BHUTAN TOUR AGENCY

There reaches of the kingdom the weather is cold during winter. Mountain peaks are perpetually covered in snow and lower parts are still cool in summer owing to the high altitude terrain.

The Indian summer monsoon lasts from late-June through late-September and is mostly confined to the southern border region of Bhutan. It brings heavy rain and high humidity, to the southern region. These rains bring between 60 and 90 percent of the western region’s rainfall.

Annual precipitation ranges widely in various parts of the country. In the northern border region of Tibet gets about forty millimeters of precipitation a year which is primarily snow. In the temperate central regions, a yearly average of around 1,000 millimeters is more common, and 7,800 millimeters per year has been registered at some locations in the humid, subtropical south, ensuring the thick tropical forest, or savanna.

Thimphu experiences dry winter months (December through February) and almost no precipitation until March, when rainfall averages 20 millimeters a month and increases steadily thereafter to a high of 220 millimeters in August for a total annual rainfall of nearly 650 millimeters.

Bhutan’s generally dry spring starts in early March and lasts until mid-April. Summer weather commences in mid-April with occasional showers and continues to late June. The heavier summer rains last from late June through late September which is more monsoonal along the southwest border.

Autumn, from late September or early October to late November, follows the rainy season. It is characterized by bright, sunny days and some early snowfalls at higher elevations.

From late November until March, winter sets in, with frost throughout much of the country and snowfall common above elevations of 3,000 meters. The winter northeast monsoon brings gale-force winds at the highest altitudes through high mountain passes, giving Bhutan its name – Drukyul, which in the Dzongkha language mean Land of the Thunder Dragon.

Average Temperatures in Bhutan

It should be noted that average temperatures are recorded from valley floors. There can be considerable divergences from the recorded figures depending upon elevation.