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• W3041331012 endingPage "101660" @default.
• W3041331012 startingPage "101660" @default.
• W3041331012 abstract "Coupling between the atmosphere and ocean is scale-dependent. For example, in the mid-latitudes and at oceanic mesoscales (spatial scales between 10 and hundreds of kilometers), the air–sea interactions are driven by the oceanic variability, and the atmosphere responds to the changes in the sea surface temperature anomalies (SSTA), which are created by fast oceanic advection. This study explores these interactions, using a regional high-resolution atmosphere–ocean coupled model with a realistic atmospheric component and a semi-idealized oceanic model of a zonal flow. The atmospheric component consists of two nested domains: the inner domain fully coupled with the ocean model, and the outer domain one-way coupled with the observed SST. Two 2-year simulations are discussed here: one in which the oceanic isopycnals are steep and ocean currents are strong (“Strong Currents” or SC) and another with less steep isopycnals and weaker currents (“Weak Currents” or WC). Simulated mesoscale variability occurs on a wide range of spatial scales, and we distinguish large-mesoscale (hundreds of kilometers and shorter) and small-mesoscale (tens of kilometers and shorter) anomalies. The model is most applicable to the mid-latitude Southern Ocean far from any boundaries. Relationships between atmospheric variables and SSTA are studied using temporal correlations and coupling coefficients, and for both large-mesoscale and small-mesoscale anomalies. Significant positive correlations between large-mesoscale anomalies are found for following pairs of variables: equivalent neutral stability (ENS) 10-meter winds and SSTA, wind stress and SSTA, and wind stress divergence/curl and SSTA downwind/crosswind gradients. The temporal correlations are smaller for the small-mesoscale anomalies. The correlation coefficients are also higher for the model SC region, whereas the corresponding coupling coefficients are higher in the model WC region. Among all pairs, the coupling coefficients for the ENS winds and SSTA are the most consistent in time and various environmental conditions. Coupling coefficients for the wind stress and SSTA show a nearly linear dependence on the ENS wind speed. As a result, the reported variability in these coupling coefficients indicates a complex, nonlinear relationship between the wind and SST anomalies. Our numerical analysis indicates strong presence of the Vertical Mixing Mechanism involving the downward momentum mixing on both small- and large-mesoscales. In contrast, the active presence of the Pressure Adjustment Mechanism in the Marine Boundary Layer could not be confirmed on the spatial and time scales considered in this study." @default.
• W3041331012 created "2020-07-16" @default.
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• W3041331012 date "2020-09-01" @default.
• W3041331012 modified "2023-09-26" @default.
• W3041331012 title "A study of mesoscale air–sea interaction in the Southern Ocean with a regional coupled model" @default.
• W3041331012 cites W1518066253 @default.
• W3041331012 cites W1809262161 @default.
• W3041331012 cites W1963549306 @default.
• W3041331012 cites W1964247113 @default.
• W3041331012 cites W1964342496 @default.
• W3041331012 cites W1971354502 @default.
• W3041331012 cites W1972472964 @default.
• W3041331012 cites W1973526623 @default.
• W3041331012 cites W1974745955 @default.
• W3041331012 cites W1979102222 @default.
• W3041331012 cites W1985160364 @default.
• W3041331012 cites W1987598828 @default.
• W3041331012 cites W1991530696 @default.
• W3041331012 cites W1993415310 @default.
• W3041331012 cites W1993887370 @default.
• W3041331012 cites W2000966706 @default.
• W3041331012 cites W2002862759 @default.
• W3041331012 cites W2004359105 @default.
• W3041331012 cites W2009306433 @default.
• W3041331012 cites W2010644803 @default.
• W3041331012 cites W2012908222 @default.
• W3041331012 cites W2013531313 @default.
• W3041331012 cites W2020875959 @default.
• W3041331012 cites W2025293160 @default.
• W3041331012 cites W2035363503 @default.
• W3041331012 cites W2038742869 @default.
• W3041331012 cites W2039780599 @default.
• W3041331012 cites W2044036103 @default.
• W3041331012 cites W2048488219 @default.
• W3041331012 cites W2053030936 @default.
• W3041331012 cites W2060548054 @default.
• W3041331012 cites W2064152497 @default.
• W3041331012 cites W2066720902 @default.
• W3041331012 cites W2074302136 @default.
• W3041331012 cites W2079864053 @default.
• W3041331012 cites W2082628835 @default.
• W3041331012 cites W2088488961 @default.
• W3041331012 cites W2089727804 @default.
• W3041331012 cites W2092249832 @default.
• W3041331012 cites W2093401535 @default.
• W3041331012 cites W2098863440 @default.
• W3041331012 cites W2100986500 @default.
• W3041331012 cites W2104345346 @default.
• W3041331012 cites W2106984327 @default.
• W3041331012 cites W2117130932 @default.
• W3041331012 cites W2120659867 @default.
• W3041331012 cites W2128092034 @default.
• W3041331012 cites W2128217437 @default.
• W3041331012 cites W2129694430 @default.
• W3041331012 cites W2131070146 @default.
• W3041331012 cites W2133348729 @default.
• W3041331012 cites W2134430121 @default.
• W3041331012 cites W2138301110 @default.
• W3041331012 cites W2141299041 @default.
• W3041331012 cites W2148272468 @default.
• W3041331012 cites W2158070223 @default.
• W3041331012 cites W2158829590 @default.
• W3041331012 cites W2165118342 @default.
• W3041331012 cites W2166935430 @default.
• W3041331012 cites W2173892647 @default.
• W3041331012 cites W2175329654 @default.
• W3041331012 cites W2183389450 @default.
• W3041331012 cites W2227670575 @default.
• W3041331012 cites W2293053967 @default.
• W3041331012 cites W2344333489 @default.
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• W3041331012 doi "https://doi.org/10.1016/j.ocemod.2020.101660" @default.
• W3041331012 hasPublicationYear "2020" @default.
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