Atmospheric physics
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Atmospheric sciences [cat.] |
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Meteorology [cat.] |
Climatology [cat.] |
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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.
In the UK, atmospheric studies are underpinned by the Meteorological Office. Divisions of the U.S National Oceanic and Atmospheric Administration (NOAA) oversee research projects and weather modeling involving atmospheric physics. The US National Astronomy and Ionosphere Center also carries out studies of the high atmosphere.
[edit] See also
- Adiabatic lapse rate
- Atmospheric electricity
- Atmospheric tides
- Baroclinic instability
- Barotropic instability
- Barotropic vorticity equation
- David Bates (physicist)
- Convective instability
- Coriolis effect
- Effect of sun angle on climate
- Euler equations
- Geostrophic wind
- Gravity wave
- Hydrostatic balance
- Kelvin-Helmholtz instability
- Madden-Julian oscillation
- Navier Stokes equations
- New Mexico Institute of Mining and Technology
- Potential vorticity
- Pressure gradient force
- Primitive equations
- Rossby number
- Rossby radius of deformation
- Space weather
- Thermal wind
- Vorticity equation