Arid
DOI10.1080/19475705.2018.1531942
Temporal-spatial variations and influencing factors of Lakes in inland arid areas from 2000 to 2017: a case study in Xinjiang
Yang Jin-Ming1; Ma Li-Gang1; Li Cheng-Zhi2; Liu Yang3; Ding Jian-Li4; Yang Sheng-Tian1
通讯作者Yang Jin-Ming
来源期刊GEOMATICS NATURAL HAZARDS & RISK
ISSN1947-5705
EISSN1947-5713
出版年2019
卷号10期号:1页码:519-543
英文摘要Lakes are the most important water resource in arid and semi-arid regions and are good indicators of climate change. The study of lake expansion and contraction can reveal important information about climate change and regional responses. In this study, MOD09A1 global surface reflectance data of MODIS are used to extract the water areas of 12 main lakes in Xinjiang using a support vector machine method to investigate the temporal-spatial dynamics and driving factors of lake area variations between 2000 and 2017. The results indicate that (1) In general, the Xinjiang lakes exhibited large fluctuations between 2000 and 2017; the area of the lakes shrunk by 16.98 km(2)/year during 2007-2009 but expanded by 80.67 km(2)/year after 2010. (2) The changes in the Xinjiang lakes exhibited obvious spatial differences. There were strong fluctuations in the areas of the Tail-end lakes and the K value describing the degree of fluctuation in the lake area was 0.2%. The fluctuations in the areas of the Mountain lakes were more stable with a K value of 0.09% and the area of the Plateau lakes increased every year, with an annual increase of 19.90 km(2). (3) The lakes with the larger fluctuations in the area were Ebinur Lake, Manasi Lake, and Barkol Lake, and the range of the areas was 370.85, 276.55, and 61.5 km(2), respectively. Because of the regional diversity of Xinjiang, the driving forces that affect the area of the lakes differ in different areas. The main factors affecting the lake area change in the Tail-end lakes are the amount of inflowing water and the water use by agriculture and animal husbandry. The main reason for the stability of the Mountain lakes is the balance between water inflow and outflow. The main factor contributing to the expansion of the Plateau lakes area is the abundant supply of glacier/snow melt water. Overall, the main factor contributing to the expansion of Plateau lakes area is abundant glacier snow melt water supply. On the whole, the main factors affecting the temporal and spatial variation of the lake areas in Xinjiang are precipitation (r = .67, p = .003 < .01), temperature (r = .611, p = .007 < .01), and the increase in cultivated land area (r = -.021, p = .004 < .01).
英文关键词Arid area support vector machine lake area driving forces remote sensing MODIS
类型Article
语种英语
国家Peoples R China
开放获取类型gold
收录类别SCI-E
WOS记录号WOS:000455441800001
WOS关键词SUPPORT VECTOR MACHINES ; TIME-SERIES ; WATER ; INFORMATION ; MANAGEMENT ; CHINA
WOS类目Geosciences, Multidisciplinary ; Meteorology & Atmospheric Sciences ; Water Resources
WOS研究方向Geology ; Meteorology & Atmospheric Sciences ; Water Resources
来源机构中国科学院新疆生态与地理研究所 ; 新疆大学
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/215987
作者单位1.Xinjiang Univ, Coll Resources & Environm Sci, Urumqi, Peoples R China;
2.Xinjiang Univ, Inst Arid Ecol & Environm, Urumqi, Peoples R China;
3.Chinese Acad Sci, Xinjiang Inst Ecol & Geog, State Key Lab Desert & Oasis Ecol, Urumqi, Peoples R China;
4.Xinjiang Univ, Inst Geol & Min Engn, Urumqi, Peoples R China
推荐引用方式
GB/T 7714
Yang Jin-Ming,Ma Li-Gang,Li Cheng-Zhi,et al. Temporal-spatial variations and influencing factors of Lakes in inland arid areas from 2000 to 2017: a case study in Xinjiang[J]. 中国科学院新疆生态与地理研究所, 新疆大学,2019,10(1):519-543.
APA Yang Jin-Ming,Ma Li-Gang,Li Cheng-Zhi,Liu Yang,Ding Jian-Li,&Yang Sheng-Tian.(2019).Temporal-spatial variations and influencing factors of Lakes in inland arid areas from 2000 to 2017: a case study in Xinjiang.GEOMATICS NATURAL HAZARDS & RISK,10(1),519-543.
MLA Yang Jin-Ming,et al."Temporal-spatial variations and influencing factors of Lakes in inland arid areas from 2000 to 2017: a case study in Xinjiang".GEOMATICS NATURAL HAZARDS & RISK 10.1(2019):519-543.
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