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• W4281479216 endingPage "1991" @default.
• W4281479216 startingPage "1969" @default.
• W4281479216 abstract "Abstract The impacts of rainy days (>24 mm) on the physics of the surface atmosphere and upper ocean are characterized in the central Pacific Ocean (140°–170°W) on the equator, where deep-cycle turbulence substantially influences the sea surface temperature and air–sea heat flux on diurnal and longer time scales. Here, rainfall is relatively weak on average (1–3 mm day −1 ), and enough rain to substantially alter the diurnal cycle of upper-ocean buoyancy only occurs on the order of once in 100 days, albeit more frequently to the west and during El Niño and boreal winter. Rainy days are associated with multiple systematic changes in the surface atmosphere, but the freshwater and the reduction in daily downwelling shortwave radiation (by ∼50 W m −2 ) are codominant and drive systematic changes in the ocean during and the day after the rainy day. These two drivers explain ensemble average reductions in the upper-ocean salinity (−0.12 psu at 1 m) and temperature (−0.16°C at 1 m) and increases in buoyancy (+0.0005 m s −2 at 1 m), which are typically confined to a shallow fresh/warm mixing layer on the order of 10 m thick in the daytime. At deeper depths, the intrinsic ocean temperature, salinity, and velocity variability make it challenging to extract an ensemble average response to rainy days in observations, but some examples from observations and large-eddy simulations suggest that rainfall can significantly reduce the vertical extent and heat flux in the deep-cycle turbulence, although the bulk energetics and buoyancy flux of the turbulence are not necessarily modified by rain. Significance Statement Rain significantly impacts social and ecological systems in many ways that are readily apparent in populated areas, but the impacts of rain over the ocean are not as well known. In this paper, sustained in situ observations over decades and highly resolved numerical simulations of ocean turbulence during a few rain events are used to characterize the impacts of rainy days on the surface–atmosphere and upper-ocean physics in the center of action of El Niño in the central equatorial Pacific. These results contribute to broader efforts to observe, understand, and accurately model the surface atmosphere, the upper ocean, and air–sea interaction in the central Pacific and thereby improve long-range weather and climate observations and predictions." @default.
• W4281479216 created "2022-05-26" @default.
• W4281479216 creator A5085040833 @default.
• W4281479216 date "2022-09-01" @default.
• W4281479216 modified "2023-10-15" @default.
• W4281479216 title "Rain Impacts on the Surface Atmosphere and Upper Ocean in the Central Equatorial Pacific" @default.
• W4281479216 cites W1686175988 @default.
• W4281479216 cites W1913555461 @default.
• W4281479216 cites W1922578668 @default.
• W4281479216 cites W1963549306 @default.
• W4281479216 cites W1967578396 @default.
• W4281479216 cites W1971781571 @default.
• W4281479216 cites W1975360915 @default.
• W4281479216 cites W1979615106 @default.
• W4281479216 cites W1985856245 @default.
• W4281479216 cites W1989537327 @default.
• W4281479216 cites W1990452437 @default.
• W4281479216 cites W1993196883 @default.
• W4281479216 cites W1994379703 @default.
• W4281479216 cites W1995871939 @default.
• W4281479216 cites W1995892971 @default.
• W4281479216 cites W2000496340 @default.
• W4281479216 cites W2010201797 @default.
• W4281479216 cites W2013900698 @default.
• W4281479216 cites W2016216840 @default.
• W4281479216 cites W2018304142 @default.
• W4281479216 cites W2018955470 @default.
• W4281479216 cites W2024187952 @default.
• W4281479216 cites W2030858832 @default.
• W4281479216 cites W2031127053 @default.
• W4281479216 cites W2040882433 @default.
• W4281479216 cites W2053616059 @default.
• W4281479216 cites W2063423292 @default.
• W4281479216 cites W2064477787 @default.
• W4281479216 cites W2068204246 @default.
• W4281479216 cites W2069560926 @default.
• W4281479216 cites W2084461152 @default.
• W4281479216 cites W2089004326 @default.
• W4281479216 cites W2091455287 @default.
• W4281479216 cites W2093595399 @default.
• W4281479216 cites W2097403444 @default.
• W4281479216 cites W2098475715 @default.
• W4281479216 cites W2100986500 @default.
• W4281479216 cites W2105914586 @default.
• W4281479216 cites W2114838592 @default.
• W4281479216 cites W2117914273 @default.
• W4281479216 cites W2121264610 @default.
• W4281479216 cites W2121673593 @default.
• W4281479216 cites W2128159534 @default.
• W4281479216 cites W2132297963 @default.
• W4281479216 cites W2137324683 @default.
• W4281479216 cites W2145201046 @default.
• W4281479216 cites W2146892358 @default.
• W4281479216 cites W2150278022 @default.
• W4281479216 cites W2160051225 @default.
• W4281479216 cites W2164092372 @default.
• W4281479216 cites W2173276343 @default.
• W4281479216 cites W2175239376 @default.
• W4281479216 cites W2178035735 @default.
• W4281479216 cites W2179108396 @default.
• W4281479216 cites W2179166521 @default.
• W4281479216 cites W2319604610 @default.
• W4281479216 cites W2495322778 @default.
• W4281479216 cites W2520546940 @default.
• W4281479216 cites W2597692941 @default.
• W4281479216 cites W2618100771 @default.
• W4281479216 cites W2621071828 @default.
• W4281479216 cites W2624385262 @default.
• W4281479216 cites W2725729834 @default.
• W4281479216 cites W2738516213 @default.
• W4281479216 cites W2749586915 @default.
• W4281479216 cites W2762227938 @default.
• W4281479216 cites W2806095947 @default.
• W4281479216 cites W2807238442 @default.
• W4281479216 cites W2883537372 @default.
• W4281479216 cites W2896439350 @default.
• W4281479216 cites W2898164139 @default.
• W4281479216 cites W2901772771 @default.
• W4281479216 cites W2905087556 @default.
• W4281479216 cites W2940024754 @default.
• W4281479216 cites W2944239970 @default.
• W4281479216 cites W2949975224 @default.
• W4281479216 cites W2950833212 @default.
• W4281479216 cites W2952137205 @default.
• W4281479216 cites W2980020044 @default.
• W4281479216 cites W2986795300 @default.
• W4281479216 cites W2990932811 @default.
• W4281479216 cites W2992005820 @default.
• W4281479216 cites W3000660099 @default.
• W4281479216 cites W3011000872 @default.
• W4281479216 cites W3040146841 @default.
• W4281479216 cites W3042741854 @default.
• W4281479216 cites W3045959668 @default.
• W4281479216 cites W3134374768 @default.
• W4281479216 cites W3134591872 @default.
• W4281479216 cites W3139102892 @default.
• W4281479216 cites W3141822946 @default.
• W4281479216 cites W3199845479 @default.

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