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干旱区科学  2015, Vol. 7 Issue (2): 146-158    DOI: 10.1007/s40333-014-0081-x
  学术论文 本期目录 | 过刊浏览 | 高级检索 |
Characterizing regional precipitation-driven lake area change in Mongolia
Sinkyu KANG1, Gyoungbin LEE1, Chuluun TOGTOKH2, Keunchang JANG1
1 Department of Environmental Science, Kangwon National University, Chuncheon 200-701, South Korea;
2 Institute for Sustainable Development, National University of Mongolia, Ulaanbaatar 14201, Mongolia
Characterizing regional precipitation-driven lake area change in Mongolia
Sinkyu KANG1, Gyoungbin LEE1, Chuluun TOGTOKH2, Keunchang JANG1
1 Department of Environmental Science, Kangwon National University, Chuncheon 200-701, South Korea;
2 Institute for Sustainable Development, National University of Mongolia, Ulaanbaatar 14201, Mongolia
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摘要 Lake area is an important indicator for climate change and its relationship with climatic factors is critical for understanding the mechanisms that control lake level changes. In this study, lake area changes and their relations to precipitation were investigated using multi-temporal Landsat Thermatic Mapper (TM) and Enhanced Thermatic Mapper plus (ETM+) images collected from 10 different regions of Mongolia since the late 1980s. A linear-regression analysis was applied to examine the relationship between precipitation and lake area change for each region and across different regions of Mongolia. The relationships were interpreted in terms of re-gional climate regime and hydromorphological characteristics. A total of 165 lakes with areas greater than 10 hm2 were identified from the Landsat images, which were aggregated for each region to estimate the regional lake area. Temporal lake area variability was larger in the Gobi regions, where small lakes are densely dis-tributed. The regression analyses indicated that the regional patterns of precipitation-driven lake area changes varied considerably (R2=0.028–0.950), depending on regional climate regime and hydromorphological char-acteristics. Generally, the lake area change in the hot-and-dry Gobi regions showed higher correlations with precipitation change. The precedent two-month precipitation was the best determining factor of lake area change across Mongolia. Our results indicate the usefulness of regression analysis based on satellite-derived multi-temporal lake area data to identify regions where factors other than precipitation might play important roles in determining lake area change.
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Sinkyu KANG
Gyoungbin LEE
Chuluun TOGTOKH
Keunchang JANG
关键词:  Dunhuang city  Crescent Moon Spring  pyramid dunes  dynamic characteristics  erosion and deposition    
Abstract: Lake area is an important indicator for climate change and its relationship with climatic factors is critical for understanding the mechanisms that control lake level changes. In this study, lake area changes and their relations to precipitation were investigated using multi-temporal Landsat Thermatic Mapper (TM) and Enhanced Thermatic Mapper plus (ETM+) images collected from 10 different regions of Mongolia since the late 1980s. A linear-regression analysis was applied to examine the relationship between precipitation and lake area change for each region and across different regions of Mongolia. The relationships were interpreted in terms of re-gional climate regime and hydromorphological characteristics. A total of 165 lakes with areas greater than 10 hm2 were identified from the Landsat images, which were aggregated for each region to estimate the regional lake area. Temporal lake area variability was larger in the Gobi regions, where small lakes are densely dis-tributed. The regression analyses indicated that the regional patterns of precipitation-driven lake area changes varied considerably (R2=0.028–0.950), depending on regional climate regime and hydromorphological char-acteristics. Generally, the lake area change in the hot-and-dry Gobi regions showed higher correlations with precipitation change. The precedent two-month precipitation was the best determining factor of lake area change across Mongolia. Our results indicate the usefulness of regression analysis based on satellite-derived multi-temporal lake area data to identify regions where factors other than precipitation might play important roles in determining lake area change.
Key words:  Dunhuang city    Crescent Moon Spring    pyramid dunes    dynamic characteristics    erosion and deposition
收稿日期:  2014-02-10      修回日期:  2014-05-12           出版日期:  2015-04-10      发布日期:  2014-06-03      期的出版日期:  2015-04-10
基金资助: 

This work was supported by research grants from Korea Forest Service (S211212L06301) and from National Research Founda-tion of Korea (NRF-2013R1A1A4A01008632). Sinkyu KANG was partly supported by Kangwon National University (C1009843-01-01).

通讯作者:  Sinkyu KANG    E-mail:  kangsk@kangwon.ac.kr
引用本文:    
Sinkyu KANG, Gyoungbin LEE, Chuluun TOGTOKH, Keunchang JANG. Characterizing regional precipitation-driven lake area change in Mongolia[J]. 干旱区科学, 2015, 7(2): 146-158.
Sinkyu KANG, Gyoungbin LEE, Chuluun TOGTOKH, Keunchang JANG. Characterizing regional precipitation-driven lake area change in Mongolia. Journal of Arid Land, 2015, 7(2): 146-158.
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