General circulation of Lake Superior: Mean, variability, and trends from 1979 to 2006
Version of Record online: 4 DEC 2010
Copyright 2010 by the American Geophysical Union.
Journal of Geophysical Research: Oceans (1978–2012)
Volume 115, Issue C12, December 2010
How to Cite
2010), General circulation of Lake Superior: Mean, variability, and trends from 1979 to 2006, J. Geophys. Res., 115, C12015, doi:10.1029/2010JC006261., , , and (
- Issue online: 4 DEC 2010
- Version of Record online: 4 DEC 2010
- Manuscript Accepted: 24 AUG 2010
- Manuscript Revised: 8 JUL 2010
- Manuscript Received: 12 MAR 2010
Auxiliary material for this article contains clarification of model forcing selection and sensitivity experiments run with the model at 10 km horizontal resolution.
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|jgrc11737-sup-0001-readme.txt||plain text document||4K||readme.txt|
|jgrc11737-sup-0002-ts01.txt||plain text document||1K||Table S1. Root mean square error of modeled lake surface temperatures at each of the three NCDC buoys.|
|jgrc11737-sup-0003-fs01.pdf||PDF document||39K||Figure S1. April–November average lake surface temperatures at the three NDBC buoy locations in the model and data for 1979–2006.|
|jgrc11737-sup-0004-fs02.pdf||PDF document||1688K||Figure S2. Daily average 10 m air temperature from the North American Regional Reanalysis Project is plotted against observed air temperature at the three NDBC buoy locations in Lake Superior for all days of available observations between April and September 1979–2006.|
|jgrc11737-sup-0005-fs03.pdf||PDF document||98K||Figure S3. Zonal velocity (U), meridional velocity (V), and temperature (T) at ADCP location E4 during the summer of 1998.|
|jgrc11737-sup-0006-fs04.pdf||PDF document||97K||Figure S4. Zonal velocity (U), meridional velocity (V), and temperature (T) at ADCP location E4 during the summer of 1999.|
|jgrc11737-sup-0007-fs05.pdf||PDF document||179K||Figure S5. Mean depth-average current speeds for January–December 1979–2006.|
|jgrc11737-sup-0008-fs06.pdf||PDF document||195K||Figure S6. Mean depth-average current direction and speed during winter (DJFM) and summer (JJAS) of 1997–2001 when the model with 10 km horizontal resolution is run (a and b) without wind, (c and d) without heat fluxes, (e and f) with a spatially uniform wind field, and (g and h) control.|
|jgrc11737-sup-0009-ms01.mp4||7769K||Animation S1. Daily mean of modeled (1979–2006) (top) surface temperatures and currents, (middle) depth-average temperatures and currents, and (bottom) below 50 m temperatures and currents.|
|jgrc11737-sup-0010-txts01.txt||plain text document||4K||Text S1. The selection of model forcing is discussed in section 1; section 2 includes a description of circulation sensitivity studies and the conclusions drawn from these studies.|
|jgrc11737-sup-0011-t01.txt||plain text document||0K||Tab-delimited Table 1.|
|jgrc11737-sup-0012-t02.txt||plain text document||1K||Tab-delimited Table 2.|
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