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008			170505s2017 sz a o 001 0 eng d
020			_a331954571X _q(electronic bk.)
020			_a9783319545714 _q(electronic bk.)
020			_z3319545698
020			_z9783319545691 _q(print)
040			_aN$T _cN$T _dEBLCP _dGW5XE _dYDX _dN$T _dOCLCF _dSTF _dAZU _dUPM _dCOO _dMERER _dOCLCQ _dUAB _dES-MaUEC _bspa
050		4	_aGC116 _b.M634 2017 EB
245	0	0	_aModeling coastal hypoxia : _bnumerical simulations of patterns, controls and effects of dissolved oxygen dynamics _cDubravko Justic, Kenneth A. Rose, Robert D. Hetland, Katja Fennel, editors.
264		1	_aCham, Switzerland _bSpringer _c2017.
300			_a1 recurso en línea (xii, 433 páginas) _bilustraciones (algunas a color)
336			_aTexto _btxt _2rdacontent
337			_aelectrónico _bc _2rdamedia
338			_arecurso electrónico _bcr _2rdacarrier
347			_atext file _bPDF
500			_aIncluye índice
500			_aSpringerLink
505	0		_aPreface; Contents; Editors and Contributors; 1 Numerical Experiment of Stratification Induced by Diurnal Solar Heating Over the Louisiana Shelf; Abstract; 1.1 Background; 1.2 Numerical Model; 1.3 Model Specification; 1.3.1 Modeling Period and Data; 1.3.2 Model Inputs; 1.3.2.1 Heat Flux; 1.3.2.2 Wind Data; 1.3.2.3 Initial Temperature Profile; 1.3.3 Boundary Conditions; 1.4 Simulation Results; 1.4.1 Model Evaluation; 1.4.2 Sea Surface Temperature; 1.4.3 Vertical Distribution of Temperature; 1.5 Representing Stratification Based on Gradient Richardson Number.
505	8		_a1.6 Diurnal Heating/Stratification and Measured Bottom Oxygen Concentration1.7 Summary and Conclusion; Acknowledgements; Appendix A: Formulation of Different Surface Heat Components; References; 2 Physical Drivers of the Circulation and Thermal Regime Impacting Seasonal Hypoxia in Green Bay, Lake Michigan; Abstract; 2.1 Introduction; 2.2 Methods; 2.2.1 New Field Measurements; 2.2.2 Historical Observations; 2.2.3 Meteorological Forcing; 2.2.4 Modeling; 2.2.5 Model Validation; 2.2.6 Spectral Analysis; 2.2.7 Effects of Earth's Rotation; 2.3 Results and Discussion.
505	8		_a2.3.1 Relation Between the Surface Heat Flux and Stratification2.3.2 Relation Between Wind Fields and Circulation Pattern; 2.3.3 Relation Between Wind Direction and Water Exchange Between Green Bay and Lake Michigan; 2.3.4 Estimation of Water Transport Between Lower and Upper Green Bay; 2.3.5 Effects of Wind, Stratification, Earth's Rotation, and the Bay and Lake Topography on Two-Layer Flows; 2.3.6 Effects of Stratification, Earth's Rotation, and the Bay and Lake Topography on the Direction of Currents; 2.4 Conclusions; References.
505	8		_a3 Interannual Variation in Stratification over the Texas -- Louisiana Continental Shelf and Effects on Seasonal Hypoxia3.1 Introduction; 3.2 Model Setup; 3.3 Results; 3.4 Discussion; 3.5 Conclusions; References; 4 A Reduced Complexity, Hybrid Empirical-Mechanistic Model of Eutrophication and Hypoxia in Shallow Marine Ecosystems; Abstract; 4.1 Introduction; 4.2 Methods; 4.2.1 Study System; 4.2.2 Ecosystem Model Kinetics; 4.2.2.1 Phytoplankton Biomass and Production; 4.2.2.2 Pelagic Respiration; 4.2.2.3 Carbon Deposition and Sediment Fluxes; 4.2.2.4 Remaining Formulations.
505	8		_a4.2.3 Forcing Functions4.2.4 Spatial Elements and Transport Model; 4.2.5 Calibration and Sensitivity Analysis; 4.3 Results and Discussion; 4.3.1 Phytoplankton; 4.3.2 Nutrients; 4.3.3 Dissolved Oxygen; 4.3.4 Rate Processes; 4.3.5 Model Skill; 4.3.6 Sensitivity Analysis; 4.4 Conclusions and Future Directions; Acknowledgements; References; 5 Modeling Physical and Biogeochemical Controls on Dissolved Oxygen in Chesapeake Bay: Lessons Learned from Simple and Complex Approaches; Abstract; 5.1 Introduction; 5.2 Methods and Approach; 5.2.1 Box Model with Biogeochemistry (BM-RCA).
520	3		_aThis 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.
988			_aEBOOK, asignarmaterias, EBSPRINGER_2017D
650		7	_aOceanografía _2embne _0(OCoLC)fst00853069 _9138147
700	1		_aFennel, Katja, _eeditor literario
700	1		_aHetland, Robert D., _eeditor literario
700	1		_aJustić, Dubravko, _eeditor literario
700	1		_aRose, Kenneth A., _eeditor literario
856	4	0	_uhttps://go.openathens.net/redirector/universidadeuropea.es?url=http://link.springer.com/10.1007/978-3-319-54571-4 _zAcceso a este recurso digital (usuarios Universidad Europea de Madrid)
942			_2lcc _cLE
998			_b02/2018 _dz _e- _zSI