FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1966290721> ?p ?o ?g. }

• W1966290721 endingPage "121" @default.
• W1966290721 startingPage "111" @default.
• W1966290721 abstract "The characteristics of westward copropagating features in satellite altimetry, sea surface temperature and ocean colour data are investigated throughout the global oceans between 50° north and 50° south for the period 1998–2008. A new ‘hybrid’ filtering approach allowing features with periods between 37 and 410 days to pass polewards of 20° north and south and features with periods between 37 and 205 days to pass within 20° of the equator is found to isolate features whose speed is consistent with predictions of long planetary wave theory throughout much of the oceans. Features with wavelengths between 300 and 800 km and periods between 205 and 410 days are shown to be a significant source of temperature and chlorophyll variability between 20° and 50° north and south, whilst within 20° of the equator, signals in the 800–1500 km and 37–205 days range are predominant. Between 15° and 50° north and south, observed propagation speeds are found to closely match those predicted for first-mode baroclinic Rossby waves by theory. In the equatorial Pacific and Atlantic Oceans, features with wavelengths (800–2000 km), periods (15–40 days) and phase speeds (20–50 cm s − 1 ) characteristic of tropical instability waves are preferentially observed. The amplitude and phase relationship between copropagating signals in ocean colour and altimetry and sea surface temperature and altimetry is interpreted in terms of the horizontal (meridional) advection of mean temperature and chlorophyll gradients by Rossby waves, similar to what has recently been observed for non-linear eddies at shorter length scales. The observed phase relationships are in good agreement with the range of phases expected for horizontal advection throughout much of the oceans and consistent with the sign of the mean meridional gradients of temperature and chlorophyll. These results support the view that horizontal advection (be it from waves and/or eddies) is the dominant mode of covariation of temperature and chlorophyll with sea surface height throughout most of the oceans, although the agreement between predicted and observed amplitude and phase relationships is insufficient to completely rule out vertical mechanisms in a few regions. We believe that a ‘one size fits all’ approach for global Rossby wave studies can no longer be considered valid, and although we have modified our technique to take this into account, we advocate future work to develop a fully latitudinally dependent filtering methodology. ► First global analysis of signals in sea surface height, temperature and chlorophyll. ► Significant agreement between observed signals and predictions from extended theory. ► Strong evidence for Rossby waves influencing global surface chlorophyll variability. ► Demonstrate role of both Rossby waves and eddies in observed variability. ► Reinforce the significance of the horizontal advection mechanism." @default.
• W1966290721 created "2016-06-24" @default.
• W1966290721 creator A5002520313 @default.
• W1966290721 creator A5009428799 @default.
• W1966290721 creator A5086467972 @default.
• W1966290721 date "2013-02-01" @default.
• W1966290721 modified "2023-09-24" @default.
• W1966290721 title "Manifestation of oceanic Rossby waves in long-term multiparametric satellite datasets" @default.
• W1966290721 cites W1537634431 @default.
• W1966290721 cites W1645950804 @default.
• W1966290721 cites W1657439887 @default.
• W1966290721 cites W1661612813 @default.
• W1966290721 cites W1964231350 @default.
• W1966290721 cites W1965215353 @default.
• W1966290721 cites W1965901620 @default.
• W1966290721 cites W1967165739 @default.
• W1966290721 cites W1970503413 @default.
• W1966290721 cites W1975103979 @default.
• W1966290721 cites W1976094605 @default.
• W1966290721 cites W1976332901 @default.
• W1966290721 cites W1980218150 @default.
• W1966290721 cites W1984678116 @default.
• W1966290721 cites W2007263313 @default.
• W1966290721 cites W2013689051 @default.
• W1966290721 cites W2014231250 @default.
• W1966290721 cites W2017647804 @default.
• W1966290721 cites W2021172142 @default.
• W1966290721 cites W2023321109 @default.
• W1966290721 cites W2030120338 @default.
• W1966290721 cites W2033996837 @default.
• W1966290721 cites W2038903541 @default.
• W1966290721 cites W2044416822 @default.
• W1966290721 cites W2050658323 @default.
• W1966290721 cites W2051366116 @default.
• W1966290721 cites W2051620405 @default.
• W1966290721 cites W2059707589 @default.
• W1966290721 cites W2067785578 @default.
• W1966290721 cites W2077177453 @default.
• W1966290721 cites W2085488537 @default.
• W1966290721 cites W2098741246 @default.
• W1966290721 cites W2099753271 @default.
• W1966290721 cites W2103275536 @default.
• W1966290721 cites W2109218525 @default.
• W1966290721 cites W2122112420 @default.
• W1966290721 cites W2131070146 @default.
• W1966290721 cites W2133572887 @default.
• W1966290721 cites W2159602351 @default.
• W1966290721 cites W2162691261 @default.
• W1966290721 cites W2164038112 @default.
• W1966290721 cites W2170572159 @default.
• W1966290721 cites W2172901597 @default.
• W1966290721 cites W2180178848 @default.
• W1966290721 cites W2331730236 @default.
• W1966290721 doi "https://doi.org/10.1016/j.rse.2012.10.024" @default.
• W1966290721 hasPublicationYear "2013" @default.
• W1966290721 type Work @default.
• W1966290721 sameAs 1966290721 @default.
• W1966290721 citedByCount "13" @default.
• W1966290721 countsByYear W19662907212015 @default.
• W1966290721 countsByYear W19662907212016 @default.
• W1966290721 countsByYear W19662907212017 @default.
• W1966290721 countsByYear W19662907212018 @default.
• W1966290721 countsByYear W19662907212020 @default.
• W1966290721 countsByYear W19662907212021 @default.
• W1966290721 countsByYear W19662907212022 @default.
• W1966290721 countsByYear W19662907212023 @default.
• W1966290721 crossrefType "journal-article" @default.
• W1966290721 hasAuthorship W1966290721A5002520313 @default.
• W1966290721 hasAuthorship W1966290721A5009428799 @default.
• W1966290721 hasAuthorship W1966290721A5086467972 @default.
• W1966290721 hasConcept C110992570 @default.
• W1966290721 hasConcept C111368507 @default.
• W1966290721 hasConcept C121332964 @default.
• W1966290721 hasConcept C122523270 @default.
• W1966290721 hasConcept C127313418 @default.
• W1966290721 hasConcept C12980444 @default.
• W1966290721 hasConcept C13280743 @default.
• W1966290721 hasConcept C134097258 @default.
• W1966290721 hasConcept C142672198 @default.
• W1966290721 hasConcept C145151356 @default.
• W1966290721 hasConcept C17534553 @default.
• W1966290721 hasConcept C180205008 @default.
• W1966290721 hasConcept C49040817 @default.
• W1966290721 hasConcept C49204034 @default.
• W1966290721 hasConcept C5072599 @default.
• W1966290721 hasConcept C53631411 @default.
• W1966290721 hasConcept C62520636 @default.
• W1966290721 hasConcept C6260449 @default.
• W1966290721 hasConcept C97355855 @default.
• W1966290721 hasConceptScore W1966290721C110992570 @default.
• W1966290721 hasConceptScore W1966290721C111368507 @default.
• W1966290721 hasConceptScore W1966290721C121332964 @default.
• W1966290721 hasConceptScore W1966290721C122523270 @default.
• W1966290721 hasConceptScore W1966290721C127313418 @default.
• W1966290721 hasConceptScore W1966290721C12980444 @default.
• W1966290721 hasConceptScore W1966290721C13280743 @default.
• W1966290721 hasConceptScore W1966290721C134097258 @default.
• W1966290721 hasConceptScore W1966290721C142672198 @default.

• next