大気中のCO2は,植物の急激な変化を局所的に引き起こすが,地球規模では起こらない
Steven I Higgins1, Simon Scheiter
1Institut für Physische Geographie, Goethe Universität Frankfurt am Main, 60438 Frankfurt am Main, Germany. higgins@em.uni-frankfurt.de
Nature
|July 6, 2012
まとめ
人為的な気候変動は,地球システムを新しい状態に押し込む可能性があります. 熱帯の生態系は,二酸化炭素のレベルが上昇しているため,より高いバイオマスまたは木質状態に移行する可能性が高い.
科学分野:
- 地球システム科学 地球システム科学
- 気候変動 生物学
- エコロジー エコロジー エコロジー
背景:
- 地球系科学者は,国家を急激にシフトさせることができる大規模な構成要素であるティッピング要素について懸念しています.
- 大規模な植生系が転覆行動を示す可能性は十分に理解されていません.
- 熱帯の草原,サバンナ,森林の生態系は,地球システムの重要な構成要素です.
研究 の 目的:
- 熱帯植生系が代替状態に転移する可能性があるかどうかを調査する.
- 大気中の二酸化炭素の増加が植生状態に与える影響を判断する.
- 植生体制の変化のタイミングと場所に影響を与える要因を分析する.
主な方法:
- 気候変動シナリオに対する植物の反応のモデリング.
- 熱帯の草原,サバンナ,森林の生態系における転換点の分析.
- CO2濃度,気温上昇,火災の重症度,降雨の変動による影響の評価.
主要な成果:
- 熱帯の草原,サバンナ,森林の生態系は,代替状態に移行する可能性が高い.
- 大気中のCO2濃度の上昇は,より高いバイオマスおよび/または木質植物の優位性のある状態への移行を促すでしょう.
- これらのシフトのタイミングは,気温上昇率,火災の深刻さ,降雨量,そしてビスタブルな植生地帯の移動に依存します.
結論:
- 陸上の生態系における大規模な方向的体制のシフトは,気候変動による可能性が高い.
- 異なる地域における非同期的なシフトは,地球システムに対する全体的な影響を軽減するかもしれないが,排除することは出来ない.
- これらの植生の臨界点を理解することは,将来の地球システム状態を予測するために極めて重要です.
関連する概念動画
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