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南極の氷の動態は,北半球の海面圧迫によって増幅される

Natalya Gomez1, Michael E Weber2, Peter U Clark3,4

  • 1Department of Earth and Planetary Sciences, McGill University, Montreal, Quebec, Canada. natalya.gomez@mcgill.ca.

Nature
|November 26, 2020
PubMed
まとめ

北半球の海面の変化は南極の氷床 (AIS) の動態を強めた. この半球間相互作用は,氷河期中にAISの量を増やし,脱氷期中に撤退と質量損失を増加させた.

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