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There is a huge variation in the climatic conditions of Himachal Pradesh due to variation in altitude (360–6500 metres). The climate varies from hot and sub-humid tropical (450–900 metres) in the southern low tracts, warm and temperate (900–1800 metres), cool and temperate (1800–2400 metres) and cold glacial and alpine (2400–4800 metres) in the northern and eastern high elevated ...
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The temperature in Kullu valley in summer season is about 20 to 30 degree C. December and January during winter observe lowest temperatures ranging from −4 to 20 °C (25 to 68 °F), with heavy snowfall in the higher regions and very light snowfall in the main town, though the frequency is declining. Evenings and mornings are cold during winters.
Manali is a resort town, near Kullu town in Kullu district in the Indian state of Himachal Pradesh. [2] It is situated in the northern end of the Kullu Valley , formed by the Beas River . The town is located in the Kullu district , approximately 270 kilometres (170 mi) north of the state capital of Shimla and 544 kilometres (338 mi) northeast ...
Climate charts provide an overview of the climate in a particular place. The letters in the top row stand for months: January, February, etc. The bars and numbers convey the following information: The blue bars represent the average amount of precipitation (rain, snow etc.) that falls in each month.
The weather is hot and humid for most of the year, and the region features a tropical wet and dry climate. The northeast monsoon winds brings seasonal rainfall in the region from September to December, and occasionally cyclones. The annual rainfall in the region is about 1400 mm (55 in).
Kaza-Pooh-Tabo-Shimla route is open whole year, but the Manali-Kaza route is closed for 7 winter months every year during which Kunzum Pass (15,000 ft) is closed. NHAI is planning to construct a tunnel under the Kunzum Pass to provide all-weather connectivity between Manali and Spiti valley.
A col, also called saddle point or neutral point, is in meteorology, the point of intersection of a trough and a ridge in the pressure pattern of a weather map. It takes the form of a saddle where the air pressure is relatively higher than that of the low-pressure regions, but lower than that of the anticyclonic zones.