Key Laboratory of Tibetan Environment Changes and Land Surface
Processes, Institute of Tibetan Plateau Research, Chinese Academy of
Sciences, Beijing 100101, China
CAS Center for Excellence in Tibetan Plateau Earth System Sciences, Beijing 100101, China
Tandong Yao
Key Laboratory of Tibetan Environment Changes and Land Surface
Processes, Institute of Tibetan Plateau Research, Chinese Academy of
Sciences, Beijing 100101, China
CAS Center for Excellence in Tibetan Plateau Earth System Sciences, Beijing 100101, China
Kun Yang
Key Laboratory of Tibetan Environment Changes and Land Surface
Processes, Institute of Tibetan Plateau Research, Chinese Academy of
Sciences, Beijing 100101, China
CAS Center for Excellence in Tibetan Plateau Earth System Sciences, Beijing 100101, China
Department of Earth System Science, Tsinghua University, Beijing
10084, China
Key Laboratory of Tibetan Environment Changes and Land Surface
Processes, Institute of Tibetan Plateau Research, Chinese Academy of
Sciences, Beijing 100101, China
Key Laboratory of Tibetan Environment Changes and Land Surface
Processes, Institute of Tibetan Plateau Research, Chinese Academy of
Sciences, Beijing 100101, China
CAS Center for Excellence in Tibetan Plateau Earth System Sciences, Beijing 100101, China
University of Chinese Academy of Sciences, Beijing, China
Broxton W. Bird
Department of Earth Sciences, Indiana University–Purdue University
Indianapolis (IUPUI), Indianapolis, IN 46202, USA
Viewed
Total article views: 3,716 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
2,580
1,029
107
3,716
215
132
179
HTML: 2,580
PDF: 1,029
XML: 107
Total: 3,716
Supplement: 215
BibTeX: 132
EndNote: 179
Views and downloads (calculated since 13 Jul 2020)
Cumulative views and downloads
(calculated since 13 Jul 2020)
Total article views: 3,100 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
2,314
699
87
3,100
215
110
156
HTML: 2,314
PDF: 699
XML: 87
Total: 3,100
Supplement: 215
BibTeX: 110
EndNote: 156
Views and downloads (calculated since 10 Jun 2021)
Cumulative views and downloads
(calculated since 10 Jun 2021)
Total article views: 616 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
266
330
20
616
22
23
HTML: 266
PDF: 330
XML: 20
Total: 616
BibTeX: 22
EndNote: 23
Views and downloads (calculated since 13 Jul 2020)
Cumulative views and downloads
(calculated since 13 Jul 2020)
Viewed (geographical distribution)
Total article views: 3,716 (including HTML, PDF, and XML)
Thereof 3,504 with geography defined
and 212 with unknown origin.
Total article views: 3,100 (including HTML, PDF, and XML)
Thereof 2,947 with geography defined
and 153 with unknown origin.
Total article views: 616 (including HTML, PDF, and XML)
Thereof 557 with geography defined
and 59 with unknown origin.
Lake evaporation from Paiku Co on the TP is low in spring and summer and high in autumn and early winter. There is a ~ 5-month lag between net radiation and evaporation due to large lake heat storage. High evaporation and low inflow cause significant lake-level decrease in autumn and early winter, while low evaporation and high inflow cause considerable lake-level increase in summer. This study implies that evaporation can affect the different amplitudes of lake-level variations on the TP.
Lake evaporation from Paiku Co on the TP is low in spring and summer and high in autumn and...
