まとめ
1963年から1970年の火山噴火は,灰とガスを平流層に注入した. 赤道と北極圏の火山帯は主要な源であり,北極下の熱帯は潜在的に平流層の補給を強化する可能性がある.
科学分野:
- 火山学 火山学とは
- 大気科学 大気科学
- 地質物理学 地質物理学とは地質物理学です.
背景:
- 1956年以降,平流層の火山活動は1963年まで最小限であった.
- 1960年代の火山噴火は,平流層に大きな影響を与えた.
研究 の 目的:
- 1963年から1970年までの間,大平流層の灰とガスの主要な火山の源を特定する.
- ストラトスフィアの補充を担う潜在的緯度帯を調査する.
主な方法:
- 噴火記録と日付の分析.
- 火山活動の地理的マッピング.
- 大気動態の考慮,特に熱帯圏の高さ.
主要な成果:
- 2つの主要な火山帯が平流層の物質に貢献しました:赤道と亜北極です.
- 亜北極帯は,その低い熱帯地帯で,平流圏の塵とガスの主要な源泉であったかもしれない.
- 潜水艦とフレーティック噴火は,おそらく平流層の水蒸気を増加させた.
結論:
- 1960年代の火山活動により,質層圏に物質が注入されたことが実証されています.
- 火山の緯度分布と熱帯圏の高さは,平流圏の火山の衝撃における重要な要因である.
- 準層圏の水蒸気への潜水艦とフレーティック噴火の影響に関するさらなる研究は正当化されています.
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