NEC / Southeast Indian Ridge / Central Indian / Carlsberg / Stephens / Chagos-Laccadive Ridges / /
Continent
Antarctica / Africa / /
Country
Sri Lanka / Pakistan / Australia / Oman / Madagascar / Mozambique / Timor / Somalia / /
Event
Natural Disaster / M&A / /
IndustryTerm
ridge systems / monsoonal current systems / /
NaturalFeature
Gulf of Carpentaria / Arabian Sea / Persian Gulf / Mascarene Plateau / Atlantic ocean / Southern Ocean / island of Madagascar / Arabia / Timor sea / South Indian Ocean / Indonesian seas / Sverdrup stream / Pacific Ocean / Australian coast / Somalia / Red Sea / Tibetan Plateau / Broken Plateau / Indonesian islands / Bay of Bengal / Indian Ocean / Australasian Mediterranean Sea / Arafura sea / Andaman Islands / Gulf of Oman / /
Organization
Federal Government / U.S. Securities and Exchange Commission / /
Position
representative for the depth-averaged flow / /
Region
southern Africa / northern Indian Ocean / South Indian Ocean / northwestern Indian Ocean / Indian Ocean / East Madagascar / Southwest of Australia / Persian Gulf / mediterranean / southern Indian Ocean / western Australia / east Asia / /
Chapter 11 The Indian Ocean We now turn to the Indian Ocean, which is in several respects very different from the Pacific Ocean. The most striking difference is the seasonal reversal of the monsoon winds and its effects