Western cyclonic disturbances, originating in the Mediterranean region, bring rainfall to the Indian subcontinent primarily during the winter months. These disturbances are characterized by low-pressure systems that move eastward, drawing moist air from the ocean. As this moist air ascends, it cools and condenses, leading to cloud formation and precipitation. The rainfall associated with these disturbances is often crucial for winter cropping in many regions of India.
"Phet" is a term commonly used in the Indian subcontinent to refer to a tropical cyclone. It typically denotes a powerful and destructive cyclonic storm that can bring heavy rainfall, strong winds, and storm surges to coastal areas.
The southwest monsoon brings less rainfall to Tamil Nadu primarily due to its geographical position and the prevailing wind patterns. The state is situated on the leeward side of the Western Ghats, which block much of the moisture-laden winds from reaching it. As a result, while the Western Ghats receive significant rainfall, Tamil Nadu experiences a rain shadow effect, leading to reduced precipitation during the southwest monsoon season. Additionally, the monsoon winds tend to weaken as they move further south, further contributing to lower rainfall in the region.
There have been no cyclones reported in Brisbane, capital of Queensland, Australia. Brisbane can be affected by cyclones which occur further north, but no cyclone has ever directly hit Brisbane.
India does not typically experience hurricanes; instead, it is more susceptible to cyclones. The North Indian Ocean region, including the Bay of Bengal and the Arabian Sea, is prone to cyclones that can bring strong winds, heavy rainfall, and storm surges. Cyclones in this region are typically classified as tropical cyclones or severe cyclonic storms.
Hurricanes can bring much needed rainfall to drought-stricken regions and clear the air of pollutants.
The winter rainfall in northwestern India is typically associated with cyclonic disturbances originating from the western disturbances. These systems bring rainfall during the winter months. Monsoonal rainfall, on the other hand, occurs in the summer months due to the southwest monsoon winds.
the western cyclonic disturbance is the weather phenomena of the winter months brought in by the westerly flow from the Mediterranean region .the usually influence the weather of the north and the north Western regions of India .
The northern Indian state of Himachal Pradesh receives rainfall due to western disturbances. These weather systems bring moisture-laden winds from the Mediterranean and cause precipitation in this region, particularly during the winter months.
temperate cyclones causes rainfall. westerlies are strong winds..............
It is because the south west monsoons which bring 80 percent of rainfall every year touches the western coast of India first and by the time it moves into the interiors and east, the moisture and rainfall gets reduced. So, the western region is wetter than eastern region.
Mumbai receives more rainfall than Kochi primarily due to its geographic location and the influence of the Western Ghats. While both cities are on the western coast of India, Mumbai is situated further north and is directly impacted by the monsoon winds that bring moisture from the Arabian Sea. The Western Ghats act as a barrier, causing orographic rainfall, which is more pronounced in Mumbai. In contrast, Kochi, located further south, experiences slightly less rainfall due to its position relative to these geographical features.
"Phet" is a term commonly used in the Indian subcontinent to refer to a tropical cyclone. It typically denotes a powerful and destructive cyclonic storm that can bring heavy rainfall, strong winds, and storm surges to coastal areas.
summer monsoons.
Asia doesn't get any rainfall during the winter because of the monsoon season which does not bring any rainfall during the winter months.
Northern winds
"Jet stream is a swiftly blowing wind at a height of 3 to 5 kms above the subtropical high pressure belt. Himalayas act as a barrier in their path and as such, the jet streams are divided into westerly and easterly jet steams. the westerly jet is responsible for bringing western disturbances into north-west India and Pakistan which bring winter rainfall. the easterly jet blowing over northern India is responsible for bringing tropical depressions over India and Bangladesh. these depressions play an important role in the distribution of rainfall." source: icse geo textbook
The prevailing winds of the west are what generally bring wet weather to Europe. It first crosses over Western Europe, dropping most of its rain there. By the time it reaches Eastern Europe, there is less rainfall.