FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2180620766> ?p ?o ?g. }

• W2180620766 endingPage "1806" @default.
• W2180620766 startingPage "1786" @default.
• W2180620766 abstract "This study attempts to reproduce the salient features of the variability in the depth of the thermocline in the marginally eddy-resolving Parallel Ocean Climate Model (POCM) of Semtner and Chervin, using a simple linear vorticity model that only permits local Ekman pumping and the propagation of long Rossby waves. The dynamic upper-ocean variability in the POCM is examined in response to changes in daily European Centre for Medium-Range Weather Forecasts wind stresses across the tropical and subtropical Pacific Ocean (31°S–31°N) between 1983 and 1989. The POCM provides a complete and physically consistent representation of the state of the Pacific Ocean, with the phase of the thermocline depth anomalies being consistent with the observed El Niño/La Niña variations in the near-equatorial zone and southwest Pacific during the decade. A series of vorticity model sensitivity experiments, incorporating scaled Rossby wave speeds based on recent observations from the TOPEX/Poseidon satellite altimeter, is used to examine and compare the phase and amplitude variations in the depth of the internal surface against changes in the depth of the 14°C isotherm (D14, used as a proxy for the depth of the thermocline, or pycnocline) as simulated in the POCM. This study demonstrates that the simple linear vorticity model can reproduce the Pacific Ocean thermocline depth anomalies in the interior of the subtropical gyres as simulated by the POCM. These variations are both qualitatively and quantitatively consistent with an ocean forced by only Ekman pumping and Rossby waves that traverse the basin, with isolated topographic and background influences. Further, a number of experiments demonstrate that the phase similarities, from correlation analyses, between results from the POCM and those from the simple dynamical model are statistically significant (at the 95% level) across the majority of the 11°S, 11°N, and 21°N transects in the western, central, or eastern Pacific basin. At 11° and 21° latitude, the amplitude of the variability is similarly comparable across much of the basin. The model is generally less successful at 31° latitude where higher baroclinic modes of the mean flow become important." @default.
• W2180620766 created "2016-06-24" @default.
• W2180620766 creator A5033579815 @default.
• W2180620766 creator A5034180550 @default.
• W2180620766 date "2001-07-01" @default.
• W2180620766 modified "2023-10-14" @default.
• W2180620766 title "Can Pacific Ocean Thermocline Depth Anomalies Be Simulated by a Simple Linear Vorticity Model?" @default.
• W2180620766 cites W1966837318 @default.
• W2180620766 cites W1973776704 @default.
• W2180620766 cites W1975017436 @default.
• W2180620766 cites W1981669700 @default.
• W2180620766 cites W1985937382 @default.
• W2180620766 cites W1989872308 @default.
• W2180620766 cites W1994270612 @default.
• W2180620766 cites W1998385183 @default.
• W2180620766 cites W1998920780 @default.
• W2180620766 cites W2004324590 @default.
• W2180620766 cites W2004656500 @default.
• W2180620766 cites W2012502901 @default.
• W2180620766 cites W2027485125 @default.
• W2180620766 cites W2027710320 @default.
• W2180620766 cites W2031127053 @default.
• W2180620766 cites W2038903541 @default.
• W2180620766 cites W2049040721 @default.
• W2180620766 cites W2051282586 @default.
• W2180620766 cites W2060584417 @default.
• W2180620766 cites W2064376429 @default.
• W2180620766 cites W2083886652 @default.
• W2180620766 cites W2087060090 @default.
• W2180620766 cites W2087458387 @default.
• W2180620766 cites W2093000609 @default.
• W2180620766 cites W2102777270 @default.
• W2180620766 cites W2103275536 @default.
• W2180620766 cites W2116098321 @default.
• W2180620766 cites W2145533184 @default.
• W2180620766 cites W2147440604 @default.
• W2180620766 cites W2158610056 @default.
• W2180620766 cites W2161372764 @default.
• W2180620766 cites W2170572159 @default.
• W2180620766 cites W2172901597 @default.
• W2180620766 cites W2175097533 @default.
• W2180620766 cites W4248415553 @default.
• W2180620766 doi "https://doi.org/10.1175/1520-0485(2001)031<1786:cpotda>2.0.co;2" @default.
• W2180620766 hasPublicationYear "2001" @default.
• W2180620766 type Work @default.
• W2180620766 sameAs 2180620766 @default.
• W2180620766 citedByCount "11" @default.
• W2180620766 countsByYear W21806207662016 @default.
• W2180620766 countsByYear W21806207662018 @default.
• W2180620766 countsByYear W21806207662020 @default.
• W2180620766 countsByYear W21806207662021 @default.
• W2180620766 countsByYear W21806207662022 @default.
• W2180620766 crossrefType "journal-article" @default.
• W2180620766 hasAuthorship W2180620766A5033579815 @default.
• W2180620766 hasAuthorship W2180620766A5034180550 @default.
• W2180620766 hasBestOaLocation W21806207661 @default.
• W2180620766 hasConcept C105824904 @default.
• W2180620766 hasConcept C111368507 @default.
• W2180620766 hasConcept C121332964 @default.
• W2180620766 hasConcept C127313418 @default.
• W2180620766 hasConcept C130333735 @default.
• W2180620766 hasConcept C134097258 @default.
• W2180620766 hasConcept C140820882 @default.
• W2180620766 hasConcept C14168384 @default.
• W2180620766 hasConcept C142672198 @default.
• W2180620766 hasConcept C145151356 @default.
• W2180620766 hasConcept C149348798 @default.
• W2180620766 hasConcept C150320492 @default.
• W2180620766 hasConcept C153294291 @default.
• W2180620766 hasConcept C154808844 @default.
• W2180620766 hasConcept C157331469 @default.
• W2180620766 hasConcept C187599188 @default.
• W2180620766 hasConcept C200114574 @default.
• W2180620766 hasConcept C25924097 @default.
• W2180620766 hasConcept C30380174 @default.
• W2180620766 hasConcept C38349280 @default.
• W2180620766 hasConcept C49204034 @default.
• W2180620766 hasConcept C505870484 @default.
• W2180620766 hasConcept C57879066 @default.
• W2180620766 hasConcept C7228185 @default.
• W2180620766 hasConcept C86803240 @default.
• W2180620766 hasConceptScore W2180620766C105824904 @default.
• W2180620766 hasConceptScore W2180620766C111368507 @default.
• W2180620766 hasConceptScore W2180620766C121332964 @default.
• W2180620766 hasConceptScore W2180620766C127313418 @default.
• W2180620766 hasConceptScore W2180620766C130333735 @default.
• W2180620766 hasConceptScore W2180620766C134097258 @default.
• W2180620766 hasConceptScore W2180620766C140820882 @default.
• W2180620766 hasConceptScore W2180620766C14168384 @default.
• W2180620766 hasConceptScore W2180620766C142672198 @default.
• W2180620766 hasConceptScore W2180620766C145151356 @default.
• W2180620766 hasConceptScore W2180620766C149348798 @default.
• W2180620766 hasConceptScore W2180620766C150320492 @default.
• W2180620766 hasConceptScore W2180620766C153294291 @default.
• W2180620766 hasConceptScore W2180620766C154808844 @default.
• W2180620766 hasConceptScore W2180620766C157331469 @default.
• W2180620766 hasConceptScore W2180620766C187599188 @default.
• W2180620766 hasConceptScore W2180620766C200114574 @default.

• next