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Statements

Subject Item
dbr:Tropical_Atlantic_SST_Dipole
rdf:type
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Tropical Atlantic SST Dipole
rdfs:comment
The Tropical Atlantic SST Dipole refers to a cross-equatorial sea surface temperature (SST) pattern that appears dominant on decadal timescales. It has a period of about 12 years, with the SST anomalies manifesting their most pronounced features around 10–15 degrees of latitude off of the Equator. It is also referred to as the interhemispheric SST gradient or the Meridional Atlantic mode.
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dbc:Regional_climate_effects dbc:Physical_oceanography dbc:Atlantic_Ocean
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34028512
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1087430788
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dbr:Pacific_Ocean dbr:Cyclogenesis dbr:Atlantic_Equatorial_Mode dbr:South_America dbr:Diabatic dbr:Zonal_and_meridional dbc:Atlantic_Ocean dbr:Sea-level_pressure dbr:Sahel dbr:Low-pressure_area dbr:Principal_component_analysis dbr:Easterlies dbr:North_Pacific dbr:Atlantic_hurricane dbr:El_Niño dbr:Climate_variability_and_change dbr:Atlantic_Equatorial_mode dbr:Sea_surface_temperature dbr:Cyclone dbr:Wind_stress dbr:Tropical_Atlantic_Variability dbr:Northern_Hemisphere dbr:Ocean_current dbr:ITCZ dbc:Physical_oceanography dbr:Ekman_pumping dbc:Regional_climate_effects dbr:Thermocline dbr:North_Brazil_Current dbr:Subtropics dbr:Tropical_cyclone_basins dbr:Equator dbr:Southern_Hemisphere dbr:Orthogonality dbr:Sub-Saharan_Africa dbr:Equatorial_region dbr:North_Atlantic_Oscillation dbr:ENSO dbr:Northeast_Region,_Brazil dbr:Meridional_line
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dbo:abstract
The Tropical Atlantic SST Dipole refers to a cross-equatorial sea surface temperature (SST) pattern that appears dominant on decadal timescales. It has a period of about 12 years, with the SST anomalies manifesting their most pronounced features around 10–15 degrees of latitude off of the Equator. It is also referred to as the interhemispheric SST gradient or the Meridional Atlantic mode. This decadal-scale SST pattern constitutes one of the key features of SST variability in the Tropical Atlantic Ocean. Another one is the Atlantic Equatorial Mode, which occurs in the zonal (east-west) direction at interannual timescales, with sea surface temperature and heat content anomalies being observed in the eastern equatorial basin. Its importance in climate dynamics and decadal-scale climate prediction is evident when investigating its impact on adjacent continental regions such as the Northeast Brazil, the Sahel as well as its influence on North Atlantic cyclogenesis.
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