Abstract

This study developed a cell-based daily soil water analysis model (CellSW) for evaluating agricultural drought and calculated an agricultural drought index called the “Rainfall Effectiveness Index for Crop” (REIC). The model analyzed a daily soil water balance based on crop types, growth stages, soils, and climate. It adopted the rasterized daily rainfall, daily evapotranspiration, crop coefficient (by crop growth stage), and root depth as input parameters; it also consecutively generated the daily surface layers of the water balance items in each cell, such as the consumptive use, effective rainfall, available soil water, and irrigation requirements. The model was applied in a test area in Illinois and Iowa, targeting corn and soybeans; the soil water balance was analyzed during the growing period from 2000 to 2018. The model calculated the seasonal REIC, defined as the ratio of supply quantity (effective rainfall) to demand quantity (crop evapotranspiration). In addition, the accumulated REIC values were estimated. The REIC was confirmed to accurately reflect drought situations in the relevant areas, based on comparisons with drought records. The cell-based model can be applied to different types of cultivated crops, growth stages, and soil conditions without spatial and temporal limitations, even in mixed farming.

Highlights

  • Drought is a natural disaster with a random nature, and it causes longer, wider, and greater damage than any other natural disaster

  • Drought refers to a state in which the required water cannot be supplied owing to a lack of precipitation; it is classified into meteorological or climatological, agricultural, hydrological, and socioeconomic drought [6]

  • For studies using the soil moisture analysis model, agricultural drought was evaluated by using meteorological data, soil data, and farming data as input data [14,15,16,17]

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Summary

Introduction

Drought is a natural disaster with a random nature, and it causes longer, wider, and greater damage than any other natural disaster. For studies using the soil moisture analysis model, agricultural drought was evaluated by using meteorological data (precipitation and evapotranspiration), soil data (soil properties, field capacity, wilting point, and hydrological soil group), and farming data (cultivation period, crop coefficient, and root depth) as input data [14,15,16,17]. Their spatiotemporal distribution, has mostly been expressed very as limited soil data were used or the soil moisture was estimated by assuming a single crop. Based on the results of the soil water balance, an agricultural drought index (Rainfall Effectiveness Index for Crop (REIC)) was calculated, and the progress and severity of the drought were analyzed

Materials and Methods
Agricultural Drought Index
Study Area
Data Collection and Preprocessing
Change in Soil Water Balance from 2000 to 2018
Conclusions
Full Text
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