Evolution of the dry-wet variations since 1834 CE in the Lüliang Mountains, north China and its relationship with the Asian summer monsoon-Reference-Cited by-同舟云学术

Evolution of the dry-wet variations since 1834 CE in the Lüliang Mountains, north China and its relationship with the Asian summer monsoon

Published:2021-02 Issue: Volume:121 Page:107089
ISSN:1470-160X
Container-title:Ecological Indicators
language:en
Short-container-title:Ecological Indicators

Author:

Cai Qiufang^ORCID,Liu Yu,Zhang Hanyu,Song Huiming,Li Qiang,Sun Changfeng^ORCID,Wang Lu,Fang Congxi,Liu Ruoshi

Funder

Chinese Academy of Sciences

National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Ecology,Ecology, Evolution, Behavior and Systematics,General Decision Sciences

Reference49 articles.

1. Academy of Meteorological Science. Yearly charts of dryness/wetness in China for the last 500-year period. Beijing: China Cartographic Publishing House, 1981, 1–332. (in Chinese).

2. Response of Pinus Tabulaeformis tree-ring growth to three moisture indices and January to July Walter index reconstruction in Helan Mountian;Cai;Marine Geol. Quaternary Geol.,2009

3. Climatic response of three tree species growing at different elevations in the Lüliang Mountains of Northern China;Cai;Dendrochronologia,2013

4. Climatic response of Chinese pine and PDSI variability in the middle Taihang Mountains, north China since 1873;Cai;Trees,2013

5. Tree-ring-based May-July mean temperature history for Lüliang Mountains, China, since 1836;Cai;Chin. Sci. Bull.,2010

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