Oceanography Study Guide Sample Pages

Thermohaline circulation is mainly vertical. It is driven by the formation and sinking of deep water in the Greenland-Iceland-Norwegian Sea, and is probably responsible for the large flow of surface water past Indonesia, from the Pacific to the Indian Ocean. Deep and shallow currents Adapted from http---www.rapid.ac.uk- sis-popups-currents_thc.php.jpg Page 263 2018 TRIAL EDITION Copyright Wet Paper Publications Sa mple page