. The effect of stochastic surface heat fluxes on the climatology of the seasonal Meteorology; Oceanography. TIME (DAYS] SER SURFRCE TEMPERATURE. -i r i 1 1 1 1 1 1 r 2«.0 TIME (DAYS) Figure Typical year with stochastic forcing. a) The same annual heat flux cycle shown in Figure , a random daily heat flux component Q added, b) The SST over the model year. The mixed layer depth h=100 m. 27. Please note that these images are extracted from scanne
. The effect of stochastic surface heat fluxes on the climatology of the seasonal Meteorology; Oceanography. TIME (DAYS] SER SURFRCE TEMPERATURE. -i r i 1 1 1 1 1 1 r 2«.0 TIME (DAYS) Figure Typical year with stochastic forcing. a) The same annual heat flux cycle shown in Figure , a random daily heat flux component Q added, b) The SST over the model year. The mixed layer depth h=100 m. 27. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Copley, David Monterey, California: U. S. Naval Postgraduate School
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Keywords: ., bookcentury1900, booksubjectmeteorology, booksubjectoceanography
