2022
DOI: 10.1016/j.scitotenv.2022.153607
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Influence patterns of soil moisture change on surface-air temperature difference under different climatic background

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Cited by 24 publications
(12 citation statements)
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“…The temporal change in soil temperature is closely related to the growth period of cotton, and PFM can change the latent heat flux, such as cotton population water evaporation and soil water transpiration ( Jiang et al, 2022 ; Li et al, 2021 ), and then increase thermal radiation capture and topsoil temperature, especially in the early and middle stages of cotton growth ( Zong et al, 2020 ; Ghosh et al, 2006 ). In this study, before the initial flowering stage (July 1), especially before the first irrigation (June 20), the temperature of the 0–50 cm soil layer in the cotton field covered with plastic film was higher by approximately 2−4 °C than that in the uncovered cotton field.…”
Section: Discussionmentioning
confidence: 99%
“…The temporal change in soil temperature is closely related to the growth period of cotton, and PFM can change the latent heat flux, such as cotton population water evaporation and soil water transpiration ( Jiang et al, 2022 ; Li et al, 2021 ), and then increase thermal radiation capture and topsoil temperature, especially in the early and middle stages of cotton growth ( Zong et al, 2020 ; Ghosh et al, 2006 ). In this study, before the initial flowering stage (July 1), especially before the first irrigation (June 20), the temperature of the 0–50 cm soil layer in the cotton field covered with plastic film was higher by approximately 2−4 °C than that in the uncovered cotton field.…”
Section: Discussionmentioning
confidence: 99%
“… 39 ERA5-Land is an enhanced ERA5 surface component dataset that describes surface hydrothermal variability and has a globally improved spatial resolution of 9 km (0.1°) created by a more advanced surface modeling technique and has been widely used for regional and global analysis. 16 , 45 , 65 , 66 , 67 …”
Section: Methodsmentioning
confidence: 99%
“…Climate warming would increase evaporation rates and atmospheric humidity (Song et al., 2022). Higher atmospheric humidity strengthens the greenhouse effect of water vapor, contributing to further warming (Jiang et al., 2023; Sherwood et al., 2018). Moreover, General Circulation Models (GCMs) in CMIP5 and observational data suggest that the warming climate will alter convective precipitation patterns, resulting in a phenomenon known as “wet‐get‐wetter” and “dry‐get‐drier” (Dittus et al., 2016; Donat et al., 2016; Du et al., 2022; IPCC et al., 2021).…”
Section: Introductionmentioning
confidence: 99%
“…Generally, higher soil moisture can contribute to temperature reduction due to the energy consumption involved in leaf/soil evaporation processes (Xu et al., 2004). However, it is essential to note the influence of soil moisture on climate warming varies depending on different background temperature thresholds (Jiang et al., 2023). These interactive climate changes are expected to have a significant impact on crop yield and soil GHG emissions, particularly in regions with stronger temperature‐moisture couplings (Griffis et al., 2017; Gupta et al., 2021; IPCC et al., 2021; Lesk et al., 2021; Tian, Lu, et al., 2016; Tian, Ren, et al., 2016; Tian et al., 2020).…”
Section: Introductionmentioning
confidence: 99%