3 edition of Atmospheric and oceanic processes, dynamics, and climate change found in the catalog.
Atmospheric and oceanic processes, dynamics, and climate change
Includes bibliographical references and index.
|Statement||Zhaobo Sun, Fei-Fei Jin, Toshiki Iwasaki, chairs/editors ; sponsors, CSO--Chinese Society of Oceanography (China), SPIE--the International Society for Optical Engineering ...|
|Series||SPIE proceedings series,, v. 4899, Proceedings of SPIE--the International Society for Optical Engineering ;, v. 4899.|
|Contributions||Sun, Zhaobo., Jin, Feifei., Iwasaki, Toshiki., Zhongguo hai yang xue hui., Society of Photo-optical Instrumentation Engineers.|
|LC Classifications||QC880.4.A8 A88 2003|
|The Physical Object|
|Pagination||ix, 184 p. :|
|Number of Pages||184|
|LC Control Number||2003284172|
Instabilities, Waves and Turbulence: 6. Atmospheric Chemistry Research is focused on understanding the chemical composition of the atmosphere and its evolution to better determine impacts on climate, air quality, ecosystems, and human health. Krasting, M. Prior to taking up his position there, he taught for many years at Princeton University, New Jersey. What processes control ocean heat and carbon uptake, and ultimately transient climate change?
Large-Scale Atmospheric Circulation: Highly recommended! Topics in this research area include fundamental process studies in oceanic and atmospheric biogeochemical cycles; numerical model development to better understand and simulate marine and terrestrial biospheres; modeling of the interactions between climate and biosphere; analysis of remote sensing and in-situ data; and fusion of observational data and numerical models to uncover underlying processes related to global change. He has also written upon occasion for a broad, educated audience on the policy implications of his work. The book strikes an ideal balance between mathematical rigor and physical intuition, and between atmosphere- and ocean-relevant applications.
Wind and buoyancy driven circulation; Appendix: miscellaneous relationships in a layered model; Index. Climate and Climate Change Climate and Climate Change The climate system is composed of many subsystems, including the atmosphere, cryosphere, biosphere, and hydrosphere. Phenomena of climatological interest include the atmospheric boundary layercirculation patternsheat transfer radiativeconvective and latentinteractions between the atmosphere and the oceans and land surface particularly vegetationland use and topographyand the chemical and physical composition of the atmosphere. Modeling studies focus on the the decadal and interannual variability of climate, including the role of the ocean, while observations help us diagnose the on the seasonal and intraseasonal variability in the large scale atmospheric circulation.
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The vertical structure of the atmosphere. After undergraduate and graduate work in physics and geology, he obtained his Ph.
The equations of fluid motion. Barotropic and baroclinic instability; 7. We also show that ocean heat uptake occurring at subpolar latitudes has a stronger cooling effect on global atmospheric surface temperature than ocean heat uptake occurring in low latitudes Winton et al.
He has also written upon occasion for a broad, educated audience on the policy implications of his work. Instabilities, Waves and Turbulence: 6. Large-Scale Atmospheric Circulation: While by no means downplaying the threat of global warming, Ramanathan is more optimistic than some of his confreres about the possibility of mitigating its worst effects without the enormous economic and social dislocations that strict curtailment of carbon emissions would entail.
Readership Undergraduate or master-course students in meteorology, oceanography and climatology are the main target. The advanced sections can easily be omitted for a more introductory course, as they are clearly marked in the text.
It differs from other books at this level in both style and content: as well as very basic material it includes some elementary introductions to more advanced topics. Mann has authored or co-authored Atmospheric and oceanic processes than peer-reviewed journal articles and book chapters, as well as delivering countless invited lectures and presentations.
Remote sensing also replaces costly and slow data collection on the ground, ensuring in the process that areas or objects are not disturbed. He has also been one of the most tireless defenders of the mainstream view on climate change in the popular and political arena; to this end, he has given government testimony, co-founded the RealClimate.
Manabe is currently Senior Meteorologist at Princeton University. Topics include modeling and measurement of aerosol particles and gases; studies of biosphere-chemistry-climate interactions, cloud formation, fog and cloud chemistry, and aerosol-cloud-climate interactions; laboratory and field studies of ice nuclei and their climate impacts; interpretation of satellite observations of tropospheric composition; studies of pollutant emission, transport, and deposition; and studies of aerosol impacts on regional haze and air quality.
A few of the most influential and otherwise important of these are listed below. Here at the University of Wisconsin—Madison, we are using appropriate observational information and numerical models of these components in an interactive system to study past and present climates and to make predictions about the future.
Planetary atmospheres are affected by the varying degrees of energy received from either the Sun or their interiors, leading to the formation of dynamic weather systems such as hurricaneson Earthplanet-wide dust storms on Marsan Earth-sized anticyclone on Jupiter called the Great Red Spotand holes in the atmosphere on Neptune.
Research is conducted on convection, mesoscale instabilities, gravity currents and waves, precipitation physics, cloud ice and liquid water processes, atmospheric electricity, aerosol indirect effects, vortices, tornadogenesis, storm interactions, orographic influences, boundary layer processes, frontal processes, effects of surface heterogeneities, coastal boundaries, and urban effects on weather.
The global energy balance. Kushner, University of Toronto. Solar radiation contains variety of wavelengths.Background: Atmospheric and oceanic climate refers to the monthly/seasonal averaged distributions of circulation, temperature, moisture, and related eddy transports.
The course will provide a dynamically oriented description of the observed distributions, with the intent of. Our research addresses physical climate processes in the context of anthropogenic perturbations to the earth system as the underlying cause of climate change.
Focal points of our research are cloud and aerosol physics, their interactions and their role in the climate system. Student problems and exercises are included at the end of each chapter.
Atmospheric and Oceanic Fluid Dynamics: Fundamentals and Large-Scale Circulation will be an invaluable graduate textbook on advanced courses in GFD, meteorology, atmospheric science and oceanography, and an excellent review volume for atlasbowling.com: $ Student problems and exercises are included at the end of each chapter.
Atmospheric and Oceanic Fluid Dynamics: Fundamentals and Large-Scale Circulation will be an invaluable graduate textbook on advanced courses in GFD, meteorology, atmospheric science and oceanography, and an excellent review volume for researchers.
Atmospheric physics is the application of physics to the study of the atlasbowling.comheric physicists attempt to model Earth's atmosphere and the atmospheres of the other planets using fluid flow equations, chemical models, radiation budget, and energy transfer processes in the atmosphere (as well as how these tie into other systems such as the oceans).
Atmospheric and Oceanic Processes, Dynamics, and Climate Change Zhaobo Sun Fei-Fei Jin Toshiki Iwasaki Chairs/Editors 25 and 27 October Hangzhou, China Sponsors CSO Chinese Society of Oceanography (China) SPIE The International Society for Optical Engineering Cosponsors and Supporting Organizations.