Preface -- 1. Numerical experiment of stratification induced by diurnal solar heating over the Louisiana shelf -- 2. Physical Drivers of the Circulation and Thermal Regime Impacting Seasonal Hypoxia in Green Bay, Lake Michigan -- 3. Interannual variation in stratification over the Texas-Louisiana Continental Shelf and Effects on Seasonal Hypoxia -- 4. A Reduced Complexity, Hybrid Empirical-Mechanistic Model of Eutrophication and Hypoxia in Shallow Marine Ecosystems -- 5. Modeling Physical and Biogeochemical Controls on Dissolved Oxygen in Chesapeake Bay: Lessons Learned from Simple and Complex Approaches -- 6. Modeling Hypoxia and its Ecological Consequences in Chesapeake Bay -- 7. Modeling River-Induced Phosphorus Limitation in the Context of Coastal Hypoxia -- 8. Predicted Effects of Climate Change on Northern Gulf of Mexico Hypoxia -- 9. Oregon Shelf Hypoxia Modeling -- 10. Comparing Default Movement Algorithms for Individual Fish Avoidance of Hypoxia in the Gulf of Mexico -- 11. Hypoxia Effects Within an Intraguild Predation Food Web of Mnemiopsis leidyi ctenophores, larval fish, and copepods -- 12. Simulating the Effects of Hypoxia on Bay Anchovy in the Chesapeake Bay Using Coupled Hydrodynamic, Water Quality, and Individual-Based Fish Models -- 13. Simulation of the Population-Level Responses of Fish to Hypoxia: Should We Expect Sampling to Detect Responses?- 14. Using Ecosystem Modeling to Determine Hypoxia Effect on Fish and Fisheries -- 15. Numerical Modeling of Hypoxia and its Effects: Synthesis and Going Forward.

This book provides a snapshot of representative modeling analyses of coastal hypoxia and its effects. Hypoxia refers to conditions in the water column where dissolved oxygen falls below levels that can support most metazoan marine life (i.e., 2 mg O2 l-1). The number of hypoxic zones has been increasing at an exponential rate since the 1960s; there are currently more than 600 documented hypoxic zones in the estuarine and coastal waters worldwide. Hypoxia develops as a synergistic product of many physical and biological factors that affect the balance of dissolved oxygen in seawater, including temperature, solar radiation, wind, freshwater discharge, nutrient supply, and the production and decay of organic matter. A number of modeling approaches have been increasingly used in hypoxia research, along with the more traditional observational and experimental studies. Modeling is necessary because of rapidly changing coastal circulation and stratification patterns that affect hypoxia, the large spatial extent over which hypoxia develops, and limitations on our capabilities to directly measure hypoxia over large spatial and temporal scales. This book consists of 15 chapters that are broadly organized around three main topics: (1) Modeling of the physical controls on hypoxia, (2) Modeling of biogeochemical controls and feedbacks, and, (3) Modeling of the ecological effects of hypoxia. The final chapter is a synthesis chapter that draws generalities from the earlier chapters, highlights strengths and weaknesses of the current state-of-the-art modeling, and offers recommendations on future directions.

Available to subscribing member institutions only. Доступно лише організаціям членам підписки.

Online access from local network of NaUOA.

Online access with authorization at https://link.springer.com/

Онлайн-доступ з локальної мережі НаУОА.

Онлайн доступ з авторизацією на https://link.springer.com/