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Physics and Dynamics of the Atmosphere

2019
This chapter describes the basic physics and thermodynamics of the atmosphere, starting from the ideal gas law and the hydrostatic equation, from which the lapse rate in the troposphere is derived. The effect of atmospheric moisture on the lapse rate is identified and the Clausius–Clapeyron equation giving the saturated humidity is derived.
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Atmospheric Dynamics: Fundamentals

1997
The equation of state for dry air (ideal gas law) is given by $$ p\alpha = RT{\kern 1pt} or{\kern 1pt} p = pRT $$ (1) where p, T, ρ, α, and R (= 287 Jkg-1K-1) denote pressure, temperature, density, specific volume, and the gas constant for dry air, respectively.
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On the Dynamics of a Combustible Atmosphere

1985
The paper considers plane gas-dynamic waves of small amplitude that propagate through an exothermically reacting (combustible) atmosphere. The latter is spatially uniform but its temperature and pressure are both increasing with time. Any such problem needs several parameters for its description, but four have particular significance; they are the ...
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Ab Initio Nonadiabatic Quantum Molecular Dynamics

Chemical Reviews, 2018
Basile F E Curchod, Todd J Martínez
exaly  

Exciton Dynamics in Semiconductor Nanocrystals

Advanced Materials, 2013
Jin Z Zhang
exaly  

Moisture‐Responsive Wrinkling Surfaces with Tunable Dynamics

Advanced Materials, 2017
Songshan Zeng   +2 more
exaly  

The cell biology of mitochondrial membrane dynamics

Nature Reviews Molecular Cell Biology, 2020
Marta Giacomello   +2 more
exaly  

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