General wind patterns in Indonesia - Winds in the tropics will range from the extreme tropics to the lowest tropics. These winds are called Northeast Commercial Winds in the Northern Hemisphere, and Southeastern Commercial Winds in the Southern Hemisphere.
Commercial winds carry a lot of water vapor as they blow in the open sea. However, in some parts of the Earth's surface , commercial winds change direction due to the influence of the local environment.
In Indonesia, which is geographically located between the continents (Asia և Australia) և between the two oceans և, the position of the Sun, which changes every six months, is north of the equator և six months south.
The experience of commercial winds then changed to the monsoon (monsoon) of the western 's eastern monsoons (Wyrtki, 1987). South-East Commercial Winds Blow in the Equatorial Pacific
The experience of commercial winds then changed to the monsoon (monsoon) of the western 's eastern monsoons (Wyrtki, 1987). South-East Commercial Winds Blow in the Equatorial Pacific
normal year.
Commercial winds transport the mass of the warm waters of the eastern Pacific Ocean to the waters of eastern Indonesia. In some parts of the Indonesian Sea, the movement of water mass is decreasing.
General wind patterns from Indonesia
The same thing happens when the wind blows at the equator in transition. This led to the Indonesian archipelago, which lies between the eastern Indian and western Pacific Oceans, providing the largest heat (heat) storage space in the world's oceans. High sea surface temperatures (> 28 ° C) have been found in and around Indonesia .
Higher temperatures will affect the exchange of substances և atmosphere ների between the oceans, which will have a significant impact on the Indonesian archipelago և local world climate.
Southwestern winds, which blow constantly throughout the year, have caused sea levels to rise along the west coast of the Mindanao -Halmahera-Irian Jaya Pacific Ocean , with sea level rising along the Sumatra-Java coast of the western Indian Ocean.
The wind horse, which plays a very important role in Indonesia , is the monsoon , as Indonesia is in the middle of " Australia" in Asia, and the Pacific Ocean is bordered by the Indian Ocean . According to Wiertke (1961), the weather in Indonesia is divided into three groups, namely:
Higher temperatures will affect the exchange of substances և atmosphere ների between the oceans, which will have a significant impact on the Indonesian archipelago և local world climate.
Southwestern winds, which blow constantly throughout the year, have caused sea levels to rise along the west coast of the Mindanao -Halmahera-Irian Jaya Pacific Ocean , with sea level rising along the Sumatra-Java coast of the western Indian Ocean.
The wind horse, which plays a very important role in Indonesia , is the monsoon , as Indonesia is in the middle of " Australia" in Asia, and the Pacific Ocean is bordered by the Indian Ocean . According to Wiertke (1961), the weather in Indonesia is divided into three groups, namely:
General wind patterns from Indonesia
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| angina pectoris from Indonesian |
1. Western season (December - April)
High pressure develops on the western monsoon over Benoit Asia, and the center of low pressure occurs on the continent of Australia, so winds blow from northwest to southeast.This island in Java is known as the Northwest Monsoon. Western monsoon mainly falls in Java.
The western monsoon blows in October -April, and is located in the southern hemisphere, causing the hemisphere, especially Australia, to heat up more than the Asian continent.
Temperature rise in Australia ցածր due to low (minimum) air pressure. On the other hand, in Asia, where the temperature is low and the pressure is high (maximum). The winds then move from the Asian continent to the Australian continent as the western monsoon.
These winds blow the Pacific Ocean, the Indonesian Ocean and the South China Sea. Because crossing the ocean, of course, contains a lot of water vapor , it "rains" after reaching the Indonesian archipelago . Every November, December and January, the rainy season in western Indonesia is marked by heavy rainfall.
2. Ar-Season (April-October)
During the Eastern monsoon, the center of pressure on the lace, which occurs on the Asian Benoit ական the central pressure on the Australian Benito, the winds blow from south-east to north-west . A southeastern monsoon is blowing on the island of Java.
During the Eastern monsoon, there was usually a drought in Java. The solar monsoon blows every April-October, when the sun begins to move to the northern hemisphere.
In the Northern Hemisphere, especially in Asia, the temperature is high and the air pressure is low (minimum). On the other hand, in the continent of Australia, where the sun has gone, the place is low and the shock pressure is high (maximum).
There is a movement of winds from Australian Benoit to Asian Benoit through Indonesia as an eastern monsoon . This wind does not rain much, as it passes only through small seas with narrow passages, such as the Timor Sea, the Aravur Sea, the southern part of the Irian Jaya, as well as the Nusa Tengara Islands.
So, Oleg from Indonesia is serving me as a dry season. Between the two seasons, between the rainy and the dry seasons , there is a season called the transition season.
Transition from rainy season to dry season Yesterday 's song is called rainy season from dry season.
Characteristics of the transition season (transition), which include hot air, irregular wind direction և Abrupt frequent frequent rains in a short time.
During the Eastern monsoon, there was usually a drought in Java. The solar monsoon blows every April-October, when the sun begins to move to the northern hemisphere.
In the Northern Hemisphere, especially in Asia, the temperature is high and the air pressure is low (minimum). On the other hand, in the continent of Australia, where the sun has gone, the place is low and the shock pressure is high (maximum).
There is a movement of winds from Australian Benoit to Asian Benoit through Indonesia as an eastern monsoon . This wind does not rain much, as it passes only through small seas with narrow passages, such as the Timor Sea, the Aravur Sea, the southern part of the Irian Jaya, as well as the Nusa Tengara Islands.
So, Oleg from Indonesia is serving me as a dry season. Between the two seasons, between the rainy and the dry seasons , there is a season called the transition season.
Transition from rainy season to dry season Yesterday 's song is called rainy season from dry season.
Characteristics of the transition season (transition), which include hot air, irregular wind direction և Abrupt frequent frequent rains in a short time.
3. Transition season (March - May - September - November)
The period from March to May is known as the first transition season or the end of the year transition period, while the period from September to November is known as the second season of the songs or the end of the year transition period. During the transition seasons, the moon moves along the equator, so the winds are weak and the direction is irregular.
4. In addition to the West-East monsoons, there are local winds.
These winds come every day, like the wild breeze, the sea breeze, the valley breeze, the mountain breeze. The location of the wind can be described as follows:1. Land breeze ով sea wind
These winds occur in coastal areas due to differences in the nature of land and sea. At night it is cooler than the continental ocean, և it is the maximum area that causes wind on land. On the other hand, the daytime wind is sea.
These two winds are widely used by traditional fishermen for sea fishing . At night, when the sea breeze blows, the thing is that the fishermen go fishing at sea. On the other hand, the day when the sea wind blows for fishermen
These two winds are widely used by traditional fishermen for sea fishing . At night, when the sea breeze blows, the thing is that the fishermen go fishing at sea. On the other hand, the day when the sea wind blows for fishermen
house arrest.
2. Limbach winds և mountain winds
During the day, mountain peaks heat up faster than closed valleys. Peak pressure reaches a minimum and Lembach pressure reaches a maximum. Due to this position, the Poppy coupe moves down the slope from the valley to the top of the mountain. The wind coming from the valley is called the valley wind.
At night the top of the mountain releases heat faster than the valley. As a result, the pressure on the top of the mountain is higher (maximum) than in the valley (minimum), so winds blow from the top of the mountain down the slope into the valley. The wind coming from the top of this mountain is called the mountain wind
At night the top of the mountain releases heat faster than the valley. As a result, the pressure on the top of the mountain is higher (maximum) than in the valley (minimum), so winds blow from the top of the mountain down the slope into the valley. The wind coming from the top of this mountain is called the mountain wind
General wind patterns from Indonesia
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