The responses of the Hadley circulation to different meridional SST structures in the seasonal cycle
The meridional structure of sea surface temperature (SST) plays an important role in determining the variations of the Hadley circulation (HC). The quantitative differences in the HC caused by the changing meridional structures of SST over seasonal cycles remain unclear. To determine the quantitativ...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Feng, Juan [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2017 |
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| Rechteinformationen: |
Nutzungsrecht: © 2017. American Geophysical Union. All Rights Reserved. |
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| Schlagwörter: |
equatorially asymmetric variation |
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| Übergeordnetes Werk: |
Enthalten in: Journal of geophysical research / D - Washington, DC : Union, 1984, 122(2017), 15, Seite 7785-7799 |
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| Übergeordnetes Werk: |
volume:122 ; year:2017 ; number:15 ; pages:7785-7799 |
| Links: |
|---|
| DOI / URN: |
10.1002/2017JD026953 |
|---|
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| 245 | 1 | 4 | |a The responses of the Hadley circulation to different meridional SST structures in the seasonal cycle |
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| 520 | |a The meridional structure of sea surface temperature (SST) plays an important role in determining the variations of the Hadley circulation (HC). The quantitative differences in the HC caused by the changing meridional structures of SST over seasonal cycles remain unclear. To determine the quantitative response of the HC to the meridional structure of SST during the seasonal cycle, this study decomposes the variations of the SST and HC into two components: equatorially asymmetric components (i.e., SEA for SST and HEA for HC) and equatorially symmetric components (i.e., SES for SST and HES for HC). Variations in HEA (HES) are closely associated with those in SEA (SES). In this study, five atmospheric reanalyses and two SST reanalyses are analyzed, focusing on the period of 1979–2013. The response amplitude of HEA to SEA is about four times than that of HES to SES in most of the reanalyses. This result provides a possible explanation for the dominance of the equatorially asymmetric mode over the variability of the HC during the seasonal march. The impact of meridional structures of tropical SST on the Hadley circulation (HC) is quantitatively evaluated during the seasonal cycle The amplitude of the HC response to the equatorially asymmetric SST is four times than that of the equatorially symmetric SST The NCEP1 reanalysis shows limitations in depicting the seasonal cycle of the equatorially symmetric variations of the HC | ||
| 540 | |a Nutzungsrecht: © 2017. American Geophysical Union. All Rights Reserved. | ||
| 650 | 4 | |a equatorially asymmetric variation | |
| 650 | 4 | |a equatorially symmetric variation | |
| 650 | 4 | |a sea surface temperature | |
| 650 | 4 | |a Hadley circulation | |
| 650 | 4 | |a seasonal cycle | |
| 650 | 4 | |a Temperature effects | |
| 650 | 4 | |a Sea surface | |
| 650 | 4 | |a Surface temperatures | |
| 650 | 4 | |a Variability | |
| 650 | 4 | |a Amplitude | |
| 650 | 4 | |a Circulation | |
| 650 | 4 | |a Components | |
| 650 | 4 | |a Studies | |
| 650 | 4 | |a Structures | |
| 650 | 4 | |a Surface temperature | |
| 650 | 4 | |a Tropical environment | |
| 650 | 4 | |a Seasons | |
| 650 | 4 | |a Asymmetry | |
| 650 | 4 | |a Sea surface temperature | |
| 650 | 4 | |a Sea surface temperatures | |
| 650 | 4 | |a Seasonal variations | |
| 700 | 1 | |a Li, Jianping |4 oth | |
| 700 | 1 | |a Jin, Feifei |4 oth | |
| 700 | 1 | |a Zhao, Sen |4 oth | |
| 700 | 1 | |a Xie, Fei |4 oth | |
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| 856 | 4 | 1 | |u http://dx.doi.org/10.1002/2017JD026953 |3 Volltext |
| 856 | 4 | 2 | |u http://onlinelibrary.wiley.com/doi/10.1002/2017JD026953/abstract |
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10.1002/2017JD026953 doi PQ20171228 (DE-627)OLC1997847612 (DE-599)GBVOLC1997847612 (PRQ)p1370-7422415840fffd8b1d18c964f172b439528eaf9822f20de360bb39f8f8d7586d0 (KEY)0137985220170000122001507785responsesofthehadleycirculationtodifferentmeridion DE-627 ger DE-627 rakwb eng 550 DNB Feng, Juan verfasserin aut The responses of the Hadley circulation to different meridional SST structures in the seasonal cycle 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The meridional structure of sea surface temperature (SST) plays an important role in determining the variations of the Hadley circulation (HC). The quantitative differences in the HC caused by the changing meridional structures of SST over seasonal cycles remain unclear. To determine the quantitative response of the HC to the meridional structure of SST during the seasonal cycle, this study decomposes the variations of the SST and HC into two components: equatorially asymmetric components (i.e., SEA for SST and HEA for HC) and equatorially symmetric components (i.e., SES for SST and HES for HC). Variations in HEA (HES) are closely associated with those in SEA (SES). In this study, five atmospheric reanalyses and two SST reanalyses are analyzed, focusing on the period of 1979–2013. The response amplitude of HEA to SEA is about four times than that of HES to SES in most of the reanalyses. This result provides a possible explanation for the dominance of the equatorially asymmetric mode over the variability of the HC during the seasonal march. The impact of meridional structures of tropical SST on the Hadley circulation (HC) is quantitatively evaluated during the seasonal cycle The amplitude of the HC response to the equatorially asymmetric SST is four times than that of the equatorially symmetric SST The NCEP1 reanalysis shows limitations in depicting the seasonal cycle of the equatorially symmetric variations of the HC Nutzungsrecht: © 2017. American Geophysical Union. All Rights Reserved. equatorially asymmetric variation equatorially symmetric variation sea surface temperature Hadley circulation seasonal cycle Temperature effects Sea surface Surface temperatures Variability Amplitude Circulation Components Studies Structures Surface temperature Tropical environment Seasons Asymmetry Sea surface temperature Sea surface temperatures Seasonal variations Li, Jianping oth Jin, Feifei oth Zhao, Sen oth Xie, Fei oth Enthalten in Journal of geophysical research / D Washington, DC : Union, 1984 122(2017), 15, Seite 7785-7799 (DE-627)130444391 (DE-600)710256-2 (DE-576)015978818 2169-897X nnns volume:122 year:2017 number:15 pages:7785-7799 http://dx.doi.org/10.1002/2017JD026953 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2017JD026953/abstract https://search.proquest.com/docview/1931706322 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 AR 122 2017 15 7785-7799 |
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10.1002/2017JD026953 doi PQ20171228 (DE-627)OLC1997847612 (DE-599)GBVOLC1997847612 (PRQ)p1370-7422415840fffd8b1d18c964f172b439528eaf9822f20de360bb39f8f8d7586d0 (KEY)0137985220170000122001507785responsesofthehadleycirculationtodifferentmeridion DE-627 ger DE-627 rakwb eng 550 DNB Feng, Juan verfasserin aut The responses of the Hadley circulation to different meridional SST structures in the seasonal cycle 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The meridional structure of sea surface temperature (SST) plays an important role in determining the variations of the Hadley circulation (HC). The quantitative differences in the HC caused by the changing meridional structures of SST over seasonal cycles remain unclear. To determine the quantitative response of the HC to the meridional structure of SST during the seasonal cycle, this study decomposes the variations of the SST and HC into two components: equatorially asymmetric components (i.e., SEA for SST and HEA for HC) and equatorially symmetric components (i.e., SES for SST and HES for HC). Variations in HEA (HES) are closely associated with those in SEA (SES). In this study, five atmospheric reanalyses and two SST reanalyses are analyzed, focusing on the period of 1979–2013. The response amplitude of HEA to SEA is about four times than that of HES to SES in most of the reanalyses. This result provides a possible explanation for the dominance of the equatorially asymmetric mode over the variability of the HC during the seasonal march. The impact of meridional structures of tropical SST on the Hadley circulation (HC) is quantitatively evaluated during the seasonal cycle The amplitude of the HC response to the equatorially asymmetric SST is four times than that of the equatorially symmetric SST The NCEP1 reanalysis shows limitations in depicting the seasonal cycle of the equatorially symmetric variations of the HC Nutzungsrecht: © 2017. American Geophysical Union. All Rights Reserved. equatorially asymmetric variation equatorially symmetric variation sea surface temperature Hadley circulation seasonal cycle Temperature effects Sea surface Surface temperatures Variability Amplitude Circulation Components Studies Structures Surface temperature Tropical environment Seasons Asymmetry Sea surface temperature Sea surface temperatures Seasonal variations Li, Jianping oth Jin, Feifei oth Zhao, Sen oth Xie, Fei oth Enthalten in Journal of geophysical research / D Washington, DC : Union, 1984 122(2017), 15, Seite 7785-7799 (DE-627)130444391 (DE-600)710256-2 (DE-576)015978818 2169-897X nnns volume:122 year:2017 number:15 pages:7785-7799 http://dx.doi.org/10.1002/2017JD026953 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2017JD026953/abstract https://search.proquest.com/docview/1931706322 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 AR 122 2017 15 7785-7799 |
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10.1002/2017JD026953 doi PQ20171228 (DE-627)OLC1997847612 (DE-599)GBVOLC1997847612 (PRQ)p1370-7422415840fffd8b1d18c964f172b439528eaf9822f20de360bb39f8f8d7586d0 (KEY)0137985220170000122001507785responsesofthehadleycirculationtodifferentmeridion DE-627 ger DE-627 rakwb eng 550 DNB Feng, Juan verfasserin aut The responses of the Hadley circulation to different meridional SST structures in the seasonal cycle 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The meridional structure of sea surface temperature (SST) plays an important role in determining the variations of the Hadley circulation (HC). The quantitative differences in the HC caused by the changing meridional structures of SST over seasonal cycles remain unclear. To determine the quantitative response of the HC to the meridional structure of SST during the seasonal cycle, this study decomposes the variations of the SST and HC into two components: equatorially asymmetric components (i.e., SEA for SST and HEA for HC) and equatorially symmetric components (i.e., SES for SST and HES for HC). Variations in HEA (HES) are closely associated with those in SEA (SES). In this study, five atmospheric reanalyses and two SST reanalyses are analyzed, focusing on the period of 1979–2013. The response amplitude of HEA to SEA is about four times than that of HES to SES in most of the reanalyses. This result provides a possible explanation for the dominance of the equatorially asymmetric mode over the variability of the HC during the seasonal march. The impact of meridional structures of tropical SST on the Hadley circulation (HC) is quantitatively evaluated during the seasonal cycle The amplitude of the HC response to the equatorially asymmetric SST is four times than that of the equatorially symmetric SST The NCEP1 reanalysis shows limitations in depicting the seasonal cycle of the equatorially symmetric variations of the HC Nutzungsrecht: © 2017. American Geophysical Union. All Rights Reserved. equatorially asymmetric variation equatorially symmetric variation sea surface temperature Hadley circulation seasonal cycle Temperature effects Sea surface Surface temperatures Variability Amplitude Circulation Components Studies Structures Surface temperature Tropical environment Seasons Asymmetry Sea surface temperature Sea surface temperatures Seasonal variations Li, Jianping oth Jin, Feifei oth Zhao, Sen oth Xie, Fei oth Enthalten in Journal of geophysical research / D Washington, DC : Union, 1984 122(2017), 15, Seite 7785-7799 (DE-627)130444391 (DE-600)710256-2 (DE-576)015978818 2169-897X nnns volume:122 year:2017 number:15 pages:7785-7799 http://dx.doi.org/10.1002/2017JD026953 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2017JD026953/abstract https://search.proquest.com/docview/1931706322 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 AR 122 2017 15 7785-7799 |
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10.1002/2017JD026953 doi PQ20171228 (DE-627)OLC1997847612 (DE-599)GBVOLC1997847612 (PRQ)p1370-7422415840fffd8b1d18c964f172b439528eaf9822f20de360bb39f8f8d7586d0 (KEY)0137985220170000122001507785responsesofthehadleycirculationtodifferentmeridion DE-627 ger DE-627 rakwb eng 550 DNB Feng, Juan verfasserin aut The responses of the Hadley circulation to different meridional SST structures in the seasonal cycle 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The meridional structure of sea surface temperature (SST) plays an important role in determining the variations of the Hadley circulation (HC). The quantitative differences in the HC caused by the changing meridional structures of SST over seasonal cycles remain unclear. To determine the quantitative response of the HC to the meridional structure of SST during the seasonal cycle, this study decomposes the variations of the SST and HC into two components: equatorially asymmetric components (i.e., SEA for SST and HEA for HC) and equatorially symmetric components (i.e., SES for SST and HES for HC). Variations in HEA (HES) are closely associated with those in SEA (SES). In this study, five atmospheric reanalyses and two SST reanalyses are analyzed, focusing on the period of 1979–2013. The response amplitude of HEA to SEA is about four times than that of HES to SES in most of the reanalyses. This result provides a possible explanation for the dominance of the equatorially asymmetric mode over the variability of the HC during the seasonal march. The impact of meridional structures of tropical SST on the Hadley circulation (HC) is quantitatively evaluated during the seasonal cycle The amplitude of the HC response to the equatorially asymmetric SST is four times than that of the equatorially symmetric SST The NCEP1 reanalysis shows limitations in depicting the seasonal cycle of the equatorially symmetric variations of the HC Nutzungsrecht: © 2017. American Geophysical Union. All Rights Reserved. equatorially asymmetric variation equatorially symmetric variation sea surface temperature Hadley circulation seasonal cycle Temperature effects Sea surface Surface temperatures Variability Amplitude Circulation Components Studies Structures Surface temperature Tropical environment Seasons Asymmetry Sea surface temperature Sea surface temperatures Seasonal variations Li, Jianping oth Jin, Feifei oth Zhao, Sen oth Xie, Fei oth Enthalten in Journal of geophysical research / D Washington, DC : Union, 1984 122(2017), 15, Seite 7785-7799 (DE-627)130444391 (DE-600)710256-2 (DE-576)015978818 2169-897X nnns volume:122 year:2017 number:15 pages:7785-7799 http://dx.doi.org/10.1002/2017JD026953 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2017JD026953/abstract https://search.proquest.com/docview/1931706322 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 AR 122 2017 15 7785-7799 |
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10.1002/2017JD026953 doi PQ20171228 (DE-627)OLC1997847612 (DE-599)GBVOLC1997847612 (PRQ)p1370-7422415840fffd8b1d18c964f172b439528eaf9822f20de360bb39f8f8d7586d0 (KEY)0137985220170000122001507785responsesofthehadleycirculationtodifferentmeridion DE-627 ger DE-627 rakwb eng 550 DNB Feng, Juan verfasserin aut The responses of the Hadley circulation to different meridional SST structures in the seasonal cycle 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The meridional structure of sea surface temperature (SST) plays an important role in determining the variations of the Hadley circulation (HC). The quantitative differences in the HC caused by the changing meridional structures of SST over seasonal cycles remain unclear. To determine the quantitative response of the HC to the meridional structure of SST during the seasonal cycle, this study decomposes the variations of the SST and HC into two components: equatorially asymmetric components (i.e., SEA for SST and HEA for HC) and equatorially symmetric components (i.e., SES for SST and HES for HC). Variations in HEA (HES) are closely associated with those in SEA (SES). In this study, five atmospheric reanalyses and two SST reanalyses are analyzed, focusing on the period of 1979–2013. The response amplitude of HEA to SEA is about four times than that of HES to SES in most of the reanalyses. This result provides a possible explanation for the dominance of the equatorially asymmetric mode over the variability of the HC during the seasonal march. The impact of meridional structures of tropical SST on the Hadley circulation (HC) is quantitatively evaluated during the seasonal cycle The amplitude of the HC response to the equatorially asymmetric SST is four times than that of the equatorially symmetric SST The NCEP1 reanalysis shows limitations in depicting the seasonal cycle of the equatorially symmetric variations of the HC Nutzungsrecht: © 2017. American Geophysical Union. All Rights Reserved. equatorially asymmetric variation equatorially symmetric variation sea surface temperature Hadley circulation seasonal cycle Temperature effects Sea surface Surface temperatures Variability Amplitude Circulation Components Studies Structures Surface temperature Tropical environment Seasons Asymmetry Sea surface temperature Sea surface temperatures Seasonal variations Li, Jianping oth Jin, Feifei oth Zhao, Sen oth Xie, Fei oth Enthalten in Journal of geophysical research / D Washington, DC : Union, 1984 122(2017), 15, Seite 7785-7799 (DE-627)130444391 (DE-600)710256-2 (DE-576)015978818 2169-897X nnns volume:122 year:2017 number:15 pages:7785-7799 http://dx.doi.org/10.1002/2017JD026953 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2017JD026953/abstract https://search.proquest.com/docview/1931706322 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 AR 122 2017 15 7785-7799 |
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Enthalten in Journal of geophysical research / D 122(2017), 15, Seite 7785-7799 volume:122 year:2017 number:15 pages:7785-7799 |
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The quantitative differences in the HC caused by the changing meridional structures of SST over seasonal cycles remain unclear. To determine the quantitative response of the HC to the meridional structure of SST during the seasonal cycle, this study decomposes the variations of the SST and HC into two components: equatorially asymmetric components (i.e., SEA for SST and HEA for HC) and equatorially symmetric components (i.e., SES for SST and HES for HC). Variations in HEA (HES) are closely associated with those in SEA (SES). In this study, five atmospheric reanalyses and two SST reanalyses are analyzed, focusing on the period of 1979–2013. The response amplitude of HEA to SEA is about four times than that of HES to SES in most of the reanalyses. This result provides a possible explanation for the dominance of the equatorially asymmetric mode over the variability of the HC during the seasonal march. The impact of meridional structures of tropical SST on the Hadley circulation (HC) is quantitatively evaluated during the seasonal cycle The amplitude of the HC response to the equatorially asymmetric SST is four times than that of the equatorially symmetric SST The NCEP1 reanalysis shows limitations in depicting the seasonal cycle of the equatorially symmetric variations of the HC</subfield></datafield><datafield tag="540" ind1=" " ind2=" "><subfield code="a">Nutzungsrecht: © 2017. American Geophysical Union. 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Feng, Juan ddc 550 misc equatorially asymmetric variation misc equatorially symmetric variation misc sea surface temperature misc Hadley circulation misc seasonal cycle misc Temperature effects misc Sea surface misc Surface temperatures misc Variability misc Amplitude misc Circulation misc Components misc Studies misc Structures misc Surface temperature misc Tropical environment misc Seasons misc Asymmetry misc Sea surface temperature misc Sea surface temperatures misc Seasonal variations The responses of the Hadley circulation to different meridional SST structures in the seasonal cycle |
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550 DNB The responses of the Hadley circulation to different meridional SST structures in the seasonal cycle equatorially asymmetric variation equatorially symmetric variation sea surface temperature Hadley circulation seasonal cycle Temperature effects Sea surface Surface temperatures Variability Amplitude Circulation Components Studies Structures Surface temperature Tropical environment Seasons Asymmetry Sea surface temperature Sea surface temperatures Seasonal variations |
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ddc 550 misc equatorially asymmetric variation misc equatorially symmetric variation misc sea surface temperature misc Hadley circulation misc seasonal cycle misc Temperature effects misc Sea surface misc Surface temperatures misc Variability misc Amplitude misc Circulation misc Components misc Studies misc Structures misc Surface temperature misc Tropical environment misc Seasons misc Asymmetry misc Sea surface temperature misc Sea surface temperatures misc Seasonal variations |
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ddc 550 misc equatorially asymmetric variation misc equatorially symmetric variation misc sea surface temperature misc Hadley circulation misc seasonal cycle misc Temperature effects misc Sea surface misc Surface temperatures misc Variability misc Amplitude misc Circulation misc Components misc Studies misc Structures misc Surface temperature misc Tropical environment misc Seasons misc Asymmetry misc Sea surface temperature misc Sea surface temperatures misc Seasonal variations |
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The responses of the Hadley circulation to different meridional SST structures in the seasonal cycle |
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The responses of the Hadley circulation to different meridional SST structures in the seasonal cycle |
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responses of the hadley circulation to different meridional sst structures in the seasonal cycle |
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The responses of the Hadley circulation to different meridional SST structures in the seasonal cycle |
| abstract |
The meridional structure of sea surface temperature (SST) plays an important role in determining the variations of the Hadley circulation (HC). The quantitative differences in the HC caused by the changing meridional structures of SST over seasonal cycles remain unclear. To determine the quantitative response of the HC to the meridional structure of SST during the seasonal cycle, this study decomposes the variations of the SST and HC into two components: equatorially asymmetric components (i.e., SEA for SST and HEA for HC) and equatorially symmetric components (i.e., SES for SST and HES for HC). Variations in HEA (HES) are closely associated with those in SEA (SES). In this study, five atmospheric reanalyses and two SST reanalyses are analyzed, focusing on the period of 1979–2013. The response amplitude of HEA to SEA is about four times than that of HES to SES in most of the reanalyses. This result provides a possible explanation for the dominance of the equatorially asymmetric mode over the variability of the HC during the seasonal march. The impact of meridional structures of tropical SST on the Hadley circulation (HC) is quantitatively evaluated during the seasonal cycle The amplitude of the HC response to the equatorially asymmetric SST is four times than that of the equatorially symmetric SST The NCEP1 reanalysis shows limitations in depicting the seasonal cycle of the equatorially symmetric variations of the HC |
| abstractGer |
The meridional structure of sea surface temperature (SST) plays an important role in determining the variations of the Hadley circulation (HC). The quantitative differences in the HC caused by the changing meridional structures of SST over seasonal cycles remain unclear. To determine the quantitative response of the HC to the meridional structure of SST during the seasonal cycle, this study decomposes the variations of the SST and HC into two components: equatorially asymmetric components (i.e., SEA for SST and HEA for HC) and equatorially symmetric components (i.e., SES for SST and HES for HC). Variations in HEA (HES) are closely associated with those in SEA (SES). In this study, five atmospheric reanalyses and two SST reanalyses are analyzed, focusing on the period of 1979–2013. The response amplitude of HEA to SEA is about four times than that of HES to SES in most of the reanalyses. This result provides a possible explanation for the dominance of the equatorially asymmetric mode over the variability of the HC during the seasonal march. The impact of meridional structures of tropical SST on the Hadley circulation (HC) is quantitatively evaluated during the seasonal cycle The amplitude of the HC response to the equatorially asymmetric SST is four times than that of the equatorially symmetric SST The NCEP1 reanalysis shows limitations in depicting the seasonal cycle of the equatorially symmetric variations of the HC |
| abstract_unstemmed |
The meridional structure of sea surface temperature (SST) plays an important role in determining the variations of the Hadley circulation (HC). The quantitative differences in the HC caused by the changing meridional structures of SST over seasonal cycles remain unclear. To determine the quantitative response of the HC to the meridional structure of SST during the seasonal cycle, this study decomposes the variations of the SST and HC into two components: equatorially asymmetric components (i.e., SEA for SST and HEA for HC) and equatorially symmetric components (i.e., SES for SST and HES for HC). Variations in HEA (HES) are closely associated with those in SEA (SES). In this study, five atmospheric reanalyses and two SST reanalyses are analyzed, focusing on the period of 1979–2013. The response amplitude of HEA to SEA is about four times than that of HES to SES in most of the reanalyses. This result provides a possible explanation for the dominance of the equatorially asymmetric mode over the variability of the HC during the seasonal march. The impact of meridional structures of tropical SST on the Hadley circulation (HC) is quantitatively evaluated during the seasonal cycle The amplitude of the HC response to the equatorially asymmetric SST is four times than that of the equatorially symmetric SST The NCEP1 reanalysis shows limitations in depicting the seasonal cycle of the equatorially symmetric variations of the HC |
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The responses of the Hadley circulation to different meridional SST structures in the seasonal cycle |
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