monsoon winds are called periodic winds. why ?
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Seasonal winds are movements of air repetitively and predictably driven by changes in large-scale weather patterns. Seasonal winds occur in many locations throughout the world. The name assigned to a particular seasonal wind—and the underlying physical forces that drive the winds—depend upon the unique geographic location.
One of the most commonly recognized seasonal winds are the monsoon winds. Although monsoons are often erroneously identified as rainstorms, they are actually a seasonal wind. A monsoon is a wind in low-latitude climates that seasonally changes direction between winter and summer. Monsoons usually blow from the land in winter (called the dry phase, because the wind is composed of cool, dry air), and from water to the land in summer (called the wet phase, because the wind is composed of warm, moist air), causing a drastic change in the precipitation and temperature patterns of the area impacted by the monsoon.
The word monsoon originates from Arabic mauzim, meaning season. It was first used to depict the winds in the Arabian Sea, but later it was extended for seasonally changing wind systems all over the world. The driving force shaping monsoons is the difference in the heating of land and water surfaces, which results in land-ocean pressure differences. On a small scale, land-sea breezes, to maintain the energy balance between land and water, transfer heat. On a larger scale, in winter when the air over the continents is colder than over the oceans, a large, high-pressure area builds up over Siberia, resulting in air motion over the Indian Ocean and South China, causing dry, clear skies for East and South Asia (the winter monsoon). The opposite of this happens with the summer monsoon in Southwest Asia. The air over the continents is much warmer than over the ocean, leading to moisture-carrying wind from the ocean towards the continent. When the humid air unites with relatively drier west airflow and crosses over mountains, it rises, reaches its saturation point, and thunderstorms and heavy showers develop.
Although the most pronounced monsoon system is in eastern and southern Asia, monsoons can also be observed in West Africa, Australia, or the Pacific Ocean. Even in the southwestern United States, a smaller scale monsoonal circulation system exists (called North American monsoon, Mexican monsoon, or Arizona monsoon). The North American monsoon is a regional-scale circulation over southwest North America between July and September, bringing dramatic increases in rainfall in a normally arid region of Arizona, New Mexico, and northwestern Mexico. It is a monsoonal circulation because of its similarities to the original Southwest Asian monsoon—the west or northwest winds turn more south or southeast, bringing moisture from the Pacific Ocean, Gulf of California and Gulf of Mexico. As the moist air moves in, it is lifted by mountain terrain that, combined with daytime heating from the Sun, causes thunderstorms.
The monsoon is an important feature of atmospheric circulation, because large areas in the tropics and subtropics are under the influence of monsoons, bringing humid air from over the oceans to produce rain over the land. The agricultural economies of impacted areas (e.g., Asia or India) frequently depend on the moisture provided by monsoon wind driven storm. The variations in the wind and precipitation patterns are so great, however, that more severe winds and storms can result in flooding that can cost thousands of lives.
A similar phenomenon to the monsoon also occurs in a smaller spatial and temporal scale, the mountain and valley breezes. The main reason they occur is also the difference in heating of the areas: during the day, the valley and the air around it warms and because it is less dense, it rises, and thus, a gentle upslope wind occurs. This wind is called the valley breeze. If the upslope valley winds carry sufficient moisture in the air, showers, even thunderstorms can develop in the ear
One of the most commonly recognized seasonal winds are the monsoon winds. Although monsoons are often erroneously identified as rainstorms, they are actually a seasonal wind. A monsoon is a wind in low-latitude climates that seasonally changes direction between winter and summer. Monsoons usually blow from the land in winter (called the dry phase, because the wind is composed of cool, dry air), and from water to the land in summer (called the wet phase, because the wind is composed of warm, moist air), causing a drastic change in the precipitation and temperature patterns of the area impacted by the monsoon.
The word monsoon originates from Arabic mauzim, meaning season. It was first used to depict the winds in the Arabian Sea, but later it was extended for seasonally changing wind systems all over the world. The driving force shaping monsoons is the difference in the heating of land and water surfaces, which results in land-ocean pressure differences. On a small scale, land-sea breezes, to maintain the energy balance between land and water, transfer heat. On a larger scale, in winter when the air over the continents is colder than over the oceans, a large, high-pressure area builds up over Siberia, resulting in air motion over the Indian Ocean and South China, causing dry, clear skies for East and South Asia (the winter monsoon). The opposite of this happens with the summer monsoon in Southwest Asia. The air over the continents is much warmer than over the ocean, leading to moisture-carrying wind from the ocean towards the continent. When the humid air unites with relatively drier west airflow and crosses over mountains, it rises, reaches its saturation point, and thunderstorms and heavy showers develop.
Although the most pronounced monsoon system is in eastern and southern Asia, monsoons can also be observed in West Africa, Australia, or the Pacific Ocean. Even in the southwestern United States, a smaller scale monsoonal circulation system exists (called North American monsoon, Mexican monsoon, or Arizona monsoon). The North American monsoon is a regional-scale circulation over southwest North America between July and September, bringing dramatic increases in rainfall in a normally arid region of Arizona, New Mexico, and northwestern Mexico. It is a monsoonal circulation because of its similarities to the original Southwest Asian monsoon—the west or northwest winds turn more south or southeast, bringing moisture from the Pacific Ocean, Gulf of California and Gulf of Mexico. As the moist air moves in, it is lifted by mountain terrain that, combined with daytime heating from the Sun, causes thunderstorms.
The monsoon is an important feature of atmospheric circulation, because large areas in the tropics and subtropics are under the influence of monsoons, bringing humid air from over the oceans to produce rain over the land. The agricultural economies of impacted areas (e.g., Asia or India) frequently depend on the moisture provided by monsoon wind driven storm. The variations in the wind and precipitation patterns are so great, however, that more severe winds and storms can result in flooding that can cost thousands of lives.
A similar phenomenon to the monsoon also occurs in a smaller spatial and temporal scale, the mountain and valley breezes. The main reason they occur is also the difference in heating of the areas: during the day, the valley and the air around it warms and because it is less dense, it rises, and thus, a gentle upslope wind occurs. This wind is called the valley breeze. If the upslope valley winds carry sufficient moisture in the air, showers, even thunderstorms can develop in the ear
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These winds are known to blow for a certain time in a certain direction – it may be for a part of a day or a particular season of the year.
They are land and sea breezes on a large scale. The word ‘monsoon’ comes from the Arabic word ‘mausim’ meaning weather. They change or reverse their directions according to the seasons.
They are land and sea breezes on a large scale. The word ‘monsoon’ comes from the Arabic word ‘mausim’ meaning weather. They change or reverse their directions according to the seasons.
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