Dynamic effect of the South Asian high on the interannual zonal extension of the western North Pacific subtropical high-Reference-Cited by-同舟云学术

Dynamic effect of the South Asian high on the interannual zonal extension of the western North Pacific subtropical high

Published:2019-06-10 Issue:14 Volume:39 Page:5367-5379
ISSN:0899-8418
Container-title:International Journal of Climatology
language:en
Short-container-title:Int J Climatol

Author:

Wei Wei¹²³^ORCID,Zhang Renhe⁴,Wen Min⁵,Yang Song¹³^ORCID,Li Wenhong⁶

Affiliation:

1. School of Atmospheric Sciences and Guangdong Province Key Laboratory for Climate Change and Natural Disaster StudiesSun Yat‐sen University Zhuhai China

2. Key Laboratory of Meteorological Disaster of Ministry of Education, Nanjing University of Information Science and Technology Nanjing China

3. Southern Laboratory of Ocean Science and Engineering (Guangdong, Zhuhai) Zhuhai China

4. Institute of Atmospheric SciencesFudan University Shanghai China

5. State Key Laboratory of Severe WeatherChinese Academy of Meteorological Sciences Beijing China

6. Earth and Ocean Sciences, Nicholas School of the EnvironmentDuke University Durham North Carolina

Funder

National Natural Science Foundation of China

Key Laboratory of Meteorological Disaster

Nanjing University of Information Science and Technology

Publisher

Wiley

Subject

Atmospheric Science

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/joc.6160

Reference53 articles.

1. Mechanisms for concurrent low-latitude circulation anomalies responsible for persistent extreme precipitation in the Yangtze River Valley

2. Understanding Land–Sea Warming Contrast in Response to Increasing Greenhouse Gases. Part I: Transient Adjustment

3. Subseasonal Zonal Oscillation of the Western Pacific Subtropical High during Early Summer

4. Vertical circulation structure,interannual variation features and variation mechanism of western pacific subtropical high

5. Using eddy geopotential height to measure the western North Pacific subtropical high in a warming climate

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