Review article: Earth's ice imbalance
Autor: | Isobel R. Lawrence, Noel Gourmelen, Paul Tepes, Peter Nienow, Livia Jakob, Ines Otosaka, Andrew Shepherd, Thomas Slater, Lin Gilbert |
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Jazyk: | angličtina |
Rok vydání: | 2021 |
Předmět: |
lcsh:GE1-350
geography geography.geographical_feature_category 010504 meteorology & atmospheric sciences lcsh:QE1-996.5 Ice calving Antarctic ice sheet Greenland ice sheet Glacier 010502 geochemistry & geophysics 01 natural sciences Arctic ice pack Ice shelf lcsh:Geology Cryosphere Physical geography Ice sheet Geology lcsh:Environmental sciences 0105 earth and related environmental sciences Earth-Surface Processes Water Science and Technology |
Zdroj: | The Cryosphere, Vol 15, Pp 233-246 (2021) Slater, T, Lawrence, I R, Otosaka, I N, Shepherd, A, Gourmelen, N, Jakob, L, Tepes, P, Gilbert, L & Nienow, P 2021, ' Review Article: Earth’s ice imbalance ', Cryosphere . https://doi.org/10.5194/tc-15-233-2021 |
ISSN: | 1994-0424 1994-0416 |
DOI: | 10.5194/tc-15-233-2021 |
Popis: | We combine satellite observations and numerical models to show that Earth lost 28 trillion tonnes of ice between 1994 and 2017. Arctic sea ice (7.6 trillion tonnes), Antarctic ice shelves (6.5 trillion tonnes), mountain glaciers (6.1 trillion tonnes), the Greenland ice sheet (3.8 trillion tonnes), the Antarctic ice sheet (2.5 trillion tonnes), and Southern Ocean sea ice (0.9 trillion tonnes) have all decreased in mass. Just over half (58 %) of the ice loss was from the Northern Hemisphere, and the remainder (42 %) was from the Southern Hemisphere. The rate of ice loss has risen by 57 % since the 1990s – from 0.8 to 1.2 trillion tonnes per year – owing to increased losses from mountain glaciers, Antarctica, Greenland and from Antarctic ice shelves. During the same period, the loss of grounded ice from the Antarctic and Greenland ice sheets and mountain glaciers raised the global sea level by 34.6 ± 3.1 mm. The majority of all ice losses were driven by atmospheric melting (68 % from Arctic sea ice, mountain glaciers ice shelf calving and ice sheet surface mass balance), with the remaining losses (32 % from ice sheet discharge and ice shelf thinning) being driven by oceanic melting. Altogether, these elements of the cryosphere have taken up 3.2 % of the global energy imbalance. |
Databáze: | OpenAIRE |
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