Abstract

Planning agricultural procedures needs to take into account meteorological conditions. However, because of high associated costs, the density of meteorological stations is often not enough to cover all the cultivated or potentially cultivated areas. In this article we present a methodology to estimate seasonal maximum and minimum mean temperature in cultivated area using data registered in a sole or a few meteorological stations. The procedure is based on mesoscale modeling, which allows meteorological variables to be spatially distributed considering synoptic data and local characteristics. Simulated daily cycle of temperature was compared with data registered at six meteorological stations located in the cultivated floor of the semiarid Limari Valley (Chile, 31°S). Although in some cases the simulated temperature differs in about 2°C with the observed one, a good fit between model results and experimental data was observed. Using the simulated seasonal minimum and maximum mean temperature fields, maps of temperature differences with respect to a reference station were drawn. In order to observe the influence of the orography on the lapse rate around a station, the methodology was applied for two reference stations located in places with different orographic characteristics. Results for winter and summer seasons are shown. These generated maps can be used by farmers and agricultural planners to obtain information of seasonal minimum and maximum mean temperature from a station in any site of the cultivated area. This technique is a good alternative to obtain meteorological information at low costs, contributing to territorial planning for climate resilient agriculture sustainability.

Highlights

  • Agricultural productivity is severely affected by meteorological parameters such as rainfall, wind speed, solar radiation and air temperature (Hatfield et al, 2011)

  • In this article we report a methodology based on atmospheric modeling, which allows the estimation of temperature over an area from data registered at a meteorological station

  • In order to estimate the temperature from a reference station (RS), we evaluated the field of temperature difference ΔT (x, y) with respect to it over the entire study site

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Summary

Introduction

Agricultural productivity is severely affected by meteorological parameters such as rainfall, wind speed, solar radiation and air temperature (Hatfield et al, 2011). Because of the close relationship between meteorology and yield production, knowing the meteorological characteristics of a site could help the selection of crops and cultivars best adapted to the area. Farmers often install meteorological stations within their cultivated area. It is an expensive undertaking, and currently many cultivable places do not possess a sufficient number of meteorological stations. For this reason, farmers use the nearby station to get meteorological information. The validity of this procedure depends on spatial distribution of the meteorological variable in the area (Gomez et al, 2008; Lookingbill & Urban, 2003), factors for which confidence data are generally not known

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