Southeast Indian Ridge / NEC / EMC / Central Indian / Carlsberg / Stephens / Chagos-Laccadive Ridges / /
Continent
Africa / Antarctica / /
Country
Oman / Mozambique / Sri Lanka / Pakistan / Australia / Madagascar / Timor / Somalia / /
Event
Natural Disaster / M&A / /
IndustryTerm
ridge systems / monsoonal current systems / /
NaturalFeature
Gulf of Carpentaria / Arabian Sea / Persian Gulf / Atlantic ocean / Southern Ocean / Arabia / Australian coast / Red Sea / Somalia / Broken Plateau / Indonesian islands / Bay of Bengal / Andaman Islands / Mascarene Plateau / Kerguelen Islands / island of Madagascar / Timor sea / Malacca Strait / Indonesian seas / South Indian Ocean / Pacific Ocean / Sverdrup stream / Tibetan Plateau / Indian Ocean / Australasian Mediterranean Sea / Arafura sea / Gulf of Oman / /
Organization
U.S. Securities and Exchange Commission / Federal Government / British Meteorological Office / /
Position
representative for the depth-averaged flow / /
ProvinceOrState
Tasmania / Zanzibar / /
Region
southern Sri Lanka / northern Indian Ocean / northwestern Indian Ocean / Indian Ocean / northern Australia / Persian Gulf / west coast / east Asia / southern Africa / South Indian Ocean / southern Asia / East Madagascar / eastern Madagascar / Southwest of Australia / southern Indian Ocean / mediterranean / western Australia / western Indian Ocean / /
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