ClimateSearch

Nay Pyi Taw, Nay Pyi Taw

Myanmar · 925k people · 120 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 high84°F (29°C)90°F (32°C)96°F (36°C)100°F (38°C)93°F (34°C)85°F (30°C)83°F (29°C)83°F (29°C)85°F (29°C)86°F (30°C)85°F (30°C)83°F (29°C)
Average low58°F (15°C)61°F (16°C)68°F (20°C)75°F (24°C)76°F (25°C)75°F (24°C)74°F (24°C)74°F (23°C)74°F (23°C)73°F (23°C)68°F (20°C)61°F (16°C)
Dew point56°F (13°C)54°F (12°C)56°F (13°C)63°F (17°C)72°F (22°C)74°F (24°C)74°F (24°C)74°F (24°C)74°F (24°C)74°F (23°C)67°F (20°C)60°F (16°C)
Rainfall0.3 in (8 mm)0.1 in (3 mm)0.3 in (7 mm)0.9 in (23 mm)6.1 in (156 mm)11.2 in (284 mm)12.4 in (315 mm)13.1 in (333 mm)9.1 in (231 mm)5.2 in (133 mm)1.1 in (29 mm)0.4 in (9 mm)
Rainy days101419282930272152
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)
Sunshine328 h311 h355 h358 h325 h226 h191 h190 h241 h302 h312 h327 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

+1.0°F (+0.6°C)

Models range from +0.0°F (+0.0°C) to +2.1°F (+1.1°C)

Days above 90°F (32°C) a year

100 116

About 1.2× as many

Warming by month
  • January: +1.1°F (+0.6°C)
  • February: +0.9°F (+0.5°C)
  • March: +0.6°F (+0.3°C)
  • April: +1.6°F (+0.9°C)
  • May: +1.9°F (+1.0°C)
  • June: +1.4°F (+0.8°C)
  • July: +0.8°F (+0.5°C)
  • August: +0.7°F (+0.4°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.1°F (+0.6°C)
  • November: +0.3°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.