ClimateSearch

Trabzon, Trabzon

Turkey · 244k people · 41 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 high48°F (9°C)48°F (9°C)53°F (11°C)59°F (15°C)66°F (19°C)72°F (22°C)76°F (25°C)77°F (25°C)73°F (23°C)67°F (20°C)59°F (15°C)51°F (11°C)
Average low37°F (3°C)36°F (2°C)40°F (5°C)47°F (8°C)55°F (13°C)63°F (17°C)68°F (20°C)69°F (21°C)64°F (18°C)57°F (14°C)47°F (9°C)40°F (5°C)
Dew point34°F (1°C)35°F (1°C)39°F (4°C)47°F (8°C)56°F (13°C)63°F (17°C)67°F (20°C)69°F (20°C)63°F (17°C)56°F (13°C)46°F (8°C)38°F (3°C)
Rainfall4.4 in (111 mm)3.7 in (94 mm)4.8 in (122 mm)5 in (126 mm)5.8 in (147 mm)5.3 in (135 mm)4.7 in (120 mm)5.7 in (145 mm)8.4 in (213 mm)8.6 in (219 mm)5.4 in (137 mm)4.3 in (110 mm)
Rainy days151416171716161817171314
Snowfall10.4 in (26.5 cm)9.4 in (23.9 cm)6.7 in (17.1 cm)0.6 in (1.6 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0.1 cm)1.5 in (3.9 cm)4.9 in (12.4 cm)
Sunshine193 h204 h251 h290 h339 h361 h377 h354 h291 h243 h214 h184 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 +1.3°F (+0.7°C) to +2.9°F (+1.6°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +1.8°F (+1.0°C)
  • February: +1.7°F (+0.9°C)
  • March: +2.6°F (+1.4°C)
  • April: +2.5°F (+1.4°C)
  • May: +2.1°F (+1.2°C)
  • June: +2.4°F (+1.3°C)
  • July: +2.6°F (+1.4°C)
  • August: +1.9°F (+1.1°C)
  • September: +2.4°F (+1.3°C)
  • October: +2.0°F (+1.1°C)
  • November: +1.5°F (+0.8°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.