ピナトゥボ山の噴火に対する葉の森の反応:光合成の強化
Lianhong Gu1, Dennis D Baldocchi, Steve C Wofsy
1Environmental Sciences Division, Building 1509, Oak Ridge National Laboratory, Oak Ridge, TN 37831-6335, USA. lianhong-gu@ornl.gov
まとめ
1991年のピナトゥボ山の噴火です.
科学分野:
- 大気科学と生態学.
- 火山学と気候への影響.
背景:
- 1991年のピナトゥボ山の噴火は,膨大な量の火山性エアロソルを平流層に注入した.
- これらのエアロゾールは,噴火後の数年間,世界的な放射線予算を大幅に変化させた.
研究 の 目的:
- 森林の光合成に対する拡散放射線の増加の影響を定量化するために.
- 地上の炭素吸収の調節における火山性エアロゾールの役割を評価する.
主な方法:
- 拡散放射線の増加に基づく推定値を使用した.
- 葉っぱの森の曇りのない環境で正午の光合成の効果を分析した.
主要な成果:
- 拡散放射線強化により,1992年には光合成が23%,1993年には8%増加した.
- これは,地球上の炭素吸収能力の大幅な増加を示唆しています.
結論:
- 火山性エアロゾールによって引き起こされる拡散放射線の増加は,地上の炭素吸収を高める可能性があります.
- この現象は,噴火後の大気中の二酸化炭素の増加率を一時的に減少させた.
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