ClimateSearch

Myingyan, Mandalay Region

Myanmar · 142k people · 76 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)93°F (34°C)100°F (38°C)104°F (40°C)99°F (37°C)95°F (35°C)94°F (34°C)93°F (34°C)93°F (34°C)92°F (33°C)90°F (32°C)85°F (29°C)
Average low57°F (14°C)61°F (16°C)69°F (21°C)77°F (25°C)78°F (26°C)79°F (26°C)78°F (26°C)78°F (26°C)77°F (25°C)75°F (24°C)68°F (20°C)60°F (16°C)
Dew point56°F (14°C)54°F (12°C)55°F (13°C)62°F (17°C)71°F (21°C)74°F (23°C)73°F (23°C)74°F (23°C)75°F (24°C)74°F (23°C)67°F (20°C)60°F (16°C)
Rainfall0.1 in (2 mm)0 in (1 mm)0.2 in (6 mm)1 in (26 mm)4.5 in (115 mm)3.7 in (94 mm)2.9 in (74 mm)4 in (101 mm)5.7 in (144 mm)4.2 in (107 mm)0.7 in (19 mm)0.4 in (9 mm)
Rainy days0012776812921
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)
Sunshine273 h265 h300 h287 h239 h144 h118 h116 h128 h186 h232 h260 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

+0.9°F (+0.5°C)

Models range from −0.2°F (−0.1°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

169 → 193

About 1.1× as many

Warming by month
  • January: +1.0°F (+0.6°C)
  • February: +0.7°F (+0.4°C)
  • March: +0.6°F (+0.3°C)
  • April: +1.2°F (+0.7°C)
  • May: +1.3°F (+0.7°C)
  • June: +1.2°F (+0.6°C)
  • July: +0.8°F (+0.5°C)
  • August: +0.8°F (+0.4°C)
  • September: +1.1°F (+0.6°C)
  • October: +1.4°F (+0.8°C)
  • November: +0.6°F (+0.3°C)
  • December: +0.8°F (+0.5°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.