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Tipping point (climatology) : ウィキペディア英語版 | Tipping point (climatology)
A climate tipping point is a somewhat ill-defined concept of a point when global climate changes from one stable state to another stable state, in a similar manner to a wine glass tipping over. After the tipping point has been passed, a transition to a new state occurs. The tipping event ''may be'' irreversible, comparable to wine spilling from the glass: standing up the glass will not put the wine back. ==Definition== The ''IPCC AR5'' report stated with medium confidence that precise levels of climate change sufficient to trigger a tipping point, defined as a threshold for abrupt and irreversible change, remain uncertain, and that the risk associated with crossing multiple tipping points increases with rising temperature.〔(【引用サイトリンク】title=Climate change 2014, Impacts, Adaptation and Vulnerability )〕
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Tipping point (climatology)」の詳細全文を読む
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