| Simulation of double cold cores of the 35°N section in the YellowSea with a wave-tide-circulation coupled model |
| |
| 引用本文： | 夏长水,乔方利,张勐宁,杨永增,袁业立.Simulation of double cold cores of the 35°N section in the YellowSea with a wave-tide-circulation coupled model[J].中国海洋与湖沼学报,2004(3). |
| |
| 作者姓名： | 夏长水 乔方利 张勐宁 杨永增 袁业立 |
| |
| 作者单位： | The First Institute of Oceanography，State Oceanic Administration (SOA)，Qingdao 266061，China Key Laboratory of Marine Science and Numerical Modeling (MASNUM)，SOA，Qingdao 266061，China The Marine Environment College，Ocean University of China，Qingdao 266003，China，The First Institute of Oceanography，State Oceanic Administration (SOA)，Qingdao 266061，China Key Laboratory of Marine Science and Numerical Modeling (MASNUM)，SOA，Qingdao 266061，China，Guest Researcher ofMASNUM，SOA，China，The First Institute of Oceanography，State Oceanic Administration (SOA)，Qingdao 266061，China Key Laboratory of Marine Science and Numerical Modeling (MASNUM)，SOA，Qingdao 266061，China，The First Institute of Oceanography，State Oceanic Administration (SOA)，Qingdao 266061，China Key Laboratory of Marine Science and Numerical Modeling (MASNUM)，SOA，Qingdao 266061，China) |
| |
| 基金项目： | SupportedbytheNationalBasicResearchProgramofChina(No.G1999043809)
theNationalScienceFoundationofChina(No.49736190). |
| |
| 摘 要： | Based on the MASNUM wave-tide-circulation coupled numerical model, the temperature structure along 35°N in the Yellow Sea was simulated and compared with the observations. One of the notable features of the temperature structure along 35°N section is the double cold cores phenomena during spring and summer. The double cold cores refer to the two cold water centers located near 122°E and 125°E from the depth of 30m to bottom. The formation, maintenance and disappearance of the double cold cores are discussed. At least two reasons make the temperature in the center (near 123°E) of the section higher than that near the west and east shores in winter. One reason is that the water there is deeper than the west and east sides so its heat content is higher. The other is invasion of the warm water brought by the Yellow Sea Warm Current (YSWC) during winter. This temperature pattern of the lower layer (from 30m to bottom) is maintained through spring and summer when the upper layer (0 to 30m) is heated and s
|
| 本文献已被 CNKI 等数据库收录！ |
