The climate of Hyderabad remains fairly warm through most parts of the year and does not receive much rainfall in the monsoon. With the onset of winters in North and central parts of India, temperatures marginally come down in the months of December and January and the nights become quite cool in and around the Hyderabad city. During the summer months, the mercury goes as high as 42° C while in winters the minimum temperature may come down to as low as 12° C. June to November are the months of monsoons, accompanied by rains. During the Monsoons also the temperature goes down at times. Thus, for most parts of the year the weather and climate of Hyderabad remains fairly moderate and you can visit the Hyderabad city anytime in the year but the best season to visit Hyderabad is between October-February.

Clothes to Wear While Traveling to Hyderabad

While traveling to Hyderabad during the summer months, you must carry and wear light cotton clothes while in winter season, especially in December and January, you need to carry some light warm clothes as the mercury dips significantly.

Best Time to Visit Hyderabad

In order to have pleasant trip, the climatic conditions of the place to be visited should be known in advance. Hyderabad is a city that has a moderate climate throughout the year. The best time to visit this city is after the monsoons i.e., October to March. The summers can get really hot and one can see temperatures soaring upto 45o Celsius. Evenings are usually pleasant thanks to the cool sea breeze. At night, the temperature usually drops down to 25o - 30o Celsius.

The city does not experience harsh winters and it becomes moderately cool towards the end of the year. The maximum temperature remains at a pleasant 22o - 25o Celsius. The minimum can go down till 13o Celsius. The monsoons are from June to September after which the weather becomes very pleasant and enjoyable. The average annual rainfall in Hyderabad is around 80 - 90 centimeters. The place also witnesses cyclonic depressions every now and then due to the low-pressure trough forming over the plateau.