Access the full text.
Sign up today, get DeepDyve free for 14 days.
M. Weisman, J. Klemp (1982)
The Dependence of Numerically Simulated Convective Storms on Vertical Wind Shear and BuoyancyMonthly Weather Review, 110
J. Kain, J. Fritsch (1992)
The role of the convective “trigger function” in numerical forecasts of mesoscale convective systemsMeteorology and Atmospheric Physics, 49
F. Baer (2000)
Numerical weather predictionAdv. Comput., 52
J. Kain, J. Fritsch (1993)
Convective parameterization for mesoscale models : The Kain-Fritsch Scheme
K. Knupp (1989)
Numerical Simulation of Low-Level Downdraft Initiation within Precipitating Cumulonimbi: Some Preliminary ResultsMonthly Weather Review, 117
H. Bluestein, C. Parks (1983)
A Synoptic and Photographic Climatology of Low-Precipitation Severe Thunderstorms in the Southern PlainsMonthly Weather Review, 111
Brad Ferrier, J. Simpson, W. Tao (1996)
Factors Responsible for Precipitation Efficiencies in Midlatitude and Tropical Squall SimulationsMonthly Weather Review, 124
R. Srivastava (1987)
A model of intense downdrafts driven by the melting and evaporation of precipitationJournal of the Atmospheric Sciences, 44
David Blanchard (1998)
Assessing the vertical distribution of convective available potential energyWeather and Forecasting, 13
(2001)
Verification of mesoscale features in NWP models. Preprints
R. Wakimoto (1985)
Forecasting Dry Microburst Activity over the High PlainsMonthly Weather Review, 113
E. Rasmussen, David Blanchard (1998)
A Baseline Climatology of Sounding-Derived Supercell and Tornado Forecast ParametersWeather and Forecasting, 13
R. Johns, C. Doswell (1992)
Severe Local Storms ForecastingWeather and Forecasting, 7
J. Kain, J. Fritsch (1990)
A One-Dimensional Entraining/Detraining Plume Model and Its Application in Convective ParameterizationJournal of the Atmospheric Sciences, 47
K. Knupp, W. Cotton (1985)
Convective cloud downdraft structure: An interpretive surveyReviews of Geophysics, 23
Z. Janjic (1994)
The Step-Mountain Eta Coordinate Model: Further Developments of the Convection, Viscous Sublayer, and Turbulence Closure SchemesMonthly Weather Review, 122
T. Black (1994)
The new NMC mesoscale Eta Model: description and forecast examplesWeather and Forecasting, 9
J. Fritsch, C. Chappell, L. Hoxit (1976)
The Use of Large-Scale Budgets for Convective ParameterizationMonthly Weather Review, 104
(1998)
Considerations for the implementation of a convective parameterization scheme in an operational mesoscale model
C. Cohen (2000)
A Quantitative Investigation of Entrainment and Detrainment in Numerically Simulated Cumulonimbus CloudsJournal of the Atmospheric Sciences, 57
(1998)
The operational RUC-2
Parameterized updraft mass flux, available as a unique predictive field from the Kain–Fritsch (KF) convective parameterization, is presented as a potentially valuable predictor of convective intensity. The KF scheme is described in some detail, focusing on a version that is currently being run semioperationally in an experimental version of the Eta Model. It is shown that updraft mass flux computed by this scheme is a function of the specific algorithm that it utilizes and is very sensitive to the thermodynamic characteristics of input soundings. These same characteristics appear to be related to the severity of convection, suggesting that updraft mass flux predicted by the KF scheme has value for predicting severe weather. This argument is supported by anecdotal evidence and a case study.
Weather and Forecasting – American Meteorological Society
Published: Mar 28, 2002
Read and print from thousands of top scholarly journals.
Already have an account? Log in
Bookmark this article. You can see your Bookmarks on your DeepDyve Library.
To save an article, log in first, or sign up for a DeepDyve account if you don’t already have one.
Copy and paste the desired citation format or use the link below to download a file formatted for EndNote
Access the full text.
Sign up today, get DeepDyve free for 14 days.
All DeepDyve websites use cookies to improve your online experience. They were placed on your computer when you launched this website. You can change your cookie settings through your browser.