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 high55°F (13°C)56°F (13°C)61°F (16°C)68°F (20°C)77°F (25°C)85°F (30°C)89°F (32°C)91°F (33°C)85°F (29°C)76°F (25°C)65°F (18°C)57°F (14°C)
Average low41°F (5°C)43°F (6°C)47°F (8°C)55°F (13°C)64°F (18°C)72°F (22°C)75°F (24°C)75°F (24°C)70°F (21°C)61°F (16°C)49°F (10°C)43°F (6°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)
Rainfall3.5 in (88 mm)2.9 in (75 mm)2.4 in (61 mm)1.2 in (30 mm)0.9 in (24 mm)0.9 in (23 mm)1 in (26 mm)1.9 in (49 mm)4.5 in (114 mm)6 in (151 mm)5.5 in (140 mm)4 in (101 mm)
Rainy days121211732248101211
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)
Sunshine157 h150 h177 h194 h230 h249 h250 h256 h201 h188 h150 h151 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.