Under
typical atmospheric conditions, the denominator of the exponent depends weakly on T -LCB- \ displaystyle T -RCB-(for which the unit is Celsius).
Therefore, the August - Roche - Magnus equation implies that saturation water vapor pressure changes approximately exponentially with temperature under
typical atmospheric conditions, and hence the water - holding capacity of the atmosphere increases by about 7 % for every 1 °C rise in temperature.
The Clausius — Clapeyron equation for water vapor under
typical atmospheric conditions (near standard temperature and pressure) is
That release disrupts
typical atmospheric conditions, thereby affecting how the jet stream behaves.
Not exact matches
For the study, researchers tracked the
atmospheric conditions for the wettest and driest and coolest and warmest years of the state's
typical winter seasons from 1948 to 2015.