| QIN Huiling,JIAN Maoqiu,YUAN Zhuojian. 2004. Relationship between SSTA in the northwestern Pacific and winter climate anomaly in China. Acta Oceanologica Sinica, (1):73－82 |
| Relationship between SSTA in the northwestern Pacific and winter climate anomaly in China |
| Relationship between SSTA in the northwestern Pacific and winter climate anomaly in China |
| Received:September 03, 2003 Revised:November 25, 2003 |
| DOI： |
| Key words:climate anomaly SSTA “seesaw” pattern anticyclone (cyclone) anomalous anti-Hadley circulation surface heat flux |
| 中文关键词: climate anomaly SSTA “seesaw” pattern anticyclone (cyclone) anomalous anti-Hadley circulation surface heat flux |
| 基金项目: |
| Author Name | Affiliation | E-mail | | QIN Huiling | Department of Atmospheric Sciences, Zhongshan University, Guangzhou 510275, China
Key Laboratory of Tropical Marine Environmental Dynamics, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China | qhling@scsio.ac.cn | | JIAN Maoqiu | Department of Atmospheric Sciences, Zhongshan University, Guangzhou 510275, China | | | YUAN Zhuojian | Department of Atmospheric Sciences, Zhongshan University, Guangzhou 510275, China | |
|
| Hits: 979 |
| Download times: 744 |
| Abstract: |
| The relationship between sea surface temperature anomaly (SSTA) in the domain from the northwest of thc Pacific to Chinaseas (NWP-CS) andclimate (precipitation and surface temperature) anomaly in winters over east of Chinese Mainland (ECM) are investigated with composite analysis. The results suggest that (1) SSTA in NWP-CS usually appears as "seesaw" pattern, I.e., sign of SSTA in the northwest of thc Philippines is positive (negative) while in the southeast it is negative (positive), defmed as SSTA "seesaw" positive (negative) pattern. When SSTA "seesaw" positive(negative) pattern appears, the surface temperature in ECM is higher (lower) than the normal winters but thc precipitation anomaly is not distinct; (2) there are two anomalous anticyclones (cyclones) locating in the northwest Pacific and east of the Philippines at 850 hPa level and an anomalous anti-Hadley (Hadley) circulation, which descends (ascends)south of 18°N, ascends (descends) north of 18°N; (3) heat flux anomaly from ocean into atmosphere is weaker (stronger)in the northwest of the Philippines but stronger (weaker) in the southeast of the Philippines than the normal winters, because the weaker (stronger) northerly prevails in thc northwest of the Philippines and stronger (weaker) northeaster in the southeast of the Philippines induced by anomalous anticyclones (cyclones). |
| 中文摘要: |
| The relationship between sea surface temperature anomaly (SSTA) in the domain from the northwest of thc Pacific to Chinaseas (NWP-CS) andclimate (precipitation and surface temperature) anomaly in winters over east of Chinese Mainland (ECM) are investigated with composite analysis. The results suggest that (1) SSTA in NWP-CS usually appears as "seesaw" pattern, I.e., sign of SSTA in the northwest of thc Philippines is positive (negative) while in the southeast it is negative (positive), defmed as SSTA "seesaw" positive (negative) pattern. When SSTA "seesaw" positive(negative) pattern appears, the surface temperature in ECM is higher (lower) than the normal winters but thc precipitation anomaly is not distinct; (2) there are two anomalous anticyclones (cyclones) locating in the northwest Pacific and east of the Philippines at 850 hPa level and an anomalous anti-Hadley (Hadley) circulation, which descends (ascends)south of 18°N, ascends (descends) north of 18°N; (3) heat flux anomaly from ocean into atmosphere is weaker (stronger)in the northwest of the Philippines but stronger (weaker) in the southeast of the Philippines than the normal winters, because the weaker (stronger) northerly prevails in thc northwest of the Philippines and stronger (weaker) northeaster in the southeast of the Philippines induced by anomalous anticyclones (cyclones). |
|
HTML
View Full Text
View/Add Comment Download reader |
| Close |
|
|
|
