At global scale, lakes are warming faster than both the atmosphere and the oceans (O'Reilly et al., 2015). Given that, all lakes are land-locked, these changes could be intensified by the projected changing climate under the future influence of anthropogenic stressors (Jane et al., 2021;Modabberi et al., 2020;Woolway et al., 2021). This could have deep implications for the lake ecological services (Kraemer et al., 2021;Pilla et al., 2020) and threaten both the quantity and quality of the most important sources of freshwater for humankind (Kraemer et al., 2015;Noori et al., 2018). Despite the global warming impact on the lakes, the rate of increase in the lake surface-water temperature (LST) is not consistent with that in the lake deep-water temperature (LDT). O'Reilly et al. ( 2015) calculated a significant global mean warming rate of 0.34°C per decade in LST, while no such significant warming was found in the LDT at global scale (Kraemer et al., 2015;Pilla et al., 2020). These results suggest a progressive divergence between the LST and LDT at global scale that intensifies both strength and duration of lake thermal stratification (Oleksy & Richardson, 2021).Although there is consensus on the increase in LSTs globally, the changing rates are not consistent even in a local geographical region. Studies show both cooling and warming trends in the LST in high-latitude lakes (e.g., in Alaska and Northern Europe), high altitude lakes (e.g., in Tibetan Plateau), and temperate lakes (e.g., in Central Europe; Kraemer et al., 2015;O'Reilly et al., 2015; Wan et al., 2018). Regarding the LDT, relatively few longterm databases on freshwater lakes are available compared to the LST. They mainly cover three or four decades. On the other hand, the changes reported in relatively LST-rich databases cannot simply reveal the more complex nature of LDT influenced by multiple stressors. Pilla et al. (2020) concluded that the trends in the LDT were not explained by those observed in the LST and thermal stability. Thus, we understand less about changes in the LDT than the LST (Richardson et al., 2017).