Journal of Arid Meteorology ›› 2022, Vol. 40 ›› Issue (5): 791-803.DOI: 10.11755/j.issn.1006-7639(2022)-05-0791
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LI Liang(), YANG Zesu(), HE Hang
Received:
2022-09-23
Revised:
2022-10-03
Online:
2022-10-31
Published:
2022-11-10
Contact:
YANG Zesu
通讯作者:
杨泽粟
作者简介:
李梁(2001—),男,学士,主要从事陆面过程研究. E-mail:3011974904@qq.com。
基金资助:
CLC Number:
LI Liang, YANG Zesu, HE Hang. Evapotranspiration-precipitation coupling strength response to hydrothermal factors over northern China[J]. Journal of Arid Meteorology, 2022, 40(5): 791-803.
李梁, 杨泽粟, 何杭. 中国北方蒸散-降水耦合度时空变化与水热因子的关系[J]. 干旱气象, 2022, 40(5): 791-803.
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URL: http://www.ghqx.org.cn/EN/10.11755/j.issn.1006-7639(2022)-05-0791
Fig.2 Spatial distribution of climate state (a, c) and standard deviation (b, d) of annual precipitation (a, b) and evapotranspiration (c, d) in northern China (Unit: mm)
Fig.3 Spatial distribution of total evapotranspiration-precipitation coupling strength in northern China (the circle dot areas passing α=0.05 significance test. the same as below)
Fig.4 Spatial distribution of evapotranspiration-precipitation coupling strength in northern China in winter (a), spring (b), summer (c) and autumn (d)
Fig.6 The spatial distribution of climate state (a, c) and standard deviation (b, d) of soil moisture (a,b) and air temperature (c, d) (Unit: ℃) in northern China
Fig.7 The scatter plots of evapotranspiration-precipitation coupling strength with average soil moisture (a), average temperature (b), soil moisture standard deviation (c) and temperature standard deviation (d)
Fig.8 Multiple linear regression of evapotranspiration-precipitation coupling strength with average soil moisture and average temperature (a), and soil moisture standard deviation and temperature standard deviation (b)
Fig.9 Intra-annual (a) and inter-annual (b) fluctuations of evapotranspiration-precipitation coupling strength in different dry and wet climate background regions
Fig.10 Monthly change of climate state (a, c) and standard deviation (b, d) of soil moisture (a, b), temperature (c, d)in different dry and wet climate background regions
Fig.11 Pearson correlation coefficients of evapotranspiration-precipitation coupling strength with average soil moisture, average temperature, soil moisture standard deviation, temperature standard deviation (a), and complex correlation coefficients of evapotranspiration-precipitation coupling strength with average soil moisture and average temperature, and with soil moisture standard deviation, temperature standard deviation (b)in different dry and wet climate background regions (the asterisk indicates correlation coefficient or multiple correlation coefficient passing α=0.05 significance test. the same as below)
Fig.12 Inter-annual variation of average soil moisture (a) and soil moisture standard deviation (b), average temperature (c) and temperature standard deviation (d) in different dry and wet climate background regions in the northern China
Fig.13 Pearson correlation coefficients of evapotranspiration-precipitation coupling strength with average soil moisture, average temperature, soil moisture standard deviation, temperature standard deviation (a), and complex correlation coefficients of evapotranspiration-precipitation coupling strength with average soil moisture and average temperature, and with soil moisture standard deviation, temperature standard deviation (b) in different dry and wet climate background regions
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