| Gao Shiying,Wang Jingshu.Changes of equatorial wind fields in the Western Pacific and El Nino[J].Acta Oceanologica Sinica,1988,(2):214-225 |
| Changes of equatorial wind fields in the Western Pacific and El Nino |
| Changes of equatorial wind fields in the Western Pacific and El Nino |
| 投稿时间：1986-08-20 修订日期：1987-06-13 |
| DOI： |
| 中文关键词: |
| 英文关键词: |
| 基金项目: |
|
| 摘要点击次数: 755 |
| 全文下载次数: 552 |
| 中文摘要: |
The relationship between SST in the Eastern Pacific and equatorial wind fields in the Western Pacific is analysed by using COADS.
It is pointed out that in the year before El Nino, the continuative easterly anomalies and the meridional anomalies blowing from the Equator to both sides in the Equatorial Western Pacific cause the sea level in the Western Pacific to rise higher than in the Eastern Pacific and the sea level at the Equator to drop lower than on both sides of it. In the El Nino year, the westerly anomalies and the meridional anomalies blowing from both sides to the Equator bring warm water to build up around the Equator. At such times Kelvin waves are generated and they play an important role in raising SST in the Eastern Pacific. It is also emphatically pointed out that in the El Nino year the two maxima of the equatorial westerly anomalies, the two cross-equatorial air flows from the Northern Hemisphere to the Southern one and the two maxima of the near-equatorial tropical cyclones in the Equatorial Western Pacific coincide with the two maxima of the positive SST anomalies in the Eastern Pacific. |
| 英文摘要: |
The relationship between SST in the Eastern Pacific and equatorial wind fields in the Western Pacific is analysed by using COADS.
It is pointed out that in the year before El Nino, the continuative easterly anomalies and the meridional anomalies blowing from the Equator to both sides in the Equatorial Western Pacific cause the sea level in the Western Pacific to rise higher than in the Eastern Pacific and the sea level at the Equator to drop lower than on both sides of it. In the El Nino year, the westerly anomalies and the meridional anomalies blowing from both sides to the Equator bring warm water to build up around the Equator. At such times Kelvin waves are generated and they play an important role in raising SST in the Eastern Pacific. It is also emphatically pointed out that in the El Nino year the two maxima of the equatorial westerly anomalies, the two cross-equatorial air flows from the Northern Hemisphere to the Southern one and the two maxima of the near-equatorial tropical cyclones in the Equatorial Western Pacific coincide with the two maxima of the positive SST anomalies in the Eastern Pacific. |
|
查看全文
查看/发表评论 下载PDF阅读器 |
| 关闭 |