Study on the driving factors of spring agricultural drought in Northeast China from the perspective of atmosphere and snow cover

IF 5.9 1区 农林科学 Q1 AGRONOMY
Wei Pei , Yi Su , Qiang Fu , Yongtai Ren , Tianxiao Li
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引用次数: 0

Abstract

Drought is closely related to the early stages of the water cycle. Due to the influence of snow cover and soil freezethaw processes, the water cycle process in cold regions presents specific and complex characteristics in the early spring. Therefore, the driving factors of spring drought in cold regions are different from those in warmer regions. This work takes the cold region of Northeast China as the study area. The early spring period was divided into four periods: the prefreezing period, rapid freezing period, stable freezing period, and melting period. Precipitation, evapotranspiration, and snow depth were selected as candidate driving factors in each period. The rough set conditional information entropy method was used to calculate the weights of the driving factors, and the main driving factors were preferably selected. The results indicated that as soil depth increased, the range of drought expanded. Spring drought was mainly concentrated in the western, central, and central western regions of the study area, whereas the northern, eastern, and southeastern regions were relatively humid. The precipitation and evapotranspiration during the prefreezing and melting periods had a considerable impact on spring drought, and for shallow spring drought, the impact of precipitation was greater, whereas the impact of evapotranspiration during deep drought was greater. The impermeability and evaporation suppression function of frozen soil resulted in early water retention in the soil, which in turn affected the soil moisture of the following year. During the rapid freezing period, snow depth was the main factor driving spring drought. The snow during the freezing period helped to suppress soil moisture evaporation, and the infiltration of snowmelt effectively increased the soil moisture content. Studying the driving factors of spring drought can help identify the formation mechanism of agricultural drought in cold regions and provide a reference for disaster prevention.
基于大气和积雪的东北春季农业干旱驱动因素研究
干旱与水循环的早期阶段密切相关。由于积雪和土壤冻融过程的影响,寒区初春水循环过程呈现出特定而复杂的特征。因此,寒区春旱的驱动因素与暖区不同。本文以东北寒区为研究区域。早春期分为预冻期、速冻期、稳冻期和融化期四个阶段。选取降水、蒸散发和雪深作为各时段的候选驱动因子。采用粗糙集条件信息熵法计算驱动因素权重,优选出主要驱动因素。结果表明,随着土壤深度的增加,干旱范围扩大。春季干旱主要集中在研究区的西部、中部和中西部地区,而北部、东部和东南部地区相对湿润。冻融期降水和蒸散发对春旱的影响较大,且浅区春旱受降水影响较大,深区春旱受蒸散发影响较大。冻土的抗渗和抑制蒸发作用导致土壤早期水分滞留,进而影响次年的土壤水分。在速冻期,积雪深度是导致春旱的主要因素。冻结期降雪有助于抑制土壤水分蒸发,融雪的入渗有效地增加了土壤水分含量。研究春季干旱的驱动因素有助于明确寒区农业干旱的形成机制,为防灾减灾提供参考。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Agricultural Water Management
Agricultural Water Management 农林科学-农艺学
CiteScore
12.10
自引率
14.90%
发文量
648
审稿时长
4.9 months
期刊介绍: Agricultural Water Management publishes papers of international significance relating to the science, economics, and policy of agricultural water management. In all cases, manuscripts must address implications and provide insight regarding agricultural water management.
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