'Thermal advection' presentation slideshows

Quasi-geostrophic theory (Continued)

Quasi-geostrophic theory (Continued). John R. Gyakum. The quasi-geostrophic omega equation:. ( s ? 2 + f 0 2 ? 2 /?p 2 ) ? = f 0 ? / ? p{v g ?? (1/ f 0 ? 2 ? + f )} + ? 2 {v g ? ? (- ?? / ? p)}+ ? 2 (heating) +friction. The Q-vector form of the quasi-geostrophic omega equation.

579 views • 20 slides

METR 2413 31 March 2004

METR 2413 31 March 2004. Dynamics II: Thermal wind and thermal advection. Review. Hydrostatic balance Ideal gas law p = ? R d T v , ? = p / R d T v Take layer average virtual temperature , R and g as constants and integrate LHS. Thickness.

289 views • 18 slides

Conservation of PV

253 views • 17 slides

Quiz 07

B. A. Quiz 07. Radar Scan Mode for the large radar image: CAPPI or PPI ? Hint, both radar images are for the same time. Why is the Doppler Image showing no precipitation near the radar? Pick from the list of possible options. No Pcpn 3.5 Cone of Silence Virga Hole Attenuation

309 views • 17 slides

METR 2413 20 February 2004

METR 2413 20 February 2004. Thermal Advection Since we do not directly measure vertical motions, the analysis of thermal advection on maps will provide a very useful tool for determining the vertical motions currently occurring in the atmosphere. Why use Temp. Advection?.

233 views • 12 slides

Observed

Probing the Baiu Dynamics. A. Kuwano-Yoshida and B. Taguchi (JAMSTEC), and S.P. Xie (IPRC). Observed. CFES mini. AFES. Monthly mean rainfall in mm/day (shading) and SST (contours) in observations, CFES and AFES runs.

153 views • 1 slides