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Rückamp, Martin; Braun, Matthias Holger; Suckro, Sonja K; Blindow, Norbert (2011): Mass balance measurements on King George Island ice cap in 2007 and 2008 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.773308, Supplement to: Rückamp, M et al. (2011): Observed glacial changes on the King George Island ice cap, Antarctica, in the last decade. Global and Planetary Change, 79(1-2), 99-109, https://doi.org/10.1016/j.gloplacha.2011.06.009

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Abstract:
The Antarctic Peninsula has been identified as a region of rapid on-going climate change with impacts on the cryosphere. The knowledge of glacial changes and freshwater budgets resulting from intensified glacier melt is an important boundary condition for many biological and integrated earth system science approaches. We provide a case study on glacier and mass balance changes for the ice cap of King George Island. The area loss between 2000 and 2008 amounted to about 20 km**2 (about 1.6% of the island area) and compares to glacier retreat rates observed in previous years. Measured net accumulation rates for two years (2007 and 2008) show a strong interannual variability with maximum net accumulation rates of 4950 mm w.e./a and 3184 mm w.e./a, respectively. These net accumulation rates are at least 4 times higher than reported mean values (1926-95) from an ice core. An elevation dependent precipitation rate of 343 mm w.e./a (2007) and 432 mm w.e./a (2008) per 100 m elevation increase was observed. Despite these rather high net accumulation rates on the main ice cap, consistent surface lowering was observed at elevations below 270 m above ellipsoid over an 11-year period. These DGPS records reveal a linear dependence of surface lowering with altitude with a maximum annual surface lowering rate of 1.44 m/a at 40 m and -0.20 m/a at 270 m above ellipsoid. These results fit well to observations by other authors and surface lowering rates derived from the ICESat laser altimeter. Assuming that climate conditions of the past 11 years continue, the small ice cap of Bellingshausen Dome will disappear in about 285 years.
Funding:
German Research Foundation (DFG), grant/award no. 5472008: Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas
Coverage:
Median Latitude: -62.068374 * Median Longitude: -58.510997 * South-bound Latitude: -62.139620 * West-bound Longitude: -58.765030 * North-bound Latitude: -61.973930 * East-bound Longitude: -58.241760
Date/Time Start: 2007-01-01T00:00:00 * Date/Time End: 2008-01-01T00:00:00
Minimum ELEVATION: 390 m a.s.l. * Maximum ELEVATION: 691 m a.s.l.
Event(s):
King_George_Island * Latitude: -62.022000 * Longitude: -58.294000 * Location: King George Island, Antarctic Peninsula
Comment:
We provide mass balance measurements on the King George Island ice cap on several locations for two subsequent time periods. The measured net accumulation rates for two years (2007 and 2008) show a strong interannual variability with maximum net accumulation rates of 4950 mm w.e. a^-1 and 3184 mm w.e. a^-1, respectively. These net accumulation rates are at least 4 times higher than reported mean values (1926-95) from an ice core. An elevation dependent precipitation rate of 343 mm w.e. a^-1 (2007) and 432 mm w.e. a^-1 (2008) per 100 m elevation increase was observed.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DATE/TIMEDate/TimeGeocode
LATITUDELatitudeGeocode
LONGITUDELongitudeGeocode
UTM Northing, Universal Transverse MercatorUTM northmRückamp, Martin
UTM Easting, Universal Transverse MercatorUTM eastmRückamp, Martin
UTM Zone, Universal Transverse MercatorUTM ZoneRückamp, Martin
ELEVATIONElevationm a.s.l.Geocode
Mass balance in water equivalent per yearMBmm w.e./aRückamp, Martin
Size:
124 data points

Data

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Date/Time

Latitude

Longitude

UTM north [m]

UTM east [m]

UTM Zone

Elevation [m a.s.l.]

MB [mm w.e./a]
2007-62.13163-58.76503407960310990321E3903680
2007-62.10121-58.70281411115311337821E4174120
2007-62.09452-58.65799413435311418321E4883756
2007-62.13962-58.72745409943310906521E4893735
2007-62.11401-58.57761417684311211721E5523976
2007-62.10624-58.58332417365311297521E5684839
2007-62.06893-58.59818416487311711221E6124634
2007-62.13131-58.66848412993311007221E6223994
2007-62.12857-58.58744417211311048321E6314388
2007-62.11921-58.60038416510311150921E6395047
2007-61.97393-58.33533430003312800421E4283891
2007-61.99154-58.37435427999312600021E4343942
2007-62.00905-58.41344425994312400621E4543361
2007-62.00950-58.37516427999312399821E5154178
2007-61.99191-58.33619429999312600021E5204321
2007-61.97433-58.29734431995312800021E5383639
2007-61.99231-58.29793432004312599721E5614180
2007-62.01062-58.26062433998312399621E5934950
2007-62.00981-58.33705429995312400621E5944157
2007-62.01978-58.24176435005312299421E6274574
2007-62.04589-58.31934431004312000621E6524288
2007-62.01943-58.28002433002312299421E6584911
2007-62.04630-58.28109433005312000021E6914279
2008-62.13163-58.76503407960310990321E3903184
2008-62.10121-58.70281411115311337821E4171639
2008-62.09452-58.65799413435311418321E4881854
2008-62.13962-58.72745409943310906521E4891574
2008-62.10624-58.58332417365311297521E5682244
2008-62.06893-58.59818416487311711221E6122611
2008-62.12857-58.58744417211311048321E6312133
2008-62.11921-58.60038416510311150921E6392590