基于shap的短期干旱动态研究受到中国昼夜温度变化的干扰

IF 5.9 1区 农林科学 Q1 AGRONOMY
Yao Feng , Fubao Sun , Fa Liu
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引用次数: 0

摘要

短期干旱动态对农业生产和水资源管理至关重要,但作为影响地表能量和水循环的关键气候变量,日温差(DTR)在干旱过程中的复杂作用仍然知之甚少。本研究通过将高分辨率气象数据集(1961-2022)整合到基于SHapley加性解释(SHAP)的归因框架中,量化了DTR对中国不同气气带短期干旱的影响(月尺度标准化降水-蒸散指数,SPEI-1),解决了这一空白。月DTR与SPEI-1呈显著负相关,表明DTR直接加剧了短期干旱条件,这种影响自2000年以来显著增强。DTR通过双重途径影响干旱:通过增加蒸散需求直接加剧干旱,通过与降水和相对湿度(RH)负相关以及与日照时数和风速正相关间接调节干旱。在干旱地区,DTR与降水和相对湿度协同作用加剧干旱,而在潮湿地区,DTR与日照时数正相关,部分缓解干旱严重程度。重要的是,DTR被确定为短期干旱的主要驱动因素,其次是相对湿度和日照时数。DTR每升高1°C, SPEI-1降低0.04 ~ 0.26(加重干旱),而DTR每降低1°C, SPEI-1升高0.03 ~ 0.28(减轻干旱),这在半干旱、干旱和超干旱地区尤为明显。该研究促进了我们对DTR在短期干旱动态中的多方面作用的理解,并强调了迫切需要有针对性的适应策略,如适应性灌溉计划和水资源分配,以缓解干旱加剧,特别是在生态脆弱地区。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
SHAP-powered insights into short-term drought dynamics disturbed by diurnal temperature range across China
Short-term drought dynamics are critical for agricultural production and water resource management, yet the complex role of diurnal temperature range (DTR), as a key climate variable influencing surface energy and water cycles, remains poorly understood in drought processes. This study addresses this gap by integrating a high-resolution meteorological dataset (1961–2022) into a SHapley Additive exPlanations (SHAP)-based attribution framework, quantifying DTR’s impacts on short-term drought (the monthly-scale standardized precipitation-evapotranspiration index, SPEI-1) across China’s diverse climatic zones. A significant negative correlation between monthly DTR and SPEI-1 indicates that DTR directly intensifies short-term drought conditions, an effect that has strengthened significantly since 2000. DTR influences drought through dual pathways: direct exacerbation via enhanced evapotranspiration demand and indirect modulation through negative associations with precipitation and relative humidity (RH) and positive links with sunshine duration and wind speed. In arid regions, DTR interacts synergistically with precipitation and RH to exacerbate drought, whereas in humid regions, DTR’s positive association with sunshine duration partially mitigates drought severity. Importantly, DTR is identified as the primary driver of short-term drought, followed by RH and sunshine duration. A 1°C increase in DTR reduces SPEI-1 by −0.04 to −0.26 (worsening drought), while a 1°C decrease in DTR increases SPEI-1 by 0.03–0.28 (alleviating drought), which is particularly pronounced in semi-arid, arid, and hyper-arid regions. This study advances our understanding of DTR’s multifaceted role in short-term drought dynamics and highlights the urgent need for targeted adaptation strategies, such as adaptive irrigation scheduling and water resource allocation, to mitigate drought intensification, particularly in ecologically vulnerable regions.
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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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