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: 3,501 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
2,445
965
91
3,501
200
120
157
HTML: 2,445
PDF: 965
XML: 91
Total: 3,501
Supplement: 200
BibTeX: 120
EndNote: 157
Views and downloads (calculated since 13 Jul 2020)
Cumulative views and downloads
(calculated since 13 Jul 2020)
Total article views: 2,913 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
2,183
657
73
2,913
200
99
134
HTML: 2,183
PDF: 657
XML: 73
Total: 2,913
Supplement: 200
BibTeX: 99
EndNote: 134
Views and downloads (calculated since 10 Jun 2021)
Cumulative views and downloads
(calculated since 10 Jun 2021)
Total article views: 588 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
262
308
18
588
21
23
HTML: 262
PDF: 308
XML: 18
Total: 588
BibTeX: 21
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: 3,501 (including HTML, PDF, and XML)
Thereof 3,321 with geography defined
and 180 with unknown origin.
Total article views: 2,913 (including HTML, PDF, and XML)
Thereof 2,788 with geography defined
and 125 with unknown origin.
Total article views: 588 (including HTML, PDF, and XML)
Thereof 533 with geography defined
and 55 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...
