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Remote Sensing technology can be used to monitor and manage the marine environment. The project done by our group during the Environmental Studies Institute of the Woodrow Wilson Foundation (1999) has allowed us to understand how data are gathered and used for studies of coastal waters. We were able to identify imagery showing upwelling events and compare the sea surface temperature images to corresponding images of algal productivity. The qualitative comparison of color patterns in the imagery as well as the more definitive comparison of temperature and chlorophyll-a concentrations along co-located plot lines, show that upwelling along the New Jersey Long Island coasts has resulted in algal blooms. Look at data from the graphs for specifics- distance, temperature, and chlorophyll-a concentration. (See SSTand Chlorophyll Density images). In the images for sea surface temperature, the wavelengths from the thermal portion of the electromagnetic spectrum are used to identify temperature. The colors range from red to violet, with red having the highest sea surface temperature, and violet the lowest. In the SeaWiFs images, the colors range from red to violet, but red has the highest chlorophyll density, and violet the lowest. The graphs show that the low temperatures along the coast are associated with high chlorophyll density, whereas, further from the coast, the low temperatures are associated low chlorophyll density. We can deduce from this occurrence that the cold water associated with the upwelling along the coast is responsible for the algal blooms- hence high chlorophyll density along the coast.
The upwelling events have special significance for commercial fishermen
and weather enthusiasts. Algal blooms result in the proliferation of several
species of marine organisms that are used by humans as a source of food.
At the same time, large blooms can use up all the oxygen in the bottom
waters as the algae settle and decay, leading to stress or mortality of
shellfish and other bottom dwelling species. Further research into the
dynamics of upwelling can result in better fisheries and marine resource
management. The interpretations extrapolated from the remote sensing are
limited, and more careful studies by scientists involved in coastal environmental
management are needed, so that the entire populace will be aware of the
importance of the caring for and protecting the marine environment. The
marine environment serves us as a source of food, leisure, and relaxation.
The study and interpretation done by the 1999 Environmental Institute
was limited to a quick sampling of modern research capabilities using remote
sensing data. Given more time and a curricular focus, this project
can be adapted to a classroom investigation of oceanic processes, especially
in the context of Earth System Science. The upwelling events are a good
vehicle for exploring coupled systems (i.e. physical and biological), feedback
loops, and policy aspects of managing our coastal resources.
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Woodrow Wilson National Fellowship Foundation
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