Northern circars coast
The seasonal winds that bring large amounts of rainfall to Asia's coastland are the southwest monsoon and the northeast monsoon. The southwest monsoon occurs in summer, bringing moisture-laden air from the Indian Ocean to countries like India, Sri Lanka, and Bangladesh. The northeast monsoon occurs in winter, bringing rain to countries like Thailand, Cambodia, and Vietnam.
India experiences four primary types of rain: the southwest monsoon, the northeast monsoon, convectional rainfall, and cyclonic rainfall. These rainfall patterns vary across the country due to diverse geographical features and climatic conditions.
Breaking monsoon is a weather phenomenon that occurs when the monsoon rains in a region suddenly weaken or stop after a period of sustained heavy rainfall. This can lead to drought conditions and impact agriculture and water resources in the affected area. Various factors such as changes in atmospheric circulation patterns, sea surface temperatures, and local topography can contribute to a breaking monsoon.
Mountains influence the distribution of rainfall by causing air to rise and cool, leading to condensation and precipitation on the windward side. This results in more rainfall on the windward side of the mountain and a rain shadow effect on the leeward side, where less rainfall occurs.
The southeast monsoon is a seasonal wind pattern that brings moist air from the Indian Ocean to Southeast Asia. It typically occurs from May to September, bringing heavy rainfall to countries like Thailand, Indonesia, and Malaysia. This monsoon is important for agriculture and water resources in the region.
The retreating rainfall monsoon occurs when the temperature on land is significantly warmer or cooler than the temperature of the ocean.
The retreating Indian monsoon is commonly referred to as the "withdrawal of the southwest monsoon." This phase occurs typically between late September and October, when the monsoon winds start to reverse and retreat from the Indian subcontinent. The withdrawal is marked by a gradual decrease in rainfall and the onset of drier conditions as the season transitions to winter.
The three main types of monsoons are the Southwest Monsoon, the Northeast Monsoon, and the Retreating Monsoon. The Southwest Monsoon occurs from June to September, bringing heavy rainfall to South Asia due to winds from the Indian Ocean. The Northeast Monsoon, occurring from October to December, affects southeastern regions, such as India and Sri Lanka, bringing dry air. The Retreating Monsoon happens from October to November as the southwest winds withdraw, leading to a transition in weather patterns.
The South-West monsoon becomes a weak current and withdraws from Punjab by mid-September. It leaves the Ganga delta by late October. By early November, it leaves the southern part of the peninsula. These particular months from September to November are termed as the period of 'retreating monsoon'. During this time, the days are hot, nights are cool and the daily range of temperature is high.
Northeast monsoon , are the monsoon that come from south . This season starts from June and in the month of September . retreating monsoon starts from the mid of september month and ends in the november month .
Tamil Nadu experiences monsoon rainfall twice a year due to its geographical location and the influence of two major monsoon systems. The southwest monsoon, which occurs from June to September, brings rainfall to the state as it moves across the Western Ghats. Additionally, the northeast monsoon, from October to December, primarily affects Tamil Nadu, as the winds pick up moisture from the Bay of Bengal. This dual monsoon pattern ensures that the region receives significant rainfall during both seasons, supporting its agriculture and water resources.
The seasonal winds that bring large amounts of rainfall to Asia's coastland are the southwest monsoon and the northeast monsoon. The southwest monsoon occurs in summer, bringing moisture-laden air from the Indian Ocean to countries like India, Sri Lanka, and Bangladesh. The northeast monsoon occurs in winter, bringing rain to countries like Thailand, Cambodia, and Vietnam.
India's monsoon season accounts for about 80 percent of the country's annual rainfall. The southwest monsoon, which occurs from June to September, is crucial for the country's agriculture and water resources. India's economy and livelihoods are heavily dependent on the success of the monsoon season.
The two main types of monsoon are the southwest monsoon and the northeast monsoon. The southwest monsoon occurs in the summer and brings heavy rainfall to regions like South Asia, driven by the temperature difference between land and ocean. In contrast, the northeast monsoon occurs during winter, primarily affecting southeastern India and parts of Southeast Asia, bringing dry conditions to some areas and rainfall to others. Both monsoons are crucial for agricultural practices in the regions they affect.
India primarily receives rainfall through the southwest monsoon, which occurs from June to September. This seasonal wind pattern brings moisture-laden winds from the Indian Ocean, resulting in heavy rainfall across most parts of the country. Additionally, the northeast monsoon affects the southeastern coast from October to December, while localized weather systems like cyclones can also contribute to rainfall. The diverse topography and geography of India further influence rainfall distribution and intensity across different regions.
During a monsoon, heavy rainfall occurs due to the seasonal shift in wind patterns. This can result in prolonged periods of intense rainfall, leading to flooding and landslides in some regions. Monsoons are characterized by a distinct wet season followed by a dry season.
The monsoon season in Chembakolli, located in the Western Ghats of India, typically occurs from June to September. During this period, the region experiences heavy rainfall, which is crucial for agriculture and replenishing local water sources. The peak rainfall usually occurs in July, making it a significant time for the local ecosystem.