ClimateSearch

Hlaingthaya, Yangon

Myanmar · 688k people · 5 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)97°F (36°C)99°F (37°C)92°F (33°C)86°F (30°C)85°F (29°C)84°F (29°C)85°F (30°C)87°F (30°C)87°F (31°C)86°F (30°C)
Average low65°F (19°C)67°F (20°C)72°F (22°C)78°F (25°C)78°F (26°C)77°F (25°C)76°F (25°C)76°F (24°C)76°F (24°C)76°F (24°C)73°F (23°C)68°F (20°C)
Dew point61°F (16°C)60°F (16°C)64°F (18°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)1.5 in (38 mm)11 in (280 mm)18.7 in (475 mm)19.4 in (493 mm)19.5 in (495 mm)15.2 in (385 mm)8.3 in (210 mm)1.8 in (45 mm)0.2 in (5 mm)
Rainy days102523303131292261
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 h348 h288 h191 h165 h161 h217 h290 h312 h333 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

+1.8°F (+1.0°C)

Models range from +1.1°F (+0.6°C) to +3.4°F (+1.9°C)

Days above 90°F (32°C) a year

109 144

About 1.3× as many

Warming by month
  • January: +1.5°F (+0.8°C)
  • February: +1.7°F (+0.9°C)
  • March: +1.2°F (+0.7°C)
  • April: +2.4°F (+1.3°C)
  • May: +2.7°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: +1.6°F (+0.9°C)
  • October: +1.4°F (+0.8°C)
  • November: +1.4°F (+0.8°C)
  • December: +1.5°F (+0.8°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.