---
res:
  bibo_abstract:
  - The Qinghai-Tibet Plateau possesses the largest alpine lake system, which plays
    a crucial role in the land-atmosphere interaction. We report first observations
    on the thermal and radiation regime under ice of the largest freshwater lake of
    the Plateau. The results reveal that freshwater lakes on the Tibetan Plateau fully
    mix under ice. Due to strong solar heating, water temperatures increase above
    the maximum density value 1–2 months before the ice break, forming stable thermal
    stratification with subsurface temperatures >6°C. The resulting heat flow from
    water to ice makes a crucial contribution to ice cover melt. After the ice breakup,
    the accumulated heat is released into the atmosphere during 1–2 days, increasing
    lake-atmosphere heat fluxes up to 500 W m−2. The direct biogeochemical consequences
    of the deep convective mixing are aeration of the deep lake waters and upward
    supply of nutrients to the upper photic layer.@eng
  bibo_authorlist:
  - foaf_Person:
      foaf_givenName: Georgiy B
      foaf_name: Kirillin, Georgiy B
      foaf_surname: Kirillin
  - foaf_Person:
      foaf_givenName: Tom
      foaf_name: Shatwell, Tom
      foaf_surname: Shatwell
      foaf_workInfoHomepage: http://www.librecat.org/personId=86424
    orcid: 0000-0002-4520-7916
  - foaf_Person:
      foaf_givenName: Lijuan
      foaf_name: Wen, Lijuan
      foaf_surname: Wen
  bibo_doi: 10.1029/2021gl093429
  bibo_issue: '14'
  bibo_volume: 48
  dct_date: 2021^xs_gYear
  dct_isPartOf:
  - http://id.crossref.org/issn/0094-8276
  - http://id.crossref.org/issn/1944-8007
  dct_language: eng
  dct_publisher: Wiley@
  dct_subject:
  - alpine lakes
  - extreme environments
  - ake-atmosphere interaction
  - lake ice
  - radiatively driven convection
  - winter limnology
  dct_title: Ice‐Covered Lakes of Tibetan Plateau as Solar Heat Collectors@
...