virtual temperature sentence in Hindi
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- Therefore, storms that have a large radial variation in virtual temperature will have stronger outer winds.
- This virtual temperature T _ v in units of Kelvin can be used seamlessly in any thermodynamic equation necessitating it.
- The virtual temperature correction usually is rather small and to a good approximation; it can be ignored when computing buoyancy.
- Neglecting the virtual temperature correction may result in substantial relative errors in the calculated value of CAPE for small CAPE values.
- Assuming an atmosphere that is in hydrostatic balance, the average column virtual temperature contributes the most to the surface pressure.
- The virtual temperatures of the three F09 storms varied with the Kessler storm having temperatures several degrees warmer than the other storms.
- Considerations of moist air and cloud theories typically involve various temperatures, such as equivalent potential temperature, wet-bulb and virtual temperatures.
- 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.
- 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.
- 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.
- On a sounding diagram, CAPE is the " positive area " above the LFC, the area between the parcel's virtual temperature line and the environmental virtual temperature line where the ascending parcel is warmer than the environment.
- On a sounding diagram, CAPE is the " positive area " above the LFC, the area between the parcel's virtual temperature line and the environmental virtual temperature line where the ascending parcel is warmer than the environment.
- The z-bottom and z-top limits of integration in the equation represent the bottom and top altitudes ( in meters ) of a single CIN layer, T _ { v, parcel } is the virtual temperature of the specific parcel and T _ { v, env } is the virtual temperature of the environment.
- The z-bottom and z-top limits of integration in the equation represent the bottom and top altitudes ( in meters ) of a single CIN layer, T _ { v, parcel } is the virtual temperature of the specific parcel and T _ { v, env } is the virtual temperature of the environment.
- Where z _ \ mathrm { f } is the height of the level of free convection and z _ \ mathrm { n } is the height of the equilibrium level ( neutral buoyancy ), where T _ \ mathrm { v, parcel } is the virtual temperature of the specific parcel, where T _ \ mathrm { v, env } is the virtual temperature of the environment, and where g is the sounding diagram ( e . g ., a Skew-T log-P diagram ) using air temperature and dew point data usually measured by a weather balloon.
- Where z _ \ mathrm { f } is the height of the level of free convection and z _ \ mathrm { n } is the height of the equilibrium level ( neutral buoyancy ), where T _ \ mathrm { v, parcel } is the virtual temperature of the specific parcel, where T _ \ mathrm { v, env } is the virtual temperature of the environment, and where g is the sounding diagram ( e . g ., a Skew-T log-P diagram ) using air temperature and dew point data usually measured by a weather balloon.
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