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Cited by 375

The DOI matches its Crossref record; 15 of the 15 references it cites were found in a registry or an index.

Does the climate warming hiatus exist over the Tibetan Plateau?

Open access
Duan, Anmin, Xiao, Zhixiang·2015·Scientific Reports

Abstract

The surface air temperature change over the Tibetan Plateau is determined based on historical observations from 1980 to 2013. In contrast to the cooling trend in the rest of China and the global warming hiatus post-1990s, an accelerated warming trend has appeared over the Tibetan Plateau during 1998–2013 (0.25 °C decade−1), compared with that during 1980–1997 (0.21 °C decade−1). Further results indicate that, to some degree, such an accelerated warming trend might be attributable to cloud–radiation feedback. The increased nocturnal cloud over the northern Tibetan Plateau would warm the nighttime temperature via enhanced atmospheric back-radiation, while the decreased daytime cloud over the southern Tibetan Plateau would induce the daytime sunshine duration to increase, resulting in surface air temperature warming. Meanwhile, the in situ surface wind speed has recovered gradually since 1998 and thus the energy concentration cannot explain the accelerated warming trend over the Tibetan Plateau after the 1990s. It is suggested that cloud–radiation feedback may play an important role in modulating the recent accelerated warming trend over the Tibetan Plateau.

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Metadata

Authors
Duan, A., & Xiao, Z.
Venue
Scientific Reports
Published
2015-09-02
Volume
5
Issue
1
Pages
13711-13711
ISSN
2045-2322 (ISSN-L)
OpenAlex
W2410135257
Cited by
375
References
15
FWCI
16.66
Type
journal article
Language
en
Open access
gold

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CoChat. (2026). Citation check: Does the climate warming hiatus exist over the Tibetan Plateau? https://app.cochat.ai/papers/10.1038/srep13711
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Duan, A., & Xiao, Z. (2015). Does the climate warming hiatus exist over the Tibetan Plateau? Scientific Reports. https://doi.org/10.1038/srep13711

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