Matches in SemOpenAlex for { <https://semopenalex.org/work/W3193830032> ?p ?o ?g. }
- W3193830032 endingPage "61" @default.
- W3193830032 startingPage "1" @default.
- W3193830032 abstract "Abstract This study examines the role of the relative wind (RW) effect (wind relative to ocean current) in the regional ocean circulation and extratropical storm track in the South Indian Ocean. Comparison of two high-resolution regional coupled model simulations with/without the RW effect reveals that the most conspicuous ocean circulation response is the significant weakening of the overly energetic anticyclonic standing eddy off Port Elizabeth, South Africa, a biased feature ascribed to upstream retroflection of the Agulhas Current (AC). This opens a pathway through which the AC transports the warm and salty water mass from the subtropics, yielding marked increases in sea surface temperature (SST), upward turbulent heat flux (THF), and meridional SST gradient in the Agulhas retroflection region. These thermodynamic and dynamic changes are accompanied by the robust strengthening of the local low-tropospheric baroclinicity and the baroclinic wave activity in the atmosphere. Examination of the composite lifecycle of synoptic-scale storms subjected to the high THF events indicates a robust strengthening of the extratropical storms far downstream. Energetics calculations for the atmosphere suggest that the baroclinic energy conversion from the basic flow is the chief source of increased eddy available potential energy, which is subsequently converted to eddy kinetic energy, providing for the growth of transient baroclinic waves. Overall, the results suggest that the mechanical and thermal air-sea interactions are inherently and inextricably linked together to substantially influence the extratropical storm tracks in the South Indian Ocean." @default.
- W3193830032 created "2021-08-30" @default.
- W3193830032 creator A5031807181 @default.
- W3193830032 creator A5041524854 @default.
- W3193830032 creator A5045304397 @default.
- W3193830032 creator A5087723951 @default.
- W3193830032 creator A5090783675 @default.
- W3193830032 date "2021-08-25" @default.
- W3193830032 modified "2023-10-08" @default.
- W3193830032 title "Impacts of ocean currents on the South Indian Ocean extratropical storm track through the relative wind effect" @default.
- W3193830032 cites W1518066253 @default.
- W3193830032 cites W1870166365 @default.
- W3193830032 cites W1963549306 @default.
- W3193830032 cites W1963854497 @default.
- W3193830032 cites W1966981265 @default.
- W3193830032 cites W1970937204 @default.
- W3193830032 cites W1978241036 @default.
- W3193830032 cites W1978388108 @default.
- W3193830032 cites W1979299009 @default.
- W3193830032 cites W1984619077 @default.
- W3193830032 cites W1985157606 @default.
- W3193830032 cites W1986236687 @default.
- W3193830032 cites W1987314552 @default.
- W3193830032 cites W1989942040 @default.
- W3193830032 cites W1990116443 @default.
- W3193830032 cites W1992825131 @default.
- W3193830032 cites W1995337603 @default.
- W3193830032 cites W1995871939 @default.
- W3193830032 cites W2000966706 @default.
- W3193830032 cites W2001025768 @default.
- W3193830032 cites W2003663561 @default.
- W3193830032 cites W2004917297 @default.
- W3193830032 cites W2012827201 @default.
- W3193830032 cites W2015862255 @default.
- W3193830032 cites W2018663920 @default.
- W3193830032 cites W2028979275 @default.
- W3193830032 cites W2029048330 @default.
- W3193830032 cites W2033500929 @default.
- W3193830032 cites W2040221902 @default.
- W3193830032 cites W2046953059 @default.
- W3193830032 cites W2048747697 @default.
- W3193830032 cites W2050917322 @default.
- W3193830032 cites W2051377221 @default.
- W3193830032 cites W2052472981 @default.
- W3193830032 cites W2053040264 @default.
- W3193830032 cites W2054012124 @default.
- W3193830032 cites W2060548054 @default.
- W3193830032 cites W2060613078 @default.
- W3193830032 cites W2062695009 @default.
- W3193830032 cites W2069195661 @default.
- W3193830032 cites W2072228305 @default.
- W3193830032 cites W2073401570 @default.
- W3193830032 cites W2075165750 @default.
- W3193830032 cites W2081216378 @default.
- W3193830032 cites W2082405640 @default.
- W3193830032 cites W2084698730 @default.
- W3193830032 cites W2086044846 @default.
- W3193830032 cites W2086903500 @default.
- W3193830032 cites W2091888384 @default.
- W3193830032 cites W2098743982 @default.
- W3193830032 cites W2100986500 @default.
- W3193830032 cites W2103009057 @default.
- W3193830032 cites W2116442714 @default.
- W3193830032 cites W2119007429 @default.
- W3193830032 cites W2119818057 @default.
- W3193830032 cites W2121264610 @default.
- W3193830032 cites W2121745948 @default.
- W3193830032 cites W2127874835 @default.
- W3193830032 cites W2131070146 @default.
- W3193830032 cites W2149675166 @default.
- W3193830032 cites W2153499851 @default.
- W3193830032 cites W2162161505 @default.
- W3193830032 cites W2165411109 @default.
- W3193830032 cites W2167080687 @default.
- W3193830032 cites W2168832918 @default.
- W3193830032 cites W2172782380 @default.
- W3193830032 cites W2172798192 @default.
- W3193830032 cites W2174204990 @default.
- W3193830032 cites W2175329654 @default.
- W3193830032 cites W2175701662 @default.
- W3193830032 cites W2178029576 @default.
- W3193830032 cites W2180942909 @default.
- W3193830032 cites W2183389450 @default.
- W3193830032 cites W2186784637 @default.
- W3193830032 cites W2194036184 @default.
- W3193830032 cites W2210562210 @default.
- W3193830032 cites W2301236322 @default.
- W3193830032 cites W2463070645 @default.
- W3193830032 cites W2495381740 @default.
- W3193830032 cites W2517784939 @default.
- W3193830032 cites W2531838422 @default.
- W3193830032 cites W2548021534 @default.
- W3193830032 cites W2549828088 @default.
- W3193830032 cites W2557685753 @default.
- W3193830032 cites W2562756005 @default.
- W3193830032 cites W2604125915 @default.
- W3193830032 cites W2606882059 @default.
- W3193830032 cites W2610448000 @default.