The role of mindanao dome in the variability of the Pacific North equatorial current bifurcation | |
Zhao, Jun1,2; Li, Yuanlong1,3; Wang, Fan1; Wang, F | |
刊名 | JOURNAL OF OCEANOGRAPHY |
2013-06-01 | |
卷号 | 69期号:3页码:313-327 |
关键词 | Mindanao dome North equatorial current bifurcation Seasonal cycle Philippine Sea Asymmetry Sea surface height Rossby wave |
ISSN号 | 0916-8370 |
通讯作者 | Wang, F |
中文摘要 | The Mindanao Dome (MD) features prominent oceanic variability and is located geographically close to the bifurcation latitude Y (b) of the Pacific North Equatorial Current. In this study, the role of the MD in the variability of Y (b) is examined with 20 years of satellite altimetric sea surface height (SSH) data and a 1.5-layer linear Rossby wave model. It is shown that the seasonal variations of surface Y (b) are related to not only the SSH fluctuations near the bifurcation point (bifurcation box; 125A degrees-130A degrees E, 12A degrees-15A degrees N) but also those outstanding in the MD region (MD box; 127A degrees-132A degrees E, 6A degrees-9A degrees N). The impact of the MD SSH changes is significant when the bifurcation point stays at southerly latitudes during February-September, which hinders (delays) the southward leap (northward retreat) of Y (b) in April-May (July-August) and thus leads to the asymmetry of the mean Y (b) seasonal cycle (with a positive skewness of gamma = +0.64). Such asymmetry also shows year-to-year variations depending on yearly mean Y (b) value. A southerly yearly mean Y (b) involves larger contribution of the MD and thus causes larger asymmetry of Y (b) seasonal cycle. At interannual and longer timescales, the MD acts to amplify the fluctuations of the bifurcation. It is responsible for about 20 % of the total low-frequency Y (b) variances and plays an important role in the 0.12A degrees A year(-1) southward trend of Y (b) in the past two decades. The impact of the MD on Y (b) changes is becoming increasingly significant at various timescales such as the bifurcation point migrating southward in recent years. |
英文摘要 | The Mindanao Dome (MD) features prominent oceanic variability and is located geographically close to the bifurcation latitude Y (b) of the Pacific North Equatorial Current. In this study, the role of the MD in the variability of Y (b) is examined with 20 years of satellite altimetric sea surface height (SSH) data and a 1.5-layer linear Rossby wave model. It is shown that the seasonal variations of surface Y (b) are related to not only the SSH fluctuations near the bifurcation point (bifurcation box; 125A degrees-130A degrees E, 12A degrees-15A degrees N) but also those outstanding in the MD region (MD box; 127A degrees-132A degrees E, 6A degrees-9A degrees N). The impact of the MD SSH changes is significant when the bifurcation point stays at southerly latitudes during February-September, which hinders (delays) the southward leap (northward retreat) of Y (b) in April-May (July-August) and thus leads to the asymmetry of the mean Y (b) seasonal cycle (with a positive skewness of gamma = +0.64). Such asymmetry also shows year-to-year variations depending on yearly mean Y (b) value. A southerly yearly mean Y (b) involves larger contribution of the MD and thus causes larger asymmetry of Y (b) seasonal cycle. At interannual and longer timescales, the MD acts to amplify the fluctuations of the bifurcation. It is responsible for about 20 % of the total low-frequency Y (b) variances and plays an important role in the 0.12A degrees A year(-1) southward trend of Y (b) in the past two decades. The impact of the MD on Y (b) changes is becoming increasingly significant at various timescales such as the bifurcation point migrating southward in recent years. |
学科主题 | Oceanography |
WOS标题词 | Science & Technology ; Physical Sciences |
类目[WOS] | Oceanography |
研究领域[WOS] | Oceanography |
关键词[WOS] | WESTERN TROPICAL PACIFIC ; BAROCLINIC ROSSBY WAVES ; INTERANNUAL VARIABILITY ; PHILIPPINE SEA ; BOUNDARY CURRENTS ; OCEAN ; CIRCULATION ; KUROSHIO ; LATITUDE ; LEVEL |
收录类别 | SCI |
原文出处 | 10.1007/s10872-013-0175-7 |
语种 | 英语 |
WOS记录号 | WOS:000319421300003 |
公开日期 | 2014-07-17 |
内容类型 | 期刊论文 |
源URL | [http://ir.qdio.ac.cn/handle/337002/16442] |
专题 | 海洋研究所_海洋环流与波动重点实验室 |
通讯作者 | Wang, F |
作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao 266071, Peoples R China 2.Univ Chinese Acad Sci, Beijing, Peoples R China 3.Univ Colorado, Dept Atmospher & Ocean Sci, Boulder, CO 80309 USA |
推荐引用方式 GB/T 7714 | Zhao, Jun,Li, Yuanlong,Wang, Fan,et al. The role of mindanao dome in the variability of the Pacific North equatorial current bifurcation[J]. JOURNAL OF OCEANOGRAPHY,2013,69(3):313-327. |
APA | Zhao, Jun,Li, Yuanlong,Wang, Fan,&Wang, F.(2013).The role of mindanao dome in the variability of the Pacific North equatorial current bifurcation.JOURNAL OF OCEANOGRAPHY,69(3),313-327. |
MLA | Zhao, Jun,et al."The role of mindanao dome in the variability of the Pacific North equatorial current bifurcation".JOURNAL OF OCEANOGRAPHY 69.3(2013):313-327. |
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