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Related articles:
Lapse rate
Tropopause
Stratosphere
Water vapor
Weather
Key terms: air math dz height temperature frac troposphere lapse rate pressure decreases atmosphere parcel stands dry heat gamma altitude tropopause equation layer lower rises saturated water vapor mixing change higher average surface density expands stratosphere constant adiabatic lapse rate generally structure inversion ideal gas air parcel composition temperature drops parcel of air approximately vapor pressure temperature decreases environmental lapse rate than its surroundings decreases with height rate at which temperature Search external links cited by footnotes on Wikipedia page Troposphere: |
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