FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2037526232> ?p ?o ?g. }

• W2037526232 endingPage "757" @default.
• W2037526232 startingPage "749" @default.
• W2037526232 abstract "Complex empirical orthogonal function (CEOF) analysis is used to investigate the coastal Kelvin wave driven Rossby wave response in the northeast Pacific. Using CEOF analysis, a spatial structure function is obtained from model upper layer thickness data. The model is a nonlinear, reduced gravity model of the northeast Pacific forced by coastal Kelvin waves originating in the equatorial Pacific. The spatial structure function is used to extract the interannual Rossby wave response from observed 300-m-depth temperature anomalies. The observed Rossby wave signal is termed the projection mode. Rossby wavelike features observed in the projection mode are order 1000 km long with most periods ranging between 2 and 4 years. The wave numbers and frequencies found are consistent with Rossby dynamics. The mean phase speed of the Rossby wavelike features within the projection mode is 1.3 cm s−1, in agreement with the theoretical Rossby wave phase speed at 40°N. Large amplitude nearshore and decreasing amplitude away from shore suggests nearshore generation of these waves. An important source of sea level variability along the east coast of North America at periods of 2–4 years was identified by Pares-Sierra and O'Brien (1989) as poleward propagating Kelvin waves. Since the Rossby wavelike features observed in the projection mode have a majority of their periods ranging between 2 and 4 years, their forcing can be attributed to long-period Kelvin waves. Spectral comparisons between the nearshore values in the projection mode and coastal sea level show greater than 90% coherence in the period band 3–4.4 years. The high coherence between coastal sea level variations and the projection mode shows that there is a strong correlation between the Rossby wavelike features within the projection mode and coastal Kelvin wave propagation. It is concluded that the Rossby waves within the projection mode are forced by coastal Kelvin wave propagation. The projection mode accounts for 47.5% of the variance in the 300-m-depth temperature anomalies. The implication of this result is that the physical mechanism of the numerical model, i.e., Rossby waves excited by coastal Kelvin wave propagation, accounts for 47.5% of the variance in the observed 300-m depth temperature anomalies." @default.
• W2037526232 created "2016-06-24" @default.
• W2037526232 creator A5027927334 @default.
• W2037526232 creator A5043797348 @default.
• W2037526232 creator A5051785628 @default.
• W2037526232 date "1991-01-15" @default.
• W2037526232 modified "2023-09-26" @default.
• W2037526232 title "Analysis of remotely forced oceanic Rossby waves off California" @default.
• W2037526232 cites W1998373005 @default.
• W2037526232 cites W2018981124 @default.
• W2037526232 cites W2033254152 @default.
• W2037526232 cites W2034672135 @default.
• W2037526232 cites W2040870535 @default.
• W2037526232 cites W2041475200 @default.
• W2037526232 cites W2043060586 @default.
• W2037526232 cites W2050010643 @default.
• W2037526232 cites W2056406073 @default.
• W2037526232 cites W2065833160 @default.
• W2037526232 cites W2070766630 @default.
• W2037526232 cites W2075853865 @default.
• W2037526232 cites W2075974917 @default.
• W2037526232 cites W2080479509 @default.
• W2037526232 cites W2085091203 @default.
• W2037526232 cites W2140602065 @default.
• W2037526232 cites W4253862496 @default.
• W2037526232 doi "https://doi.org/10.1029/90jc01973" @default.
• W2037526232 hasPublicationYear "1991" @default.
• W2037526232 type Work @default.
• W2037526232 sameAs 2037526232 @default.
• W2037526232 citedByCount "27" @default.
• W2037526232 countsByYear W20375262322014 @default.
• W2037526232 countsByYear W20375262322018 @default.
• W2037526232 countsByYear W20375262322019 @default.
• W2037526232 crossrefType "journal-article" @default.
• W2037526232 hasAuthorship W2037526232A5027927334 @default.
• W2037526232 hasAuthorship W2037526232A5043797348 @default.
• W2037526232 hasAuthorship W2037526232A5051785628 @default.
• W2037526232 hasConcept C110992570 @default.
• W2037526232 hasConcept C111368507 @default.
• W2037526232 hasConcept C127313418 @default.
• W2037526232 hasConcept C145151356 @default.
• W2037526232 hasConcept C153294291 @default.
• W2037526232 hasConcept C205649164 @default.
• W2037526232 hasConcept C49204034 @default.
• W2037526232 hasConcept C8058405 @default.
• W2037526232 hasConceptScore W2037526232C110992570 @default.
• W2037526232 hasConceptScore W2037526232C111368507 @default.
• W2037526232 hasConceptScore W2037526232C127313418 @default.
• W2037526232 hasConceptScore W2037526232C145151356 @default.
• W2037526232 hasConceptScore W2037526232C153294291 @default.
• W2037526232 hasConceptScore W2037526232C205649164 @default.
• W2037526232 hasConceptScore W2037526232C49204034 @default.
• W2037526232 hasConceptScore W2037526232C8058405 @default.
• W2037526232 hasIssue "C1" @default.
• W2037526232 hasLocation W20375262321 @default.
• W2037526232 hasOpenAccess W2037526232 @default.
• W2037526232 hasPrimaryLocation W20375262321 @default.
• W2037526232 hasRelatedWork W1538922834 @default.
• W2037526232 hasRelatedWork W2041538734 @default.
• W2037526232 hasRelatedWork W2175537541 @default.
• W2037526232 hasRelatedWork W2400441211 @default.
• W2037526232 hasRelatedWork W2744821264 @default.
• W2037526232 hasRelatedWork W2802340201 @default.
• W2037526232 hasRelatedWork W2990624757 @default.
• W2037526232 hasRelatedWork W4231494591 @default.
• W2037526232 hasRelatedWork W578940708 @default.
• W2037526232 hasRelatedWork W2522104620 @default.
• W2037526232 hasVolume "96" @default.
• W2037526232 isParatext "false" @default.
• W2037526232 isRetracted "false" @default.
• W2037526232 magId "2037526232" @default.
• W2037526232 workType "article" @default.