Listing 1 - 10 of 53 | << page >> |
Sort by
|
Choose an application
Aéronomie --- Aëronomie --- Atmosphere, Upper. --- Atmosphere, upper
Choose an application
Microwave remote sensing --- Radiometers --- Atmosphere --- Earth (Planet)
Choose an application
Meteorology --- Weather forecasting --- climate --- Atmosphere. --- Atmosphere --- Climatic change --- precipitation. --- precipitation --- Weather hazards --- air pollution --- mathematics
Choose an application
Atmosphere. --- Atmosphere --- Atmospheric formations --- Atmospheric formations --- Atmospheric circulation --- Atmospheric circulation --- Dynamic models --- Dynamic models
Choose an application
Atmospheric chemistry. --- Chimie de l'atmosphère --- Chimie de l'atmosphère --- Pollution atmosphérique --- Atmosphere precipitation --- Biogeochemical cycle --- Atmosphere (earth) --- Atmospheric aerosols
Choose an application
forests --- carbon dioxide --- Respiration --- Photosynthesis --- ecosystems --- Relation plante atmosphere --- Europe
Choose an application
As the regional models required to understand and control the generation, distribution and deposition of air pollutants become more precise, the need to understand the detailed effects of hilly and mountainous terrain becomes more acute. The Alpine regions and the mountainous Mediterranean coasts have large effets on the way the pollutant burden is spread in their areas. Similarly an understanding of the effects of chemical and physical processes controlling pollutant deposition and the emission of biogenic compounds is essential to the correct modelling of the coastal regions which surround so much of Europe.The results from two projects on these problems are presented in this volume: one involved a series of field campaigns in the Alps and in the Rhine valley, the other involves ships and platforms in the North Sea and also in the Mediterranean.
Air --- Atmospheric deposition --- Marine pollution --- Ocean-atmosphere interaction. --- Pollution --- Mathematical models. --- Measurement. --- Air pollutant deposition --- Air-sea interaction --- Air-sea interactions --- Atmosfeer-oceaan interactie --- Atmosphere-ocean interaction --- Atmosphere-ocean interactions --- Atmospheric pollutant deposition --- Atmospheric-oceanic interactions --- Atmosphère-océan [Interaction ] --- Deposition at atmospheric pollutants --- Interaction air-mer --- Interaction atmosphere-ocean --- Interaction mer-air --- Interaction océan-atmosphère --- Interaction of atmosphere and ocean --- Interactions of atmosphere and ocean --- Lucht-zee interaktie --- Oceaan-atmosfeer interactie --- Ocean-atmosphere interaction --- Ocean-meteorological relations --- Oceanic-atmospheric interactions --- Océan-atmosphère [Interaction ] --- Sea-air interaction --- Sea-air interactions --- Zee-lucht interactie --- Atmosphère --- Interaction mer-atmosphère. --- Mer --- Mathematical models --- Modèles mathématiques --- Europe --- Alpine regions --- Modèles mathématiques. --- Pollution atmosphérique --- Atmospheric sciences. --- Air pollution. --- Atmospheric Sciences. --- Atmospheric Protection/Air Quality Control/Air Pollution. --- Air contaminants --- Air pollutants --- Air pollution --- Air pollution control --- Air toxics --- Airborne pollutants --- Atmosphere --- Contaminants, Air --- Control of air pollution --- Pollutants, Air --- Toxics, Air --- Air quality --- Atmospheric sciences --- Earth sciences --- Control --- Pollution atmosphérique --- Interaction mer-atmosphère. --- Modèles mathématiques.
Choose an application
While ocean waves are the most visible example of oceanic mixing processes, this macroscale mixing process represents but one end of the spectrum of mixing processes operating in the ocean. At the scale of a typical phytoplanktoic diatom or larval fish inhabiting these seas, the most important mixing processes occur on the molecular scale - at the scale of turbulence. Physical-biological interactions at this scale are of paramount importance to the productivity of the seas (fisheries) and the heat balance that controls large scale ocean climate phenomena such as El Niño and tornadoes. This
Air-sea interaction --- Air-sea interactions --- Atmosfeer-oceaan interactie --- Atmosphere-ocean interaction --- Atmosphere-ocean interactions --- Atmospheric-oceanic interactions --- Atmosphère-océan [Interaction ] --- Dynamique des fluides --- Fluid dynamics --- Geofysica --- Geological physics --- Geophysics --- Géophysique --- Interaction air-mer --- Interaction atmosphere-ocean --- Interaction mer-air --- Interaction océan-atmosphère --- Interaction of atmosphere and ocean --- Interactions of atmosphere and ocean --- Lucht-zee interaktie --- Oceaan-atmosfeer interactie --- Ocean-atmosphere interaction --- Ocean-meteorological relations --- Oceanic-atmospheric interactions --- Océan-atmosphère [Interaction ] --- Physics [Terrestrial ] --- Sea-air interaction --- Sea-air interactions --- Terrestrial physics --- Vloeistofdynamica --- Zee-lucht interactie --- Geophysics. --- Fluid dynamics. --- Oceanography. --- Oceanography, Physical --- Oceanology --- Physical oceanography --- Thalassography --- Earth sciences --- Marine sciences --- Ocean --- Dynamics --- Fluid mechanics --- Physics
Choose an application
Meteorology. Climatology --- Atmospheric physics --- Physique de l'atmosphère --- Periodicals. --- Périodiques --- Meteorology --- Atmosphere --- Atmosphere. --- Atmospheric physics. --- Meteorology. --- Physics. --- Aerology --- Aerophysics --- Atmospheric sciences --- Physical meteorology --- Physic --- Atmospheres --- Physics --- atmosphere --- dynamical meteorology --- ocean-atmosphere systems --- climate change --- hydrometeorology --- numerical weather prediction --- Earth sciences --- Geophysics --- Atmospheric science --- Meteorology, Physical --- Física atmosfèrica. --- Meteorologia.
Choose an application
Remote sounding of the atmosphere has proved to be a fruitful method of obtaining global information about the atmospheres of the earth and other planets. This book treats comprehensively the inverse problem of remote sounding, and discusses a wide range of retrieval methods for extracting atmospheric parameters of interest from the quantities (thermal emission, for example) that can be measured remotely. Inverse theory is treated in depth from an estimation-theory point of view, but practical questions are also emphasized, such as designing observing systems to obtain the maximum quantity of
Inverse problems (Differential equations) --- Atmosphere --- Atmospheric science --- Differential equations --- Measurement. --- Sounding and soundings. --- Sondage (Océanographie) --- Atmosphère --- Mesure --- Sounding and soundings --- Measurement --- Atmosphere - Measurement
Listing 1 - 10 of 53 | << page >> |
Sort by
|