About: Tropical Atlantic SST Dipole

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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.

Attributes	Values
rdf:type	yago:WikicatClimatePatterns yago:Abstraction100002137 yago:Cognition100023271 yago:Form105930736 yago:PsychologicalFeature100023100 yago:Structure105726345
rdfs:label	Tropical Atlantic SST Dipole (en)
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. (en)
dcterms:subject	Regional climate effects Atlantic Ocean Physical oceanography
Wikipage page ID	34028512 (xsd:integer)
Wikipage revision ID	1087430788 (xsd:integer)
Link from a Wikipage to another Wikipage	Regional climate effects Atlantic Ocean Atlantic Equatorial Mode Cyclogenesis North Brazil Current Sahel Wind stress Climate variability and change Equator Orthogonality Sub-Saharan Africa Zonal and meridional Tropical cyclone basins Cyclone North Atlantic Oscillation North Pacific Northeast Region, Brazil Pacific Ocean Ocean current Principal component analysis Atlantic Equatorial mode Hurricane Physical oceanography El Niño Ekman pumping Tropical Atlantic Variability Diabatic South America Meridional line Northern Hemisphere Southern Hemisphere Sea surface temperature Low-pressure area Thermocline Subtropics Equatorial region Easterlies ENSO ITCZ Sea-level pressure
Link from a Wikipage to an external page	http://onlinelibrary.wiley.com/doi/10.1111/j.2153-3490.1960.tb01279.x/abstract
sameAs	Tropical Atlantic SST Dipole Tropical Atlantic SST Dipole Tropical Atlantic SST Dipole Tropical Atlantic SST Dipole
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has 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. (en)
prov:wasDerivedFrom	wikipedia-en:Tropical_Atlantic_SST_Dipole?oldid=1087430788&ns=0
page length (characters) of wiki page	12974 (xsd:nonNegativeInteger)
foaf:isPrimaryTopicOf	wikipedia-en:Tropical_Atlantic_SST_Dipole
is Link from a Wikipage to another Wikipage of	Prediction and Research Moored Array in the Atlantic Outline of oceanography
is foaf:primaryTopic of	wikipedia-en:Tropical_Atlantic_SST_Dipole

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