世界 水循環 の 永久 的 な 変化
1Department of Computational Hydrosystems, UFZHelmholtz Centre for Environmental Research, Leipzig, Germany.
まとめ
何十年にもわたる陸上水貯蔵データから 明らかに土壌の水分が 回復不能に減少していることがわかります この長期的傾向は,世界の水資源の重大な変化を強調しています.
科学分野:
- 地球科学
- 環境科学
- 水学
背景:
- 地上水貯蔵 (TWS) は地球の水循環の重要な構成要素です.
- TWSの長期的な傾向を理解することは,水資源管理と気候変動の影響評価に不可欠です.
研究 の 目的:
- 地上水の貯蔵の変化を分析する.
- 土壌の水分レベルにおける長期的な傾向を特定する.
主な方法:
- 衛星による重力測定データ (GRACE/GRACE-FOなど) を利用し,数十年を記録した.
- TWSデータに タイムシリーズの分析技術を適用した.
主要な成果:
- 数十年にわたって地球上の土壌の湿度が 統計的に有意で不可逆的に減少した.
- 土壌の水分減少の速度と大きさの地域的変動を特定した.
結論:
- 発見は陸上の生態系における 乾燥傾向が持続していることを示しています
- この不可逆的な土壌の水分減少は 農業,水資源,生態系の安定性に大きな影響を及ぼします
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