大気汚染量とオログラフィック降雨量との間には逆の関係がある
Daniel Rosenfeld1, Jin Dai, Xing Yu
1Institute of Earth Sciences, Hebrew University of Jerusalem, Jerusalem, Israel. daniel.rosenfeld@huji.ac.il
まとめ
大気汚染は,霧状の状況では,丘面の降水量を30-50%大幅に減少させます. この微粒子の影響は,特に中国では,風の下の丘陵地帯の水資源を脅かしています.
科学分野:
- 環境科学 環境科学
- 大気科学 大気科学
- 水文学 水文学とは
背景:
- 微粒子の大気汚染は,都市の中心部からの風の下にある丘陵地帯の降水率の低下と関連しています.
- 観測された傾向は,丘陵地帯と低地の降水比率の10-25%の減少を示しています.
研究 の 目的:
- 自由なトロポスフィアのエアロゾールとオログラフィの降水増強の関係を定量化するために.
- 丘陵地帯における水資源の利用可能性に対する大気汚染の影響を評価する.
主な方法:
- エアロゾールと降水量の測定は,マウントで行われました. 華,中国中部.
- 分析は,異なるエアロゾール濃度下でのオログラフィック降水増強因子に焦点を当てた.
主要な成果:
- 霧状の状況 (視界>8km) で,丘面の降水量は30~50%減少した.
- エアロゾール汚染は,オログラフィック降水増強因子を大幅に減少させます.
結論:
- 空気汚染は,丘陵地帯の水資源の減少に重要な役割を果たしています.
- この現象は,中国および世界における水管理に重大な課題をもたらしています.
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