Using the Weather Research and Forecasting (WRF) Model for Precipitation Forecasting in an Andean Region with Complex Topography

The Weather Research and Forecasting (WRF) model has been successfully used in weather prediction, but its ability to simulate precipitation over areas with complex topography is not optimal. Consequently, WRF has problems forecasting rainfall events over Chilean mountainous terrain and foothills, w...

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Main Authors: Gonzalo Yáñez-Morroni, Jorge Gironás, Marta Caneo, Rodrigo Delgado, René Garreaud
Format: Article
Language:English
Published: MDPI AG 2018-08-01
Series:Atmosphere
Subjects:
Online Access:http://www.mdpi.com/2073-4433/9/8/304
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author Gonzalo Yáñez-Morroni
Jorge Gironás
Marta Caneo
Rodrigo Delgado
René Garreaud
author_facet Gonzalo Yáñez-Morroni
Jorge Gironás
Marta Caneo
Rodrigo Delgado
René Garreaud
author_sort Gonzalo Yáñez-Morroni
collection DOAJ
description The Weather Research and Forecasting (WRF) model has been successfully used in weather prediction, but its ability to simulate precipitation over areas with complex topography is not optimal. Consequently, WRF has problems forecasting rainfall events over Chilean mountainous terrain and foothills, where some of the main cities are located, and where intense rainfall occurs due to cutoff lows. This work analyzes an ensemble of microphysics schemes to enhance initial forecasts made by the Chilean Weather Agency in the front range of Santiago. We first tested different vertical levels resolution, land use and land surface models, as well as meteorological forcing (GFS/FNL). The final ensemble configuration considered three microphysics schemes and lead times over three rainfall events between 2015 and 2017. Cutoff low complex meteorological characteristics impede the temporal simulation of rainfall properties. With three days of lead time, WRF properly forecasts the rainiest N-hours and temperatures during the event, although more accuracy is obtained when the rainfall is caused by a meteorological frontal system. Finally, the WSM6 microphysics option had the best performance, although further analysis using other storms and locations in the area are needed to strengthen this result.
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spelling doaj.art-2d1cd9805de64e6d8592406685a0794e2022-12-21T17:49:34ZengMDPI AGAtmosphere2073-44332018-08-019830410.3390/atmos9080304atmos9080304Using the Weather Research and Forecasting (WRF) Model for Precipitation Forecasting in an Andean Region with Complex TopographyGonzalo Yáñez-Morroni0Jorge Gironás1Marta Caneo2Rodrigo Delgado3René Garreaud4Departamento de Ingeniería Hidráulica y Ambiental, Pontificia Universidad Católica de Chile, Vicuña Mackenna 4860, Macul, Santiago 7820436, ChileDepartamento de Ingeniería Hidráulica y Ambiental, Pontificia Universidad Católica de Chile, Vicuña Mackenna 4860, Macul, Santiago 7820436, ChileDirección Meteorológica de Chile (DMC), Portales 3450, Estación Central, Santiago 9170018, ChileDirección Meteorológica de Chile (DMC), Portales 3450, Estación Central, Santiago 9170018, ChileDepartamento de Geofísica, Centro de Ciencia del Clima y la Resiliencia, Universidad de Chile, Blanco Encalada 2002, Santiago Centro, Santiago 8370449, ChileThe Weather Research and Forecasting (WRF) model has been successfully used in weather prediction, but its ability to simulate precipitation over areas with complex topography is not optimal. Consequently, WRF has problems forecasting rainfall events over Chilean mountainous terrain and foothills, where some of the main cities are located, and where intense rainfall occurs due to cutoff lows. This work analyzes an ensemble of microphysics schemes to enhance initial forecasts made by the Chilean Weather Agency in the front range of Santiago. We first tested different vertical levels resolution, land use and land surface models, as well as meteorological forcing (GFS/FNL). The final ensemble configuration considered three microphysics schemes and lead times over three rainfall events between 2015 and 2017. Cutoff low complex meteorological characteristics impede the temporal simulation of rainfall properties. With three days of lead time, WRF properly forecasts the rainiest N-hours and temperatures during the event, although more accuracy is obtained when the rainfall is caused by a meteorological frontal system. Finally, the WSM6 microphysics option had the best performance, although further analysis using other storms and locations in the area are needed to strengthen this result.http://www.mdpi.com/2073-4433/9/8/304WRF forecastrainfallcomplex topographyAndean watershedflash floods
spellingShingle Gonzalo Yáñez-Morroni
Jorge Gironás
Marta Caneo
Rodrigo Delgado
René Garreaud
Using the Weather Research and Forecasting (WRF) Model for Precipitation Forecasting in an Andean Region with Complex Topography
Atmosphere
WRF forecast
rainfall
complex topography
Andean watershed
flash floods
title Using the Weather Research and Forecasting (WRF) Model for Precipitation Forecasting in an Andean Region with Complex Topography
title_full Using the Weather Research and Forecasting (WRF) Model for Precipitation Forecasting in an Andean Region with Complex Topography
title_fullStr Using the Weather Research and Forecasting (WRF) Model for Precipitation Forecasting in an Andean Region with Complex Topography
title_full_unstemmed Using the Weather Research and Forecasting (WRF) Model for Precipitation Forecasting in an Andean Region with Complex Topography
title_short Using the Weather Research and Forecasting (WRF) Model for Precipitation Forecasting in an Andean Region with Complex Topography
title_sort using the weather research and forecasting wrf model for precipitation forecasting in an andean region with complex topography
topic WRF forecast
rainfall
complex topography
Andean watershed
flash floods
url http://www.mdpi.com/2073-4433/9/8/304
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