ClimateSearch

Yangon, Yangon

Myanmar · 4.5M people · 26 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 high87°F (31°C)92°F (33°C)96°F (36°C)98°F (37°C)91°F (33°C)85°F (30°C)84°F (29°C)84°F (29°C)85°F (29°C)86°F (30°C)87°F (31°C)86°F (30°C)
Average low65°F (18°C)67°F (20°C)72°F (22°C)77°F (25°C)78°F (26°C)77°F (25°C)76°F (24°C)76°F (24°C)76°F (24°C)76°F (24°C)72°F (22°C)67°F (20°C)
Dew point61°F (16°C)61°F (16°C)65°F (19°C)70°F (21°C)75°F (24°C)76°F (25°C)76°F (24°C)76°F (24°C)76°F (24°C)75°F (24°C)71°F (22°C)64°F (18°C)
Rainfall0.2 in (5 mm)0.1 in (2 mm)0.5 in (12 mm)1.6 in (40 mm)10.6 in (269 mm)17.7 in (448 mm)18.6 in (471 mm)18.8 in (478 mm)14.2 in (360 mm)7.3 in (184 mm)1.5 in (39 mm)0.2 in (5 mm)
Rainy days102523303131292151
Snowfall0 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 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)
Sunshine329 h314 h354 h349 h288 h194 h169 h165 h221 h294 h313 h334 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

+1.9°F (+1.0°C)

Models range from +1.2°F (+0.6°C) to +3.4°F (+1.9°C)

Days above 90°F (32°C) a year

103 138

About 1.3× as many

Warming by month
  • January: +1.5°F (+0.9°C)
  • February: +1.7°F (+1.0°C)
  • March: +1.2°F (+0.7°C)
  • April: +2.4°F (+1.3°C)
  • May: +2.6°F (+1.5°C)
  • June: +2.2°F (+1.2°C)
  • July: +1.9°F (+1.1°C)
  • August: +1.4°F (+0.8°C)
  • September: +1.7°F (+0.9°C)
  • October: +1.4°F (+0.8°C)
  • November: +1.4°F (+0.8°C)
  • December: +1.6°F (+0.9°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.