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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