Northward expansion of the western Pacific Warm Pool in late 1990s and early 2000s
Based on 48-year (1958–2006) ocean reanalysis data of Simple Ocean Data Assimilation and 23-year (1984–2006) global ocean-surface heat flux products developed by the Objectively Analyzed Air-Sea Heat Flux Project, meridional variation of the western Pacific Warm Pool (WPWP) is addressed. The results...
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| Published in | Chinese journal of oceanology and limnology Vol. 30; no. 4; pp. 684 - 689 |
|---|---|
| Main Author | |
| Format | Journal Article |
| Language | English |
| Published |
Heidelberg
Springer-Verlag
01.07.2012
SP Science Press Springer Nature B.V |
| Subjects | |
| Online Access | Get full text |
| ISSN | 0254-4059 2096-5508 1993-5005 2523-3521 |
| DOI | 10.1007/s00343-012-1209-5 |
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| Abstract | Based on 48-year (1958–2006) ocean reanalysis data of Simple Ocean Data Assimilation and 23-year (1984–2006) global ocean-surface heat flux products developed by the Objectively Analyzed Air-Sea Heat Flux Project, meridional variation of the western Pacific Warm Pool (WPWP) is addressed. The results show that there is a significant expansion of the northern edge of the WPWP in the late 1990s and early 2000s. This variation is mainly within 120°E–160°E by 8°N–20°N, we define this region (120°E-1 by 8°N–20°N) as the core region. Furthermore, analyses on upper ocean heat budget show that the short wave radiation plays a key role in the northward expansion of the northern edge of the WPWP in the core region. It is proved that the northward expansion may be caused by the change of the mixed layer which became shallower in 1994–2006 compared with 1984–1993 in the study region. The short wave radiation flux distribution within the shallower mixed layer leads to a positive anomaly in seawater temperature, promoting the northward expansion of the WPWP. |
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| AbstractList | Based on 48-year (1958-2006) ocean reanalysis data of Simple Ocean Data Assimilation and 23-year (1984-2006) global ocean-surface heat flux products developed by the Objectively Analyzed Air-Sea Heat Flux Project, meridional variation of the western Pacific Warm Pool (WPWP) is addressed. The results show that there is a significant expansion of the northern edge of the WPWP in the late 1990s and early 2000s. This variation is mainly within 120 degree E-160 degree E by 8 degree N-20 degree N, we define this region (120 degree E-1 by 8 degree N-20 degree N) as the core region. Furthermore, analyses on upper ocean heat budget show that the short wave radiation plays a key role in the northward expansion of the northern edge of the WPWP in the core region. It is proved that the northward expansion may be caused by the change of the mixed layer which became shallower in 1994-2006 compared with 1984-1993 in the study region. The short wave radiation flux distribution within the shallower mixed layer leads to a positive anomaly in seawater temperature, promoting the northward expansion of the WPWP. Based on 48-year (1958–2006) ocean reanalysis data of Simple Ocean Data Assimilation and 23-year (1984–2006) global ocean-surface heat flux products developed by the Objectively Analyzed Air-Sea Heat Flux Project, meridional variation of the western Pacific Warm Pool (WPWP) is addressed. The results show that there is a significant expansion of the northern edge of the WPWP in the late 1990s and early 2000s. This variation is mainly within 120°E–160°E by 8°N–20°N, we define this region (120°E-1 by 8°N–20°N) as the core region. Furthermore, analyses on upper ocean heat budget show that the short wave radiation plays a key role in the northward expansion of the northern edge of the WPWP in the core region. It is proved that the northward expansion may be caused by the change of the mixed layer which became shallower in 1994–2006 compared with 1984–1993 in the study region. The short wave radiation flux distribution within the shallower mixed layer leads to a positive anomaly in seawater temperature, promoting the northward expansion of the WPWP. Based on 48-year （1958-2006） ocean reanalysis data of Simple Ocean Data Assimilation and 23-year （1984-2006） global ocean-surface heat flux products developed by the Objectively Analyzed AirSea Heat Flux Project, meridional variation of the western Pacific Warm Pool （WPWP） is addressed. The results show that there is a significant expansion of the northern edge of the WPWP in the late 1990s and early 2000s. This variation is mainly within 120°E-160°E by 8°N-20°N, we define this region （120°E-160°E by 8°N-20°N） as the core region. Furthermore, analyses on upper ocean heat budget show that the short wave radiation plays a key role in the northward expansion of the northern edge of the WPWP in the core region. It is proved that the northward expansion may be caused by the change of the mixed layer which became shallower in 1994-2006 compared with 1984-1993 in the study region. The short wave radiation flux distribution within the shallower mixed layer leads to a positive anomaly in seawater temperature, promoting the northward expansion of the WPWP. |
| Author | Wang, Faming Yang, Yuxing |
| AuthorAffiliation | Key Laboratory of Ocean Circulation and Wave, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China |
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| Keywords | mixed layer western Pacific Warm Pool (WPWP) northward expansion |
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| Notes | YANG Yuxing , WANG Faming （ Key Laboratory of Ocean Circulation and Wave, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China） western Pacific Warm Pool （WPWP）; northward expansion; mixed layer 37-1150/P Based on 48-year （1958-2006） ocean reanalysis data of Simple Ocean Data Assimilation and 23-year （1984-2006） global ocean-surface heat flux products developed by the Objectively Analyzed AirSea Heat Flux Project, meridional variation of the western Pacific Warm Pool （WPWP） is addressed. The results show that there is a significant expansion of the northern edge of the WPWP in the late 1990s and early 2000s. This variation is mainly within 120°E-160°E by 8°N-20°N, we define this region （120°E-160°E by 8°N-20°N） as the core region. Furthermore, analyses on upper ocean heat budget show that the short wave radiation plays a key role in the northward expansion of the northern edge of the WPWP in the core region. It is proved that the northward expansion may be caused by the change of the mixed layer which became shallower in 1994-2006 compared with 1984-1993 in the study region. The short wave radiation flux distribution within the shallower mixed layer leads to a positive anomaly in seawater temperature, promoting the northward expansion of the WPWP. http://dx.doi.org/10.1007/s00343-012-1209-5 ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 14 content type line 23 |
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| Snippet | Based on 48-year （1958-2006） ocean reanalysis data of Simple Ocean Data Assimilation and 23-year （1984-2006） global ocean-surface heat flux products developed... Based on 48-year (1958–2006) ocean reanalysis data of Simple Ocean Data Assimilation and 23-year (1984–2006) global ocean-surface heat flux products developed... Based on 48-year (1958-2006) ocean reanalysis data of Simple Ocean Data Assimilation and 23-year (1984-2006) global ocean-surface heat flux products developed... |
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| SubjectTerms | Chemical analysis Data collection Earth and Environmental Science Earth Sciences Fluctuations Heat Heat budget Heat flux Heat transfer Marine Mixed layer Ocean temperature Oceanography Physics Radiation Seawater Short wave radiation temperature Upper ocean Water analysis Water temperature 再分析资料 后期 年代 数据同化 海洋表面 短波辐射 经向变化 西太平洋暖池 |
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| Title | Northward expansion of the western Pacific Warm Pool in late 1990s and early 2000s |
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