Chapter 13. Acquisition of Weather Information 10,000 land-based stations, hundreds of ships and buoys; four times a day, airports hourly Upper level:
The High Wind Event of 7 March 2004 in the Piedmont of the Western Carolinas Harry Gerapetritis National Weather Service Greer, SC.
Day 1 Severe Storms Forecasting Jim LaDue – WDTB 08 June, 2005.
Stability & Movement Figure 7.1 A rock, like a parcel of air, that is in stable equilibrium will return to its original position when pushed. If the rock.
Seminar by SSgt Channing Weinmeister. l Clear Air Turbulence (CAT) refers to turbulence caused by relatively strong vertical or horizontal shear in speed.
Lecture 14: Cloud development and forms (Ch 6)
The formation of surface circulation systems
Middle Latitude Cyclones This chapter discusses: 1.The location, vertical structure, and developmental stages of middle latitude cyclones 2.How upper level.
High Impact Event
ETA 6-hr fcst. Valid 18z 02/19/02
Weather Forecasting
1.4 thermal wind balance geostrophic wind hypsometric eqn plug (2) into (1) finite difference expression: this is the thermal wind: an increase in wind.
