陸地と大気とのフィードバックによって可能になる乾燥地の自己膨張
Akash Koppa1,2, Jessica Keune1,3, Dominik L Schumacher4
1Hydro-Climate Extremes Lab (H-CEL), Ghent University, Ghent, Belgium.
まとめ
地球温暖化によって 乾燥地は拡大しています 新しく形成された乾地は,風の下の空気を暖め,乾燥させ,乾燥を加速させ,水不足を助長します.
科学分野:
- 気候科学
- 環境科学
- エコロジー
背景:
- 乾燥地帯の拡大は水不足と生物多様性の減少につながります
- 地球温暖化による 干ばつの影響は知られていますが 干ばつの広がりにおける 干ばつの役割は 十分に研究されていません
研究 の 目的:
- 乾燥地帯の自己拡大メカニズムを調査する
- 干ばつの自己乾燥への寄与を定量化する.
主な方法:
- 乾燥地帯の空気の流れを追跡する
- 大気中の水分と熱伝達の動態を分析する.
主要な成果:
- 乾燥地の上空の温暖化と乾燥は 逆風による膨張に寄与します
- 乾燥した土地は水分を少なく 隣接する湿った地域にはより多くの熱を放出します
- このプロセスは降水量を減らし,大気中の水需要を増加させ,乾燥を引き起こします.
結論:
- 最近の乾燥地帯の約40%では,自己拡大が乾燥化の50%以上を占めています.
- その拡大を遅らせるために 乾燥地帯での緊急の気候変動緩和が必要なのです
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