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气候变化背景下黄土高原干湿演变特征及成因分析OACSTPCD

Alterations in drying and wetting spells and their determinants in the Loess Plateau under the influence of climate change

中文摘要英文摘要

[目的]干旱频发对农业生产和生态健康造成了严重影响,探究黄土高原干湿演变特征及其成因.[方法]基于黄土高原 71 个站点获取 1961-2020 年温度、降水量、相对湿度、日照时间、风速等气象数据,采用标准化降水蒸散指数(SPEI)、Mann-Kendall 检验、游程理论等方法,分析了黄土高原 1961-2020 年干湿演变规律及其成因.[结果]1961-2020年,黄土高原地区的温度整体呈明显上升趋势,有变暖趋势,而风速、相对湿度、日照时间呈明显下降趋势.从时间变化来看,降水量呈微弱下降趋势,ET0 呈先上升后下降趋势;从空间变化来看,西北部降水量增加,ET0降低,有变"湿"趋势,而东北部降水量和ET0都呈降低趋势,其干湿变化仍需讨论;从干湿演变规律来看,SPEI在 1999 年之前呈减小趋势,之后呈增大趋势,东南部干旱频率高,干旱历时、干旱严重度、干旱峰值低,极端干旱事件少有发生,西北部情况则与东南部相反;从干湿演变的成因来看,温度增加、降水量增大、ET0减小属于黄土高原干湿演变特征的主要成因,黄土高原整体区域的温度与SPEI相关性较大,降水量和ET0对黄土高原的干湿演变有较大影响,且 ET0 对黄土高原干湿演变规律的影响强于降水量;此外,环流指数与 SPEI的线性相关较弱,表明其对黄土高原的干湿演变影响较小,黄土高原干湿变化与中纬度西风带强弱和太阳黑子活动程度有较弱的相关性.[结论]综上可知,黄土高原从 1960 年开始呈暖干化趋势,1999年后呈暖湿化趋势.

[Objective]Frequent droughts have significantly impacted agricultural productivity and ecological health of the Loess Plateau.This study investigates the characteristics and driving factors of dry-wet evolution in the region.[Method]The analysis was based on meteorological data,including temperature,precipitation,relative humidity,sunshine hours,and wind speed,measured from 1961 to 2020 at 71 weather stations across the Loess Plateau.The changes in wet and dry spells and their underlying determinants were analyzed using standardized precipitation evapotranspiration index(SPEI),Mann Kendall test,and run length theory.[Result]Temporally,temperature showed a significant increase,while wind speed,relative humidity and sunshine hours showed significant decreases from 1961 to 2020.In contrast,precipitation showed a weak decrease,while ET0(reference crop evapotranspiration)exhibited a first increase followed by a decrease during this period.Spatially,the Northwest saw increased precipitation and decreased ET0.Conversely,the Northeast experienced declines in both precipitation and ET0.From 1999 onward,the SPEI showed an initial decrease followed by an increase.The Southeast experienced high drought frequency but with shorter durations and lower severity,extreme drought events in which were rare.In contrast,the Northwest had fewer but more severe and prolonged droughts.Rising temperatures,increasing precipitation and decreasing ET0 were the primary drivers of dry-wet alterations.ET0 had a stronger influence on dryness and wetness patterns than precipitation.The correlation between the mid-latitude westerly belt,sunspot activity,and SPEI was weak,indicating limited influence of large-scale atmospheric and solar factors.[Conclusion]The Loess Plateau showed a warm-drying trend from 1961 to 1999,followed by a warm-wetting trend thereafter.These findings improve our understanding of hydrological changes and help develop mitigating strategies for managing drought and water resources in the region.

郝睿超;王淇葆;王辰;董冰雪;玛尔比亚古丽·斯拉依;张天旭;姚宁

西北农林科技大学 水利与建筑工程学院,陕西 杨凌 712100

大气科学

干湿变化标准化降水蒸散发指数演变特征成因分析黄土高原

dry and wet changesstandardized precipitation evapotranspiration indexevolutionary characteristicscause analysisthe Loess Plateau

《灌溉排水学报》 2024 (012)

74-83 / 10

国家自然科学基金项目(52209070);大学生创新创业训练项目(202210712164)

10.13522/j.cnki.ggps.2023544

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