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|title=Melting of Ice Sheets | |title=Melting of Ice Sheets | ||
}} | }}<ref>[https://www.ipcc.ch/site/assets/uploads/2018/03/WG1AR5_SummaryVolume_FINAL_FRENCH.pdf#page=56 Page 41 of the Technical Summary of the 5th IPCC Report]</ref> | ||
== Explanation == | == Explanation == | ||
These illustrations represent the gain or loss of mass of the caps, indicated in centimetres of water per year (cm of water/year) and measured gravimetrically. In blue the mass gain (because it snows more) and in red the losses (glaciers flow faster towards the ocean). | |||
== Definition == | |||
An ice cap (or ice sheet or ice sheet) is a continental-scale mass of land ice, thick enough (between 1600 and 6400m<ref>[https://www.nationalgeographic.org/encyclopedia/ice-sheet/ National Geographic Resource Library]</ref>) to cover most of the underlying rock formations. There are currently only two major ice sheets, one in Greenland and one in Antarctica.<ref>[https://archive.ipcc.ch/pdf/assessment-report/ar5/wg1/WG1AR5_SummaryVolume_FINAL_FRENCH.pdf IPCC, 2013: Glossary (Planton, S. (coord.)). P.196. (French)]</ref> | |||
We will speak here of melting of the ice caps when the total mass of ice has decreased over the period under consideration, whatever the processes involved. | |||
== To go further == | |||
=== Numbers === | |||
Between 2006 and 2015, the loss of ice from the ice caps is : | |||
* 278 billion tonnes per year for Greenland | |||
* 155 billion tonnes per year for the Antarctic<ref>[https://www.ipcc.ch/site/assets/uploads/sites/3/2019/11/03_SROCC_SPM_FINAL.pdf#page=6 IPCC, Special report on cryosphere and oceans]</ref>. | |||
== References == | |||
<references /> |
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