1. Increase Asymmetric Warming Rates Between Daytime and Nighttime Temperatures Over Global Land During Recent Decades.
- Author
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Liu, Ge, Guo, Yan, Xia, Haoming, Liu, Xingya, Song, Hongquan, Yang, Jia, and Zhang, Yuqing
- Subjects
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CLIMATE change adaptation , *HILBERT-Huang transform , *CLIMATE change , *GLOBAL warming , *SOLAR radiation - Abstract
Diurnal asymmetric warming, a critical feature of climate change, significantly impacts water‐carbon exchange in terrestrial ecosystems. This study analyzes the spatiotemporal characteristics and long‐term trends of the global diurnal temperature range (DTR) from 1961 to 2022 using ensemble empirical mode decomposition (EEMD). Our results reveal a trend reversal in global averaged DTR around 1988, shifting from a decrease to an increase, affecting 47% of global land areas. Subsequent to the reversal, the most pronounced increases were observed in temperate regions. Seasonal analysis shows earlier reversals in spring and summer, with accelerated change rates following the reversal. Additionally, increased surface solar radiation from reduced cloud cover caused daily maximum (Tmax) temperatures to warm faster than the minimum (Tmin), leading to a reversal and intensified DTR. These complex patterns underscore the need for targeted climate policies and adaptation strategies to tackle global warming. Plain Language Summary: Global climate change is causing uneven warming patterns, which significantly affect how ecosystems exchange water and carbon. One important way to understand this is through the diurnal temperature range (DTR), which measures the difference between daytime and nighttime temperatures. In this study, we examined DTR changes globally from 1961 to 2022 using a method called ensemble empirical mode decomposition (EEMD). We discovered that the overall trend in DTR reversed around 1988, changing from a decline to an increase, which affected nearly half of the world's land areas. Subsequent to the reversal, the most pronounced increases were observed in temperate regions, whereas tropical areas exhibited a more subdued rate of rise. Interestingly, we found that the rate of increase in DTR is stronger in southern latitudes compared to northern latitudes. Additionally, increased surface solar radiation from reduced cloud cover caused daily maximum temperatures (Tmax) to rise faster than minimum temperatures (Tmin), resulting in a higher DTR. These findings highlight the need for more effective climate policies and adaptation strategies to tackle the complex challenges posed by global warming. Understanding these changes is crucial for informing decisions related to climate resilience and environmental sustainability. Key Points: Around 1988, the global diurnal temperature range (DTR) reversed from a long‐term decline to an increase, impacting 47% area of landThe reversal in the DTR was most pronounced in spring and summer, with greater changes in temperate regions and southern latitudesDaily maximum temperatures are warming faster than minimum temperatures, driving the DTR reversal and intensification [ABSTRACT FROM AUTHOR]
- Published
- 2024
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