ClimateSearch

Nizhny Tagil, Sverdlovsk Oblast

Russia · 381k people · 189 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 high12°F (-11°C)16°F (-9°C)30°F (-1°C)45°F (7°C)60°F (16°C)68°F (20°C)72°F (22°C)66°F (19°C)56°F (13°C)42°F (5°C)25°F (-4°C)15°F (-9°C)
Average low2°F (-17°C)4°F (-15°C)17°F (-8°C)28°F (-2°C)41°F (5°C)52°F (11°C)57°F (14°C)53°F (12°C)44°F (7°C)33°F (0°C)16°F (-9°C)6°F (-15°C)
Dew point2°F (-17°C)4°F (-15°C)17°F (-8°C)27°F (-3°C)38°F (4°C)50°F (10°C)55°F (13°C)52°F (11°C)43°F (6°C)31°F (-1°C)15°F (-9°C)6°F (-14°C)
Rainfall0.8 in (20 mm)0.6 in (16 mm)1.1 in (27 mm)1.5 in (37 mm)2.2 in (57 mm)3.3 in (83 mm)3.4 in (87 mm)3.3 in (83 mm)2.5 in (62 mm)1.7 in (44 mm)1.2 in (30 mm)0.8 in (21 mm)
Rainy days657910131313121186
Snowfall6.6 in (16.8 cm)5.4 in (13.8 cm)7.8 in (19.9 cm)4.9 in (12.5 cm)1.7 in (4.2 cm)0.3 in (0.7 cm)0 in (0 cm)0 in (0 cm)0.4 in (1.1 cm)4.9 in (12.5 cm)7.8 in (19.8 cm)7.1 in (18 cm)
Sunshine89 h142 h212 h280 h353 h366 h362 h288 h194 h123 h84 h65 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

+3.6°F (+2.0°C)

Models range from +2.8°F (+1.6°C) to +4.5°F (+2.5°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +3.7°F (+2.0°C)
  • February: +2.1°F (+1.2°C)
  • March: +2.6°F (+1.4°C)
  • April: +2.8°F (+1.6°C)
  • May: +2.8°F (+1.6°C)
  • June: +3.5°F (+2.0°C)
  • July: +3.9°F (+2.2°C)
  • August: +3.4°F (+1.9°C)
  • September: +1.8°F (+1.0°C)
  • October: +3.1°F (+1.7°C)
  • November: +4.8°F (+2.7°C)
  • December: +3.3°F (+1.9°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.