1995
DOI: 10.1016/0278-4343(95)91432-t
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Satellite observations of the Texas Current

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Cited by 14 publications

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“…The combinations of these unusual factors allowed for Mexican salty surface water to travel onto the Texas shelf as the coastal currents reversed and potentially weakened the stratification potential along the shelf, which is evident in the histogram (Fig. 9) [13]. Due to flooding events from central Texas storms, the freshwater inflow reached the coast about three weeks after allowing episodic and severe stratification resulting in hypoxic areas of up to 6 meters off the bottom.…”
Section: B 2010 Gigem Oos Results
mentioning
confidence: 95%