Slide 1Chapter 10 Geostrophic Balance Slide 2 (1) Wind and Height Gradients On a contour analysis of a pressure surface: Strong winds associated with contours close together;…
Slide 1Chapter 10 Geostrophic Balance Slide 2 (1) Wind and Height Gradients On a contour analysis of a pressure surface: Strong winds associated with contours close together;…
Objectives: Types of blocking ridges Storms that typically accompany the block. Numerical models and ensembles forecast these ridges as much as 10 days in advance of occurrence.…
Objectives: Types of blocking ridges Storms that typically accompany the block. Numerical models and ensembles forecast these ridges as much as 10 days in advance of occurrence.…
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…