Colorado State University. Department of Atmospheric Science.
Author
Series
Atmospheric science paper volume no. 440
Pub. Date
1989.
Description
The concept of "moist available energy," defined by Lorenz is applied to study the potential energy available for cumulus convection in a conditionally unstable atmosphere.
5) The influence of forest fire induced albedo differences on the generation of mesoscale circulations
Author
Series
Atmospheric science paper volume no. 527
Pub. Date
1993.
Description
The development of a mesoscale circulation by the thermal contrast between a fire burned area surrounded by untouched vegetation was simulated by the Regional Atmospheric Modeling System (RAMS) in order to show the circulation's ability to generate clouds and precipitation.
Author
Series
Atmospheric science paper volume no. 749
Pub. Date
2004.
Description
This research offers a new methodology for forecasting extended range ENSO events, utilizing global data and a statistical model.
Author
Series
Atmospheric science paper volume no. 341
Pub. Date
1982.
Description
The net influence of sub-grid or smaller unresolvable scale processes (which cannot be directly detected from conventional observations) on the tangential momentum field in tropical cyclones has been calculated as a residual from the grid-scale momentum budgets of sixteen rawinsonde composite data sets.
Author
Series
Atmospheric science paper volume no. 114
Pub. Date
1967.
Description
A global observational study of atmospheric conditions associated with tropical disturbance and storm development is presented.
Author
Series
Atmospheric science paper volume no. 307
Pub. Date
1979.
Description
A new approach to the problem of deducing wind speed and pressure around tropical cyclones is presented.
Author
Series
Atmospheric science paper volume no. 537
Pub. Date
1993.
Description
A dynamic version of the two dimensional kinematic cloud model of Rutledge and Houze (1987) has been developed to investigate the effect of microphysics on circulations within the stratiform region associated with mesoscale convective systems. The design of the model allows for specified inputs of hydrometeors, water vapor and heat from the convective region.