Therefore, storms that have a large radial variation in virtual temperature will have stronger outer winds.
2.
This virtual temperature T _ v in units of Kelvin can be used seamlessly in any thermodynamic equation necessitating it.
3.
The virtual temperature correction usually is rather small and to a good approximation; it can be ignored when computing buoyancy.
4.
Neglecting the virtual temperature correction may result in substantial relative errors in the calculated value of CAPE for small CAPE values.
5.
Assuming an atmosphere that is in hydrostatic balance, the average column virtual temperature contributes the most to the surface pressure.
6.
The virtual temperatures of the three F09 storms varied with the Kessler storm having temperatures several degrees warmer than the other storms.
7.
Considerations of moist air and cloud theories typically involve various temperatures, such as equivalent potential temperature, wet-bulb and virtual temperatures.
8.
On a skew-T log-P diagram, CIN is any area between the warmer environment virtual temperature profile and the cooler parcel virtual temperature profile.
9.
On a skew-T log-P diagram, CIN is any area between the warmer environment virtual temperature profile and the cooler parcel virtual temperature profile.
10.
A plot of geopotential height for a single pressure level shows the troughs and ridges, hPa and 1000 hPa geopotential heights for example is proportional to mean virtual temperature in that layer.
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