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4.1
2.9
Journals
Atmosphere
Special Issues
New Insights in Atmospheric Teleconnection
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New Insights in Atmospheric Teleconnection

A special issue of Atmosphere (ISSN 2073-4433). This special issue belongs to the section "Meteorology".

Deadline for manuscript submissions: 27 June 2024 | Viewed by 1483

Special Issue Editors

Prof. Dr. Dongxiao Wang

E-Mail Website
Guest Editor
School of Marine Sciences, Sun Yat-Sen University, Zhuhai 519082, China
Interests: air–sea interaction; ocean circulation
Dr. Marco Y.-T. Leung

E-Mail Website
Guest Editor
School of Marine Sciences, Sun Yat-Sen University, Zhuhai 519082, China
Interests: atmospheric planetary waves; East Asian monsoon; cold surges
Dr. Zifeng Hu

E-Mail Website
Guest Editor
School of Marine Sciences, Sun Yat-Sen University, Zhuhai 519082, China
Interests: ocean remote sensing; coastal oceanography

Special Issue Information

Dear Colleagues,

Since the pioneer papers by J. Bjerknes were published about 50 years ago, it has become clear that atmospheric teleconnection accounts for a major share of the interannual-to-multidecadal variance in meteorological fields all over the world. Atmospheric teleconnection stems from large-scale disturbances generated within the climate system. They spread far from the region of generation through the general atmosphere circulation and planetary waves. There are numerous excellent publications concerning this phenomenon. It is worth summarizing some recent results concerning the global and regional consequences of atmospheric teleconnection in this Special Issue of Atmosphere. Any articles concerning different manifestations of atmospheric teleconnection, including meteorological extremes, are welcome.

Prof. Dr. Dongxiao Wang
Dr. Marco Y.-T. Leung
Dr. Zifeng Hu
Guest Editors

Manuscript Submission Information

Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. All submissions that pass pre-check are peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.

Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Atmosphere is an international peer-reviewed open access monthly journal published by MDPI.

Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 2400 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.

Keywords

  • atmospheric teleconnection
  • coupled ocean–atmosphere modes
  • global and regional manifestations
  • three-ocean interactions and ENSO
  • climate change and environmental health
  • ocean/atmospheric heat waves

Published Papers (2 papers)

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Research

18 pages, 6002 KiB  
Article
The Impacts of Regime Shift in Summer Arctic Oscillation on Precipitation in East Asia
by Xuxin Zou, Li Yan, Jianjun Xu and Shaojun Zheng
Atmosphere 2024, 15(3), 283; https://doi.org/10.3390/atmos15030283 - 26 Feb 2024
Viewed by 579
Abstract
Using multiple observational and reanalysis data, this paper investigates the impact of the interdecadal shift in summer Arctic Oscillation (AO) on precipitation in East Asia, by removing ENSO influences. The results indicate that the lower-layer activity center of summer AO in Atlantic shifted [...] Read more.
Using multiple observational and reanalysis data, this paper investigates the impact of the interdecadal shift in summer Arctic Oscillation (AO) on precipitation in East Asia, by removing ENSO influences. The results indicate that the lower-layer activity center of summer AO in Atlantic shifted eastward after the mid-1980s. This regime shift of summer AO has a significant impact on precipitation in East Asia. Before the mid-1980s, the key regions in which precipitation was affected by AO in East Asia were northern East Asia and Northeastern China and adjacent regions. After the mid-1980s, the key regions in which precipitation was affected by AO in East Asia were central Inner Mongolia and Southern China. The mechanism of precipitation changes can be attributed to changes in atmospheric circulation and water vapor transport related to AO changes. After the mid-1980s, the influence of AO on geopotential height over northern East Asia weakened; meanwhile, the impact of AO on geopotential height over China increased. Consistent with the changes in atmospheric circulation, water vapor transport in East Asia also underwent interdecadal changes before and after the mid-1980s. The differences in atmospheric circulation and water vapor transport in East Asia can be traced back to the North Atlantic. Before the mid-1980s, wave activity flux related to summer AO tended to propagate in high latitudes and subtropics; after the mid-1980s, the wave activity flux changed in its subtropical path and propagated eastward from the North Atlantic through the Middle East to China, significantly affecting the summer precipitation in China. Full article
(This article belongs to the Special Issue New Insights in Atmospheric Teleconnection)
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18 pages, 6488 KiB  
Article
Projected Changes of Wind Energy Input to Surface Waves in the North Indian Ocean Based on CMIP6
by Juan Li, Yuexuan Zhao, Menglu Wang, Wei Tan and Jiyuan Yin
Atmosphere 2024, 15(1), 139; https://0-doi-org.brum.beds.ac.uk/10.3390/atmos15010139 - 22 Jan 2024
Viewed by 724
Abstract
This paper explores the effects of climate change on the wind energy input (WEI) to the surface waves (SWs) in the northern Indian Ocean (NIO), a region with great potential for green renewable energy from waves and wind. We used the newly developed [...] Read more.
This paper explores the effects of climate change on the wind energy input (WEI) to the surface waves (SWs) in the northern Indian Ocean (NIO), a region with great potential for green renewable energy from waves and wind. We used the newly developed Coupled Model Intercomparison Project Phase 6 (CMIP6) model data to predict the spatiotemporal variations of the WEI to the SW. We found that, under the global warming scenario, the WEI to the SWs decreased significantly in most of the NIO, and it will drop by 18% to 27% in the central and southern regions by the end of the 21st century under the SSP5–8.5 scenario. However, the WEI to the SWs increased in the Red Sea, Persian Gulf, northwestern Arabian Sea, and northern Bay of Bengal, with the largest increase in the Persian Gulf region (up to 27%). We also examined the interannual and interdecadal variability characteristics of the WEI to the SW after the accumulation of the whole study region and found that it showed a long-term increasing trend only under the SSP1–2.6 scenario, while it showed a significant decreasing trend under the SSP2–4.5 and SSP5–8.5 scenarios. Furthermore, we show that the WEI to the SWs in the Indian Ocean mainly occurs in summer, followed by winter. Full article
(This article belongs to the Special Issue New Insights in Atmospheric Teleconnection)
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