'300 mb' presentation slideshows

The Extreme East-Central Missouri Flash Flood of 6-7 May 2000 James T. Moore, John P. Gagan

The Extreme East-Central Missouri Flash Flood of 6-7 May 2000 James T. Moore, John P. Gagan Cooperative Institute for Precipitation Systems Department of Earth and Atmospheric Sciences Saint Louis University and Fred H. Glass NWSFO St. Charles, MO.

978 views • 77 slides

Mapping the Earth

Mapping the Earth. Differentiate between planimetric and hypsometric maps List and recognize the ways in which 3 dimensions can be portrayed on a paper (2 dimensional) map. Define/describe map projections Identify common projection shapes Define/describe an undevelopable surface

682 views • 56 slides

Mesoscale Gravity Waves

Mesoscale Gravity Waves. MEA 444 January 20, 2005. Outline. Gravity Wave Theory Overview Numerical Model Description Synoptic Overview Uccellini and Koch (1987) Synoptic Pattern Surface & 300mb Generation Mechanisms Moist Convection Geostrophic Adjustment Shearing Instability.

676 views • 38 slides

Welcome

381 views • 31 slides

409 views • 29 slides

Using the SPoRT MET Scripts to Assess the WRF EMS for a Southeast Texas Heavy Rainfall Event

Using the SPoRT MET Scripts to Assess the WRF EMS for a Southeast Texas Heavy Rainfall Event Patrick Blood and Lance Wood. 19 Z. SPoRT Model Simulation Matrix Cold Season Heavy Rainfall - WFO Houston Case Study November 8-9, 2011 Andrew Molthan.

267 views • 26 slides

Adiabatic Processes

1.27k views • 25 slides

PRESSURE ALOFT

351 views • 25 slides

Further development of a model for a broad range of spatial and temporal scales Zavisa Janjic

Further development of a model for a broad range of spatial and temporal scales Zavisa Janjic. NMM-B Dynamical Core. Nonhydrostatic Multiscale Model on B grid (N M M-B) Further evolution of WRF NMM (Nonhydrostatic Mesoscale Model)

415 views • 23 slides

The April 18 th 2009 Extreme Rain Event Presentation by Lance Wood

The April 18 th 2009 Extreme Rain Event Presentation by Lance Wood. My house. Image Courtesy: Galveston Daily News. Friendswood, TX. Taylor Lake Village, TX. The April 18 th 2009 Extreme Rain Event. 19 Z. The April 18 th 2009 Extreme Rain Event. 24 Hour Rainfall.

331 views • 18 slides

The quasi-geostrophic omega equation (see Bluestein, Volume I; eq. 5.6.14

The quasi-geostrophic omega equation (see Bluestein, Volume I; eq. 5.6.14. ( ? 2 + ( f 0 2 / ?)? 2 /?p 2 ) ? = ( -f 0 / ?) ? / ? p{-v g ?? p ( ? g + f )} + (-R/ ?p) ? 2 p {v g ? ? p T} + (-R/ ?p) ? 2 p {1/C p (dQ/dt)} + ( -f 0 / ?) ? / ? p{k ? ? x F}. Where

379 views • 15 slides

Geostrophic and thermal wind

Geostrophic and thermal wind. Reminder. Geostrophic wind in pressure coordinates In the free atmosphere, wind is usually close to geostrophic . The departure from geostrophy is the ageostrophic wind Convergence is due to the ageostrophic wind. Why does wind increase with height?.

305 views • 7 slides

Geostrophic and thermal wind

130 views • 5 slides