Abstract
In November 2009, an autonomous underwater glider (AUG) was deployed for a period of 12 days on the Wisconsin Shelf of Lake Superior. During this period, the AUG made repeated cross-shelf transects from 3 km to 13 km offshore, making 26 cross-shelf transects in all, during which time temperature was measured. Each of these transects displayed a mid-shelf temperature maximum roughly 8 km offshore, with cooler waters both inshore and offshore of this. This is hypothesized to be due to a balance of persistent cooling at the surface and vertical mixing of cooler sub-thermocline waters offshore.
Original language | English (US) |
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Pages (from-to) | 316-321 |
Number of pages | 6 |
Journal | Aquatic Ecosystem Health and Management |
Volume | 15 |
Issue number | 3 |
DOIs | |
State | Published - Jul 2012 |
Bibliographical note
Funding Information:This research was made possible through funding from the Great Lakes Observing System (GLOS) and the National Science Foundation, Geosciences Directorate Grant 0825633.
Keywords
- autonomous glider
- physical limnology
- shelf cooling
- shelf dynamics
- thermal structure