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25-m total water content


125-m total water content


255-m total water content


500-m total water content


705-m total water content


950-m total water content


1250-m total water content


1420-m total water content


2000-m total water content


25-m temperature


125-m temperature


255-m temperature


500-m temperature


705-m temperature


950-m temperature


1250-m temperature


1420-m temperature


2000-m temperature


25-m temperature advection


125-m temperature advection


255-m temperature advection


500-m temperature advection


705-m temperature advection


950-m temperature advection


1250-m temperature advection


1420-m temperature advection


2000-m temperature advection


25-m dewpoint temperature


125-m dewpoint temperature


255-m dewpoint temperature


500-m dewpoint temperature


705-m dewpoint temperature


950-m dewpoint temperature


1250-m dewpoint temperature


1420-m dewpoint temperature


2000-m dewpoint temperature


300-mb wind, 1000- to 500-mb thickness


950- to 700-mb buoyancy frequency


300-mb divergence and potential vorticity


700- to 400-mb differential vorticity


850- to 600-mb Eady growth rate


700-mb Ertel PV and Height


850-mb frontogenesis


900- to 700-mb frontogenesis


700-mb Diabatic Heating, Height, and Theta


850-mb Diabatic Heating, Height, and Theta


25-m diabatic heating


125-m diabatic heating


255-m diabatic heating


500-m diabatic heating


705-m diabatic heating


950-m diabatic heating


1250-m diabatic heating


1420-m diabatic heating


2000-m diabatic heating


Sensible Heat Flux


Integrated Vapor Transport and 700-mb Height


Latent Heat Flux


700-mb Q Forcing and Height


850-mb Q Forcing and Height


Moisture Flux


25-m PBL water vapor tendency


125-m PBL water vapor tendency


255-m PBL water vapor tendency


500-m PBL water vapor tendency


25-m water vapor


125-m water vapor


255-m water vapor


500-m water vapor


705-m water vapor


950-m water vapor


1250-m water vapor


25-m water vapor advection


125-m water vapor advection


255-m water vapor advection


500-m water vapor advection


705-m water vapor advection


950-m water vapor advection


1250-m water vapor advection


1420-m water vapor advection


2000-m water vapor advection


700-mb Q Vectors, Temperature, and Height


850-mb Q Vectors, Temperature, and Height


900- to 700-mb QG static stability


950–500-mb Thickness Gradient, Sea-level Pressure


25-m CU temperature tendency


125-m CU temperature tendency


255-m CU temperature tendency


500-m CU temperature tendency


705-m CU temperature tendency


950-m CU temperature tendency


1250-m CU temperature tendency


1420-m CU temperature tendency


2000-m CU temperature tendency


25-m PBL temperature tendency


125-m PBL temperature tendency


255-m PBL temperature tendency


500-m PBL temperature tendency


25-m radiative temperature tendency


125-m radiative temperature tendency


255-m radiative temperature tendency


500-m radiative temperature tendency


705-m radiative temperature tendency


950-m radiative temperature tendency


1250-m radiative temperature tendency


1420-m radiative temperature tendency


2000-m radiative temperature tendency


700-mb Relative Vorticity and Height


850-mb Relative Vorticity and Height


125-m vertical wind


255-m vertical wind


500-m vertical wind


705-m vertical wind


950-m vertical wind


1250-m vertical wind


1420-m vertical wind


2000-m vertical wind












Kyle Ahern

Postdoctoral Research Associate

kkahern@albany.edu


State University of New York, University at Albany

ETEC Building, Room 424D

1220 Washington Ave.

Albany, NY 12226