1. ULSW that remains in the DWBC dilutes as it moves equatorward . 2. This cold, high-pressure air mass then travels equatorward . 3. The deep convection continued to build along with the strong equatorward outflow. 4. Thus, tropical storms seldom swirl to life equatorward of 8 degrees latitude. 5. The current is an equatorward flowing current that carries cold and relatively fresh subantarctic water. 6. Meanwhile, mid-latitudinal storm tracks in the temperate zones increased and moved equatorward . 7. The resulting Sverdrup transport is equatorward . 8. Warm equatorial sea surface temperatures lower surface air pressure which induces more equatorward flow than normal. 9. An equatorward heat flux is induced, decreasing potential vorticity and pressure anomalies and yielding cyclolysis. 10. A polar front may form approximately along the equatorward edge of the high-level polar jet.
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