Resolving a persistent offshore surface temperature maximum in Lake Superior using an autonomous underwater glider

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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 languageEnglish (US)
Pages (from-to)316-321
Number of pages6
JournalAquatic Ecosystem Health and Management
Volume15
Issue number3
DOIs
StatePublished - 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

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