Heterogeneity analysis of main driving factors affecting potential evapotranspiration changes across different climate regions

被引:9
作者
Liu, Wenhui [1 ,2 ]
Zhang, Baozhong [1 ]
Wei, Zheng [1 ]
Wang, Yaqi [1 ]
Tong, Ling [2 ]
Guo, Jingyang [1 ]
Han, Xin [1 ,3 ]
Han, Congying [1 ]
机构
[1] China Inst Water Resources & Hydropower Res, State Key Lab Simulat & Regulat Water Cycle River, Beijing 100038, Peoples R China
[2] China Agr Univ, Coll Water Resources & Civil Engn, Beijing 100083, Peoples R China
[3] Tianjin Agr Univ, Coll Water Conservancy Engn, Tianjin 300392, Peoples R China
基金
中国国家自然科学基金;
关键词
Multi-time scale; Potential evapotranspiration; Sensitivity coefficient; Contribution amount; Climate regions; REFERENCE CROP EVAPOTRANSPIRATION; PENMAN-MONTEITH; METEOROLOGICAL FACTORS; SENSITIVITY-ANALYSIS; ARID REGION; CHINA; IRRIGATION; VARIABLES; IMPACTS; TREND;
D O I
10.1016/j.scitotenv.2023.168991
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Exploring the influencing factors of potential evapotranspiration (PET) is of great significance for further understanding the causes of climate change and improving agricultural irrigation efficiency. In this study, modified Mann-Kendall analysis was used to elucidate the temporal variation characteristics of meteorological factors and PET based on a dataset from 710 meteorological stations in China. Furthermore, we revealed the main factors that influence the temporal and climate heterogeneity of PET by combining sensitivity analysis with the contribution analysis method. The results showed that 1) climate factors and PET exhibited trend changes on a yearly scale, with slope variation ranges of temperature (T), relative humidity (RH), net radiation (RN), wind speed (U) and PET of 0.03-0.04 degrees C/a, 0.03-0.08 %/a, 0.001-0.007[MJ/(m2/day)]/a, -0.005 to -0.012(m/s)/a and - 0.30-0.38 mm/a, respectively. 2) The sensitivity coefficient fluctuated greatly inter-annually, but the trend was more pronounced inter-annually. Most sensitive factor for PET was RN in hyperarid (HAR), arid (AR) andsemiarid regions (SAR), while it changed to RH in semihumid (SHR) and humid regions (HR). PET was more sensitive to RN in dry and relatively wet hot seasons, while it changed to RH during wet and relatively dry cold seasons. 3) PET changes were determined by the relative changes and the sensitivity coefficient, and significant temporal heterogeneity was observed. In HAR, AR, SAR and SHR, the relative changes in T and U result in higher contributions. In HR, PET changes were primarily caused by its higher sensitivity to RH and RN. 4) In dry region and humid-cold seasons, the bigger relative changes of climate factors were the main drivers affecting PET changes, but in humid region and arid-hot seasons, the they were determined by the strong nonlinear relationship between PET and factors. This finding holds great significance for the scientific understanding of the evolution mechanism of PET under changing environments.
引用
收藏
页数:15
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