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In this season the Himalayas function as a barrier to cold air masses from Inner Asia, so southern Nepal and northern India have warmer winters than would otherwise be the case. April and May are dry and hot, especially below 1,200 meters (4,000 ft) where afternoon temperatures may exceed 40 °C (104 °F).
Nepal launched its National Adaptation Plan (NAP) process in September 2015. The two main objectives of the NAP are (i) to reduce vulnerability to climate change impacts by improving resilience and adaptive capacity, and (ii) to integrate climate change adaptation into new and current policies, programs, activities, and development strategies ...
The temperatures of the hot variants (BWh, BSh) of these climates have the potential to exceed 50 °C (122 °F) ... Nepal: 46.4 °C (115.5 °F) Ataria:
Dfa = Hot-summer humid continental climate; coldest month averaging below 0 °C (32 °F) (or −3 °C (26.6 °F)), at least one month's average temperature above 22 °C (71.6 °F), and at least four months averaging above 10 °C (50 °F). No significant precipitation difference between seasons (neither the abovementioned set of conditions ...
Buran (a wind which blows across eastern Asia. It is also known as Purga when over the tundra); Karakaze (strong cold mountain wind from Gunma Prefecture in Japan); East Asian Monsoon, known in China and Taiwan as meiyu (梅雨), in Korea as jangma (), and in Japan as tsuyu (梅雨) when advancing northwards in the spring and shurin (秋霖) when retreating southwards in autumn.
Other names on the list include the likes of Fiji and Nepal, and while the East Anglian coastline has plenty of showstopping beaches to rival any palm-strewn Melanesian idyll, the region’s ...
At the time of the 2011 Nepal census it had a population of 6,995 people living in 1,015 individual households. [2] The normal temperature is 29 to 35 degree Celsius in summer where as in winter it falls down 14 to 25 degree Celsius which indicates that the climatic condition of summer is extremely hot where as in winter its extremely cold.
Snow accumulation in the valleys greatly reduces the area's wintertime temperature. The northeast monsoon is the predominant feature of the Eastern Himalayan region's weather, while on the southern slopes cold season precipitation is more important.