Lake level coherence supports common driver

Eos

Volumn 89, Issue 41, 2008, Pages 389-390

  Stow, Craig A ^a   Lamon, E C ^b   Kratz, T K ^c   Sellinger, C E ^d  

^a NOAA EARTH SYSTEM RESEARCH LABORATORY   (United States)

^b DUKE UNIVERSITY   (United States)

^c UNIVERSITY OF WISCONSIN MADISON   (United States)

^d GLERL ^*

Author keywords

[No Author keywords available]

Indexed keywords

CLIMATE EFFECT; LAKE LEVEL;

GREAT LAKES [NORTH AMERICA]; LAKE SUPERIOR; NORTH AMERICA;

EID: 55849144387     PISSN: 00963941     EISSN: None     Source Type: Journal    
DOI: 10.1029/2008EO410001     Document Type: Article

References (5)

1. Austin, J. A., and S. M. Colman (2007), Lake Superior summer water temperatures are increasing more rapidly than regional air temperatures: A positive ice albedo feedback, Geophys. Res. Lett., 34, L06604, doi:10.1029/2006GL029021.
2. Holden, C. (2007), Lean times for Lake Superior, Science, 318(5852), 893.
3. Magnuson, J. J. et al. (1997). Potential effects of climate changes on aquatic systems Laurentian Great Lakes and Precambrian Shield Region, Hydrol. Processes, 11(8), 825-871.
4. Magnuson, J. J., T. K. Kratz, and B. J. Benson (2006). Long-Term Dynamics of Lakes in the Landscape. Oxford Univ. Press, New York.
5. Sellinger, C. E. C. A. Stow, E. C. Lamon, and S. S. Qian (2008). Recent water level declines in the Lake Michigan-Huron system. Environ. Sci. Technol., 42, 367-373.