Abstract

In atmospheric modeling, an accurate representation of land cover is required because such information impacts water and energy budgets and, consequently, the performance of models in simulating regional climate. This study analyzes the impact of the land cover data on an operational weather forecasting system using the Weather Research and Forecasting (WRF) model for central Mexico, with the aim of improving the quality of the operative forecast. Two experiments were conducted using different land cover datasets: a United States Geological Survey (USGS) map and an updated North American Land Change Monitoring System (NALCMS) map. The experiments were conducted as a daily 120 h forecast for each day of January, April, July, and September of 2012, and the near-surface temperature, wind speed, and hourly precipitation were analyzed. Both experiments were compared with observations from meteorological stations. The statistical analysis of this study showed that wind speed and near-surface temperature prediction may be further improved with the updated and more accurate NALCMS dataset, particularly in the forecast covering 48 to 72 h. The Root Mean Square Error (RMSE) of the average wind speed reached a maximum reduction of up to 1.2 m s−1, whereas for the near-surface temperature there was a reduction of up to 0.6 °C. The RMSE of the average hourly precipitation was very similar between both experiments, however the location of precipitation was modified.

Highlights

  • The rapid expansion of urban areas or urbanization represents one of the most notable human-caused transformations of our planet [1,2]

  • Urbanization leads to land use and land cover changes (LULCC) and modifies the biogeophysical properties of the land surface, including the albedo, emissivity, soil moisture, and surface roughness length

  • The absolute difference was calculated between the North American Land Change Monitoring System (NALCMS) and United States Geological Survey (USGS) experiments

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Summary

Introduction

The rapid expansion of urban areas or urbanization represents one of the most notable human-caused transformations of our planet [1,2]. Modifications in biophysical properties lead to changes in the surface flux, atmospheric circulation, and surface energy budget [3,4,5,6,7,8,9,10]. When the surface energy budget is altered, fluxes in heat, moisture, and momentum within the planetary boundary layer (PBL) are directly affected [8]. Local and regional wind and other climate variables are subsequently affected due to horizontal variations in the turbulent sensible heat flux and PBL depth [8,11,12,13]. The changes in the physical properties can impact the thermal inertia/heat capacity of the land surface [14].

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