Chapter 1: Algal Blooms
The phenomenon of algal bloom is due to Trichodesmium erythrium, a blue-green algae, is well known
on the northwest coast of India. Initiation takes place sometime in the end of February, reaches a peak
by the third week of March, and then generally declines by the end of April. The chlorophyll
concentration is reported to be on the order of 600 mg/m^3 during the peak. Thus it has a significant
contribution in serving as a carbon dioxide sink. In addition, it plays an important role in the
enrichment of water by fixing atmospheric nitrogen. Every year the bloom is reported to occur near
Goa on the northwest coast of India, besides other localized areas on the west and east coasts. Since the
chlorophyll concentration is very high, broad spectral bands like Landsat MSS were found useful in
mapping and monitoring the bloom dynamics. The enhanced FCC could reveal the spread of the bloom,
and FCC with a combination of band ratio helped in separating the suspended sediments from the algal
patch. The role played by the sudden appearance of the bloom is significant from the point of view of
biological productivity, carbon dioxide flux (acting as a sink) and nutrient enrichment (nitrogen
fixation). The mapping and monitoring can be done on a regular basis with the help of satellite data.

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