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The Indian Ocean Dipole (IOD), is an irregular oscillation of sea surface temperatures in which the western Indian Ocean becomes alternately warmer (positive phase) and then colder (negative phase) than the eastern part of the ocean.
Subtropical Indian Ocean Dipole related anomalies over the Southeastern Indian Ocean is also suggested to impact the position of Mascarene high and thus the Indian summer monsoon. Positive (negative) Subtropical Indian Ocean dipole events during boreal winter are always followed by weak (strong) Indian Summer Monsoons.
The Madden–Julian oscillation is characterized by an eastward progression of large regions of both enhanced and suppressed tropical rainfall, observed mainly over the Indian and Pacific Ocean. The anomalous rainfall is usually first evident over the western Indian Ocean, and remains evident as it propagates over the very warm ocean waters of ...
Extent of the Indian Ocean according to the International Hydrographic Organization. This list of sovereign states and dependent territories in the Indian Ocean consists of 38 countries, with 13 in Africa, 22 in Asia, and 1 in Oceania that either border on or are in the Indian Ocean, as well as 2 European countries which administer several dependencies or overseas territories in the region.
The Indian Ocean is the third-largest of the world's five oceanic divisions, covering 70,560,000 km 2 (27,240,000 sq mi) ... (or the Indian Ocean Dipole), ...
Developing a NW-SE orientation and influenced by the Indian Ocean dipole (IOD) and the Madden-Julian oscillation (MJO), the cloudband forms when moist and warm tropical air on the Indian ocean (near Indonesia) travels towards the southeast and passes over Australia towards the western side of a high pressure system in the southeast, where they ascend over the cooler air in the mid-latitudes ...
Witnesses have revealed what they saw take place at the moment of impact during the horrifying collision between an American Airlines jet and an Army helicopter over the Potomac River. On ...
In the Indian Ocean north of the equator, tropical cyclones can form throughout the year on either side of the Indian subcontinent, although most frequently between April and June, and between October and December. The North Indian Ocean is the least active official basin, contributing only seven percent of the world's tropical cyclones.