Heatwaves (HWs) lead to catastrophic consequences such as the mortality and morbidity of human (Xu et al., 2016), animal (Vitali et al., 2015, and crops (Brás et al., 2021), and severely deteriorate socioeconomic development. Furthermore, global climate change tends to increase the intensity, frequency, and duration of regional HWs (Clarke et al., 2022;Perkins-Kirkpatrick & Lewis, 2020), thus exacerbates the overall vulnerability of the natural environment and human society. In the past decades, studies have been focused on the evaluation of the adverse impacts from HWs and its prediction (Campbell et al., 2018;Ford et al., 2018;Ragone et al., 2018), aiming to derive the corresponding actionable mitigation and adaptation strategies.Generally, a heat wave can be defined as a prolonged period of excessive hot weather, which usually happens during summer months with a notable and sudden increase of temperature compared to the historical average (Perkins, 2015). It is recognized that the main drivers for HWs are the large-scale atmospheric circulation such as land-atmosphere exchanges and feedbacks on soil moisture and energy (Miralles et al., 2014), the external forcings such as land use change and anthropogenic emission of aerosols (