期刊
GEOPHYSICAL RESEARCH LETTERS
卷 48, 期 24, 页码 -出版社
AMER GEOPHYSICAL UNION
DOI: 10.1029/2021GL094966
关键词
microwave radar; firn stratigraphy
资金
- National Institute of Polar Research
- University of Alabama
- Norwegian Polar Institute
- University of Kansas
- MEXT
- JSPS [17H06320, 17H06104, 18H05294]
- European Union [730528]
- British Antarctic Survey
- International Polar Foundation
- Research Council of Norway's FRINATEK [315 246]
- Belgian Science Policy Office
- Grants-in-Aid for Scientific Research [17H06320, 17H06104, 18H05294] Funding Source: KAKEN
Limited SMB observations in the Antarctic inland hinder estimates of ice-sheet contribution to global sea level and million-year-old ice locations. A study on Dome Fuji over the past three centuries provides finely resolved SMB data, showing both large local variability and a negative correlation between SMB and surface slope at small scales.
The limited number of surface mass balance (SMB) observations in the Antarctic inland hampers estimates of ice-sheet contribution to global sea level and locations with million-year-old ice. We present finely resolved SMB over the past three centuries in a low-accumulation region with significant depth hoar formation on Dome Fuji derived from similar to 1,100 km of microwave radar stratigraphy dated with a firn core. The regional-mean SMB over the past 264 years is estimated to similar to 22.5 +/- 3.3 kg m(-2) a(-1), but with large local variability of up to 30%. We found that local SMB is negatively correlated with surface slope at scales of a few hundred meters, resulting in anomalous zones of low SMB which represent as much as 8-10% of the total SMB on the inland plateau if the SMB-slope relationship is more widely valid. This impact should be investigated further to improve estimates of Antarctic mass balance and sea-level contribution.
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