. An analysis of results of a high-resolution world ocean circulation model. Oceanography. 5 ON I00« 90* 80W A- 1/2 OEG B0BU5T OIAGMOSTIC RUN, CtMIUH INItHvAL • I W SCALE FACTOR • 1 70W 3 TP REST MtlU HIN fieidhax 4H /SNI 177 CASEA 2001 ITERATION 100001 Parallel OCEam CLIMATE uOOEl (POCu) rui f OCGOEE ?OSt 0 OCCAM COMibiM nor. NO. 2 POTENTIAL TEMPERATURE LEVEL BOW J0» 60* t>0\«. •MJM IOOW 90W SOW 70W A- 1/2 OEG ROBUST DIAGNOSTIC RUN,FREE THERM coniolh inilhval • i m fielo hin • SCALE FACTOR • 1M FIELD MAX- 2t» 49 7«jm> Fig


. An analysis of results of a high-resolution world ocean circulation model. Oceanography. 5 ON I00« 90* 80W A- 1/2 OEG B0BU5T OIAGMOSTIC RUN, CtMIUH INItHvAL • I W SCALE FACTOR • 1 70W 3 TP REST MtlU HIN fieidhax 4H /SNI 177 CASEA 2001 ITERATION 100001 Parallel OCEam CLIMATE uOOEl (POCu) rui f OCGOEE ?OSt 0 OCCAM COMibiM nor. NO. 2 POTENTIAL TEMPERATURE LEVEL BOW J0» 60* t>0\«. •MJM IOOW 90W SOW 70W A- 1/2 OEG ROBUST DIAGNOSTIC RUN,FREE THERM coniolh inilhval • i m fielo hin • SCALE FACTOR • 1M FIELD MAX- 2t» 49 7«jm> Figure Potential temperature in °C at in depth in the Gulf Stream region (a) for experiment 3 and (b) for experiment 4. 104. 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 Barton, Wesley Monterey, California: U. S. Naval Postgraduate School


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