Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, Gansu, 730000, China
Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, Gansu, 730000, China
Quanyan Tian
Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, Gansu, 730000, China
Aijun Ding
College of Resources and Environment, Gansu Agricultural University, Lanzhou, Gansu, 730070, China
Jiali Xie
Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, Gansu, 730000, China
Jingrong Su
Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, Gansu, 730000, China
University of Chinese Academy of Sciences, Beijing, 100049, China
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Total article views: 2,974 (including HTML, PDF, and XML)
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Total article views: 2,028 (including HTML, PDF, and XML)
Thereof 2,028 with geography defined
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Total article views: 946 (including HTML, PDF, and XML)
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Tree rings of Qinghai spruce are a good record of regional climate change. The influence of the East Asian summer monsoon (EASM) and westerlies on regional dry–wet climate changes is characterized by spatiotemporal heterogeneity. The most dramatic interplay between EASM and westerlies is observed in the Helan Mountains. Regional climate changes around the Changling Mountains are most influenced by EASM and around Dongda Mountain most influenced by westerlies.
Tree rings of Qinghai spruce are a good record of regional climate change. The influence of the...
