まとめ
セントヘレンス山の噴火は,その羽根により,表面温度を当初8°C冷却した. 後に発生した火山の塵は8°Cの温暖化を引き起こし,その結果,局所的な温暖化効果が生じた.
科学分野:
- 火山学 火山学とは
- 大気科学 大気科学
- 気候学 気候学
背景:
- 1980年のセントヘレンズ山噴火では,大量に火山物質が大気中に放出されました.
- 火山噴火の直接的な表面温度の影響を理解することは,大気と気候の研究に不可欠です.
研究 の 目的:
- 1980年5月18日のセントヘレンズ山噴火後の短期 (24時間) の地表温度効果を調査する.
- 火山の羽と塵によって引き起こされる温度抑制と上昇を定量化するために.
主な方法:
- 24時間間の温度差とモデル出力統計 (MOS) のエラーの分析.
- 選択されたステーションでの地表温度の詳細な時間的進化.
主要な成果:
- 日中の気温は火山の噴火により8°Cまで低下した.
- 夜の気温は,低レベルの火山塵により,最大8°C上昇した.
- これらの温度効果は,塵雲が散らばって東に向かって移動するにつれて急速に減少した.
結論:
- 噴火による局所的な表面温度の効果は温暖化であった.
- これは,気候スケールでの大規模な火山噴火の予想される長期の冷却効果と対照的です.
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