En-en adult card 19 melting of ice sheets: Difference between revisions

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== Definition ==
== 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>
An ice cap (or ice sheet) is a continental-scale mass of land ice, thick enough (between 1,600 and 6 400 m thick<ref>[https://www.nationalgeographic.org/encyclopedia/ice-sheet/ National Geographic Resource Library]</ref>) that covers 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.
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.
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== References ==
== References ==
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[[fr:Fr-fr_adulte_carte_19_fonte_des_calottes_glaciaires]]
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