Now
☀️
9.3°
Loading current temperature, humidity, wind, and air quality context for Doğubayazıt, Ağrı, Turkey.
Current temperature, humidity, wind, and air quality context for Doğubayazıt, Ağrı, Turkey.
Clear sky
Feels like 7.3°C
Humidity
89%
Relative humidity
Wind
5.2 km/h
SSW
UV
0
Low
Pressure
1016.1 hPa
Surface pressure
Now
☀️
9.3°
03am
☀️
8.7°
04am
🌤️
8.1°
05am
🌤️
7.7°
06am
🌤️
8.5°
07am
☀️
11°
08am
☀️
13.5°
09am
☀️
16.1°
10am
☀️
18.7°
11am
☀️
20.8°
12pm
☀️
22.3°
💧8%
01pm
⛅
22.6°
💧13%
02pm
🌤️
23.1°
💧35%
03pm
🌦️
21.4°
💧50%
04pm
☁️
20.3°
💧68%
05pm
☀️
19.5°
💧65%
06pm
🌤️
19°
💧43%
07pm
⛅
17.7°
💧23%
08pm
☁️
16°
💧18%
09pm
🌦️
13.9°
💧3%
10pm
🌤️
13.4°
💧10%
11pm
⛅
12.8°
💧15%
12am
⛅
11.7°
💧35%
01am
⛈️
11°
💧40%
Loading air quality context...
7.3°C
Similar to actual
89%
Very Humid
5.2 km/h
Direction: SSW
0
Low
2%
Sky coverage
0 mm
Current rainfall
Doğubayazıt sits as a strategic frontier outpost in the easternmost reaches of Turkey, nestled within the dramatic shadow of Mount Ararat, the region's towering sentinel. This urban settlement is characterized by its high-altitude plateau positioning, which creates a unique intersection of rugged volcanic terrain and semi-arid plains. The city's urban character is a blend of commercial transit hubs and residential pockets, serving as a vital gateway between Turkey and Iran. Geographically, the town is constrained by the surrounding mountainous topography, which significantly influences local atmospheric circulation. The absence of large bodies of water nearby means the air is naturally dry, increasing the susceptibility of the region to windborne particulate matter. While the city lacks a massive industrial belt, the prevalence of agricultural zones on the outskirts introduces seasonal organic aerosols and dust. The urban-rural gradient is sharp, with the densely built center contrasting against the stark, open landscapes of the Ağrı plateau. This basin-like configuration is critical for air quality; during periods of atmospheric stability, the surrounding peaks act as physical barriers that prevent the lateral dispersion of pollutants. Consequently, emissions from domestic heating and vehicular traffic become trapped within the lower troposphere. The intersection of high elevation and continental isolation ensures that the air remains crisp in summer but becomes a reservoir for stagnant pollutants during the freezing winter months, defining the city's environmental profile. The vast, wind-swept steppes further exacerbate the movement of fine mineral dust across the town.
The air quality narrative of Doğubayazıt is dictated by the extremes of a severe continental climate. Winter is the most challenging period, as plummeting temperatures drive a heavy reliance on coal and biomass for domestic heating. This creates a surge in particulate matter, which is frequently trapped near the surface by strong temperature inversions. During these cold snaps, a layer of warm air caps the cold air in the valley, preventing pollutants from escaping, making January and February the most hazardous months for respiratory health. Sensitive groups, including children and the elderly, should limit outdoor exertion when the horizon appears hazy. As spring arrives, the focus shifts from combustion to geology. The thawing ground and increasing wind speeds trigger dust storms across the plateau, elevating coarse particulate levels. Summer offers a reprieve, characterized by high transparency and strong ventilation. The hot, dry air typically disperses pollutants efficiently, making June through August the ideal window for outdoor activities and tourism around the Ishak Pasha Palace. Autumn serves as a transitional phase, where decreasing temperatures begin to stabilize the atmosphere once more. By November, the first frosts signal the return of heating systems, and air quality gradually declines. To maintain health, local residents are encouraged to monitor wind directions and avoid the city center during peak morning heating hours in winter. This seasonal cycle creates a rhythmic oscillation between the clarity of the high summer and the smoggy stillness of the deep, freezing winter.