中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Characterizing the Mass Elevation Effect across the Tibetan Plateau

文献类型:期刊论文

作者Han, Fang1; Zhang, Bai-ping2; Zhao, Fang3; Wan, Li4; Tan, Jing5; Liang, Tian1
刊名JOURNAL OF MOUNTAIN SCIENCE
出版日期2018-12-01
卷号15期号:12页码:2651-2665
关键词Mass Elevation Effect (MEE) Distribution Pattern Timberline Snowline Tibetan Plateau
ISSN号1672-6316
DOI10.1007/s11629-018-4978-2
通讯作者Zhang, Bai-ping(zhangbp@lreis.ac.cn)
英文摘要It is over 110 years since the term Mass Elevation Effect (MEE) was proposed by A. D. Quervain in 1904. The quantitative study of MEE has been explored in the Tibetan Plateau in recent years; however, the spatial distribution of MEE and its impact on the ecological pattern of the plateau are seldom known. In this study, we used a new method to estimate MEE in different regions of the plateau, and, then analyzed the distribution pattern of MEE, and the relationships among MEE, climate, and the altitudinal distribution of timberlines and snowlines in the Plateau. The main results are as follows: (1) The spatial distribution of MEE in the Tibetan Plateau roughly takes on an eccentric ellipse in northwestsoutheast trend. The Chang Tang Plateau and the middle part of the Kunlun Mountains are the core area of MEE, where occurs the highest MEE of above 11 degrees C; and MEE tends to decreases from this core area northwestward, northeastward and southward; (2) The distance away from the core zone of the plateau is also a very important factor for MEE magnitude, because MEE is obviously higher in the interior than in the exterior of the plateau even with similar mountain base elevation (MBE). (3) The impacts of MEE on the altitudinal distribution of timberlines and snowlines are similar, i.e., the higher the MEE, the higher timberlines and snowlines. The highest timberline (4600-4800 m) appears in the lakes and basins north of the Himalayas and in the upper and middle reach valleys of the Yarlung Zangbo River, where the estimated MEE is 10.2822 degrees C-10.6904 degrees C. The highest snowline (6000-6200 m) occurs in the southwest of the Chang Tang Plateau, where the estimated MEE is 11.2059 degrees C-11.5488 degrees C.
WOS关键词ALTITUDINAL DISTRIBUTION ; TIMBERLINE ; VEGETATION ; PATTERNS ; FOREST
资助项目Natural Science Foundation of China[41401111] ; Natural Science Foundation of China[41601091] ; National Key R&D Program of China[2017FY100900]
WOS研究方向Environmental Sciences & Ecology
语种英语
WOS记录号WOS:000453393800008
出版者SCIENCE PRESS
资助机构Natural Science Foundation of China ; National Key R&D Program of China
源URL[http://ir.igsnrr.ac.cn/handle/311030/51460]  
专题中国科学院地理科学与资源研究所
通讯作者Zhang, Bai-ping
作者单位1.Shandong Univ Technol, Sch Civil & Architectural Engn, Zibo 255000, Peoples R China
2.Chinese Acad Sci, State Key Lab Resources & Environm Informat Syst, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
3.Henan Univ, Coll Environm & Planning, Kaifeng 455000, Peoples R China
4.Chinese Res Inst Environm Sci, Beijing 100012, Peoples R China
5.Beijing Aerosp TITAN Technol Co Ltd, Beijing 100083, Peoples R China
推荐引用方式
GB/T 7714
Han, Fang,Zhang, Bai-ping,Zhao, Fang,et al. Characterizing the Mass Elevation Effect across the Tibetan Plateau[J]. JOURNAL OF MOUNTAIN SCIENCE,2018,15(12):2651-2665.
APA Han, Fang,Zhang, Bai-ping,Zhao, Fang,Wan, Li,Tan, Jing,&Liang, Tian.(2018).Characterizing the Mass Elevation Effect across the Tibetan Plateau.JOURNAL OF MOUNTAIN SCIENCE,15(12),2651-2665.
MLA Han, Fang,et al."Characterizing the Mass Elevation Effect across the Tibetan Plateau".JOURNAL OF MOUNTAIN SCIENCE 15.12(2018):2651-2665.

入库方式: OAI收割

来源:地理科学与资源研究所

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