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Monsoon trough information


August position of the ITCZ and monsoon trough in the Pacific Ocean, depicted by area of convergent streamlines in the northern Pacific

The monsoon trough is a portion of the Intertropical Convergence Zone in the Western Pacific,[1][2] as depicted by a line on a weather map showing the locations of minimum sea level pressure,[1] and as such, is a convergence zone between the wind patterns of the southern and northern hemispheres.

Westerly monsoon winds lie in its equatorward portion while easterly trade winds exist poleward of the trough.[3] Right along its axis, heavy rains can be found which usher in the peak of a location's respective rainy season. The monsoon trough plays a role in creating many of the world's rainforests.[4]

The term monsoon trough is most commonly used in monsoonal regions of the Western Pacific such as Asia and Australia. The migration of the ITCZ/monsoon trough into a landmass heralds the beginning of the annual rainy season during summer months. Depressions and tropical cyclones often form in the vicinity of the monsoon trough, with each capable of producing a year's worth of rainfall in a matter of days.

  1. ^ a b "Monsoon trough". Glossary of Meteorology. American Meteorological Society. Archived from the original on 17 June 2009. Retrieved 4 June 2009.
  2. ^ Bin Wang. The Asian Monsoon. Retrieved 2008-05-03.
  3. ^ World Meteorological Organization. Severe Weather Information Centre. Retrieved 2008-05-03.
  4. ^ Hobgood (2008)Global Pattern of Surface Pressure and Wind. Archived 18 March 2009 at the Wayback Machine Ohio State University. Retrieved 2009-03-08.

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near-equatorial trough. Where the ITCZ is drawn into and merges with a monsoonal circulation, it is sometimes referred to as a monsoon trough (a usage that...

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as a monsoon trough develops over South-East Asia and Australasia and winds are directed toward Australia. In the Philippines, northeast monsoon is called...

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especially in northern India.[citation needed] The interaction of the monsoon trough with western disturbances may occasionally cause dense clouding and...

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2019 Townsville flood

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Isa, embedded in a stalled, but vigorously active, monsoon trough. Northerly, moisture-rich monsoonal air driven by the tropical low was encountered by...

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Anticyclone

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motion and convection along the monsoon trough or intertropical convergence zone. The divergence over the near-equatorial trough leads to air rising and moving...

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Trade winds

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doldrums, near-equatorial trough, intertropical front, or the Intertropical Convergence Zone. When located within a monsoon region, this zone of low pressure...

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1984 Pacific typhoon season

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consecutive years had their first storm develop as late as June. The monsoon trough established itself across the South China Sea eastward into the Philippine...

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1985 Pacific typhoon season

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near-equatorial, or monsoon, trough. Due to strong high pressure due its north, and the associated high winds associated with the northern Asian monsoon, strongest...

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1994 Pacific typhoon season

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an area of thunderstorm activity formed within the monsoon trough. Over the next few days, a monsoon depression formed to its southwest, steering the system...

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Typhoon Tip

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Pacific typhoon season, Tip developed out of a disturbance within the monsoon trough on October 4 near Pohnpei in Micronesia. Initially, Tropical Storm Roger...

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2002 Pacific typhoon season

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weakened. Nine storms developed in July, many of which influenced the monsoon trough over the Philippines to produce heavy rainfall and deadly flooding....

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2023 Atlantic hurricane season

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(2023 USD). An area of disturbed weather within the eastern Pacific monsoon trough developed into a broad low-pressure area over the far southwestern Caribbean...

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Pressure system

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with the Intertropical Convergence Zone, it is known as a monsoon trough. Monsoon troughs reach their northerly extent in August and their southerly...

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1981 Pacific typhoon season

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airport. The monsoon trough became well-established along 20 degrees north latitude. To the east of Phyllis, part of the monsoon trough shifted east towards...

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to the dry air caused by compressional heating. The movement of the monsoon trough, or Intertropical Convergence Zone, brings rainy seasons to savannah...

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it be a depression in the Intertropical Convergence Zone (ITCZ) or monsoon trough, a broad surface front, or an outflow boundary, a low level feature...

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North American monsoon

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North American monsoon, variously known as the Southwest monsoon, the Mexican monsoon, the New Mexican monsoon, or the Arizona monsoon is a pattern of...

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1989 Pacific typhoon season

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extensive monsoon trough had become established from the Bay of Bengal eastward into the South China Sea. Typhoon Brenda developed from this trough over the...

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2003 Pacific typhoon season

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persisted along the monsoon trough between Luzon and Guam, developing into a tropical depression on October 17. The same monsoon trough later spawned Typhoon...

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Climate of Indonesia

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amounts of rain throughout many parts of the Malay Archipelago. See also monsoon trough. Prevailing wind patterns interact with local topographic conditions...

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1987 Pacific typhoon season

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to a weak surface circulation that formed on June 24 as part of the monsoon trough 370 km (230 mi) northwest of Truk. A second area of disturbed weather...

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1999 Pacific typhoon season

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accidents. The sixth tropical depression of the season formed in the monsoon trough to the east of the Philippines on June 1. The system intensified as...

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rainfall during mid-season when the intertropical convergence zone or monsoon trough moves poleward of their location during the middle of the warm season;...

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