FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2883647946> ?p ?o ?g. }

• W2883647946 endingPage "7884" @default.
• W2883647946 startingPage "7863" @default.
• W2883647946 abstract "Ocean heat uptake is the primary heat sink of the globe and modulates its surface warming rate. In situ observations during the past half century documented obvious multidecadal variations in the upper-ocean heat content (0–400 m; OHC 400 ) of the Indian Ocean (IO). The observed OHC 400 showed an increase of (5.9 ± 2.5) × 10 21 J decade −1 during 1965–79, followed by a decrease of (−5.2 ± 2.5) × 10 21 J decade −1 during 1980–96, and a rapid increase of (13.6 ± 1.1) × 10 21 J decade −1 during 2000–14. These variations are faithfully reproduced by an Indo-Pacific simulation of an ocean general circulation model (OGCM), and insights into the underlying mechanisms are gained through OGCM experiments. The Pacific wind forcing through the Indonesian Throughflow (ITF) was the leading driver of the basin-integrated OHC 400 increase during 1965–79 and the decrease during 1980–96, whereas after 2000 local wind and heat flux forcing within the IO made a larger contribution. The ITF heat transport is primarily dictated by Pacific trade winds. It directly affects the south IO, after which the signatures can enter the north IO through the meridional heat transport of the western boundary current. The prevailing warming of the western-to-central IO for 2000–14 was largely induced by equatorial easterly wind trends, Ekman downwelling off the equator, and northeasterly wind trends over the west Asia–East Africa coastal region. The increasing downward longwave radiation, probably reflecting anthropogenic greenhouse gas forcing, overcame the decreasing surface shortwave radiation and also made a significant contribution to the rapid upper-IO warming after 2000." @default.
• W2883647946 created "2018-08-03" @default.
• W2883647946 creator A5024326128 @default.
• W2883647946 creator A5033550581 @default.
• W2883647946 creator A5038836690 @default.
• W2883647946 creator A5083983357 @default.
• W2883647946 creator A5088846266 @default.
• W2883647946 date "2018-10-01" @default.
• W2883647946 modified "2023-10-16" @default.
• W2883647946 title "Multidecadal Changes of the Upper Indian Ocean Heat Content during 1965–2016" @default.
• W2883647946 cites W1484099348 @default.
• W2883647946 cites W1494084570 @default.
• W2883647946 cites W1553680878 @default.
• W2883647946 cites W1597462914 @default.
• W2883647946 cites W1843078453 @default.
• W2883647946 cites W1860063347 @default.
• W2883647946 cites W1901487749 @default.
• W2883647946 cites W1953632413 @default.
• W2883647946 cites W1966350456 @default.
• W2883647946 cites W1967014163 @default.
• W2883647946 cites W1970327765 @default.
• W2883647946 cites W1970708461 @default.
• W2883647946 cites W1972747475 @default.
• W2883647946 cites W1974038018 @default.
• W2883647946 cites W1983702205 @default.
• W2883647946 cites W1985619924 @default.
• W2883647946 cites W1987988199 @default.
• W2883647946 cites W1994064426 @default.
• W2883647946 cites W1999281562 @default.
• W2883647946 cites W2001926902 @default.
• W2883647946 cites W2004595181 @default.
• W2883647946 cites W2006165291 @default.
• W2883647946 cites W2011727210 @default.
• W2883647946 cites W2018304142 @default.
• W2883647946 cites W2018876477 @default.
• W2883647946 cites W2022330015 @default.
• W2883647946 cites W2026271766 @default.
• W2883647946 cites W2030846661 @default.
• W2883647946 cites W2032517234 @default.
• W2883647946 cites W2032963331 @default.
• W2883647946 cites W2039751512 @default.
• W2883647946 cites W2040948837 @default.
• W2883647946 cites W2044037219 @default.
• W2883647946 cites W2048792023 @default.
• W2883647946 cites W2051416171 @default.
• W2883647946 cites W2051880259 @default.
• W2883647946 cites W2052146662 @default.
• W2883647946 cites W2053132433 @default.
• W2883647946 cites W2053641591 @default.
• W2883647946 cites W2054302554 @default.
• W2883647946 cites W2054979942 @default.
• W2883647946 cites W2055151040 @default.
• W2883647946 cites W2063383542 @default.
• W2883647946 cites W2066075084 @default.
• W2883647946 cites W2069460427 @default.
• W2883647946 cites W2072228305 @default.
• W2883647946 cites W2076889589 @default.
• W2883647946 cites W2082001988 @default.
• W2883647946 cites W2082878393 @default.
• W2883647946 cites W2083059450 @default.
• W2883647946 cites W2083178128 @default.
• W2883647946 cites W2083522655 @default.
• W2883647946 cites W2093828408 @default.
• W2883647946 cites W2097536848 @default.
• W2883647946 cites W2103140451 @default.
• W2883647946 cites W2107705106 @default.
• W2883647946 cites W2111418993 @default.
• W2883647946 cites W2113264898 @default.
• W2883647946 cites W2115260777 @default.
• W2883647946 cites W2121264610 @default.
• W2883647946 cites W2121745948 @default.
• W2883647946 cites W2137520579 @default.
• W2883647946 cites W2142383510 @default.
• W2883647946 cites W2143780283 @default.
• W2883647946 cites W2146487757 @default.
• W2883647946 cites W2146703591 @default.
• W2883647946 cites W2149288172 @default.
• W2883647946 cites W2152928439 @default.
• W2883647946 cites W2153463079 @default.
• W2883647946 cites W2163654917 @default.
• W2883647946 cites W2165242200 @default.
• W2883647946 cites W2172324090 @default.
• W2883647946 cites W2173251738 @default.
• W2883647946 cites W2173720459 @default.
• W2883647946 cites W2174733190 @default.
• W2883647946 cites W2175236913 @default.
• W2883647946 cites W2176510221 @default.
• W2883647946 cites W2179379460 @default.
• W2883647946 cites W2215379395 @default.
• W2883647946 cites W2223123948 @default.
• W2883647946 cites W2262955851 @default.
• W2883647946 cites W2263496280 @default.
• W2883647946 cites W2282261199 @default.
• W2883647946 cites W2292443591 @default.
• W2883647946 cites W2311612550 @default.
• W2883647946 cites W2334140573 @default.
• W2883647946 cites W2394879936 @default.
• W2883647946 cites W2442930273 @default.

• next