ClimateSearch

Nalchik, Kabardino-Balkariya Republic

Russia · 239k people · 467 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 high34°F (1°C)36°F (2°C)44°F (7°C)56°F (13°C)66°F (19°C)73°F (23°C)77°F (25°C)76°F (25°C)68°F (20°C)58°F (14°C)45°F (7°C)37°F (3°C)
Average low20°F (-7°C)21°F (-6°C)29°F (-2°C)38°F (4°C)49°F (9°C)57°F (14°C)62°F (17°C)62°F (16°C)53°F (12°C)43°F (6°C)31°F (-1°C)23°F (-5°C)
Dew point21°F (-6°C)23°F (-5°C)31°F (0°C)40°F (5°C)51°F (10°C)57°F (14°C)61°F (16°C)60°F (16°C)54°F (12°C)45°F (7°C)33°F (0°C)24°F (-4°C)
Rainfall1.9 in (48 mm)2.1 in (54 mm)4.2 in (106 mm)5.7 in (145 mm)8 in (203 mm)8 in (204 mm)6.2 in (157 mm)5.8 in (148 mm)6 in (152 mm)4.4 in (112 mm)2.7 in (68 mm)1.9 in (48 mm)
Rainy days111116172018151415131110
Snowfall13.1 in (33.2 cm)13.1 in (33.4 cm)16.5 in (41.9 cm)4.7 in (12 cm)0.3 in (0.7 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)2.5 in (6.4 cm)9.3 in (23.5 cm)10.9 in (27.7 cm)
Sunshine214 h224 h267 h283 h326 h337 h366 h348 h279 h249 h212 h191 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

+2.2°F (+1.2°C)

Models range from +1.4°F (+0.8°C) to +2.6°F (+1.5°C)

Days above 90°F (32°C) a year

1 2

About 1.8× as many

Warming by month
  • January: +2.1°F (+1.2°C)
  • February: +2.1°F (+1.2°C)
  • March: +3.3°F (+1.8°C)
  • April: +2.8°F (+1.5°C)
  • May: +1.4°F (+0.8°C)
  • June: +2.1°F (+1.2°C)
  • July: +2.3°F (+1.3°C)
  • August: +2.0°F (+1.1°C)
  • September: +2.1°F (+1.2°C)
  • October: +2.4°F (+1.4°C)
  • November: +2.0°F (+1.1°C)
  • December: +1.7°F (+1.0°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.