4.7 Article

Morphometry and average temperature affect lake stratification responses to climate change

期刊

GEOPHYSICAL RESEARCH LETTERS
卷 42, 期 12, 页码 4981-4988

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1002/2015GL064097

关键词

lake; stratification; climate change; temperature; warming; long term

资金

  1. National Science Foundation (NSF) [DEB-1030242]
  2. Global Lake Temperature Collaboration , National Aeronautics and Space Administration (NASA) [DEB-1147666]
  3. Research Opportunities in Space and Earth Sciences (ROSES) grant
  4. Institute of Agricultural and Natural Resources (IANR)
  5. University of Nebraska-Lincoln
  6. British Open Government License, British Antarctic Survey [GB/NERC/BAS/AEDC/00063]
  7. ARES-CCD through the ECOSYKI: Studies on Lake Kivu ecosystem for its sustainable management project
  8. Belgian Federal Science Policy Office through the EAGLES: East African Great Lake Ecosystem Sensitivity to Changes (EAGLES) [SD/AR/02A]
  9. Fonds National de la Recherche Scientifique (Belgium) through the CAKI: Cycle du Carbone et des Nutriments au Lac Kivu
  10. Fonds National de la Recherche Scientifique (Belgium) through the MICKY: Microbial Diversity and Processes in Lake Kivu
  11. Tahoe Regional Planning Agency
  12. Lahontan Regional Water Quality Board
  13. UVG
  14. USAID
  15. Russian Ministry of Education and Science [GR 01201461929]
  16. Russian Science foundation project [14-14-00400]
  17. Russian Science Foundation [14-14-00400] Funding Source: Russian Science Foundation

向作者/读者索取更多资源

Climate change is affecting lake stratification with consequences for water quality and the benefits that lakes provide to society. Here we use long-term temperature data (1970-2010) from 26 lakes around the world to show that climate change has altered lake stratification globally and that the magnitudes of lake stratification changes are primarily controlled by lake morphometry (mean depth, surface area, and volume) and mean lake temperature. Deep lakes and lakes with high average temperatures have experienced the largest changes in lake stratification even though their surface temperatures tend to be warming more slowly. These results confirm that the nonlinear relationship between water density and water temperature and the strong dependence of lake stratification on lake morphometry makes lake temperature trends relatively poor predictors of lake stratification trends.

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