Terrestrial Stilling Projected to Continue in the Northern Hemisphere Mid‐Latitudes-Reference-Cited by-同舟云学术

Terrestrial Stilling Projected to Continue in the Northern Hemisphere Mid‐Latitudes

Published:2022-07 Issue:7 Volume:10 Page:
ISSN:2328-4277
Container-title:Earth's Future
language:en
Short-container-title:Earth's Future

Author:

Deng K.¹²³,Liu W.¹,Azorin‐Molina C.³⁴,Yang S.¹²^ORCID,Li H.¹,Zhang G.⁵⁶,Minola L.³,Chen D.³^ORCID

Affiliation:

1. School of Atmospheric Sciences Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai) Sun Yat‐sen University Zhuhai China

2. Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies Sun Yat‐sen University Zhuhai China

3. Department of Earth Sciences Regional Climate Group University of Gothenburg Gothenburg Sweden

4. Centro de Investigaciones sobre Desertificación Consejo Superior de Investigaciones Científicas (CIDE‐CSIC) Valencia Spain

5. State Key Laboratory of Earth Surface Processes and Resource Ecology Beijing Normal University Beijing China

6. Academy of Disaster Reduction and Emergency Management Ministry of Emergency Management and Ministry of Education Beijing Normal University Beijing China

Funder

Svenska Forskningsrådet Formas

National Natural Science Foundation of China

Vetenskapsrådet

Ministerio de Ciencia, Innovación y Universidades

Fundación BBVA

Publisher

American Geophysical Union (AGU)

Subject

Earth and Planetary Sciences (miscellaneous),General Environmental Science

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021EF002448

Reference44 articles.

1. A decline of observed daily peak wind gusts with distinct seasonality in Australia, 1941-2016

2. Recent trends in wind speed across Saudi Arabia, 1978-2013: a break in the stilling

3. Homogenization and Assessment of Observed Near-Surface Wind Speed Trends over Spain and Portugal, 1961–2011*

4. The impact of Arctic warming on the midlatitude jet‐stream: Can it? Has it? Will it?

5. Weakened evidence for mid-latitude impacts of Arctic warming

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