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- W2095535824 abstract "The large‐scale response of the Indo‐Pacific Ocean to atmospheric forcing associated with the Madden‐Julian Oscillation (MJO) is examined using an ocean general circulation model forced by canonical MJO conditions constructed from observations. The results show that for a number of equatorial areas, ocean advection processes can play an important role in determining the ocean response. In addition, mixed layer depth (MLD) variations are considerable and contribute to the sea surface temperature (SST) variability. SST variability also develops in the eastern equatorial Pacific via the propagation of ocean Kelvin waves. With regards to this variability the results suggest that advective processes, namely, meridional advection, play the most significant role. Sea level variability in the equatorial regions and eastern sides of the Indian and Pacific basins associated with the MJO is considerable. In conjunction with these sea level variations are also large variations in the Indonesian Throughflow. The results also show that the MJO forcing produces a low‐frequency rectified signal consisting of a weak cooling in the equatorial western Pacific and Indian Ocean regions, a relatively larger warming around the maritime continent, a fair amount of MLD shallowing in most of the above regions, and a westward equatorial Pacific Ocean current anomaly. In addition, the heat flux variations associated with the MJO produce systematic variations in the east‐west zonal gradient of Indian Ocean SST, which could influence the evolution of the Indian Ocean Zonal Mode. The implications and caveats associated with these results, the caveats associated with the model and forcing framework, and areas necessitating further study are discussed." @default.
- W2095535824 created "2016-06-24" @default.
- W2095535824 creator A5007801035 @default.
- W2095535824 creator A5019391361 @default.
- W2095535824 creator A5058082704 @default.
- W2095535824 date "2003-05-01" @default.
- W2095535824 modified "2023-10-15" @default.
- W2095535824 title "Indo-Pacific Ocean response to atmospheric intraseasonal variability: 1. Austral summer and the Madden-Julian Oscillation" @default.
- W2095535824 cites W1498891724 @default.
- W2095535824 cites W1965276271 @default.
- W2095535824 cites W1965889142 @default.
- W2095535824 cites W1965913330 @default.
- W2095535824 cites W1966780503 @default.
- W2095535824 cites W1967429906 @default.
- W2095535824 cites W1968709098 @default.
- W2095535824 cites W1974063055 @default.
- W2095535824 cites W1974585569 @default.
- W2095535824 cites W1976282242 @default.
- W2095535824 cites W1977116126 @default.
- W2095535824 cites W1979261581 @default.
- W2095535824 cites W1985669309 @default.
- W2095535824 cites W1985834492 @default.
- W2095535824 cites W1985867836 @default.
- W2095535824 cites W1986865911 @default.
- W2095535824 cites W1988498050 @default.
- W2095535824 cites W1993231420 @default.
- W2095535824 cites W1993905420 @default.
- W2095535824 cites W1994659182 @default.
- W2095535824 cites W2005491711 @default.
- W2095535824 cites W2007064396 @default.
- W2095535824 cites W2007358049 @default.
- W2095535824 cites W2007808376 @default.
- W2095535824 cites W2007815323 @default.
- W2095535824 cites W2010957707 @default.
- W2095535824 cites W2011365949 @default.
- W2095535824 cites W2012229267 @default.
- W2095535824 cites W2013203092 @default.
- W2095535824 cites W2016160169 @default.
- W2095535824 cites W2033609738 @default.
- W2095535824 cites W2034640254 @default.
- W2095535824 cites W2035677848 @default.
- W2095535824 cites W2041824464 @default.
- W2095535824 cites W2046804849 @default.
- W2095535824 cites W2048271710 @default.
- W2095535824 cites W2051313984 @default.
- W2095535824 cites W2054130073 @default.
- W2095535824 cites W2058017461 @default.
- W2095535824 cites W2059006152 @default.
- W2095535824 cites W2061462385 @default.
- W2095535824 cites W2062213220 @default.
- W2095535824 cites W2062914653 @default.
- W2095535824 cites W2068491339 @default.
- W2095535824 cites W2074311727 @default.
- W2095535824 cites W2077615224 @default.
- W2095535824 cites W2079340576 @default.
- W2095535824 cites W2080837504 @default.
- W2095535824 cites W2081105432 @default.
- W2095535824 cites W2081294365 @default.
- W2095535824 cites W2082001988 @default.
- W2095535824 cites W2082684467 @default.
- W2095535824 cites W2084242376 @default.
- W2095535824 cites W2089947954 @default.
- W2095535824 cites W2091897971 @default.
- W2095535824 cites W2091936442 @default.
- W2095535824 cites W2093595399 @default.
- W2095535824 cites W2095886727 @default.
- W2095535824 cites W2096223049 @default.
- W2095535824 cites W2100681014 @default.
- W2095535824 cites W2102507165 @default.
- W2095535824 cites W2108102578 @default.
- W2095535824 cites W2110138031 @default.
- W2095535824 cites W2118648278 @default.
- W2095535824 cites W2119658783 @default.
- W2095535824 cites W2121112246 @default.
- W2095535824 cites W2125529718 @default.
- W2095535824 cites W2127553837 @default.
- W2095535824 cites W2130314647 @default.
- W2095535824 cites W2131556159 @default.
- W2095535824 cites W2134257090 @default.
- W2095535824 cites W2135176773 @default.
- W2095535824 cites W2141695350 @default.
- W2095535824 cites W2142021282 @default.
- W2095535824 cites W2152873790 @default.
- W2095535824 cites W2155421514 @default.
- W2095535824 cites W2155466521 @default.
- W2095535824 cites W2162125446 @default.
- W2095535824 cites W2172524244 @default.
- W2095535824 cites W2173340763 @default.
- W2095535824 cites W2173416835 @default.
- W2095535824 cites W2173895332 @default.
- W2095535824 cites W2174609291 @default.
- W2095535824 cites W2174819551 @default.
- W2095535824 cites W2174892907 @default.
- W2095535824 cites W2175804175 @default.
- W2095535824 cites W2176118819 @default.
- W2095535824 cites W2176172641 @default.
- W2095535824 cites W2176363601 @default.
- W2095535824 cites W2176418799 @default.
- W2095535824 cites W2176756079 @default.
- W2095535824 cites W2176800941 @default.