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The production of weather charts. aerology See atmospheric science. aeronomy The branch of meteorology that studies the upper regions of the Earth's or other planetary atmospheres, specifically their atmospheric motions, chemical compositions and properties, and interactions with the other parts of the atmosphere and with space. aerosol
Dynamic meteorology generally focuses on the fluid dynamics of the atmosphere. The idea of air parcel is used to define the smallest element of the atmosphere, while ignoring the discrete molecular and chemical nature of the atmosphere. An air parcel is defined as an infinitesimal region in the fluid continuum of the atmosphere. The fundamental ...
Atmospheric thermodynamics is the study of heat-to-work transformations (and their reverse) that take place in the Earth's atmosphere and manifest as weather or climate. . Atmospheric thermodynamics use the laws of classical thermodynamics, to describe and explain such phenomena as the properties of moist air, the formation of clouds, atmospheric convection, boundary layer meteorology, and ...
The atmospheric circulation can be viewed as a heat engine driven by the Sun's energy and whose energy sink, ultimately, is the blackness of space. The work produced by that engine causes the motion of the masses of air, and in that process it redistributes the energy absorbed by the Earth's surface near the tropics to the latitudes nearer the ...
Substantial fires can create their own weather – and do it in several ways. Fire whirls and pyrocumulus clouds: How fire creates its own weather Skip to main content
Atmospheric chemistry is a branch of atmospheric science in which the chemistry of the Earth's atmosphere and that of other planets is studied. It is a multidisciplinary field of research and draws on environmental chemistry, physics, meteorology, computer modeling, oceanography, geology and volcanology and other disciplines.
The phenomenon is marked by cooler than average water temperatures in the equatorial Pacific, along with corresponding changes in upper atmosphere patterns — and these changes influence weather ...
The terrestrial region was composed of the four elements: water, earth, fire, and air; These elements were arranged in spherical strata, with Earth as its center and the Moon on the outskirts of the sphere; They were in constant interchange with one another, e.g: heat from the Sun collides with cold water, creating air and mist