The climate of Pakistan (پاکستان کی آب و ہوا) is as diverse as its geography. From the snow-covered mountains of Gilgit-Baltistan to the hot deserts of Sindh and Balochistan, Pakistan experiences a wide range of weather conditions. Understanding Pakistan’s climate is crucial for agriculture, tourism, urban development, and disaster management.
Pakistan’s geography plays a vital role in shaping its climate. Located between latitudes 24° and 37° North, Pakistan lies at the intersection of South Asia, Central Asia, and the Middle East.
This unique location results in a variety of climates across the country.
The Southwest Monsoon is the most significant weather system in Pakistan.
Arrives in July and lasts till September
Brings 60–70% of annual rainfall
Essential for agriculture but often causes floods and landslides
The Northeast Monsoon is weaker and impacts coastal areas in winter.
Cold and dry season
Northern areas like Gilgit, Hunza, and Skardu experience heavy snowfall
Southern regions remain relatively mild
Pleasant temperatures with blossoming flowers
Ideal season for tourism and agriculture
Major crops like wheat are harvested
Intense heat, especially in Sindh, Punjab, and Balochistan
Temperatures in Jacobabad and Sibi can exceed 50°C
Monsoon rains begin in July, cooling down plains but causing floods
Transition season with mild temperatures
Harvesting of rice, sugarcane, and cotton
Comfortable for travel and outdoor activities
The diverse climate supports year-round tourism:
Winter tourism – Skiing in Malam Jabba, snowfall in Murree
Summer tourism – Trekking in Hunza, Fairy Meadows, and Naran-Kaghan
Spring tourism – Visiting gardens of Lahore, Shalimar Bagh, and Swat Valley
Autumn tourism – Golden autumn leaves in Hunza and Skardu
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