国際地質物理年以来,南極の降雪の微妙な変化
Andrew J Monaghan1, David H Bromwich, Ryan L Fogt
1Polar Meteorology Group, Byrd Polar Research Center, Ohio State University, Columbus, OH 43210, USA.
まとめ
南極の降雪量は,1950年代以降,大きく変化していない. この変化の欠如は,南極の降雨が,大気温暖化にもかかわらず,予想に反して,現在,世界の海面上昇を緩和していないことを意味します.
科学分野:
- 気候科学 気候科学
- 氷河学 氷河学とは
- 海平面調査研究 海平面調査
背景:
- 南極の降雪の変動は,世界の海平面と氷床の質量バランスに影響を与えます.
- 長期の降雪傾向を理解することは,気候変動の予測にとって極めて重要です.
研究 の 目的:
- 南極大陸の50年間の積雪時間系列を導き出します.
- 南極の氷床の厚さに対する降雪の影響を評価するために.
- 南極の降雨パターンの拡大した視点を提供するため.
主な方法:
- 観測データと気候モデルのシミュレーションを組み合わせた.
- 歴史的な降雪データのために,主に氷のコアの記録を使用しました.
- 南極大陸の50年間の積雪データセットを開発しました.
主要な成果:
- 1950年代以降,南極の降雪に統計的に有意な変化は見られなかった.
- 最近の大気圏の冬の温暖化は,南極の降水量の増加につながっていない.
- 現在,南極の降雪は,世界の海面上昇を相殺していない.
結論:
- 現在,南極の降雪傾向は,世界の海面上昇を相殺していない.
- 長期の気候モデルと氷のコアのデータは,降雨の変動に関する洞察を提供します.
- 将来の南極の降雨動態を理解するためにさらなる研究が必要である.
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