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John S. Kain

Researcher at Cooperative Institute for Mesoscale Meteorological Studies

Publications -  25
Citations -  5106

John S. Kain is an academic researcher from Cooperative Institute for Mesoscale Meteorological Studies. The author has contributed to research in topics: Mesoscale meteorology & Weather Research and Forecasting Model. The author has an hindex of 17, co-authored 25 publications receiving 4412 citations.

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The Kain–Fritsch Convective Parameterization: An Update

TL;DR: Modifications to the Kain‐Fritsch convective parameterization evolved from an effort to produce desired effects in numerical weather prediction while also rendering the scheme more faithful to observations and cloud-resolving modeling studies.
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Examination of convection-allowing configurations of the WRF model for the prediction of severe convective weather : The SPC/NSSL spring program 2004

TL;DR: In this article, the utility of the Weather Research and Forecast (WRF) model was evaluated during the 2004 Storm Prediction Center-National Severe Storms Laboratory Spring Program in a simulated severe weather forecasting environment.
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Sensitivity of Several Performance Measures to Displacement Error, Bias, and Event Frequency

TL;DR: In this article, the sensitivity of various accuracy measures to displacement error, bias, and event frequency is analyzed for a simple hypothetical forecasting situation, and a newly devised measure, called the bias-adjusted threat score, does not change with varying event frequency and is relatively insensitive to bias.

A Feasibility Study for Probabilistic Convection Initiation Forecasts Based on Explicit

TL;DR: This study confirms that convection-allowing models with grid spacing ~ 4 km38 represent many aspects of the formation and development of deep convection clouds explicitly and with predictive utility and shows that automated algorithms can skillfully identify the CI process during model integration.
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The melting effect as a factor in precipitation-type forecasting

TL;DR: In this paper, the authors examined the process of atmospheric cooling due to melting precipitation to evaluate its contribution to determining precipitation type and found that melting effect is typically of second-order importance compared to other processes that influence the lower-tropospheric air temperature and hence the type of precipitation that reaches the ground.