FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4286491567> ?p ?o ?g. }

• W4286491567 endingPage "2872" @default.
• W4286491567 startingPage "2853" @default.
• W4286491567 abstract "Abstract Topographic Rossby waves (TRWs) play an important role in deep-ocean dynamics and abyssal intraseasonal variations. Observational records from 15 current- and pressure-recording inverted echo sounders (CPIESs) and two moorings deployed in the northern Manila Trench (MT), South China Sea (SCS), for over 400 days were utilized to analyze the widely existing near-21-day bottom-trapped TRWs in the trench. The TRWs were generally generated in winter and summer, dominated by perturbations in the upper ocean. Kuroshio intrusion and its related variabilities contributed to the perturbations in winter, whereas the perturbations generated north of Luzon Island dominated in summer. Eddies north of Luzon propagated northwestward in the summer of 2018; however, these eddies caused the Kuroshio meanderings in the Luzon Strait (LS) in the summer of 2019. The variations in the Kuroshio path and the Kuroshio-related eddies induced TRWs in the deep ocean in regions with steep topography. However, the spatiotemporal distributions of TRWs were complex owing to the propagation of the waves. Some cases of TRWs showed no relation to the local upper-layer perturbations but propagated from adjacent regions. Some of these TRWs were induced by perturbations in the upper ocean in adjacent regions, and propagated anticlockwise in the MT with shallow water to their right, while others may be related to the intraseasonal variations in deep-water overflow in the LS and propagated northward. This study suggests that the Kuroshio and Kuroshio-related eddies significantly contribute to the dynamic processes associated with intraseasonal variations in the deep SCS through the generation of TRWs. Significance Statement Topographic Rossby waves (TRWs) are fluctuations generated when water columns travel across sloping topography under potential vorticity conservation. Based on observations of 15 current- and pressure-recording inverted echo sounders (CPIESs) and two moorings in the northern Manila Trench (MT) in the South China Sea (SCS), TRWs with periods of approximately 21 days were observed and analyzed. This study describes the generation, propagation, and spatiotemporal distribution of TRWs west of the LS and confirms that regional Kuroshio meanderings and upper eddies play important roles in the dynamic processes associated with intraseasonal variations in the deep SCS; the study may thus contribute to knowledge on the dynamic response of the abyssal current to mesoscale perturbations in the upper ocean." @default.
• W4286491567 created "2022-07-22" @default.
• W4286491567 creator A5001758622 @default.
• W4286491567 creator A5015102287 @default.
• W4286491567 creator A5017808882 @default.
• W4286491567 creator A5018977136 @default.
• W4286491567 creator A5033047776 @default.
• W4286491567 creator A5035285302 @default.
• W4286491567 creator A5046331183 @default.
• W4286491567 creator A5048142986 @default.
• W4286491567 creator A5065754009 @default.
• W4286491567 creator A5069806496 @default.
• W4286491567 creator A5078854851 @default.
• W4286491567 date "2022-11-01" @default.
• W4286491567 modified "2023-10-18" @default.
• W4286491567 title "Observation of Bottom-Trapped Topographic Rossby Waves to the West of the Luzon Strait, South China Sea" @default.
• W4286491567 cites W1582166451 @default.
• W4286491567 cites W1967892240 @default.
• W4286491567 cites W1970678342 @default.
• W4286491567 cites W1992982340 @default.
• W4286491567 cites W1995196380 @default.
• W4286491567 cites W2002735166 @default.
• W4286491567 cites W2006140268 @default.
• W4286491567 cites W2006749556 @default.
• W4286491567 cites W2045694649 @default.
• W4286491567 cites W2048211544 @default.
• W4286491567 cites W2110582205 @default.
• W4286491567 cites W2148362593 @default.
• W4286491567 cites W2172563153 @default.
• W4286491567 cites W2315184647 @default.
• W4286491567 cites W2337066296 @default.
• W4286491567 cites W2341614228 @default.
• W4286491567 cites W2343212206 @default.
• W4286491567 cites W2524536911 @default.
• W4286491567 cites W2563330503 @default.
• W4286491567 cites W2621266504 @default.
• W4286491567 cites W2745384790 @default.
• W4286491567 cites W2890709458 @default.
• W4286491567 cites W2913067656 @default.
• W4286491567 cites W2934715347 @default.
• W4286491567 cites W2939010472 @default.
• W4286491567 cites W2968051086 @default.
• W4286491567 cites W2976876770 @default.
• W4286491567 cites W2991611957 @default.
• W4286491567 cites W3080172925 @default.
• W4286491567 cites W4210595711 @default.
• W4286491567 cites W4220994115 @default.
• W4286491567 cites W4281663752 @default.
• W4286491567 cites W4306249147 @default.
• W4286491567 cites W3168989562 @default.
• W4286491567 doi "https://doi.org/10.1175/jpo-d-22-0065.1" @default.
• W4286491567 hasPublicationYear "2022" @default.
• W4286491567 type Work @default.
• W4286491567 citedByCount "2" @default.
• W4286491567 countsByYear W42864915672022 @default.
• W4286491567 countsByYear W42864915672023 @default.
• W4286491567 crossrefType "journal-article" @default.
• W4286491567 hasAuthorship W4286491567A5001758622 @default.
• W4286491567 hasAuthorship W4286491567A5015102287 @default.
• W4286491567 hasAuthorship W4286491567A5017808882 @default.
• W4286491567 hasAuthorship W4286491567A5018977136 @default.
• W4286491567 hasAuthorship W4286491567A5033047776 @default.
• W4286491567 hasAuthorship W4286491567A5035285302 @default.
• W4286491567 hasAuthorship W4286491567A5046331183 @default.
• W4286491567 hasAuthorship W4286491567A5048142986 @default.
• W4286491567 hasAuthorship W4286491567A5065754009 @default.
• W4286491567 hasAuthorship W4286491567A5069806496 @default.
• W4286491567 hasAuthorship W4286491567A5078854851 @default.
• W4286491567 hasConcept C111368507 @default.
• W4286491567 hasConcept C127313418 @default.
• W4286491567 hasConcept C134097258 @default.
• W4286491567 hasConcept C142672198 @default.
• W4286491567 hasConcept C145151356 @default.
• W4286491567 hasConcept C150320492 @default.
• W4286491567 hasConcept C153294291 @default.
• W4286491567 hasConcept C155310634 @default.
• W4286491567 hasConcept C173815673 @default.
• W4286491567 hasConcept C178790620 @default.
• W4286491567 hasConcept C179065325 @default.
• W4286491567 hasConcept C185592680 @default.
• W4286491567 hasConcept C196558001 @default.
• W4286491567 hasConcept C205649164 @default.
• W4286491567 hasConcept C2779227376 @default.
• W4286491567 hasConcept C49204034 @default.
• W4286491567 hasConceptScore W4286491567C111368507 @default.
• W4286491567 hasConceptScore W4286491567C127313418 @default.
• W4286491567 hasConceptScore W4286491567C134097258 @default.
• W4286491567 hasConceptScore W4286491567C142672198 @default.
• W4286491567 hasConceptScore W4286491567C145151356 @default.
• W4286491567 hasConceptScore W4286491567C150320492 @default.
• W4286491567 hasConceptScore W4286491567C153294291 @default.
• W4286491567 hasConceptScore W4286491567C155310634 @default.
• W4286491567 hasConceptScore W4286491567C173815673 @default.
• W4286491567 hasConceptScore W4286491567C178790620 @default.
• W4286491567 hasConceptScore W4286491567C179065325 @default.
• W4286491567 hasConceptScore W4286491567C185592680 @default.
• W4286491567 hasConceptScore W4286491567C196558001 @default.
• W4286491567 hasConceptScore W4286491567C205649164 @default.

• next