Normal Weather conditions Of Northern Areas Of Pakistan

Normal Weather conditions Of Northern Areas Of Pakistan

The climate and temperature of Northern locations of Pakistan is managed by elevation. The large mountains previously mentioned 16000 toes continue to be snowbound in the course of the calendar year although the slender valleys have an extraordinary local climate both of those in summer months and winter season.

The region less than discussion, generally, has chilly winters and mild summers. The adhering to is a shorter description of the temperature and precipitation of the place.


The large mountains report down below freezing temperatures throughout the 12 months. While the temperatures of the deep valleys show extraordinary variants in summer and winter season. The each day temperature assortment is also pretty large. For occasion, Gilgit, at an elevation of about 4,500 toes and surrounded by substantial mountains records temperatures at mid-working day in July that typically exceeds 100 F when due to improved katabatic affect night time minimal can tumble to as very low as 60 F. This reveals a extremely large diurnal array of 40 F! The exact station throughout January, on the other hand, records temperatures as low as 20 F throughout the peak of winter.

Skardu, at a increased elevation of about 7500 ft has relatively milder summers. But even below, temperatures of over 95 F are not unusual in mid-summertime. It is interesting to notice that it is the exact area which holds the history for coldest city in Pakistan. On January 24, 1994, Skardu recorded a temperature of -16 F! This evidently reveals that deep valleys surrounded by high mountains like Gilgit and Skardu demonstrate extremes of temperature in summer season and wintertime.


The precipitation on superior mountains is in the sort of snow during the yr. On the reduced, deep vallies, it is in the sort of rain in summer months and snow in winter season.

The key rain bearing technique in this spot is the western disturbance that affects this location in between December to April each and every yr and provides average precipitation.

The summers are almost rainless. No summertime thirty day period at Gilgit records extra than .5 inch of rainfall. The figures for Skardu are similar. There is a basic deficiency of precipitation. No wonder then that at spots like Gilgit, a number of miles from the metropolis, sand dunes can be viewed.

The relative humidity is very low in the course of the yr and extremely chilly and dry wind blows from the North East, specifically at Skardu in winter season.

In brief, the climate of the Northern Areas of Pakistan display extremes of temperatures with a general deficiency in precipitation all over the 12 months.

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