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Atmospheric physics From Wikipedia, the free encyclopedia Jump to: navigation search Atmospheric sciences [cat.] ... Portal Weather Atmospheric physics is the application of physics to the study of the atmosphere . Atmospheric physicists attempt to model Earth's atmosphere and the atmospheres of the other planets using fluid flow equations, chemical models, radiation balancing, and energy transfer processes in the atmosphere (as well as how these tie in to other systems such as the oceans). In order to model weather systems, atmospheric physicists employ elements of scattering theory, wave propagation models, cloud physics statistical mechanics and spatial statistics which are highly mathematical and related to physics. It has close links to meteorology and climatology and also covers the design and construction of instruments for studying the atmosphere and the interpretation of the data they provide, including remote sensing instruments. Contents Radiation Cloud physics Atmospheric electricity Atmospheric tide ... edit Radiation This is a diagram of the seasons. In addition to the density of incident light, the

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Course Description The most fundamental atmospheric measurements are temperature, pressure, and humidity. This course explores the meaning of these in great detail, so that students should come out with a strong understanding of the thermodynamics of the particular two-component system – dry air and water – most important to understanding weather. Geog 220 presents the following sequence of steps: warming air becomes less dense (expands) and may rise, rising air cools, as the water vapor cools along with the air, it cannot stay in vapor state and starts to condense. Keep that going and a cloud will form, and eventually, under the right circumstances, rain may fall. This course repeats all those points, but tries to provide a deeper understanding, working from a few physical priniciples and using some math to get quantitative answers. Geog 420/620 Atmospheric Physics Spring 2008 Office Hours Text: M. L. Salby, Fundamentals of Atmospheric Physics Projects: Eight problem sets, mostly of pencil-paper-calculator problem solving with a little computer work. Tests: two hour exams, a comprehensive final exam.

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Forsiden Aktuelt Forskningsenheter Forskning/prosjekter ... Alfabetisk prosjektoversikt Forskning/prosjekter Alfabetisk prosjektoversikt Temasiden Postadresse: Forsvarets forskningsinstitutt Postboks 25 2027 Kjeller Instituttveien 20 Telefon: 63 80 70 00 Telefaks: 63 80 71 15 Karljohansvern Telefon Horten: 33 03 38 00 E-post FFI E-post INFO E-post Atmospheric Physics at the Norwegian Defence Research Establishment (FFI) Lidar observations of the polar middle atmosphere. The polar atmosphere is a region of dazzling phenomena and environmental importance. It is one of the most fascinating regions on Earth. It also impacts on conditions for life on this planet. Noctilucent clouds in the summer night sky over Rondane. (Photo: U.-P. Hoppe, FFI) Polar stratospheric clouds observed above Esrange in northern Sweden. (Photo: G. Baumgarten) Amazing phenomena in the summer polar atmosphere Although the sun never sets for several weeks, the atmosphere regularly cools down to 123 K near 80 km altitude. This is the coldest area on or near Earth, and the same height region is 100 K warmer during the polar night in winter. Although the height region is very dry, the cold temperatures in summer create water-ice particles. These numbers describe the approximate fraction of light intensity is scattered by NLC when they are illuminated vertically. The typical amount of water bound up in these tiny ice particles is approximately 20 cm

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