Australian monsoon: Difference between revisions
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During the "active" phase or "bursts", large regions of cloud and rain are formed, where there is a constant northwesterly wind on the north area of the trough, alongside heavy rainfall on the land, which last from about four to eight weeks. An inactive phase or "breaks" is when the monsoon trough diminishes and withdraws to the north of Australia, although light winds, sporadic showers and thunderstorm activity may occur. Later than normal monsoon arrivals, and drier ones, are generally associated with [[El Niño]] conditions in the Pacific, while [[La Niña]] is mostly associated with an early monsoon season and wetter ones as well.<ref name=BOM/> The monsoon's thickness is normally less than 1,500 metres (4,900 feet) over the sea and 2,000–2,500 metres (6,600–8,200 feet) over the land.<ref name=Britannica>{{cite web|last1=J.Smith|first1=Phillip|last2=Krishnamurti|first2=T.N |last3=Gentilli|first3= Joseph| url =https://www.britannica.com/science/Malaysian-Australian-monsoon|title=Malaysian-Australian monsoon|website= [[Britannica]] | access-date = 14 July 2023 }}</ref> |
During the "active" phase or "bursts", large regions of cloud and rain are formed, where there is a constant northwesterly wind on the north area of the trough, alongside heavy rainfall on the land, which last from about four to eight weeks. An inactive phase or "breaks" is when the monsoon trough diminishes and withdraws to the north of Australia, although light winds, sporadic showers and thunderstorm activity may occur. Later than normal monsoon arrivals, and drier ones, are generally associated with [[El Niño]] conditions in the Pacific, while [[La Niña]] is mostly associated with an early monsoon season and wetter ones as well.<ref name=BOM/> The monsoon's thickness is normally less than 1,500 metres (4,900 feet) over the sea and 2,000–2,500 metres (6,600–8,200 feet) over the land.<ref name=Britannica>{{cite web|last1=J.Smith|first1=Phillip|last2=Krishnamurti|first2=T.N |last3=Gentilli|first3= Joseph| url =https://www.britannica.com/science/Malaysian-Australian-monsoon|title=Malaysian-Australian monsoon|website= [[Britannica]] | access-date = 14 July 2023 }}</ref> |
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Although the northern Australian monsoonal bursts peak between mid-November and mid-December, they can extend well into March. The Australian monsoon rainfall variability (AUMRV) has a similar ratio in rainfall over much of the country, going as far south as the southern [[Murray–Darling Basin]]. About 28% of inter-annual AUMRV is linked with oceanic irregularity in the tropical Pacific and [[Indian Ocean]]s. Moreover, compared to the [[Asian |
Although the northern Australian monsoonal bursts peak between mid-November and mid-December, they can extend well into March. The Australian monsoon rainfall variability (AUMRV) has a similar ratio in rainfall over much of the country, going as far south as the southern [[Murray–Darling Basin]]. About 28% of inter-annual AUMRV is linked with oceanic irregularity in the tropical Pacific and [[Indian Ocean]]s. Moreover, compared to the [[East Asian Monsoon|Asian]], African and [[North American]] monsoonal regions, the AUM seems to possess the highest variation, as it is linked to [[El Niño–Southern Oscillation]], especially over northeastern Australia.<ref name=wires/> |
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==Effects== |
==Effects== |
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The monsoon seasons is generally associated with overcast conditions, extended periods of heavy rain, episodic thunderstorms and fresh to strong [[squally]] winds, which frequently lead to flooding in affected areas.<ref name=BOM/> Most of the [[fresh water]] for the sparsely populated northern Australia comes from the Australian monsoonal rains.<ref name=wires/> |
The monsoon seasons is generally associated with overcast conditions, extended periods of heavy rain, episodic thunderstorms and fresh to strong [[squally]] winds, which frequently lead to flooding in affected areas.<ref name=BOM/> Most of the [[fresh water]] for the sparsely populated northern Australia comes from the Australian monsoonal rains.<ref name=wires/> |
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Revision as of 12:55, 14 July 2023
The Australian monsoon (AUM) is a monsoon system that increases thunderstorms and rainfall over many areas of northern Australia from the far northern tropics to the semi-arid regions of the country, typically between November and mid-March (the northern Australian wet season).[1][2]
The origin of the Australian monsoon (AUM) is comparable the North African monsoon, since both develop from the seasonal motion of the Intertropical Convergence Zone (ITCZ) and the connected meridional shift in the overturning Hadley circulation, which lead to a pronounced rainfall seasonality.[2]
Mechanism
In northern Australia, the predominant wind is from the east or southeast in most occasions, which usually bring dry conditions.[1] Though during monsoon periods (between November to April), the winds change to northwesterly. When the Australian continent heats up much rapid than the surrounding ocean (the Timor, Banda and Arafura seas), low pressure systems may form, which efficaciously draw in the monsoon trough, an area of low pressure and rising air, above the hot and dry areas of northern Australia, thereby increasing humidity prior to the rains (this is known as the “build-up”).[1] The trough attracts moist air from the encompassing oceans and this inflow of moist air is referred to as the monsoon.[3]
During the "active" phase or "bursts", large regions of cloud and rain are formed, where there is a constant northwesterly wind on the north area of the trough, alongside heavy rainfall on the land, which last from about four to eight weeks. An inactive phase or "breaks" is when the monsoon trough diminishes and withdraws to the north of Australia, although light winds, sporadic showers and thunderstorm activity may occur. Later than normal monsoon arrivals, and drier ones, are generally associated with El Niño conditions in the Pacific, while La Niña is mostly associated with an early monsoon season and wetter ones as well.[3] The monsoon's thickness is normally less than 1,500 metres (4,900 feet) over the sea and 2,000–2,500 metres (6,600–8,200 feet) over the land.[4]
Although the northern Australian monsoonal bursts peak between mid-November and mid-December, they can extend well into March. The Australian monsoon rainfall variability (AUMRV) has a similar ratio in rainfall over much of the country, going as far south as the southern Murray–Darling Basin. About 28% of inter-annual AUMRV is linked with oceanic irregularity in the tropical Pacific and Indian Oceans. Moreover, compared to the Asian, African and North American monsoonal regions, the AUM seems to possess the highest variation, as it is linked to El Niño–Southern Oscillation, especially over northeastern Australia.[2]
Effects
The monsoon seasons is generally associated with overcast conditions, extended periods of heavy rain, episodic thunderstorms and fresh to strong squally winds, which frequently lead to flooding in affected areas.[3] Most of the fresh water for the sparsely populated northern Australia comes from the Australian monsoonal rains.[2]
See also
References
- ^ a b c Narsey, Sugata; Reeder, Michael (2016). "Explainer: what is the Australian monsoon?". The Conversation. Retrieved 14 July 2023.
- ^ a b c d Heidemann, Hanna; Cowan, Tim; J.Henley, Benjamin (2023). "Variability and long-term change in Australian monsoon rainfall: A review". WIREs. Retrieved 14 July 2023.
- ^ a b c "The Australian Monsoon". Bureau of Meteorology. Retrieved 14 July 2023.
- ^ J.Smith, Phillip; Krishnamurti, T.N; Gentilli, Joseph. "Malaysian-Australian monsoon". Britannica. Retrieved 14 July 2023.