOS2/87-1; ATOS2/89-1; ATOS2/90-1; ATOS2/91-1; ATOS2/92-1; Calculated; Chlorophyll fluorescence raw data; CTD, Sea-Bird, SBE 911; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; Hespérides; Latitude of event; Longitude of event; Oxygen; Pressure, water; Salinity; Scotia Sea, southwest Atlantic; Temperature, water; Temperature, water, potential; Transmission of light; Weddell Sea
    Type: Dataset
    Format: text/tab-separated-values, 58120 data points
    Location Call Number Expected Availability
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  • 3
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Schaffer, Janin; Timmermann, Ralph; Arndt, Jan Erik; Kristensen, Steen Savstrup; Mayer, Christoph; Morlighem, Mathieu; Steinhage, Daniel (2016): A global, high-resolution data set of ice sheet topography, cavity geometry, and ocean bathymetry. Earth System Science Data, 8(2), 543-557, https://doi.org/10.5194/essd-8-543-2016
    Publication Date: 2023-01-13
    Description: The ocean plays an important role in modulating the mass balance of the polar ice sheets by interacting with the ice shelves in Antarctica and with the marine-terminating outlet glaciers in Greenland. Given that the flux of warm water onto the continental shelf and into the sub-ice cavities is steered by complex bathymetry, a detailed topography data set is an essential ingredient for models that address ice–ocean interaction. We followed the spirit of the global RTopo-1 data set and compiled consistent maps of global ocean bathymetry, upper and lower ice surface topographies, and global surface height on a spherical grid with now 30 arcsec grid spacing. For this new data set, called RTopo-2, we used the General Bathymetric Chart of the Oceans (GEBCO, 2014) as the backbone and added the International Bathymetric Chart of the Arctic Ocean version 3 (IBCAOv3) and the International Bathymetric Chart of the Southern Ocean (IBCSO) version 1. While RTopo-1 primarily aimed at a good and consistent representation of the Antarctic ice sheet, ice shelves, and sub-ice cavities, RTopo-2 now also contains ice topographies of the Greenland ice sheet and outlet glaciers. In particular, we aimed at a good representation of the fjord and shelf bathymetry surrounding the Greenland continent. We modified data from earlier gridded products in the areas of Petermann Glacier, Hagen Bræ, and Sermilik Fjord, assuming that sub-ice and fjord bathymetries roughly follow plausible Last Glacial Maximum ice flow patterns. For the continental shelf off Northeast Greenland and the floating ice tongue of Nioghalvfjerdsfjorden Glacier at about 79° N, we incorporated a high-resolution digital bathymetry model considering original multibeam survey data for the region. Radar data for surface topographies of the floating ice tongues of Nioghalvfjerdsfjorden Glacier and Zachariæ Isstrøm have been obtained from the data centres of Technical University of Denmark (DTU), Operation Icebridge (NASA/NSF), and Alfred Wegener Institute (AWI). For the Antarctic ice sheet/ice shelves, RTopo-2 largely relies on the Bedmap-2 product but applies corrections for the geometry of Getz, Abbot, and Fimbul ice shelf cavities.
    Keywords: File format; File name; File size; RTopo; RTopo-2; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 76 data points
    Location Call Number Expected Availability
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  • 4
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Rackow, Thomas; Wesche, Christine; Timmermann, Ralph; Hellmer, Hartmut H; Juricke, Stephan; Jung, Thomas (2017): A simulation of small to giant Antarctic iceberg evolution: Differential impact on climatology estimates. Journal of Geophysical Research: Oceans, 21 pp, https://doi.org/10.1002/2016JC012513
    Publication Date: 2023-05-12
    Description: We present four melt climatology estimates based on a simulation of Antarctic iceberg drift and melting that includes small, medium-sized, and giant tabular icebergs with a realistic size distribution. For the first time, an iceberg model is initialized with a set of nearly 7000 observed iceberg positions and sizes around Antarctica. We simulate drift and lateral melt using iceberg-draft averaged ocean currents, temperature, and salinity. A new basal melting scheme, originally applied in ice shelf melting studies, uses in situ temperature, salinity, and relative velocities at an iceberg's bottom. The climatology estimates based on simulations of small (SMA), 'small-to-medium'-sized (MED12 & MED123), and small-to-giant icebergs (ALL) exhibit differential characteristics: successive inclusion of larger icebergs leads to a reduced seasonality of the iceberg meltwater flux and a shift of the mass input to the area north of 58°S, while less meltwater is released into the coastal areas. This highlights the necessity to account for larger and giant icebergs in order to obtain accurate melt climatologies. The four monthly melt climatologies [mm/day] are available as netCDF files with 1°x1° spatial resolution and can be used, e.g., for sensitivity studies with uncoupled sea ice-ocean models, or as spatio-temporal templates for the redistribution of land ice from the Antarctic ice sheet over the Southern Ocean in climate models.
    Keywords: File content; File format; File name; File size; pan-Antarctica; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 20 data points
    Location Call Number Expected Availability
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  • 5
    Publication Date: 2023-10-28
    Keywords: ANT-Land_2012; Atka Bay; Date/Time of event; Depth, bottom/max; DEPTH, ice/snow; Depth, top/min; Event label; Hardness description; Latitude of event; Location; Longitude of event; Magnifying glass and grid-card; NEUMAYER III; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; SNOW; Snow/ice sample; Snow grain size, maximum; Snow grain size, minimum; Snow type; SP01_ATKA03-1; SP01_ATKA03-2; SP01_ATKA03-3; SP01_ATKA03-4; SP01_ATKA03-5; SP01_ATKA03-6; SP01_ATKA11-1; SP01_ATKA21-1; SP01_ATKA21-2; SP01_ATKA21-3; SP01_ATKA21-4; SP01_ATKA21-5; SP01_SNOW01-1; SP01_SNOW03-1; SP01_SNOW04-1; SP02_ATKA07-1; SP02_ATKA07-2; SP02_ATKA11-1; SP02_ATKA11-2; SP02_ATKA16-1; SP02_ATKA21-1; SP02_ATKA24-1; SP02_SNOW03-1; SP02_SNOW03-2; SP03_ATKA07-1; SP03_ATKA11-1; SP03_ATKA21-1; SP03_ATKA24-1; SP03_SNOW01-1; SP03_SNOW02-1; SP04_ATKA16-1; SP04_ATKA21-1; SP05_ATKA16-1; SP05_ATKA21-1; SP06_ATKA21-1; SPP1158
    Type: Dataset
    Format: text/tab-separated-values, 828 data points
    Location Call Number Expected Availability
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  • 6
    Publication Date: 2023-10-28
    Keywords: ANT-Land_2012; Atka Bay; Date/Time of event; Density, snow; Depth, bottom/max; DEPTH, ice/snow; Depth, top/min; Event label; Latitude of event; Location; Longitude of event; NEUMAYER III; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; SNOW; Snow/ice sample; SP01_ATKA03-1; SP01_ATKA03-2; SP01_ATKA03-3; SP01_ATKA03-4; SP01_ATKA03-5; SP01_ATKA03-6; SP01_ATKA11-1; SP01_ATKA21-1; SP01_ATKA21-2; SP01_ATKA21-3; SP01_ATKA24-1; SP01_SNOW01-1; SP01_SNOW03-1; SP01_SNOW04-1; SP02_ATKA07-1; SP02_ATKA07-2; SP02_ATKA11-1; SP02_ATKA11-2; SP02_ATKA16-1; SP02_ATKA24-1; SP02_SNOW03-1; SP02_SNOW03-2; SP03_ATKA07-1; SP03_ATKA11-1; SP03_SNOW01-1; SP03_SNOW02-1; SP04_ATKA16-1; SP04_ATKA21-1; SP05_ATKA16-1; SP05_ATKA21-1; SP06_ATKA21-1; SP07_ATKA16-1; SPP1158; Volumetry with snow tube
    Type: Dataset
    Format: text/tab-separated-values, 240 data points
    Location Call Number Expected Availability
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  • 7
    Publication Date: 2023-10-28
    Keywords: ANT-Land_2012; Atka Bay; Date/Time of event; DEPTH, ice/snow; Digital thermometer, Testo, 110; Event label; Latitude of event; Location; Longitude of event; NEUMAYER III; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; SNOW; Snow/ice sample; SP01_ATKA03-1; SP01_ATKA03-2; SP01_ATKA03-3; SP01_ATKA03-4; SP01_ATKA03-5; SP01_ATKA03-6; SP01_ATKA11-1; SP01_ATKA21-1; SP01_ATKA21-2; SP01_ATKA21-3; SP01_ATKA21-4; SP01_ATKA21-5; SP01_ATKA24-1; SP01_SNOW01-1; SP01_SNOW03-1; SP01_SNOW04-1; SP02_ATKA07-1; SP02_ATKA07-2; SP02_ATKA11-1; SP02_ATKA11-2; SP02_ATKA11-3; SP02_ATKA16-1; SP02_ATKA21-1; SP02_ATKA24-1; SP02_SNOW02-1; SP02_SNOW03-1; SP02_SNOW03-2; SP03_ATKA07-1; SP03_ATKA11-1; SP03_ATKA11-2; SP03_ATKA21-1; SP03_ATKA24-1; SP03_SNOW01-1; SP03_SNOW02-1; SP04_ATKA16-1; SP04_ATKA21-1; SP05_ATKA16-1; SP05_ATKA21-1; SP05_ATKA24-1; SP06_ATKA21-1; SP07_ATKA16-1; SPP1158; Temperature, ice/snow
    Type: Dataset
    Format: text/tab-separated-values, 760 data points
    Location Call Number Expected Availability
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  • 8
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Hellmer, Hartmut H; Huhn, Oliver; Gomis, Damià; Timmermann, Ralph (2011): On the freshening of the northwestern Weddell Sea continental shelf. Ocean Science, 7(3), 305-316, https://doi.org/10.5194/os-7-305-2011
    Publication Date: 2023-10-28
    Description: We analyzed hydrographic data from the northwestern Weddell Sea continental shelf of the three austral winters 1989, 1997, and 2006 and two summers following the last winter cruise. During summer a thermal front exists at ~64° S separating cold southern waters from warm northern waters that have similar characteristics as the deep waters of the central basin of the Bransfield Strait. In winter, the whole continental shelf exhibits southern characteristics with high Neon (Ne) concentrations, indicating a significant input of glacial melt water. The comparison of the winter data from the shallow shelf off the tip of the Antarctic Peninsula, spanning a period of 17 yr, shows a salinity decrease of 0.09 for the whole water column, which has a residence time of 〈1 yr. We interpret this freshening as being caused by a combination of reduced salt input due to a southward sea ice retreat and higher precipitation during the late 20th century on the western Weddell Sea continental shelf. However, less salinification might also result from a delicate interplay between enhanced salt input due to sea ice formation in coastal areas formerly occupied by Larsen A and B ice shelves and increased Larsen C ice loss.
    Keywords: 06AQANTIX_2/100-1; 06AQANTIX_2/101-1; 06AQANTIX_2/102-1; 06AQANTIX_2/103-1; 06AQANTIX_2/104-1; 06AQANTIX_2/105-1; 06AQANTIX_2/106-1; 06AQANTIX_2/108-1; 06AQANTIX_2/108-2; 06AQANTIX_2/109-1; 06AQANTIX_2/113-1; 06AQANTIX_2/114-2; 06AQANTIX_2/115-1; 06AQANTIX_2/115-2; 06AQANTIX_2/35-1; 06AQANTIX_2/36-1; 06AQANTIX_2/39-1; 06AQANTIX_2/40-1; 06AQANTIX_2/41-1; 06AQANTIX_2/42-1; 06AQANTIX_2/43-1; 06AQANTIX_2/44-1; 06AQANTIX_2/45-1; 06AQANTIX_2/45-2; 06AQANTIX_2/46-1; 06AQANTIX_2/47-1; 06AQANTIX_2/48-1; 06AQANTIX_2/48-2; 06AQANTIX_2/49-1; 06AQANTIX_2/50-1; 06AQANTIX_2/51-1; 06AQANTIX_2/53-1; 06AQANTIX_2/55-1; 06AQANTIX_2/56-1; 06AQANTIX_2/56-2; 06AQANTIX_2/57-1; 06AQANTIX_2/58-1; 06AQANTIX_2/59-1; 06AQANTIX_2/60-1; 06AQANTIX_2/61-1; 06AQANTIX_2/62-1; 06AQANTIX_2/63-1; 06AQANTIX_2/63-2; 06AQANTIX_2/64-1; 06AQANTIX_2/65-1; 06AQANTIX_2/66-1; 06AQANTIX_2/67-1; 06AQANTIX_2/68-1; 06AQANTIX_2/69-1; 06AQANTIX_2/70-1; 06AQANTIX_2/71-1; 06AQANTIX_2/72-1; 06AQANTIX_2/73-1; 06AQANTIX_2/74-1; 06AQANTIX_2/75-1; 06AQANTIX_2/75-2; 06AQANTIX_2/76-1; 06AQANTIX_2/77-1; 06AQANTIX_2/78-1; 06AQANTIX_2/79-1; 06AQANTIX_2/80-1; 06AQANTIX_2/81-1; 06AQANTIX_2/82-1; 06AQANTIX_2/83-1; 06AQANTIX_2/84-1; 06AQANTIX_2/85-1; 06AQANTIX_2/86-1; 06AQANTIX_2/87-1; 06AQANTIX_2/88-1; 06AQANTIX_2/89-1; 06AQANTIX_2/90-1; 06AQANTIX_2/91-1; 06AQANTIX_2/92-1; 06AQANTIX_2/93-1; 06AQANTIX_2/94-1; 06AQANTIX_2/94-2; 06AQANTIX_2/95-1; 06AQANTIX_2/96-1; 06AQANTIX_2/97-1; 06AQANTIX_2/98-1; 06AQANTIX_2/99-1; 06AQANTVIII_2/119-1; 06AQANTVIII_2/124-1; 06AQANTVIII_2/129-1; 06AQANTVIII_2/134-1; 06AQANTVIII_2/137-1; 06AQANTVIII_2/138-1; 06AQANTVIII_2/139-1; 06AQANTVIII_2/141-1; 06AQANTVIII_2/142-1; 06AQANTVIII_2/144-1; 06AQANTVIII_2/145-1; 06AQANTVIII_2/146-1; 06AQANTVIII_2/147-1; 06AQANTVIII_2/148-1; 06AQANTVIII_2/149-1; 06AQANTVIII_2/150-1; 06AQANTVIII_2/151-1; 06AQANTVIII_2/152-1; 06AQANTVIII_2/153-1; 06AQANTVIII_2/154-1; 06AQANTVIII_2/155-1; 06AQANTVIII_2/156-1; 06AQANTVIII_2/157-1; 06AQANTVIII_2/158-2; 06AQANTVIII_2/159-1; 06AQANTVIII_2/160-1; 06AQANTVIII_2/161-1; 06AQANTVIII_2/162-1; 06AQANTVIII_2/163-1; 06AQANTVIII_2/164-1; 06AQANTVIII_2/165-1; 06AQANTVIII_2/166-1; 06AQANTVIII_2/167-1; 06AQANTVIII_2/168-1; 06AQANTVIII_2/169-1; 06AQANTVIII_2/170-1; 06AQANTVIII_2/171-1; 06AQANTVIII_2/172-1; 06AQANTVIII_2/173-1; 06AQANTVIII_2/174-1; 06AQANTVIII_2/175-1; 06AQANTVIII_2/176-1; 06AQANTVIII_2/177-1; 06AQANTVIII_2/178-1; 06AQANTVIII_2/179-1; 06AQANTVIII_2/180-1; 06AQANTVIII_2/181-1; 06AQANTVIII_2/182-1; 06AQANTVIII_2/183-1; 06AQANTVIII_2/184-1; 06AQANTVIII_2/185-1; 06AQANTVIII_2/186-1; 06AQANTVIII_2/187-1; 06AQANTVIII_2/188-1; 06AQANTVIII_2/189-1; 06AQANTVIII_2/192-1; 06AQANTVIII_2/193-1; 06AQANTVIII_2/194-1; 06AQANTVIII_2/195-1; 06AQANTVIII_2/197-1; 06AQANTVIII_2/198-1; 06AQANTVIII_2/199-1; 06AQANTVIII_2/200-1; 06AQANTVIII_2/201-1; 06AQANTVIII_2/202-1; 06AQANTVIII_2/203-1; 06AQANTVIII_2/204-1; 06AQANTVIII_2/205-1; 06AQANTVIII_2/206-1; 06AQANTVIII_2/207-1; 06AQANTVIII_2/208-1; 06AQANTVIII_2/209-1; 06AQANTVIII_2/210-1; 06AQANTVIII_2/211-1; 06AQANTVIII_2/212-1; 06AQANTVIII_2/213-1; 06AQANTVIII_2/214-1; 06AQANTVIII_2/215-1; 06AQANTVIII_2/216-1; 06AQANTVIII_2/217-1; 06AQANTVIII_2/218-1; 06AQANTVIII_2/219-1; 06AQANTVIII_2/220-1; 06AQANTVIII_2/221-1; 06AQANTVIII_2/222-1; 06AQANTVIII_2/223-1; 06AQANTXIII_4/100-1; 06AQANTXIII_4/10-1; 06AQANTXIII_4/101-1; 06AQANTXIII_4/102-2; 06AQANTXIII_4/103-1; 06AQANTXIII_4/11-1; 06AQANTXIII_4/12-1; 06AQANTXIII_4/13-1; 06AQANTXIII_4/13-3; 06AQANTXIII_4/14-3; 06AQANTXIII_4/15-2; 06AQANTXIII_4/15-4; 06AQANTXIII_4/16-1; 06AQANTXIII_4/17-1; 06AQANTXIII_4/18-1; 06AQANTXIII_4/19-1; 06AQANTXIII_4/19-3; 06AQANTXIII_4/20-1; 06AQANTXIII_4/2-1; 06AQANTXIII_4/21-1; 06AQANTXIII_4/2-2; 06AQANTXIII_4/22-1; 06AQANTXIII_4/22-3; 06AQANTXIII_4/23-1; 06AQANTXIII_4/24-1; 06AQANTXIII_4/25-1; 06AQANTXIII_4/25-3; 06AQANTXIII_4/26-1; 06AQANTXIII_4/27-1; 06AQANTXIII_4/28-1; 06AQANTXIII_4/28-3; 06AQANTXIII_4/29-1; 06AQANTXIII_4/30-1; 06AQANTXIII_4/3-1; 06AQANTXIII_4/31-1; 06AQANTXIII_4/31-4; 06AQANTXIII_4/32-1; 06AQANTXIII_4/33-1; 06AQANTXIII_4/34-1; 06AQANTXIII_4/34-3; 06AQANTXIII_4/34-4; 06AQANTXIII_4/35-1; 06AQANTXIII_4/35-4; 06AQANTXIII_4/36-1; 06AQANTXIII_4/37-1; 06AQANTXIII_4/38-1; 06AQANTXIII_4/38-4; 06AQANTXIII_4/39-1; 06AQANTXIII_4/40-1; 06AQANTXIII_4/4-1; 06AQANTXIII_4/41-1; 06AQANTXIII_4/42-1; 06AQANTXIII_4/43-1; 06AQANTXIII_4/44-1; 06AQANTXIII_4/44-3; 06AQANTXIII_4/45-1; 06AQANTXIII_4/46-1; 06AQANTXIII_4/47-1; 06AQANTXIII_4/48-1; 06AQANTXIII_4/48-3; 06AQANTXIII_4/49-1; 06AQANTXIII_4/50-1; 06AQANTXIII_4/5-1; 06AQANTXIII_4/51-1; 06AQANTXIII_4/52-1; 06AQANTXIII_4/52-3; 06AQANTXIII_4/5-3; 06AQANTXIII_4/53-1; 06AQANTXIII_4/54-1; 06AQANTXIII_4/54-3; 06AQANTXIII_4/55-1; 06AQANTXIII_4/56-2; 06AQANTXIII_4/56-4; 06AQANTXIII_4/57-1; 06AQANTXIII_4/57-4; 06AQANTXIII_4/58-1; 06AQANTXIII_4/59-1; 06AQANTXIII_4/60-1; 06AQANTXIII_4/60-4; 06AQANTXIII_4/6-1; 06AQANTXIII_4/61-1; 06AQANTXIII_4/62-1; 06AQANTXIII_4/62-3; 06AQANTXIII_4/63-1; 06AQANTXIII_4/65-2; 06AQANTXIII_4/66-1; 06AQANTXIII_4/66-3; 06AQANTXIII_4/67-1; 06AQANTXIII_4/68-1; 06AQANTXIII_4/69-1; 06AQANTXIII_4/70-1; 06AQANTXIII_4/7-1; 06AQANTXIII_4/71-1; 06AQANTXIII_4/71-5; 06AQANTXIII_4/7-2; 06AQANTXIII_4/72-1; 06AQANTXIII_4/73-1; 06AQANTXIII_4/74-2; 06AQANTXIII_4/75-1; 06AQANTXIII_4/75-4; 06AQANTXIII_4/76-1; 06AQANTXIII_4/77-1; 06AQANTXIII_4/78-1; 06AQANTXIII_4/79-1; 06AQANTXIII_4/79-3; 06AQANTXIII_4/80-1; 06AQANTXIII_4/8-1; 06AQANTXIII_4/81-1; 06AQANTXIII_4/82-1; 06AQANTXIII_4/83-1; 06AQANTXIII_4/83-2; 06AQANTXIII_4/84-1; 06AQANTXIII_4/85-1; 06AQANTXIII_4/86-1; 06AQANTXIII_4/86-3; 06AQANTXIII_4/87-1; 06AQANTXIII_4/88-1; 06AQANTXIII_4/89-1; 06AQANTXIII_4/90-1; 06AQANTXIII_4/90-4; 06AQANTXIII_4/9-1; 06AQANTXIII_4/91-1; 06AQANTXIII_4/92-1; 06AQANTXIII_4/93-1; 06AQANTXIII_4/94-1; 06AQANTXIII_4/94-3; 06AQANTXIII_4/95-1; 06AQANTXIII_4/96-1; 06AQANTXIII_4/97-1; 06AQANTXIII_4/98-1; 06AQANTXIII_4/99-1; 06AQANTXIII_4/99-4; 06AQANTXV_4/100-1; 06AQANTXV_4/10-1; 06AQANTXV_4/101-1; 06AQANTXV_4/102-1; 06AQANTXV_4/103-1; 06AQANTXV_4/104-1; 06AQANTXV_4/105-1; 06AQANTXV_4/106-1; 06AQANTXV_4/107-2; 06AQANTXV_4/107-4; 06AQANTXV_4/108-1; 06AQANTXV_4/109-1; 06AQANTXV_4/1-1; 06AQANTXV_4/110-1; 06AQANTXV_4/111-1; 06AQANTXV_4/11-2; 06AQANTXV_4/112-1; 06AQANTXV_4/11-3; 06AQANTXV_4/113-1; 06AQANTXV_4/11-4; 06AQANTXV_4/114-2; 06AQANTXV_4/114-4; 06AQANTXV_4/11-5; 06AQANTXV_4/115-1; 06AQANTXV_4/11-6; 06AQANTXV_4/116-1; 06AQANTXV_4/117-1; 06AQANTXV_4/118-1; 06AQANTXV_4/119-1; 06AQANTXV_4/120-1; 06AQANTXV_4/12-1; 06AQANTXV_4/121-1; 06AQANTXV_4/122-1; 06AQANTXV_4/122-2; 06AQANTXV_4/123-1; 06AQANTXV_4/124-1; 06AQANTXV_4/125-1; 06AQANTXV_4/126-1; 06AQANTXV_4/127-1; 06AQANTXV_4/128-1; 06AQANTXV_4/129-1; 06AQANTXV_4/130-1; 06AQANTXV_4/13-1; 06AQANTXV_4/131-1; 06AQANTXV_4/132-1; 06AQANTXV_4/133-1; 06AQANTXV_4/134-1; 06AQANTXV_4/135-1; 06AQANTXV_4/136-1; 06AQANTXV_4/14-1; 06AQANTXV_4/15-1; 06AQANTXV_4/15-2; 06AQANTXV_4/16-1; 06AQANTXV_4/17-1; 06AQANTXV_4/18-1; 06AQANTXV_4/19-1; 06AQANTXV_4/20-1; 06AQANTXV_4/20-2; 06AQANTXV_4/2-1; 06AQANTXV_4/21-1; 06AQANTXV_4/22-1; 06AQANTXV_4/23-1; 06AQANTXV_4/24-1; 06AQANTXV_4/25-1; 06AQANTXV_4/26-1; 06AQANTXV_4/27-1; 06AQANTXV_4/28-1; 06AQANTXV_4/29-1; 06AQANTXV_4/30-1; 06AQANTXV_4/30-2; 06AQANTXV_4/31-1; 06AQANTXV_4/3-2; 06AQANTXV_4/32-1; 06AQANTXV_4/33-1; 06AQANTXV_4/34-1; 06AQANTXV_4/35-1; 06AQANTXV_4/36-1; 06AQANTXV_4/37-1; 06AQANTXV_4/38-1; 06AQANTXV_4/39-1; 06AQANTXV_4/40-1; 06AQANTXV_4/41-1; 06AQANTXV_4/42-1; 06AQANTXV_4/4-3; 06AQANTXV_4/43-1; 06AQANTXV_4/44-1; 06AQANTXV_4/45-1; 06AQANTXV_4/46-1; 06AQANTXV_4/47-1; 06AQANTXV_4/47-2; 06AQANTXV_4/48-1; 06AQANTXV_4/49-1; 06AQANTXV_4/50-1; 06AQANTXV_4/5-1; 06AQANTXV_4/51-1; 06AQANTXV_4/52-1; 06AQANTXV_4/53-1; 06AQANTXV_4/54-1; 06AQANTXV_4/55-1; 06AQANTXV_4/56-1; 06AQANTXV_4/57-1; 06AQANTXV_4/58-1; 06AQANTXV_4/59-1; 06AQANTXV_4/60-1; 06AQANTXV_4/6-1; 06AQANTXV_4/61-1; 06AQANTXV_4/62-1; 06AQANTXV_4/63-1; 06AQANTXV_4/65-1; 06AQANTXV_4/66-1; 06AQANTXV_4/67-1; 06AQANTXV_4/68-1; 06AQANTXV_4/68-2; 06AQANTXV_4/69-1;
    Type: Dataset
    Format: application/zip, 8 datasets
    Location Call Number Expected Availability
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  • 9
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Paul, Stephan; Willmes, Sascha; Hoppmann, Mario; Hunkeler, Priska A; Wesche, Christine; Nicolaus, Marcel; Heinemann, Günther; Timmermann, Ralph (2015): The impact of early-summer snow properties on Antarctic landfast sea-ice X-band backscatter. Annals of Glaciology, 56(69), 263-273, https://doi.org/10.3189/2015AoG69A715
    Publication Date: 2023-10-28
    Description: Up to now, snow cover on Antarctic sea ice and its impact on radar backscatter, particularly after the onset of freeze/thaw processes, are not well understood. Here we present a combined analysis of in situ observations of snow properties from the landfast sea ice in Atka Bay, Antarctica, and high-resolution TerraSAR-X backscatter data, for the transition from austral spring (November 2012) to summer (January 2013). The physical changes in the seasonal snow cover during that time are reflected in the evolution of TerraSAR-X backscatter. We are able to explain 76-93% of the spatio-temporal variability of the TerraSAR-X backscatter signal with up to four snowpack parameters with a root-mean-squared error of 0.87-1.62 dB, using a simple multiple linear model. Over the complete study, and especially after the onset of early-melt processes and freeze/thaw cycles, the majority of variability in the backscatter is influenced by changes in snow/ice interface temperature, snow depth and top-layer grain size. This suggests it may be possible to retrieve snow physical properties over Antarctic sea ice from X-band SAR backscatter.
    Keywords: Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; SPP1158
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
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  • 10
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Schaffer, Janin; Kanzow, Torsten; von Appen, Wilken-Jon; von Albedyll, Luisa; Arndt, Jan Erik; Roberts, David H (2020): Bathymetry constrains ocean heat supply to Greenland's largest glacier tongue. Nature Geoscience, 13(3), 227-231, https://doi.org/10.1038/s41561-019-0529-x
    Publication Date: 2023-11-24
    Description: As an update to the RTopo-2.0.1 data set (https://doi.org/10.1594/PANGAEA.856844), RTopo-2.0.4 contains new original bathymetry data for the Northeast Greenland continental shelf. In the Southern Ocean, we added the Rosier et al. (JGR Oceans, 2018) bathymetry grid below Filchner Ice Shelf. This work was supported in part through the Deutsche Forschungsgemeinschaft (DFG) within the Special Priority Program (SPP) 1889 "Regional Sea Level Change and Society" (grant OGreen79), the German Federal Ministry for Education and Research (BMBF) within the GROCE project (Grant 03F0778A), the Natural Environment Research Council (NERC) large grant "Ice shelves in a warming world: Filchner Ice Shelf System" (NE/L013770/1), the NERC project "Greenland in a warmer climate: What controls the advance & retreat of the NE Greenland Ice Stream" (Grant NE/N011228/1), and the Helmholtz Climate Initiative "Regional Climate Change" (REKLIM).
    Keywords: AWI_PhyOce; File format; File name; File size; Greenland - Ice Sheet/Ocean Interaction: From process understanding to an analysis of the regional system; Greenland in a warmer climate: What controls the advance & retreat of the NE Greenland Ice Stream; GROCE; Helmholtz-Verbund Regionale Klimaänderungen = Helmholtz Climate Initiative (Regional Climate Change); Ice shelves in a warming world: Filchner Ice Shelf System; NERC_FISS; NERC_Greenland; Physical Oceanography @ AWI; Priority Programme 1889 Regional Sea Level Change and Society; REKLIM; RTopo; RTopo-2; SPP1889; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 56 data points
    Location Call Number Expected Availability
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