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: 3,269 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
2,284
903
82
3,269
188
111
146
HTML: 2,284
PDF: 903
XML: 82
Total: 3,269
Supplement: 188
BibTeX: 111
EndNote: 146
Views and downloads (calculated since 13 Jul 2020)
Cumulative views and downloads
(calculated since 13 Jul 2020)
Total article views: 2,703 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
2,027
610
66
2,703
188
91
124
HTML: 2,027
PDF: 610
XML: 66
Total: 2,703
Supplement: 188
BibTeX: 91
EndNote: 124
Views and downloads (calculated since 10 Jun 2021)
Cumulative views and downloads
(calculated since 10 Jun 2021)
Total article views: 566 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
257
293
16
566
20
22
HTML: 257
PDF: 293
XML: 16
Total: 566
BibTeX: 20
EndNote: 22
Views and downloads (calculated since 13 Jul 2020)
Cumulative views and downloads
(calculated since 13 Jul 2020)
Viewed (geographical distribution)
Total article views: 3,269 (including HTML, PDF, and XML)
Thereof 3,100 with geography defined
and 169 with unknown origin.
Total article views: 2,703 (including HTML, PDF, and XML)
Thereof 2,588 with geography defined
and 115 with unknown origin.
Total article views: 566 (including HTML, PDF, and XML)
Thereof 512 with geography defined
and 54 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...
