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NRLMSISE-00 is an empirical, global reference atmospheric model of the Earth from ground to space. [1] It models the temperatures and densities of the atmosphere's components. A primary use of this model is to aid predictions of satellite orbital decay due to atmospheric drag.
In atmospheric science, an atmospheric model is a mathematical model constructed around the full set of primitive, dynamical equations which govern atmospheric motions. It can supplement these equations with parameterizations for turbulent diffusion, radiation , moist processes ( clouds and precipitation ), heat exchange , soil , vegetation ...
Space weather models differ from meteorological models in that the amount of input is vastly smaller. A significant portion of space weather model research and development in the past two decades has been done as part of the Geospace Environmental Model (GEM) program of the National Science Foundation .
Advances in Atmospheric Sciences is a bimonthly peer-reviewed scientific journal co-published by Springer Science+Business Media and Science Press. It covers research on the dynamics, physics and chemistry of the atmosphere and oceans, including weather systems, numerical weather prediction, climate dynamics and variability, and satellite meteorology.
Journal of Atmospheric and Oceanic Technology; Journal of Atmospheric and Solar-Terrestrial Physics; Journal of the Atmospheric Sciences; Journal of Climate; Journal of Geophysical Research: section D (Atmospheres) Journal of Hydrometeorology; Meteorological Monographs; Meteorologische Zeitschrift; Monthly Weather Review; National Weather ...
The Journal of the Atmospheric Sciences (until 1962 titled Journal of Meteorology) is a scientific journal published by the American Meteorological Society. [1] It covers research related to the physics, dynamics, and chemistry of the atmosphere of Earth and other planets, with emphasis on the quantitative and deductive aspects of the subject.
A static atmospheric model has a more limited domain, excluding time. A standard atmosphere is defined by the World Meteorological Organization as "a hypothetical vertical distribution of atmospheric temperature, pressure and density which, by international agreement, is roughly representative of year-round, midlatitude conditions."
The U.S. Standard Atmosphere is a static atmospheric model of how the pressure, temperature, density, and viscosity of the Earth's atmosphere change over a wide range of altitudes or elevations. The model, based on an existing international standard, was first published in 1958 by the U.S. Committee on Extension to the Standard Atmosphere, and ...