Quetta Summer and Winter Characteristic of almost entire Pakistan are the large differences between summer and winter. Not only in the field of precipitation, but also in temperatures.
What to pack Introduction In much of Pakistan the climate is tropical or subtropical, semi-arid or desert, but in the north there are also: In the cold half of the year, from late autumn to early spring, the north is reached by weather fronts of Mediterranean origin, which cause rainfall in the lowlands and snowfall in the mountains; in spring ie March and April the clash of air masses can cause thunderstorms and strong winds; in summer, from July to mid September, the country is reached by an offshoot of the Indian monsoon, but in most of the country it is not able to bring heavy rains, while in the western part the monsoon doesn't arrive at all.
However, the warmest months are those that precede the monsoon's arrival, especially June, which is very hot in plains and hills, up to quite high altitudes. The monsoon has an irregular pattern: Rivers may overflow even at a distance from the area where the heaviest rainfall occurred, which typically happen in the north.
So the great valley of the Indus and its tributaries, may also be affected by widespread flooding in the southern area, where normally it rains less.
The cycle called ENSO can affect the monsoon's performance: Mountains In the mountainous areas of the north and west, the climate is continental, with wide temperature range between winter and summer, and often even between night and day.
The temperature naturally decreases with altitude. The northern area zone 1 on the map as well as being the coldest at equal altitude, is more vulnerable to cold fronts related to the westerly winds of the middle latitudes, from December to May.
But not all areas receive a lot of precipitation: The southern side the mountains north of Peshawar and Islamabad is much more rainy than the northern one.
Kashmir In Kashmir, in the northernmost valleys of Khyber-Pakhtunkhwa and the disputed region of Gilgit-Baltistan, the yearly rainfall is typical of the desert, below millimetres 10 inches. Anyway, at higher altitudes there can be snowfalls quite frequently in winter, and above 4, metres 14, ft there are vast glaciers, but the fact that the trekking season runs from April to October shows how this area is sheltered from the monsoon rains, although we cannot exclude some showers or thunderstorms, and maybe some snowfalls on the higher peaks.
In Pakistan there are two mountain ranges, the Karakoram and the Hindu Kush, which host some of the highest peaks on the planet, starting with K2, the second highest mountain in the world with its 8, metres 28, ft.
The highest peak of the Hindu Kush is Tirich Mir, 7, metres 25, ft high. Skardu Skardu, located at 2, metres 7, ft above sea level, is the starting point for climbing K2 and other peaks above 8, metres 26, ft ; the climate here is arid continental, with an average of Here are the average temperatures of Skardu.
Skardu - Average temperatures.Climate of pakistan 1. Climate of Pakistan 2. Weather and climate • Climate: Climate describes the temperature, precipitation, and other weather conditions of a certain area. The climate of an area describes how these variables may be over a long period, for instance the South of France in the summer is hot and dry.
Climate of Pakistan With the exception of the temperate coastal region, most of Pakistan suffers from seasonal extremes of temperature. From June to September, Pakistan has its monsoon season, with warm weather and heavy rain in some areas.
Weather and climate Best time to visit Pakistan has three seasons: winter (November to March) is warm and cooled by sea breezes on the coast; summer (April to July) has extreme temperatures and the monsoon season (July to September) has the highest rainfall on the hills.
Pakistan Weather, climate and geography Weather and climate Best time to visit. Pakistan has three seasons: winter (November to March) is warm and cooled by sea breezes on the coast; summer (April to July) has extreme temperatures and the monsoon season (July to September) has the highest rainfall on the hills.
Climate and Weather.
Pakistan lies on the western margin of one of the major climatic regions of the earth, the monsoon region. The winds in winter are north-east to south-west, and the reverse, south-west to north-east, in summer. The causes of the reversal of the wind system, and of the pulsating character of the monsoons, are varied and.
Pakistan Table of Contents. Pakistan lies in the temperate zone.
The climate is generally arid, characterized by hot summers and cool or cold winters, and wide variations between extremes of temperature at given locations.