As India further cools during September, the southwest monsoon weakens. Capital Bhopal averages low of 9 °C (48 °F) and high of 24 °C (75 °F). Photo caption: The alternate layering of wood and stone is typical to this style of architecture in Himachal Pradesh Himachal Pradesh: Weather-Friendly Architecture . | Climatic conditions [15] Groupings are assigned codes (see chart) according to the Köppen climate classification system. [31] The rainy season begins in June. It is a region of barren, arid, frigid and wind-blown wastelands. The nation's climate is strongly influenced by the Himalayas and the Thar Desert. | 25% Between the two monsoon seasons, the temperature remains cool in most parts of Kerala. Traditionally, North Indians note six seasons or Ritu, each about two months long. |- As Earth's highest and most massive mountain range, the Himalayas bar the influx of frigid katabatic winds from the icy Tibetan Plateau and northerly Central Asia. The monsoon typically breaks over Indian territory by around 25 May, when it lashes the Andaman and Nicobar Islands in the Bay of Bengal. The net atmospheric heating due to aerosol absorption causes the air to warm and convect upwards, increasing the concentration of moisture in the mid-troposphere and providing positive feedback that stimulates further heating of aerosols.[102]. It occupies a region of scenic splendor in the western Himalayas, offering a multitextured display of mountains, gorges, thickly forested valleys, lakes, fields, and streams. | 10% While the high mountainous regions remain cool throughout the year, the plains and coastal areas experience hot and humid climates. [100], Thick haze and smoke originating from burning biomass in northwestern India[101] and air pollution from large industrial cities in northern India[102] often concentrate over the Ganges Basin. To bear with the cold climate of Himachal Pradesh they wear a special shoe made of dried grass. | Up to 800 m Himalayas - Himalayas - Climate: The Himalayas, as a great climatic divide affecting large systems of air and water circulation, help determine meteorological conditions in the Indian subcontinent to the south and in the Central Asian highlands to the north. Bihar is one of the coldest regions in India with an average daily high temperature of only 26 degrees centigrade. Minimum temperatures in western Maharashtra and Chhattisgarh hover around 10 °C (50 °F); in the southern Deccan Plateau, they reach 16 °C (61 °F). The origin of the people of Himachal Pradesh dates back to the period between 2250 and 1750 BC during which the people of Indus valley civilization occupied the state. In most parts of India, this period marks the transition from wet to dry seasonal conditions. [20] Karnataka is divided into three zones – coastal, north interior and south interior. Another striking feature of summer is the Loo (wind). Hail is also common in parts of India, causing severe damage to standing crops such as rice and wheat. [23] Once their passage is hindered by the Himalayas, they are unable to proceed further, and they release significant precipitation over the southern Himalayas. Cyclones bring with them heavy rains, storm surges, and winds that often cut affected areas off from relief and supplies. Kerala and Ladakh are two mountainous regions of India that show some differences between them. Besides being a great tourist destination owing to its amazing and utmost fascinating scenic views, it also has some great religious significance. Dust storms having a velocity of 48–64 km/h (30–40 mph) are most frequent in May and with second maximum in April and June. Highest reliable temperature reading was 50.6 °C ( 25.2 °F ) Puja Schedule, map, Videos and more precipitation! 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