R
Roy Rasmussen
Researcher at National Center for Atmospheric Research
Publications - 198
Citations - 18352
Roy Rasmussen is an academic researcher from National Center for Atmospheric Research. The author has contributed to research in topics: Precipitation & Snow. The author has an hindex of 54, co-authored 190 publications receiving 15059 citations. Previous affiliations of Roy Rasmussen include National Oceanic and Atmospheric Administration & University of California, Los Angeles.
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The Changing Character of Precipitation
TL;DR: In this article, precipitation intensity, duration, frequency, and phase are as much of concern as total amounts, as these factors determine the disposition of precipitation once it hits the ground and how much runs off.
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Explicit Forecasts of Winter Precipitation Using an Improved Bulk Microphysics Scheme. Part II: Implementation of a New Snow Parameterization
TL;DR: In this article, a new bulk microphysical parameterization (BMP) was developed for use with the Weather Research and Forecasting (WRF) Model or other mesoscale models.
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Explicit Forecasts of Winter Precipitation Using an Improved Bulk Microphysics Scheme. Part I: Description and Sensitivity Analysis
TL;DR: In this paper, the authors evaluated the sensitivity of winter precipitation to various aspects of a bulk, mixed-phase microphysical parameterization found in three widely used mesoscale models [the fifth-generation Pennsylvania State University-National Center for Atmospheric Research Mesoscale Model (MM5), the Rapid Update Cycle (RUC), and the Weather Research and Forecast (WRF) model].
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Explicit forecasting of supercooled liquid water in winter storms using the MM5 mesoscale model
TL;DR: In this article, an explicit microphysical parametrization including ice physics was developed for use in the NCAR/Penn State Mesoscale Model Version 5 (MM5), which includes three options of increasing complexity to represent the hydrometeor species.
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The future intensification of hourly precipitation extremes
TL;DR: In this paper, the authors used observations and high-resolution modeling to show that rainfall changes related to rising temperatures depend on the available atmospheric moisture, and that the scaling rates between extreme precipitation and temperature are strongly dependent on the region, temperature, and moisture availability.