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Understand the principles of moisture conservation, equation of state, and energy conservation in atmospheric science. Learn about the hydrologic cycle, evapotranspiration, precipitation, and moisture advection. Join our lab session on March 22.
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Conservation of Moisture The Moisture Equation
Equation of State • 1st Law of Thermodynamics (Conservation of Energy) • Moisture Equation (Conservation of Moisture) • Continuity Equation (Conservation of Mass) • Equations of Motion (Conservation of Momentum) • Coming to an ATMS 251 lab near you on March 22
Moisture Equation • Mathematical representation of what can happen to water in a column of the atmosphere Evapotranspiration from ground Change of moisture storage in the column Precipitation Moisture Outflow from column Moisture Inflow from atmosphere
Precipitable Water • The vertical integral of the specific humidity for a column of atmosphere • Represents the upper limit to the total precipitation that may fall • Units: m (mm)
Average Specific Humidity for the layer Pressure Interval Sum up the number of levels This will yield the precipitable water in units of kg/m2. To get PW in units of meters, divide by the density of water (ρw=1000 kg/m3)
http://www.osdpd.noaa.gov/PSB/IMAGES/images/amsua_tpw_des.gifhttp://www.osdpd.noaa.gov/PSB/IMAGES/images/amsua_tpw_des.gif
Moisture Advection • Of course, moisture can be transported horizontally and vertically in the atmosphere • Moisture Advection
http://ww2010.atmos.uiuc.edu/guides/mtr/af/adv/gifs/madv1.gifhttp://ww2010.atmos.uiuc.edu/guides/mtr/af/adv/gifs/madv1.gif