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EOS 340 Assignment 3 Due date: February 24, [removed]Atmospheric Oscillations Consider an atmosphere in hydrostatic equilibrium with a constant environmental temperature gradient: dT /dz = −α. The temperature of a parc
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Document Date: 2012-02-09 12:58:30
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File Size: 71,37 KB
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IndustryTerm
moist static energy /
rst law /
internal energy changes /
internal energy /
gas law /
/
NaturalFeature
Mt δ(t) /
/
Position
mp /
/
Technology
thermodynamics /
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SocialTag
Thermodynamics
Lapse rate
Absolute zero
Moist static energy
Adiabatic process
Atmospheric thermodynamics
Atmospheric sciences
Meteorology