Climate of India | Indian Weather | Monsoon | Tawqeer Sir | One Shot | For All Competitive Exams 

If you watch closely the LP zone is shown at 60⁰ N and not exactly at the poles. The temperature at poles is very low thus there is always HP at the poles. The Low pressure zone which you are talking about is at 60⁰ and is dynamically formed.

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It is actually subpolar low pressure zone which is dynamically induced i.e by rotation of earth While as equatorial low is thermally induced because of high temperature so low pressure

@@eactclasses but you have represented poles as LP zone instead of high pressure. Kindly clear the confusion.

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The retreat of the monsoon in India typically occurs in October, marking the end of the rainy season and the transition into the dry season. Several factors and not just the movement of the sun contribute to the retreat of the monsoon in October: 1. Changing pressure systems: The retreat of the monsoon is influenced by the movement of pressure systems. During the summer, the Indian subcontinent experiences low-pressure conditions due to the intense heating of the landmass. This low-pressure area draws in moisture-laden winds from the Indian Ocean, resulting in the monsoon rains. As the summer season comes to an end, the pressure conditions change, with the formation of high-pressure systems over the Indian subcontinent and the adjacent areas. These high-pressure systems cause the monsoon winds to weaken and gradually retreat. 1. Shift in the Inter-Tropical Convergence Zone (ITCZ): The ITCZ, which is a zone of low pressure near the equator, plays a significant role in the monsoon formation. During the summer, the ITCZ is positioned north of the Indian subcontinent, allowing the monsoon winds to bring moisture to the region. However, as the sun shifts southward with the changing seasons, the ITCZ also moves southward. This southward movement leads to the retreat of the monsoon from northern India towards October. 1. Jet stream position: The jet stream, a high-altitude wind current, also influences the monsoon pattern. During the summer, the jet stream lies to the north of the Himalayas, helping to steer the monsoon winds towards India. However, as the season progresses and the jet stream starts moving southward, it weakens the monsoon winds and contributes to their retreat. It's important to note that while October is generally the month when the monsoon retreats, the exact timing and duration can vary from year to year. Weather patterns and other climatic factors can result in variations in the monsoon withdrawal, leading to deviations from the typical pattern.

Topic wise

Yeah right I m confused as well

its atmospheric pressure which is indirectly proportional to temp

You are right. That is why ITCZ shifts north and south.

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Thanks

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