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1000 Titel
  • Seasonal thermal regime and climatic trends in lakes of the Tibetan highlands
1000 Autor/in
  1. Wen, Lijuan |
  2. Kirillin, Georgiy |
  3. Shatwell, Tom |
1000 Erscheinungsjahr 2017
1000 LeibnizOpen
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2017-04-04
1000 Erschienen in
1000 Quellenangabe
  • 21: 1895-1909
1000 FRL-Sammlung
1000 Copyrightjahr
  • 2017
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/hess-21-1895-2017 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • The hydrology of the lake-rich Tibetan Plateau is important for the global climate, yet little is known about the thermal regime of Tibetan lakes due to scant data. We (i) investigated the characteristic seasonal temperature patterns and recent trends in the thermal and stratification regimes of lakes on the Tibetan Plateau and (ii) tested the performance of the one-dimensional lake parameterization scheme FLake for the Tibetan lake system. For this purpose, we combined 3 years of in situ lake temperature measurements, several decades of satellite observations, and the global reanalysis data. We chose the two largest freshwater Tibetan lakes, Ngoring and Gyaring, as study sites. The lake model FLake faithfully reproduced the specific features of the high-altitude lakes and was subsequently applied to reconstruct the vertically resolved heat transport in both lakes during the last 4 decades. The model suggested that Ngoring and Gyaring were ice-covered for about 6 months and stratified in summer for about 4 months per year with a short spring overturn and a longer autumn overturn. In summer the surface mixed boundary layer extended to 6–8 m of depth and was about 20 % shallower in the more turbid Gyaring. The thermal regime of the transparent Ngoring responded more strongly to atmospheric forcing than Gyaring, where the higher turbidity damped the response. According to the reanalysis data, air temperatures and humidity have increased, whereas solar radiation has decreased, since the 1970s. Surprisingly, the modeled mean lake temperatures did not change, nor did the phenology of the ice cover or stratification. Lake surface temperatures in summer increased only marginally. The reason is that the increase in air temperature was offset by the decrease in radiation, probably due to increasing humidity. This study demonstrates that air temperature trends are not directly coupled to lake temperatures and underscores the importance of shortwave radiation for the thermal regime of high-altitude lakes.
1000 Fächerklassifikation (DDC)
1000 Liste der Beteiligten
  1. https://frl.publisso.de/adhoc/creator/V2VuLCBMaWp1YW4=|http://orcid.org/0000-0001-7337-3586|http://orcid.org/0000-0002-4520-7916
1000 Label
1000 Förderer
  1. Opening Research Foundation of the Key Laboratory of Land Surface Process and Climate Change in Cold and Arid Regions |
  2. Chinese Academy of Sciences |
  3. German Science Foundation |
  4. National Natural Science Foundation of China |
1000 Fördernummer
  1. -
  2. LPCC201401
  3. KI-853-7/1; KI-853-11/1; KI-853-7/1
  4. 1637107; 41475011
1000 Förderprogramm
  1. -
  2. -
  3. -
  4. -
1000 Dateien
1000 Förderung
  1. 1000 joinedFunding-child
    1000 Förderer Opening Research Foundation of the Key Laboratory of Land Surface Process and Climate Change in Cold and Arid Regions |
    1000 Förderprogramm -
    1000 Fördernummer -
  2. 1000 joinedFunding-child
    1000 Förderer Chinese Academy of Sciences |
    1000 Förderprogramm -
    1000 Fördernummer LPCC201401
  3. 1000 joinedFunding-child
    1000 Förderer German Science Foundation |
    1000 Förderprogramm -
    1000 Fördernummer KI-853-7/1; KI-853-11/1; KI-853-7/1
  4. 1000 joinedFunding-child
    1000 Förderer National Natural Science Foundation of China |
    1000 Förderprogramm -
    1000 Fördernummer 1637107; 41475011
1000 Objektart article
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1000 @id frl:6405763.rdf
1000 Erstellt am 2017-12-08T12:12:47.337+0100
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1000 Vgl. frl:6405763
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