ClimateSearch

Yenangyaung, Magway

Myanmar · 111k people · 57 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 high86°F (30°C)92°F (33°C)98°F (37°C)103°F (40°C)99°F (37°C)94°F (34°C)91°F (33°C)91°F (33°C)91°F (33°C)92°F (33°C)90°F (32°C)85°F (30°C)
Average low58°F (15°C)62°F (17°C)70°F (21°C)78°F (26°C)79°F (26°C)78°F (25°C)78°F (26°C)78°F (25°C)77°F (25°C)75°F (24°C)69°F (21°C)61°F (16°C)
Dew point56°F (14°C)55°F (13°C)58°F (15°C)65°F (19°C)72°F (22°C)75°F (24°C)75°F (24°C)75°F (24°C)76°F (24°C)74°F (24°C)68°F (20°C)61°F (16°C)
Rainfall0.1 in (1 mm)0 in (0 mm)0.3 in (6 mm)0.9 in (23 mm)4.9 in (124 mm)4.2 in (107 mm)3.1 in (78 mm)3.6 in (92 mm)5 in (127 mm)4.9 in (126 mm)0.7 in (19 mm)0.5 in (13 mm)
Rainy days001167679821
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)
Sunshine274 h274 h305 h294 h239 h132 h108 h111 h129 h186 h235 h263 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

+1.1°F (+0.6°C)

Models range from −0.5°F (−0.3°C) to +2.9°F (+1.6°C)

Days above 90°F (32°C) a year

128 → 143

About 1.1× as many

Warming by month
  • January: +0.9°F (+0.5°C)
  • February: +0.7°F (+0.4°C)
  • March: +0.6°F (+0.3°C)
  • April: +1.5°F (+0.8°C)
  • May: +1.2°F (+0.6°C)
  • June: +1.3°F (+0.7°C)
  • July: +0.9°F (+0.5°C)
  • August: +1.0°F (+0.6°C)
  • September: +0.9°F (+0.5°C)
  • October: +1.4°F (+0.8°C)
  • November: +0.4°F (+0.2°C)
  • December: +0.7°F (+0.4°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.