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Cited by 303

The DOI matches its Crossref record; 1 of the 1 references it cites were found in a registry or an index.

Change of cloud amount and the climate warming on the Tibetan Plateau

Open access
Duan, Anmin, Wu, Guoxiong·2006·Geophysical Research Letters

Abstract

Based on the 6‐hourly weather observations at 71 stations across the central and eastern Tibetan Plateau (TP) during 1961–2003, the change of cloud amount and its possible connection with recent climate warming on TP were investigated. The low‐level cloud amount exhibits a significant increasing trend during the nighttimes, leading to the enhanced atmospheric counterradiation, weakened effective terrestrial radiation, and the subsequently strong nocturnal surface warming. On the other hand, both the total and low‐level cloud amounts during daytime display decreasing trends, resulting in more absorbing of direct solar radiation at the surface and the associated surface warming. Since the increase in nocturnal low‐level cloud is more than the decrease of daytime low and total cloud amounts, such changes in cloud amount contribute to at least partly of the increased surface air temperature and its diminished diurnal range on TP.

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Crossref · 10.1029/2006gl027946

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Metadata

Authors
Duan, A., & Wu, G.
Venue
Geophysical Research Letters
Published
2006-11
Volume
33
Issue
22
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W2148351602
Cited by
303
References
1
FWCI
3.35
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: Change of cloud amount and the climate warming on the Tibetan Plateau. https://app.cochat.ai/papers/10.1029/2006gl027946
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Duan, A., & Wu, G. (2006). Change of cloud amount and the climate warming on the Tibetan Plateau. Geophysical Research Letters. https://doi.org/10.1029/2006gl027946

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

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