potential temperature การใช้

• Modeled vertical profile and turbulent flux of virtual potential temperature.
• Under normal, stably stratified conditions, the potential temperature increases with height,
• Potential temperature is a useful measure of the static stability of the unsaturated atmosphere.
• The virtual potential temperature flux is given by
• With w'and \ theta _ v'perturbations of vertical velocity and virtual potential temperature, respectively.
• Almost all wind shear and all the potential temperature gradient in the CBL are confined in the surface layer.
• In the mesoscale, equivalent potential temperature is also a useful measure of the static stability of the unsaturated atmosphere.
• Situations in which the equivalent potential temperature decreases with height, indicating instability in saturated air, are quite common.
• Potential temperature, wind speed has a sharp increase across the capping inversion, while moisture has a sharp decrease.
• Observations show that turbulent mixing accounts for 50 % of the total variation of potential temperature in a typical CBL.
• The potential vorticity is absolute vorticity divided by the vertical spacing between levels of constant entropy ( or potential temperature ).
• Under almost all circumstances, potential temperature increases upwards in the atmosphere, unlike actual temperature which may increase or decrease.
• Situations in which the equivalent potential temperature decreases with height, indicating instability in saturated air, are much more common.
• Koshava's occurrence can be successfully forecast using the across-mountain mean sea level pressure and potential temperature differences.
• CLSW has characteristic potential temperature of 3 癈, salinity of 34.88 psu, and density of 34.66.
• It has a simplicity in that it uses straight lines for the three primary variables : pressure, temperature and potential temperature.
• Considerations of moist air and cloud theories typically involve various temperatures, such as equivalent potential temperature, wet-bulb and virtual temperatures.
• Virtual potential temperature \ theta _ v is often used instead of temperature T to correct for the effects of pressure and water vapor.
• Climatic variables shaping life zones include mean potential temperature, total annual precipitation, and the ratio of mean annual evapotranspiration to mean annual precipitation.
• Based on the results of the 1968 Kansas experiment, the following universal functions are determined for horizontal mean flow and mean virtual potential temperature,