Coherence of Warm-Season Continental Rainfall in Numerical Weather Prediction Models
Open Access
- 1 November 2003
- journal article
- Published by American Meteorological Society in Monthly Weather Review
- Vol. 131 (11) , 2667-2679
- https://doi.org/10.1175/1520-0493(2003)131<2667:cowcri>2.0.co;2
Abstract
A recent study by Carbone et al. revealed “episodes” of warm-season rainfall over North America characterized as coherently propagating signals often linking multiple mesoscale convective systems over spatial scales of 1000–3000 km and timescales of 1–3 days. The present study examines whether these propagating signals are found in two numerical weather prediction (NWP) models commonly used today, namely, the Eta Model from the National Centers for Environmental Prediction and the newly developed Weather Research and Forecast (WRF) model. The authors find that the diurnal cycle of rainfall over much of the United States east of the Rockies is poorly represented, particularly over the central United States, where a nocturnal rainfall maximum is observed. Associated with this nocturnal maximum is an axis of propagating rainfall emanating from the western High Plains in the late afternoon, extending across the Midwest overnight, and occasionally continuing to the Appalachians on the second day. This... Abstract A recent study by Carbone et al. revealed “episodes” of warm-season rainfall over North America characterized as coherently propagating signals often linking multiple mesoscale convective systems over spatial scales of 1000–3000 km and timescales of 1–3 days. The present study examines whether these propagating signals are found in two numerical weather prediction (NWP) models commonly used today, namely, the Eta Model from the National Centers for Environmental Prediction and the newly developed Weather Research and Forecast (WRF) model. The authors find that the diurnal cycle of rainfall over much of the United States east of the Rockies is poorly represented, particularly over the central United States, where a nocturnal rainfall maximum is observed. Associated with this nocturnal maximum is an axis of propagating rainfall emanating from the western High Plains in the late afternoon, extending across the Midwest overnight, and occasionally continuing to the Appalachians on the second day. This...Keywords
This publication has 12 references indexed in Scilit:
- Properties of the Convection Scheme in NCEP's Eta Model that Affect Forecast Sounding InterpretationWeather and Forecasting, 2002
- Inferences of Predictability Associated with Warm Season Precipitation EpisodesJournal of the Atmospheric Sciences, 2002
- Coupling an Advanced Land Surface–Hydrology Model with the Penn State–NCAR MM5 Modeling System. Part I: Model Implementation and SensitivityMonthly Weather Review, 2001
- Observed and model‐simulated diurnal cycles of precipitation over the contiguous United StatesJournal of Geophysical Research: Atmospheres, 1999
- The WSR-88D Rainfall AlgorithmWeather and Forecasting, 1998
- Nonlocal Boundary Layer Vertical Diffusion in a Medium-Range Forecast ModelMonthly Weather Review, 1996
- Evaluation of 33 Years of Quantitative Precipitation Forecasting at the NMCWeather and Forecasting, 1995
- The New NMC Mesoscale Eta Model: Description and Forecast ExamplesWeather and Forecasting, 1994
- The Step-Mountain Eta Coordinate Model: Further Developments of the Convection, Viscous Sublayer, and Turbulence Closure SchemesMonthly Weather Review, 1994
- Interaction between soil hydrology and boundary-layer developmentBoundary-Layer Meteorology, 1987