ClimateSearch

Vladikavkaz, North Ossetia–Alania

Russia · 306k people · 671 m elevation · Northern Hemisphere

Every month in detail

Thirty-year averages for each calendar month.

Monthly climate normals. Values shown as an em dash are missing from the source data.
MonthJanFebMarAprMayJunJulAugSepOctNovDec
Average high37°F (3°C)39°F (4°C)46°F (8°C)56°F (13°C)65°F (18°C)71°F (22°C)76°F (24°C)75°F (24°C)68°F (20°C)59°F (15°C)47°F (9°C)39°F (4°C)
Average low21°F (-6°C)22°F (-6°C)29°F (-2°C)38°F (4°C)48°F (9°C)55°F (13°C)60°F (15°C)60°F (15°C)53°F (12°C)44°F (6°C)32°F (0°C)24°F (-5°C)
Dew point21°F (-6°C)22°F (-5°C)30°F (-1°C)40°F (4°C)50°F (10°C)57°F (14°C)61°F (16°C)60°F (16°C)53°F (12°C)44°F (7°C)32°F (0°C)24°F (-4°C)
Rainfall1 in (26 mm)1.2 in (31 mm)2.8 in (71 mm)4 in (101 mm)6.1 in (155 mm)8.2 in (208 mm)7.5 in (191 mm)6.4 in (163 mm)3.8 in (95 mm)2.4 in (61 mm)1.5 in (38 mm)1 in (26 mm)
Rainy days77121520222220141076
Snowfall7.4 in (18.8 cm)8 in (20.2 cm)12.8 in (32.5 cm)7.3 in (18.5 cm)1 in (2.6 cm)0 in (0.1 cm)0 in (0 cm)0 in (0 cm)0.4 in (1.1 cm)3 in (7.5 cm)6.5 in (16.6 cm)6.4 in (16.2 cm)
Sunshine206 h217 h251 h260 h299 h323 h362 h340 h264 h232 h197 h185 h

Scroll the table sideways for all twelve months.

Projected change, 2031–2050

Model projection, not an observation

How this city’s climate may change, measured against the same models’ own 1995–2014 output. Nothing here affects the match score above.

Change in summer afternoon highs

+2.3°F (+1.3°C)

Models range from +1.6°F (+0.9°C) to +2.8°F (+1.6°C)

Days above 90°F (32°C) a year

1 1

About 2.0× as many

Warming by month
  • January: +1.5°F (+0.9°C)
  • February: +1.7°F (+0.9°C)
  • March: +3.0°F (+1.6°C)
  • April: +2.4°F (+1.3°C)
  • May: +1.4°F (+0.8°C)
  • June: +2.5°F (+1.4°C)
  • July: +2.6°F (+1.5°C)
  • August: +1.8°F (+1.0°C)
  • September: +2.1°F (+1.2°C)
  • October: +2.4°F (+1.4°C)
  • November: +1.6°F (+0.9°C)
  • December: +1.2°F (+0.7°C)
Scenario
SSP5-8.5 (high emissions)
Models
4 · CMIP6 HighResMIP, downscaled

This is a high-emissions pathway — the upper end of plausible futures, not a central estimate. Changes are measured by each model against its own past output and then applied to the observed record, which cancels each model’s bias but not the genuine uncertainty about how much warming occurs. Where the models disagree widely, the range above is the honest answer.