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Assessment of Drought Impact on Main Cereal Crops Using a Standardized Precipitation Evapotranspiration Index in Liaoning Province, China

机译:利用标准的降水蒸散指数评估干旱对主要谷物的影响

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Global warming has resulted in increasingly frequent and severe drought and/or precipitation events. Severe drought limits crop water availability and impacts agricultural productivity and socioeconomic development. To quantify drought-induced yield loss during the main crop stages in Liaoning province, China, aspects of drought episodes (magnitude, duration, and frequency) were investigated during the period 1960–2015 using the Standardized Precipitation Index (SPI) and the Standardized Precipitation Evapotranspiration Index (SPEI), respectively. Then the relationship between the SPI/SPEI and the standardized yield residuals series (SYRS), and the drought-induced yield loss were analyzed for maize, rice, sorghum, soybean, and millet. Liaoning underwent a province-wide increase in temperature, reduced precipitation, and reduced reference crop evapotranspiration. As expected, Liaoning experienced province-wide meteorological drying trends during the main crop growth stages, while the drought frequency, duration, and magnitude were not as serious as revealed by using the SPI. As compared to the SPI, the SPEI considering potential evapotranspiration explained 39%–78% yield variability of SYRS and evaluated the drought-induced yield loss more accurately. The increased drought frequency mainly affected the rain-fed crops (maize, sorghum, soybean, and millet), while it did not reduce irrigated rice production. No major impact was exerted on the rain-fed crops caused by mild drought. However, severe drought (SPEI < ?1.0) markedly reduced yield performance, in particular at the anthesis-silking stage for maize, the jointing-booting stage for sorghum, the flowering-podding stage for soybean, and the sowing-milking stage for millet. It is concluded that the SPEI is a more useful measure for the identification of drought episodes and the assessment of drought impact on agricultural production in Liaoning province.
机译:全球变暖导致越来越频繁和严重的干旱和/或降水事件。严重的干旱限制了作物的水供应,并影响了农业生产力和社会经济发展。为了量化中国辽宁省主要农作物时期干旱引起的单产损失,使用标准降水指数(SPI)和标准降水对1960-2015年期间干旱事件的各个方面(幅度,持续时间和频率)进行了调查。蒸散指数(SPEI)分别。然后分析了SPI / SPEI与标准化单产残差系列(SYRS)之间的关系,以及干旱引起的玉米,水稻,高粱,大豆和小米的单产损失。辽宁省气温升高,降水减少,参考作物的蒸散量减少。不出所料,辽宁在主要农作物生长阶段经历了全省范围的气象干旱趋势,而干旱频率,持续时间和强度没有使用SPI所显示的严重。与SPI相比,考虑潜在蒸散的SPEI解释了SYRS的39%–78%的产量变异性,并更准确地评估了干旱引起的产量损失。干旱频率增加主要影响雨育作物(玉米,高粱,大豆和小米),但没有减少灌溉水稻的产量。轻度干旱对雨育作物没有产生重大影响。但是,严重干旱(SPEI <1.0)显着降低了产量表现,特别是在玉米的花药剥皮期,高粱的拔节期,大豆的花荚期和小米的播种挤奶期。 。结论是,SPEI是识别辽宁干旱事件和评估干旱对农业生产影响的一种更有用的措施。

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