Meso-scale Atmospheric Circulations |
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Page 57
... troposphere and which dies away above , is not at all sensitive to the upper boundary level condition . They acknowledged that lee waves in the stratosphere and upper troposphere could occur and that different boundary conditions had to ...
... troposphere and which dies away above , is not at all sensitive to the upper boundary level condition . They acknowledged that lee waves in the stratosphere and upper troposphere could occur and that different boundary conditions had to ...
Page 58
... troposphere to within an accuracy of 2 km : but once again , amplitude calculations were difficult to verify . One of the few analyses to employ both the analytical , exponential model and numerical methods also used satellite pictures ...
... troposphere to within an accuracy of 2 km : but once again , amplitude calculations were difficult to verify . One of the few analyses to employ both the analytical , exponential model and numerical methods also used satellite pictures ...
Page 100
... Troposphere Z1 stable layer N1 U = U1 ( 1 + a , Z ) Zo = 0 U2 density FIG . 49. Density and velocity profiles in a three - layer incompressible atmosphere with constant stability and linear shear in each layer . The three layers ...
... Troposphere Z1 stable layer N1 U = U1 ( 1 + a , Z ) Zo = 0 U2 density FIG . 49. Density and velocity profiles in a three - layer incompressible atmosphere with constant stability and linear shear in each layer . The three layers ...
Common terms and phrases
airflow amplitude analysis appear areas associated atmos atmosphere bands boundary Browning cells changes chapter characteristics circulation clearly closed cloud cold component considered continuity convection cyclones density depth direction distance distribution downdraught downslope echo effects equation exist Figure flow force frequently front gravity waves ground heat height horizontal important increase initial inland later layer maximum mean mechanism meso-scale motion mountain moved noted observations occurred onset particular period positive potential precipitation pressure pressure gradient radar rainbands relative represent scale sea breeze severe shear shown shows side simulated slope Source stability storm strong structure studies suggested surface Table temperature theoretical theory tropical updraught upper valley valley wind values variation velocity vertical warm waves wind speed