. Development of a microcomputer coupled Atmospheric and Oceanic Boundary Layer prediction Meteorology; Oceanography. (o) WORK OY WHO STRESS 00 NET SURFACE BUOYANCY FLUX PLUS ABSORPTION OF SOLAH RAOlATlOM *#$$" MEAN {Pol (U2+\f^dZ = RE.(tQ) Pof jb^gz dt to-h-S A SHEAR PRODUCTION INTERIOR BUOYANCY FLUX ENTRAPMENT * BUOYANCY FLUX 0 REDISTRIBUTION () HORIZONTAL TURB. {PqJ u2 + v2 dZ -h-8 =0 c DISSIPATION VERTICAL TURB. j /°o/°W2dZ -h-8. Figure 2. Mechanical Energy Budget for the Ocean Mixed Layer efforts using the power of the computer. By varying the angle of
. Development of a microcomputer coupled Atmospheric and Oceanic Boundary Layer prediction Meteorology; Oceanography. (o) WORK OY WHO STRESS 00 NET SURFACE BUOYANCY FLUX PLUS ABSORPTION OF SOLAH RAOlATlOM *#$$" MEAN {Pol (U2+\f^dZ = RE.(tQ) Pof jb^gz dt to-h-S A SHEAR PRODUCTION INTERIOR BUOYANCY FLUX ENTRAPMENT * BUOYANCY FLUX 0 REDISTRIBUTION () HORIZONTAL TURB. {PqJ u2 + v2 dZ -h-8 =0 c DISSIPATION VERTICAL TURB. j /°o/°W2dZ -h-8. Figure 2. Mechanical Energy Budget for the Ocean Mixed Layer efforts using the power of the computer. By varying the angle of radiation (latitude), amount of radiation (month), and start time for the program, each set of output will be compared and analyzed for consistency. A typical case will then be selected and further studies will be conducted. The effects of coupled versus uncoupled oceanic mixed layer depth variations and wind speed variations will be examined. The magnitude and usefulness of this effort is illustrated in Figure 3. Outputs from the coupled model can 13. 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 Tarbet, Gary Monterey, California: U. S. Naval Postgraduate School
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Keywords: ., bookcentury1900, booksubjectmeteorology, booksubjectoceanography
