Effects of Sea Surface Temperature Anomalies in Three Tropical Oceans on Extreme Weather and Climate Events

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

Deadline for manuscript submissions: closed (30 June 2023) | Viewed by 1414

Special Issue Editors

Laboratory for Coastal Ocean Variation and Disaster Prediction, College of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang 524088, China
Interests: air–sea interaction; climate variability; physical oceanography; ENSO; monsoon; tropical cyclone

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Guest Editor
South China Sea Institute of Marine Meteorology, Guangdong Ocean University, Zhanjiang 524088, China
Interests: ocean–atmosphere interaction; marine clouds; marine atmospheric boundary layer; extreme rainfall variability; sea fog

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Guest Editor
College of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang 524088, China
Interests: air–sea interaction; climatology; extreme weather; tropical cyclone; explosive cyclone

Special Issue Information

Dear Colleagues,

The ocean plays an important role in shaping our climate and weather patterns. Understanding the roles of the three tropical oceans (tropical Pacific, Indian and Atlantic Oceans) in weather and climate variability is required for predicting weather and climate anomalies. Sea surface temperature (SST) variations that are important manifestations of ocean variability can result in anomalous diabatic heating or cooling of the overlying atmosphere and trigger atmospheric teleconnection, which can alter atmospheric circulation and then affect the weather and climate. The three tropical oceans can breed multiple active SST variation modes, including the eastern Pacific (EP) type of El Niño–Southern Oscillation (ENSO), central Pacific (CP) type of ENSO, Pacific meridional mode (PMM), Indian Ocean dipole (IOD), Indian Ocean basin (IOB) mode, Atlantic Niño, tropical north Atlantic SST, Atlantic meridional mode (AMM), etc. There is overwhelming evidence that SST anomalies in different tropical oceans can be closely related and interacted. The combined impacts of SST anomalies in the three tropical oceans on extreme weather and climate events have not yet been fully understood or revealed.

In this Special Issue, we invite contributions from studies in a wide range of topics and subtopics, focusing on the effects of SST anomalies in three tropical oceans on extreme weather and climate events. This Special Issue provides an opportunity to publish the latest observational analyses and modeling studies on the physical processes related to tropical air–sea interactions and three-ocean inter-basin interactions. This Special Issue collection will highlight recent achievements and address remaining and future challenges in understanding effects of SST anomalies in the three tropical oceans on extreme weather and climate events. The research results in this field have important implications for the further improvement of the weather and climate prediction, which is of great practical significance to the prevention and mitigation of meteorological disasters. Topics of interest include, but are not limited to:

  1. Physical processes and mechanisms of how SST anomalies in the three tropical oceans (tropical Pacific, Indian and Atlantic Oceans) affect extreme weather and climate events, including tropical cyclones, precipitations, monsoons, subtropical highs, heat waves, cold surges, etc.
  2. Tropical air–sea interactions, pantropical climate interactions, tropical three-ocean interactions, inter-basin and intra-basin climate interactions.
  3. Combined impacts of SST anomalies in the three tropical oceans on extreme weather and climate events.
  4. Assessments of the impacts of tropical three-ocean SST anomalies on the numerical simulation of extreme weather and climate events.
  5. The feasibility of using early SST precursor signals as predictors of extreme weather and climate events.
  6. Possible improvements in the predictability and prediction of extreme weather and climate events by considering and incorporating SST anomalies in the three tropical oceans.

Dr. Lei Wang
Dr. Jingchao Long
Dr. Shuqin Zhang
Guest Editors

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Keywords

  • air–sea interaction
  • sea surface temperature
  • tropical three-ocean interactions
  • pantropical climate interactions
  • inter-basin and intra-basin climate interactions
  • tropical Pacific, Indian and Atlantic oceans
  • tropical cyclone
  • precipitation
  • climate variability
  • extreme weather and climate events

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Published Papers (1 paper)

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Research

14 pages, 5387 KiB  
Article
Variations in Key Factors at Different Explosive Development Stages of an Extreme Explosive Cyclone over the Japan Sea
by Shuqin Zhang, Yuan Tang, Liwen Zhang, Qinghua Liao and Tianyu Zhang
Atmosphere 2023, 14(9), 1327; https://doi.org/10.3390/atmos14091327 - 23 Aug 2023
Viewed by 949
Abstract
Explosive cyclones (ECs) occur frequently over the Japan Sea. The most rapidly intensifying EC over the Japan Sea during the 44-year period 1979–2022, in the cold season (October–April), was examined to reveal the variations in the key factors at different explosive development stages. [...] Read more.
Explosive cyclones (ECs) occur frequently over the Japan Sea. The most rapidly intensifying EC over the Japan Sea during the 44-year period 1979–2022, in the cold season (October–April), was examined to reveal the variations in the key factors at different explosive development stages. The EC deepened at a maximum deepening rate of 3.07 bergerons and explosive development lasted for 15 h. At the initial moment of explosive development, the EC had distinctive low-level baroclinicity, the low-level water vapor convergence was weak, and mid-level cyclonic vorticity advection was far away from the EC’s center. At the moment at which the EC reached the maximum deepening rate, the low-level water vapor convergence and mid-level cyclonic vorticity advection increased distinctly and approached the EC’s center. A diagnostic analysis using the Zwack–Okossi equation showed that the main contributor to the initial explosive development was warm-air advection. Through the evolutionary process of the explosive development, the non-key factors of the cyclonic vorticity advection and diabatic heating at the initial explosive development stage increased quickly and became key factors contributing to the maximum explosive development. The key factors contributing to the explosive development varied with the stage of explosive development. The cross-section and vertical profile of each term suggested that the cyclonic vorticity advection was enhanced in the upper troposphere and diabatic heating increased in the middle troposphere. Full article
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