Technical Report, Issues 134-141 |
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Page 85
... instability is consistently satisfied , is shown in Figure 21 from T = 9 through T = 1 . The q profile maintains nearly the same shape throughout with a maximum of positive potential vorticity on the anticyclonic side of the jet . This ...
... instability is consistently satisfied , is shown in Figure 21 from T = 9 through T = 1 . The q profile maintains nearly the same shape throughout with a maximum of positive potential vorticity on the anticyclonic side of the jet . This ...
Page 98
... instability with its vorticity transport requirements could lead to overshooting which is still stable . Consideration of the potential vorticity on isentropic surfaces and the further investigation of sufficient conditions for instability ...
... instability with its vorticity transport requirements could lead to overshooting which is still stable . Consideration of the potential vorticity on isentropic surfaces and the further investigation of sufficient conditions for instability ...
Page 121
... instability . Furthermore , since this moisture is greater all the way to cloud base and slightly above , a rising parcel will entrain more moist air on hail days than on no hail days and will retain its instability . The air above 400 ...
... instability . Furthermore , since this moisture is greater all the way to cloud base and slightly above , a rising parcel will entrain more moist air on hail days than on no hail days and will retain its instability . The air above 400 ...
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advection aerosol air mass ALTITUDE amplitude analysis annulus Atmospheric Scienc PAPER Atmospheric Science average Boulder Colorado State University computed Continental Divide convective cycle decrease Denver dew point diameter difference eddy equation Figure flights flow forecasting Fort Collins GMT November gradient hail days hail intensity hailstones hailstorm haze profiles heat transfer height horizontal indicated instability isotach January kinetic energy lapse rate lee wave lifted index lower magnitude maximum mean measured Meteorological moisture mountain northeastern Colorado NUMBER OF PARTICLES observed ozone ozone sensor parameter patterns photograph potential energy potential temperature potential vorticity precipitation pressure proximity soundings radar radar echo radiosonde rawinsonde Raymer reflectivity region relative vorticity satellite shown shows Spectral storm surface synoptic Table temperature profiles term tornado tornado environment tropopause troposphere updraft upper vacillation values variation vertical motion vertical velocity vertical wind shear wave clouds wavelength wind field zonal