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Atmospheric River Precipitation Contributed to Rapid Increases in Surface Height of the West Antarctic Ice Sheet in 2019
Author(s) -
Adusumilli Susheel,
Fish Meredith,
Fricker Helen Amanda,
Medley Brooke
Publication year - 2021
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2020gl091076
Subject(s) - ice sheet , antarctic ice sheet , snow , precipitation , climatology , greenland ice sheet , environmental science , elevation (ballistics) , future sea level , altimeter , cryosphere , satellite , glacier mass balance , geology , atmospheric sciences , ice stream , sea ice , meteorology , oceanography , glacier , geography , remote sensing , geomorphology , geometry , mathematics , aerospace engineering , engineering
Estimating the relative contributions of the atmospheric and dynamic components of ice‐sheet mass balance is critical for improving projections of future sea level rise. Existing estimates of changes in Antarctic ice‐sheet height, which can be used to infer changes in mass, are only accurate at multiyear time scales. However, NASA's Ice, Cloud, and land Elevation Satellite‐2 (ICESat‐2) laser altimetry mission now allows us to accurately measure changes in ice‐sheet height at subannual time scales. Here, we use ICESat‐2 data to estimate height changes over Antarctica between April 2019 and June 2020. These data show widespread increases in surface height over West Antarctica during the 2019 austral winter. Using climate reanalysis data, we show that 41% of increases in height during winter were from snow accumulation via extreme precipitation events—63% of these events were associated with landfalling atmospheric rivers (ARs) which occurred only 5.1% of the time.