Top Locations in Azerbaijan
Azerbaijan Weather Overview
Partially landlocked and partly coastal;
The expected climatic circumstances of
Located in a region with primary surroundings of highland;
Azerbaijan is home to mountains such as Major Caucasus, Talysh, Minor Caucasus
and the North Iranian Mountains. The foot lowland located in the middle of the
Major and Minor Caucasus extends to as far as the Caspian Sea in the east of
The lowland and mountainous areas of
At the altitude of 3000 meters the sun shines brightly throughout 2200 to 2500 hours per year, equalling a total amount of 128 to 132 kcal (kilocalorie) per 1sq cm every year. As the elevation of the mountains decrease so does the amount of sunshine falling down to 120 to 124 kcal-cm², while being at a height of 500 to 600 metres above sea level. This will then progressively ascend as the level reaches 140 to 150 kcal-cm² at an altitude of over 3000 metres over the Major and Minor Caucasus.
The quantity of solarium emission released throughout the Araz plateau in Nakhchivan equals 148 to 150 kcal-cm², and inclines throughout the mountainous areas as it reaches 152 to 160 kcal-cm²; generally in Lenkoran 50 to 60 kcal-cm² and in the mountains 15 to 25 kcal-cm².
The typical climate of Azerbaijan if formed by the authority
of cold air masses of artic; Scandinavian and Kara anti-cyclones, maritime;
Azores maximum, and temperate; Siberian anti-cyclones. Nevertheless hot air
masses of the tropical regions (southern cyclones and subtropical
anti-cyclones) form Central Asian anti-cyclones and this generates the current restricted
weather circumstances. In regards to landscape, assortment in
- A semi-desert and very dry climate that covers the majority of the innermost low lying land regions. 15 to 50 percent of the annual conversation of rainfall is evaporated. Winter, however is mostly hot, but summer is very hot with occasional days seeing temperatures higher than 40ºC
- A semi-desert and dried out climate that typically experiences cold winters and extensive, hot, dry summers.
- A mild to hot climate. The lower mountainous areas feature very dry winters, but are also quite cold. Annual rainfall levels create anywhere from 50 to 100 percent of possible evaporation. Winters throughout the country are generally placid and mild, with a low average rainfall and summers are mild to hot.
- A mild to hot climate with very dry summers and mild winters. Autumn is the season that generally experiences the highest amount of precipitation, but it rains less from May until the end of August.
- A cold climate with dry mild winters and cool summers.
- A cold climate with dry, cool summers and cold winters. The majority of precipitation obtained throughout the winter is in the form of snow. While the remainder of the year is relatively dry.
- A mild to hot climate with equivalent sharing of rainfall the covers all areas of the country. Winter is mild and summers are mild to hot.
- A cold climate is a fair distribution of precipitation throughout all season. Winter is generally cold and summers are mild.
- Areas higher then 2700m of elevation. Both winter and summers are cold and in most places snow is present all year round.
- Capital: Baku
- Area: 86,600km2
- Population: 8,177,000
- Currency: Manat (AZM)