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気候学的に重要なエアロゾールの長波は,北極に間接的な影響を及ぼします
Dan Lubin1, Andrew M Vogelmann
1Scripps Institution of Oceanography, University of California San Diego, La Jolla, California 92093-0221, USA. dlubin@ucsd.edu
Nature
|January 27, 2006
まとめ
人為的なエアロゾールは,雲の性質を変えることで,北極を著しく暖める. これは これは これは これは これは
科学分野:
- 北極の気候科学 北極の気候科学
- 大気化学 大気化学
- 放射能の移転は,放射能の移転である.
背景:
- 北極の温暖化と海氷の減少は,温室効果ガスとフィードバックに関連しています.
- 雲は,北極の気候システムに,年間を通して,温暖化効果を発揮する.
- 低緯度からの人類によるエアロゾールは,定期的に北極に影響を及ぼします.
研究 の 目的:
- 北極の雲の性質に人類によるエアロゾールの影響を調査する.
- エアロゾールによって引き起こされる雲の変化の放射的効果を定量化する.
主な方法:
- マルチセンサ放射測定データを活用した.
- エアロゾールと雲の相互作用,特に"第一間接"効果を分析した.
主要な成果:
- エアロゾルの濃度が上昇すると,北極の雲の微物理的性質が変化する.
- この変化により,表面上の長波のフローが平均3.4W/m2増加する.
- 温暖化効果は,既知の温室効果ガスの効果と同等である.
結論:
- エアロゾールと雲の相互作用は,北極の気候学的に重要な温暖化メカニズムを表しています.
- エアロゾールの"最初の間接的"効果は,北極の気候動態において決定的な役割を果たしています.
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