Evaluating the timing and structure of the 4.2 ka event in the Indian summer monsoon domain from an annually resolved speleothem record from Northeast India
<p>A large array of proxy records suggests that the “4.2 ka event” marks an approximately 300-year long period (<span class="inline-formula">∼3.9</span> to 4.2 ka) of major climate change across the globe. However, the climatic manifestation of this...
Main Authors: | , , , , , , , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2018-11-01
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Series: | Climate of the Past |
Online Access: | https://www.clim-past.net/14/1869/2018/cp-14-1869-2018.pdf |