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Temperature Anomalies in the Lower Suwannee River and Tidal Creeks, Florida, 2005: Open-File Report 2007-1311
United U. S. Department of the Interior
(Author)
·
Ellen A. Raabe
(Author)
·
Elzbieta Bialkowska-Jelinska
(Author)
·
Bibliogov
· Paperback
Temperature Anomalies in the Lower Suwannee River and Tidal Creeks, Florida, 2005: Open-File Report 2007-1311 - Raabe, Ellen A. ; Bialkowska-Jelinska, Elzbieta ; U. S. Department of the Interior, United
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Synopsis "Temperature Anomalies in the Lower Suwannee River and Tidal Creeks, Florida, 2005: Open-File Report 2007-1311"
Temperature anomalies in coastal waters were detected with Thermal Infrared imagery of the Lower Suwannee River (LSR) and nearshore tidal marshes on Florida's Gulf Coast. Imagery included 1.5-m-resolution day and night Thermal Infrared (TIR) and 0.75-m-resolution Color Infrared (CIR) imagery acquired on 2-3 March 2005. Coincident temperature readings were collected on the ground and used to calibrate the imagery. The Floridan aquifer is at or near the land surface in this area and bears a constant temperature signature of 22 degrees Celsius. This consistent temperature contrasts sharply with ambient temperatures during winter and summer months. Temperature anomalies identified in the imagery during a late-winter cold spell may be correlated with aquifer seeps. Hot spots were identified as those areas exceeding ambient water temperature by 4 degrees Celsius or more. Warm-water plumes were also mapped for both day and night imagery. The plume from Manatee Spring, a first-order magnitude spring, influenced water temperature in the lower river. Numerous temperature anomalies were identified in small tributaries and tidal creeks from Shired Island to Cedar Key and were confirmed with field reconnaissance. Abundant warm-water features were identified along tidal creeks south of the Suwannee River and near Waccasassa Bay. Features were mapped in the tidal creeks north of the river but appear to be less common or have lower associated discharge. The imagery shows considerable promise in mapping coastal-aquifer seeps and understanding the underlying geology of the region. Detection of seep locations may aid research in groundwater/surface-water interactions and water quality, and in the management of coastal habitats.
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