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Published on: June 13, 2020
Northwestern Pacific typhoon intensity controlled by changes in ocean temperatures
Wei Mei1, Shang-Ping Xie2, François Primeau3
1Scripps Institution of Oceanography, University of California, San Diego, San Diego, CA 92093, USA. ; Department of Earth System Science, University of California, Irvine, Irvine, CA 92697, USA.
Upper ocean warming in the northwestern Pacific significantly increases typhoon intensity by enhancing intensification rates. This trend is expected to continue, leading to stronger typhoons by 2100.
Area of Science:
- Climatology
- Oceanography
- Meteorology
Background:
- Typhoon intensity is influenced by various climatic factors.
- Understanding these factors is crucial for predicting future storm behavior.
Purpose of the Study:
- To identify the dominant climatic factors controlling typhoon lifetime peak intensity.
- To analyze the impact of ocean temperatures on typhoon intensification.
Main Methods:
- Analysis of six decades of Pacific typhoon data.
- Correlation of typhoon intensity with upper ocean and sea surface temperatures.
Main Results:
- Upper ocean temperatures in the low-latitude northwestern Pacific (LLNWP) control typhoon intensification rates.
- Sea surface temperatures in the central equatorial Pacific influence intensification duration.
- Recent LLNWP warming has increased average typhoon intensity.
Conclusions:
- LLNWP upper ocean warming is a key driver of increased typhoon intensity.
- Continued warming under climate change scenarios like RCP 4.5 will further intensify typhoons.
- Projected increase in average typhoon intensity by 14% by 2100.
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