Transformation and mechanisms of climate wet/dry change on the northern Tibetan Plateau under global warming

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Historical patterns of climate change can provide ways to predict future climate change. During geological history, the earth has experienced many warm periods of different time scales, such as the mid-Holocene warm period, the medieval climate anomaly, etc.

Transformation and mechanisms of climate wet/dry change on the northern Tibetan Plateau under global warming: A perspective from paleoclimatology,

: Transformation and mechanisms of climate wet/dry change on the northern Tibetan Plateau under global warming retrieved 16 May 2024 from https://phys.org/news/2024-05-mechanisms-climate-wetdry-northern-tibetan.html This document is subject to copyright. Apart from any fair dealing for the purpose of private study or research, no part may be reproduced without the written permission. The content is provided for information purposes only.Jul 17, 2023Use this form if you have come across a typo, inaccuracy or would like to send an edit request for the content on this page. For general inquiries, please use ourThank you for taking time to provide your feedback to the editors.

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