. An analysis of results of a high-resolution world ocean circulation model. Oceanography. CAShA 1001 IIERA1ION 10001 PABALLCL OCEAN CLIMATE UOOEL IPOCMI ONt BCGBCC • OCEAN CONTICUNATION NO. 7 POTENTIAL TEMPERATURE LATITUDE *om 30w jow low o I0E 20E ill 9* I .. 15* - J 2 7* - £ - a. bj o - «l? «* - - _n. *ow jow row A- ROBUSI niACNO^TIC HUN cmuxn intthvw < l f» sere racron • I 88 fin o niH FIELD MX 0 655 !»8 8* - I 15* - " - 2* *I75 0 * I2R 5BV •=«» 8NI 136 SB*
. An analysis of results of a high-resolution world ocean circulation model. Oceanography. CAShA 1001 IIERA1ION 10001 PABALLCL OCEAN CLIMATE UOOEL IPOCMI ONt BCGBCC • OCEAN CONTICUNATION NO. 7 POTENTIAL TEMPERATURE LATITUDE *om 30w jow low o I0E 20E ill 9* I .. 15* - J 2 7* - £ - a. bj o - «l? «* - - _n. *ow jow row A- ROBUSI niACNO^TIC HUN cmuxn intthvw < l f» sere racron • I 88 fin o niH FIELD MX 0 655 !»8 8* - I 15* - " - 2* *I75 0 * I2R 5BV •=«» 8NI 136 SB* LONGITUDE 40-W 20* 0* I0*E. Figure Zonal cross-section near 16°S latitude in the Atlantic Ocean of (a) potential temperature in °C for experiment 1 and (b) observed temperature in °C (from Pickard and Emery, 1982). 89. 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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