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• W2009744985 abstract "Abstract The monthly surface heat budget and wind stress are calculated from three‐hourly meteorological data obtained at OWS B from 1946 to 1974 using formulae based on the best available measurements, and are then compared with earlier estimates. The surface heating is compared with the monthly heat storage in the water column calculated from hydrographic casts from 1964 to 1973. In spite of the scatter in the individual monthly heat storage values, the mean seasonal cycle agrees well with that of the surface flux. The residual, attributed to advection, is highly variable and does not have a strong seasonal cycle at this location. The long‐term heat loss from the ocean to the atmosphere at OWS B is found to be 28 W m−2, much smaller than the 98 W m−2 loss computed from the same data using Bunker's widely accepted formulae. The difference is accounted for by Bunker's 28% underestimate of the incoming short‐wave radiation and his 74 and 43% overestimates of the outgoing sensible and latent heat fluxes, respectively. Similarly, at OWS P, we find a net heat gain of 32 W m−2, compared with a loss of 21 Wm−2 by Bunker's formulae. If the surface heat flux at mid‐to‐high latitudes is revised, then currently accepted estimates of the oceanic meridional heat flux must also be revised." @default.
• W2009744985 created "2016-06-24" @default.
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• W2009744985 date "1984-03-01" @default.
• W2009744985 modified "2023-10-13" @default.
• W2009744985 title "The heat budget at ocean weather station<i>Bravo</i>" @default.
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• W2009744985 doi "https://doi.org/10.1080/07055900.1984.9649181" @default.
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