potential temperature वाक्य
उदाहरण वाक्य
मोबाइल
- 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 �C, 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,
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