Matches in SemOpenAlex for { <https://semopenalex.org/work/W2017003476> ?p ?o ?g. }
- W2017003476 endingPage "137" @default.
- W2017003476 startingPage "120" @default.
- W2017003476 abstract "A seasonal simulation from a medium-resolution ocean general circulation mode (OGCM) is used to investigate the vertical structure variability of the Southeast Pacific (SEP). The focus is on the extra-tropical Rossby wave (ETRW) variability and associated forcing mechanism. Some aspects of the model mean state are validated from available observations, which justifies a vertical mode decomposition of the model variability. The analysis of the baroclinic mode contributions to sea level indicates that the gravest mode is dominant over most of the domain at all frequencies. Annual variability is on average twice as large as the semi-annual variability which is confined near the coast for all the modes. The first baroclinic mode contribution to the annual cycle exhibits a clear westward propagation north of the critical latitude. The higher-order modes only contribute near the coast where they are associated with vertically propagating energy. The residual variability, which is the energy at all timescales other than annual and semi-annual periods peaks offshore between ∼20°S and ∼30°S for all baroclinic modes. The third baroclinic mode also exhibits a relative maximum variability off the coast of Peru south of the critical latitude of the annual cycle (∼13°S), where the Peru–Chile Undercurrent is the most intense. Sensitivity experiments to the atmospheric and boundary forcing suggest that the residual variability results from the non-linear interaction between annual Rossby waves and the mean flow, while the annual ETRWs in the model result from the summed-contribution from both the local wind stress and remote equatorial forcing. Overall the study extends the classical analysis of sea level variability in the SEP based on linear theory, and suggests that the peculiarities of the baroclinic modes need to be taken into account for interpreting the sea level variability and understanding its connection with the equatorial variability." @default.
- W2017003476 created "2016-06-24" @default.
- W2017003476 creator A5001411188 @default.
- W2017003476 creator A5023544841 @default.
- W2017003476 creator A5040026915 @default.
- W2017003476 creator A5066835757 @default.
- W2017003476 creator A5089611570 @default.
- W2017003476 date "2008-10-01" @default.
- W2017003476 modified "2023-10-15" @default.
- W2017003476 title "Vertical structure variability in a seasonal simulation of a medium-resolution regional model of the Eastern South Pacific" @default.
- W2017003476 cites W1964208519 @default.
- W2017003476 cites W1972360824 @default.
- W2017003476 cites W1972518607 @default.
- W2017003476 cites W1972997336 @default.
- W2017003476 cites W1984268795 @default.
- W2017003476 cites W1992914682 @default.
- W2017003476 cites W1994796172 @default.
- W2017003476 cites W1997409853 @default.
- W2017003476 cites W2003149632 @default.
- W2017003476 cites W2008134543 @default.
- W2017003476 cites W2010063281 @default.
- W2017003476 cites W2011601793 @default.
- W2017003476 cites W2012731639 @default.
- W2017003476 cites W2027570610 @default.
- W2017003476 cites W2029598829 @default.
- W2017003476 cites W2043893894 @default.
- W2017003476 cites W2049756167 @default.
- W2017003476 cites W2052066227 @default.
- W2017003476 cites W2057445227 @default.
- W2017003476 cites W2061243209 @default.
- W2017003476 cites W2061675037 @default.
- W2017003476 cites W2062914653 @default.
- W2017003476 cites W2069197937 @default.
- W2017003476 cites W2096814879 @default.
- W2017003476 cites W2098743982 @default.
- W2017003476 cites W2103275536 @default.
- W2017003476 cites W2104684730 @default.
- W2017003476 cites W2119172733 @default.
- W2017003476 cites W2122112420 @default.
- W2017003476 cites W2135878067 @default.
- W2017003476 cites W2144640818 @default.
- W2017003476 cites W2154221216 @default.
- W2017003476 cites W2154779252 @default.
- W2017003476 cites W2159747121 @default.
- W2017003476 cites W2172406523 @default.
- W2017003476 cites W2172901597 @default.
- W2017003476 cites W2173680414 @default.
- W2017003476 cites W2175492814 @default.
- W2017003476 cites W2179379460 @default.
- W2017003476 cites W2179655310 @default.
- W2017003476 cites W2181061944 @default.
- W2017003476 cites W4237631404 @default.
- W2017003476 doi "https://doi.org/10.1016/j.pocean.2008.10.014" @default.
- W2017003476 hasPublicationYear "2008" @default.
- W2017003476 type Work @default.
- W2017003476 sameAs 2017003476 @default.
- W2017003476 citedByCount "20" @default.
- W2017003476 countsByYear W20170034762012 @default.
- W2017003476 countsByYear W20170034762013 @default.
- W2017003476 countsByYear W20170034762014 @default.
- W2017003476 countsByYear W20170034762016 @default.
- W2017003476 countsByYear W20170034762017 @default.
- W2017003476 countsByYear W20170034762018 @default.
- W2017003476 countsByYear W20170034762019 @default.
- W2017003476 countsByYear W20170034762020 @default.
- W2017003476 countsByYear W20170034762021 @default.
- W2017003476 countsByYear W20170034762023 @default.
- W2017003476 crossrefType "journal-article" @default.
- W2017003476 hasAuthorship W2017003476A5001411188 @default.
- W2017003476 hasAuthorship W2017003476A5023544841 @default.
- W2017003476 hasAuthorship W2017003476A5040026915 @default.
- W2017003476 hasAuthorship W2017003476A5066835757 @default.
- W2017003476 hasAuthorship W2017003476A5089611570 @default.
- W2017003476 hasConcept C100858432 @default.
- W2017003476 hasConcept C110992570 @default.
- W2017003476 hasConcept C111368507 @default.
- W2017003476 hasConcept C111919701 @default.
- W2017003476 hasConcept C114148465 @default.
- W2017003476 hasConcept C122523270 @default.
- W2017003476 hasConcept C127313418 @default.
- W2017003476 hasConcept C13280743 @default.
- W2017003476 hasConcept C145151356 @default.
- W2017003476 hasConcept C162284963 @default.
- W2017003476 hasConcept C18101618 @default.
- W2017003476 hasConcept C197115733 @default.
- W2017003476 hasConcept C29712183 @default.
- W2017003476 hasConcept C39432304 @default.
- W2017003476 hasConcept C41008148 @default.
- W2017003476 hasConcept C48677424 @default.
- W2017003476 hasConcept C49204034 @default.
- W2017003476 hasConcept C53631411 @default.
- W2017003476 hasConcept C74501621 @default.
- W2017003476 hasConcept C91586092 @default.
- W2017003476 hasConceptScore W2017003476C100858432 @default.
- W2017003476 hasConceptScore W2017003476C110992570 @default.
- W2017003476 hasConceptScore W2017003476C111368507 @default.
- W2017003476 hasConceptScore W2017003476C111919701 @default.
- W2017003476 hasConceptScore W2017003476C114148465 @default.