Tree ring evidence of the retreat history of the Zepu glacier on the southeastern Tibetan Plateau since the Little Ice Age-Reference-Cited by-同舟云学术

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Tree ring evidence of the retreat history of the Zepu glacier on the southeastern Tibetan Plateau since the Little Ice Age

Published:2021-12 Issue: Volume:604 Page:60-67
ISSN:1040-6182
Container-title:Quaternary International
language:en
Short-container-title:Quaternary International

Author:

Yang Dan,Yang Fengmei^ORCID,Niu Zhenmin^ORCID,Shi Feng,Wang Naiang

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference43 articles.

1. ‘Little Ice Age’ summer temperature variations: their nature and relevance to recent global warming trends;Bradley;Holocene,1993

2. Tree-ring evidence of ‘little ice age’ glacier advances in southern Tibet;Bräuning;Holocene,2006

3. An evaluation of errors in tree age estimates based on increment cores in kahikatea (Dacrycarpus dacrydioides);Duncan;N. Z. Nat. Sci.,1989

4. Tree Rings and Climate;Fritts,1976

5. Mass balance of Xiao Dongkemadi glacier on the central Tibetan plateau from 1989 to 1995;Fujita;Ann. Glaciol.,2000

Cited by 2 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Glaciations and palaeoclimate of the last millennium in the Drongtso Lungpa Co Valley, southeastern Tibetan Plateau, based on cosmogenic 10Be exposure dating and glacier modelling;Journal of Asian Earth Sciences;2023-10

2. Quaternary glaciations in western China: A review of the chronologies established by absolute dating;Progress in Physical Geography: Earth and Environment;2023-02-25

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