Skopje, the capital of North Macedonia, sits in a basin on the Vardar River in the north of the country, ringed by mountains and far from any sea, at approximately 41.99°N, 21.43°E. Its enclosed inland position gives it a humid subtropical climate with a strong continental edge (Köppen Cfa) — hot, dry summers and cold winters — with a wide temperature range and heavy winter fog.

Summer, from June to August, is hot and dry, with July and August the hottest — average highs around 31–32°C — and heatwaves that can exceed 38–40°C, as the mountain-ringed basin traps hot, still air with little breeze. Rain is scarce, arriving mainly as occasional thunderstorms, and the long sunny days are the driest of the year.

Winter, from December to February, is cold, with January the coldest month — average highs around 5°C and lows near -3°C, and cold snaps that can drop well below -10°C. Snow falls and can lie for days, but the season's defining feature is fog: the enclosed Vardar basin traps cold, stagnant air for weeks, along with severe winter smog.

Skopje is dry, receiving only around 470–520 mm of precipitation a year, spread with spring and late-autumn maxima and a nearly rainless midsummer; the surrounding mountains shelter the basin from the wetter Adriatic air to the west. Live rainfall, humidity, and pressure readings for the city are shown in the panels above.

Skopje's mountain-ringed basin traps both the summer heat, making it one of the hottest cities in the Balkans, and the cold, stagnant winter air, which brings persistent fog and some of the worst seasonal air pollution in Europe. Spring and autumn are short, changeable transitional seasons between these two extremes.

To follow any single measurement in Skopje more closely, use our live instruments: the online barometer for atmospheric pressure, the thermometer for temperature, the hygrometer for humidity, the anemometer for wind speed, the wind vane for wind direction, and the rain gauge for rainfall.