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Owing to the fact that the invention of the original barometer by Torricelli was based on the fact that the average pressure of the atmosphere is capable of "sucking" 76 centimeters or 760 mm of mercury (Hg), a liquid metal at STP, up the inside bore of an evacuated glass tube or column, we have traditionally––and still to this day––described atmospheric pressure in terms of mm of mercury.
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The term was probably first used in 1905 by H.A. Des Voeux to describe atmospheric conditions over many British towns.
Carl-Gustaf Arvid Rossby, (born Dec. 28, 1898, Stockholm, Swed. died Aug. 19, 1957, Stockholm) Swedish American meteorologist whose innovations in the study of large-scale air movement and introduction of the equations describing atmospheric motion were largely responsible for the rapid development of meteorology as a science.
December 28 , 1898Stockholm, Sweden August 19 , 1957Stockholm, Sweden Carl-Gustaf Arvid Rossby, (born Dec. 28, 1898, Stockholm, Swed. died Aug. 19, 1957, Stockholm) Swedish American meteorologist whose innovations in the study of large-scale air movement and introduction of the equations describing atmospheric motion were largely responsible for the rapid development of meteorology as a science.
This paper uses plume development from atmospheric transport modeling to provide a power-law rule describing atmospheric dilution factors as a function of distance from the release point.
Dickinson (1968) proposed the idea of the PW waveguide describing atmospheric regions where the background wind and temperature allow wave propagation.
Large-scale forecast models are based on the numerical integration of differential equation systems, which can describe atmospheric circulation processes on account of global meteorological observations.
A particle scavenging model adopted to describe atmospheric scavenging phenomenon, once properly fitted to the experimented conditions, was used for the interpretation of experimental results.
The modelling system is based on prognostic downscaling of weather forecasts and on multi-scale chemical transport model simulation, in order to describe atmospheric circulation in a complex topographic environment, space/time variation of emissions and pollutant import from neighbouring regions.
Climate describes atmospheric behavior averaged over long time periods of decades and centuries across large geographic areas.
The B1 scenario describes atmospheric CO2 concentrations stabilizing at 550 ppm in 2100 due to a reduction in emissions rate below today's levels.
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