Indian Ocean Dipole. Indian Ocean Dipole (IOD) is an atmosphereocean coupled phenomenon in the tropical Indian Ocean (like the El Nino is in the tropical Pacific) characterised by a difference in seasurface temperatures Characteristics of IOD IOD is the difference between the temperature of eastern (Bay of Bengal) and the western Indian Ocean (Arabian Sea).
IOD is the difference between the temperature of the eastern (Bay of Bengal) and the western Indian Ocean (Arabian Sea) This temperature difference results in pressure difference which results inflowing of winds between eastern and western parts of the Indian Ocean A ‘positive IOD’ — or simply ‘IOD’ — is associated with cooler than normal Indian Ocean Dipole Read More ».
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Published 20180227Estimated Reading Time 11 minsThe Indian Ocean Dipole is a leading phenomenon of climate variability in the tropics which affects the global climate.
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Discovered at the very end of the 20th century the Indian Ocean Dipole (IOD) is a mode of natural climate variability that arises out of coupled ocean–atmosphere interaction in the Indian Ocean It is associated with some of the largest changes of ocean–atmosphere state over the equatorial Indian Ocean on interannual time scales.
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The Indian Ocean Dipole (IOD) is defined by the difference in sea surface temperature between two areas (or poles hence a dipole) – a western pole in the Arabian Sea (western Indian Ocean) and an eastern pole in the eastern Indian Ocean south of Indonesia The IOD affects the climate of Australia and other countries that surround the Indian Ocean Basin and is a significant.
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PDF fileThe Indian Ocean dipole (IOD) also referred to as the Indian Ocean Zonal Mode has received much attention since its discovery at the end of the twentieth century (eg Saji et al 1999 Webster et al 1999 Murtugudde et al 2000) As an intrinsic mode of variability of tropical Indian Ocean it has significant climate impacts across broad spa.