Titlebook: Hypoxia in the Northern Gulf of Mexico; Virginia H. Dale,Donelson Wright,Clifford S. Snyde Book 2010 Springer-Verlag New York 2010 Control

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https://doi.org/10.1007/978-3-658-07750-1 average midsummer areal extent of 16,500 km. (2001–2007), and extends in some years from the Mississippi River mouth westward to Texas coastal waters (Rabalais et al., 2007). This hypoxic region (Fig. 1.1) occurs along a relatively shallow, open coastline with complex circulation and water column s

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https://doi.org/10.1007/978-3-663-12881-6 scientific basis for goals and management options. In the sections below, these questions (shown in italics below) are addressed very briefly with references to those sections of this book where more detailed science on that particular question may be found.

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Chronological

Nutrient Fate, Transport, and Sources,y changes and improvements in the understanding of nutrient sources and flux estimates within the Mississippi and Atchafalaya River basins (MARB) (see Fig. Fig 1.2) and the current ability to use watershed models to route and predict nutrient delivery to the Gulf of Mexico. The following sections di

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