ClimateSearch

Meiktila, Mandalay Region

Myanmar · 177k people · 243 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)101°F (39°C)96°F (36°C)92°F (33°C)91°F (33°C)90°F (32°C)90°F (32°C)90°F (32°C)89°F (31°C)84°F (29°C)
Average low58°F (14°C)61°F (16°C)69°F (21°C)76°F (24°C)77°F (25°C)76°F (25°C)76°F (25°C)76°F (25°C)75°F (24°C)74°F (23°C)68°F (20°C)60°F (16°C)
Dew point53°F (12°C)51°F (10°C)53°F (11°C)61°F (16°C)70°F (21°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)72°F (22°C)65°F (19°C)58°F (14°C)
Rainfall0.2 in (4 mm)0 in (1 mm)0.3 in (6 mm)1.4 in (36 mm)5.9 in (149 mm)4.4 in (112 mm)3.3 in (84 mm)4.1 in (104 mm)6.1 in (154 mm)5.5 in (139 mm)1.1 in (28 mm)0.6 in (16 mm)
Rainy days001310979131231
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)
Sunshine277 h268 h299 h286 h229 h127 h100 h100 h123 h185 h235 h264 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

+0.7°F (+0.4°C)

Models range from −0.4°F (−0.2°C) to +1.5°F (+0.8°C)

Days above 90°F (32°C) a year

103 → 114

About 1.1× as many

Warming by month
  • January: +1.2°F (+0.7°C)
  • February: +0.9°F (+0.5°C)
  • March: +0.6°F (+0.3°C)
  • April: +1.2°F (+0.7°C)
  • May: +1.3°F (+0.7°C)
  • June: +0.8°F (+0.4°C)
  • July: +0.6°F (+0.4°C)
  • August: +0.8°F (+0.4°C)
  • September: +1.1°F (+0.6°C)
  • October: +1.1°F (+0.6°C)
  • November: +0.4°F (+0.2°C)
  • December: +0.6°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.