ClimateSearch

Āmol, Māzandarān

Iran · 238k people · 93 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 high51°F (11°C)52°F (11°C)57°F (14°C)64°F (18°C)72°F (22°C)78°F (25°C)81°F (27°C)82°F (28°C)77°F (25°C)70°F (21°C)61°F (16°C)54°F (12°C)
Average low35°F (2°C)36°F (2°C)41°F (5°C)49°F (10°C)58°F (15°C)66°F (19°C)70°F (21°C)71°F (22°C)66°F (19°C)57°F (14°C)47°F (8°C)39°F (4°C)
Dew point37°F (3°C)38°F (3°C)43°F (6°C)50°F (10°C)59°F (15°C)65°F (18°C)69°F (20°C)69°F (21°C)65°F (18°C)57°F (14°C)47°F (9°C)40°F (5°C)
Rainfall4.7 in (119 mm)4.7 in (119 mm)4.4 in (111 mm)3.2 in (82 mm)3 in (76 mm)2.3 in (58 mm)2.9 in (72 mm)3 in (77 mm)6.4 in (162 mm)6.9 in (175 mm)6.5 in (166 mm)4.8 in (122 mm)
Rainy days14141513129121214131413
Snowfall2.1 in (5.4 cm)2.9 in (7.4 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 cm)0 in (0 cm)0.4 in (1 cm)0.4 in (1 cm)
Sunshine240 h235 h280 h306 h346 h352 h360 h360 h288 h268 h225 h228 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

+2.8°F (+1.6°C)

Models range from +2.3°F (+1.3°C) to +3.5°F (+2.0°C)

Days above 90°F (32°C) a year

6 15

About 2.4× as many

Warming by month
  • January: +1.0°F (+0.6°C)
  • February: +1.4°F (+0.8°C)
  • March: +2.2°F (+1.2°C)
  • April: +2.2°F (+1.2°C)
  • May: +2.1°F (+1.2°C)
  • June: +3.1°F (+1.7°C)
  • July: +2.7°F (+1.5°C)
  • August: +2.5°F (+1.4°C)
  • September: +2.4°F (+1.3°C)
  • October: +1.8°F (+1.0°C)
  • November: +1.3°F (+0.7°C)
  • December: +1.1°F (+0.6°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.