2003Journal of Tropical MeteorologyRequires access

THE INFLUENCE OF VARIATION OF SUBSURFACE OCEAN TEMPERATURE IN THE EQUATORIAL WESTERN PACIFIC WARM POOL ON TROPICAL CYCLONES

Zhang Jun-feng

Open publisher page 1 citations

Abstract

Using observed data, the authors have analyzed the impact of the variation of subsurface ocean temperature of the equatorial Western Pacific Warm Pool and South China Sea on the tropical cyclones. The results show that the number of tropical cyclones in the Western Pacific are more(or less)than the normai year, and their intensities also stronger(or weaker), when the subsurface ocean temperature of the equatorial Westem Pacific Warm Pool persistently shows positive(or negative)anomaly. This phenomena is especially evident in the extreme years, but effects of the phenomena on tropical cyclones in South China Sea are not obvious. At the same time, the forming of the tropical cyclones in the western and Northern Pacific and in South China Sea is often ahead of time (or postpones). Usually, when the subsurface ocean temperature in the north of South China Sea appears in the positive(or negative)anomaly, the number of tropical cyclones forming in South China Sea are more(or less).

About this research paper

What this paper is about

Using observed data, the authors have analyzed the impact of the variation of subsurface ocean temperature of the equatorial Western Pacific Warm Pool and South China Sea on the tropical cyclones. The results show that the number of tropical cyclones in the Western Pacific are more(or less)than the normai year, and their intensities also stronger(or weaker), when the subsurface ocean temperature of the equatorial Westem Pacific Warm Pool persistently shows positive(or negative)anomaly. This phenomena is especially evident in the extreme years, but effects of the phenomena on tropical cyclones in South China Sea are not obvious. At the same time, the forming of the tropical cyclones in the western and Northern Pacific and in South China Sea is often ahead of time (or postpones). Usually, when the subsurface ocean temperature in the north of South China Sea appears in the positive(or negative)anomaly, the number of tropical cyclones forming in South China Sea are more(or less).

Why it matters

OpenAlex reports 1 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

Using observed data, the authors have analyzed the impact of the variation of subsurface ocean temperature of the equatorial Western Pacific Warm Pool and South China Sea on the tropical cyclones. The results show that the number of tropical cyclones in the Western Pacific are more(or less)than the normai year, and their intensities also stronger(or weaker), when the subsurface ocean temperature of the equatorial Westem Pacific Warm Pool persistently shows positive(or negative)anomaly. This phenomena is especially evident in the extreme years, but effects of the phenomena on tropical cyclones in South China Sea are not obvious. At the same time, the forming of the tropical cyclones in the western and Northern Pacific and in South China Sea is often ahead of time (or postpones). Usually, when the subsurface ocean temperature in the north of South China Sea appears in the positive(or negative)anomaly, the number of tropical cyclones forming in South China Sea are more(or less).

Key concepts: Tropical cyclone, Climatology, Oceanography, Anomaly (physics), Sea surface temperature, Geology, African easterly jet, Pacific ocean

Related papers

Back to paper searchBrowse research topicsOriginal source
THE INFLUENCE OF VARIATION OF SUBSURFACE OCEAN TEMPERATURE IN THE EQUATORIAL WESTERN PACIFIC WARM POOL ON TROPICAL CYCLONES — Research Paper | ScholarLens