Climate Dynamics : Why Does Climate Vary?.

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Published by the American Geophysical Union as part of the Geophysical Monograph Series. Climate Dynamics: Why Does Climate Vary? presents the major climate phenomena within the climate system to underscore the potency of dynamics in giving rise to climate change and variability. These phenomena inc...

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Detalles Bibliográficos
Clasificación:Libro Electrónico
Autor principal: Sun, De-Zheng
Otros Autores: Bryan, Frank M.
Formato: Electrónico eBook
Idioma:Inglés
Publicado: Washington : Wiley, 2013.
Colección:Geophysical monograph ; 189.
Temas:
Climatic changes.
Convection (Meteorology)
Dynamic meteorology.
Ocean-atmosphere interaction.
Climate Change
Climat > Changements.
Convection (Météorologie)
Météorologie dynamique.
Interaction mer-atmosphère.
climate change.
Climatic changes
Dynamic meteorology
Ocean-atmosphere interaction
Acceso en línea:Texto completo
Tabla de Contenidos:
  • Introduction; The Multiscale Organization of Moist Convection and the Intersection of Weather and Climate; 1. INTRODUCTION; 2. GLOBAL CONVECTIVE ORGANIZATION; 3. CONTROLS ON MOIST CONVECTION; 4. FUNDAMENTALS OF MESOSCALE CONVECTIVE ORGANIZATION; 5. MULTISCALE ORGANIZATION OF TROPICAL CONVECTION; 6. MULTISCALE CONVECTIVE ORGANIZATION IN NUMERICAL MODELS; 7. PARAMETERIZATION OF MCS; 8. DISCUSSION; 9. CONCLUSIONS; Monsoon Climate Variabilities; 1. INTRODUCTION; 2. STRUCTURES AND MECHANISMS OF THE NORTHWARD PROPAGATION OF BSISO.
  • 3. PROCESSES DETERMINING THE QB AND LF VARIABILITY OF THE INDIAN MONSOON4. PACIFIC-EAST ASIA TELECONNECTION; 5. TROPOSPHERIC BIENNIAL OSCILLATIONS IN THE INDO-PACIFIC WARM POOL; 6. CONCLUDING REMARKS; A Brief Introduction to El Niño and La Niña; 1. INTRODUCTION; 2. ANNUAL CYCLE; 3. EL NIñO AND LA NIñA; 4. ENSO IN THE PAST CLIMATES; A Linear Stochastic Model of Tropical Sea Surface Temperatures Related to El Niño; 1. INTRODUCTION; 2. SOME STOCHASTIC THEORY; 3. APPLICATION TO TROPICAL SEA SURFACE TEMPERATURES; 4. FORECASTS OF TROPICAL SST; 5. SUMMARY AND DISCUSSION.
  • The Diabatic and Nonlinear Aspects of the El Niño-Southern Oscillation: Implications for Its Past and Future Behavior1. INTRODUCTION; 2. THEORETICAL ADVANCES; 3. RECENT ELEVATION OF ENSO ACTIVITY; 4. ENSO IN THE PAST CLIMATES; 5. POSSIBLE PROBLEMS WITH IPCC MODELS; 6. FINAL REMARKS; El Niño-Southern Oscillation Ocean Dynamics: Simulation by Coupled General Circulation Models; 1. INTRODUCTION; 2. SPATIAL AND TEMPORAL STRUCTURE OF ENSO IN SOME OF THE IPCC-AR4 MODELS; 3. WHAT IS THE UNDERLYING ENSO DYNAMICS IN THE MODELS?; 4. WHAT DETERMINES THE ENSO PERIOD IN THE CLIMATE MODELS?; 5. CONCLUSIONS.
  • Extratropical Air-Sea Interaction, Sea Surface Temperature Variability, and the Pacific Decadal Oscillation1. INTRODUCTION; 2. MEAN UPPER OCEAN CLIMATE; 3. SST TENDENCY SURFACE HEAT BUDGET; 4. PROCESSES THAT GENERATE MIDLATITUDE SSTA (PACIFIC FOCUS); 5. PACIFIC DECADAL OSCILLATION; 6. BEYOND THE PDO; Northern Hemisphere Extratropical Tropospheric Planetary Waves and Their Low-Frequency Variability: Their Vertical Structure and Interaction With Transient Eddies and Surface Thermal Contrasts; 1. INTRODUCTION; 2. MEAN STRUCTURE OF THE NORTHERN HEMISPHERE PLANETARY WAVES.
  • 3. LOW-FREQUENCY VARIABILITY IN THE NORTHERN HEMISPHERE EXTRATROPICAL CIRCULATION4. SUMMARY AND DISCUSSION; Arctic Sea Ice and the Potential for Abrupt Loss; 1. DESCRIPTION OF ARCTIC SEA ICE; 2. ROLE OF SEA ICE IN THE CLIMATE SYSTEM; 3. OBSERVED SEA ICE TRENDS; 4. SIMULATED SEA ICE CONDITIONS; 5. POTENTIAL FOR ABRUPT SEA ICE CHANGE; 6. CONCLUSIONS; Global Warming and Tropical Cyclone Activity in the Western North Pacific From an Observational Perspective; 1. INTRODUCTION; 2. FACTORS RELATED TO TC ACTIVITY; 3. VARIATIONS IN TC ACTIVITY; 4. VARIATIONS IN TRACKS AND LANDFALL LOCATIONS.

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