'200 hpa' diaporamas de présentation

The Persistence and Dissipation of Lake Michigan-Crossing Mesoscale Convective Systems

Nicholas D. Metz* and Lance F. Bosart # * Department of Geoscience, Hobart and William Smith Colleges # Department of Atmospheric and Environmental Sciences, University at Albany E-mail: nmetz@hws.edu Support Provided by the Provost Office at Hobart and William Smith Colleges

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Nicholas D. Metz and Lance F. Bosart Department of Atmospheric and Environmental Sciences

Synoptic and Mesoscale Conditions associated with Persisting and Dissipating Mesoscale Convective Systems that Cross Lake Michigan. Nicholas D. Metz and Lance F. Bosart Department of Atmospheric and Environmental Sciences University at Albany/SUNY, Albany, NY 12222

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Chemical Weather with GEM-AQ

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CCMVal overview: The extra-tropical UTLS in chemistry-climate models

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Real time Extended Range Forecast (India Meteorological Department)

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Real time Extended Range Forecast (India Meteorological Department)

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Real time Extended Range Forecast (India Meteorological Department)

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Intraseasonal variations of upper tropospheric water vapor in Asian monsoon region

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Michael J. Bodner AOSC 617 31 March 2006

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MONSOONS

MONSOONS. 200 hPa. 850 hPa. p s (hPa). rainfall (mm day -1 ). U(ms -1 ), T( o C). ? (kg s -1 ). OLR (W per sq. m). 850hPa. Steady, linear shallow water model. 200hPa. 850hPa. 850 hPa. 500hPa. 400hPa. 850hPa. V(p,t) at Dakar. Easterly waves. Thorncroft et al., QJRMS , 1994.

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Motivation

Courtesy: D.Anwender. Motivation. ET of Tropical Cyclones. Reduction in forecast skill. ET of Maemi. Investigation of predictability using ensemble forecasts. Ensemble Spread ? Measure of predictability Different possible development scenarios

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MONSOONS

MONSOONS. 200 hPa. 850 hPa. p s (hPa). rainfall (mm day -1 ). U(ms -1 ), T( o C). ? (kg s -1 ). OLR (W per sq. m). 850hPa. Steady, linear shallow water model. 200hPa. 850hPa. 850 hPa. 500hPa. 400hPa. 850hPa. V(p,t) at Dakar. Easterly waves. Thorncroft et al., QJRMS , 1994.

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Motivation

P-3.4 Wed. October 26, 2005. Motivation Quantify the impact of interannual SST variability on the mean and the spread of Probability Density Function (PDF) of seasonal atmospheric means. Abstract

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