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Roles of dynamic and thermodynamic effects in seasonal mean surface air temperature trends over Central Asia during 1979–2018

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Abstract

The present study investigated seasonal and spatial characteristics of the trends in surface air temperature (SAT) over Central Asia during 1979–2018 and the relative contributions of dynamic and thermodynamic effects using a dynamical adjustment methodology. Regional averaged total SAT shows the largest rising rate in spring and its trend is not obvious in winter. The thermodynamically effect induces a widespread warming trend in most of Central Asia in all the four seasons. The dynamically induced SAT trends exhibit obvious seasonal and regional differences. Both dynamic and thermodynamic effects play a crucial role in the total SAT increasing trend in spring, the thermodynamic effect is predominantly responsible for SAT warming and the dynamic effect has a secondary contribution in summer, the rising temperature in autumn is attributed to the thermodynamic effect and the dynamic effect has a negative but insignificant contribution, and the total SAT trend in winter is small due to opposite contributions of thermodynamic and dynamic effects. Further analysis revealed that the changes in the Scandinavia pattern (SCAND) during 1979–2018 are likely the cause of dynamically induced temperature trends in spring, autumn and winter. The dynamical component of summer SAT trends over eastern Central Asia is contributed by the interdecadal transition of the Atlantic multidecadal oscillation (AMO) and Pacific decadal oscillation (PDO). Those climate modes contribute to SAT variations via their effects on wind-induced temperature advection and surface heat fluxes.

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The datasets in the present analysis are available for open access.

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Acknowledgements

Comments of two anonymous reviewers are appreciated. This study is supported by Sichuan Science and Technology Program (2020JDJQ0050), the National Natural Science Foundation of China grants (41721004), and Open Research Fund Program of Plateau Atmosphere and Environment Key Laboratory of Sichuan Province (PAEKL-2022-K05). The JRA-55 reanalysis datasets are available online at https://jra.kishou.go.jp/. The ERA5 products are obtained from https://cds.climate.copernicus.eu/.

Funding

The research is supported by Sichuan Science and Technology Program (2020JDJQ0050), the National Natural Science Foundation of China grants (41721004), and Open Research Fund Program of Plateau Atmosphere and Environment Key Laboratory of Sichuan Province (PAEKL-2022-K05).

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ZC and RW designed the study. ZC collected the data, performed the researh, and analyzed data. ZC and RW wrote the draft of the manuscript. All the authors revised the manuscript and acquired the funding.

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Correspondence to Renguang Wu.

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Chen, Z., Wu, R., Zhao, Y. et al. Roles of dynamic and thermodynamic effects in seasonal mean surface air temperature trends over Central Asia during 1979–2018. Clim Dyn 60, 2331–2342 (2023). https://doi.org/10.1007/s00382-022-06457-0

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  • DOI: https://doi.org/10.1007/s00382-022-06457-0

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