ClimateSearch

Amarapura, Mandalay Region

Myanmar · 238k 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 high84°F (29°C)90°F (32°C)97°F (36°C)101°F (38°C)96°F (36°C)94°F (34°C)93°F (34°C)92°F (33°C)92°F (33°C)91°F (33°C)89°F (32°C)84°F (29°C)
Average low57°F (14°C)61°F (16°C)68°F (20°C)75°F (24°C)78°F (25°C)79°F (26°C)79°F (26°C)78°F (26°C)78°F (25°C)76°F (24°C)69°F (21°C)61°F (16°C)
Dew point58°F (14°C)55°F (13°C)56°F (13°C)63°F (17°C)72°F (22°C)74°F (23°C)73°F (23°C)74°F (23°C)75°F (24°C)74°F (23°C)69°F (20°C)62°F (17°C)
Rainfall0.1 in (2 mm)0.1 in (2 mm)0.2 in (6 mm)1.8 in (45 mm)5.3 in (135 mm)4 in (103 mm)3 in (75 mm)4.2 in (107 mm)5.2 in (131 mm)4.3 in (110 mm)1.1 in (27 mm)0.3 in (9 mm)
Rainy days00131086811921
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)
Sunshine271 h262 h295 h282 h233 h135 h105 h105 h124 h184 h223 h250 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

+0.8°F (+0.5°C)

Models range from −0.6°F (−0.3°C) to +2.0°F (+1.1°C)

Days above 90°F (32°C) a year

138 → 156

About 1.1× as many

Warming by month
  • January: +1.2°F (+0.7°C)
  • February: +0.7°F (+0.4°C)
  • March: +0.3°F (+0.2°C)
  • April: +1.0°F (+0.6°C)
  • May: +1.4°F (+0.8°C)
  • June: +1.1°F (+0.6°C)
  • July: +0.7°F (+0.4°C)
  • August: +0.8°F (+0.4°C)
  • September: +1.0°F (+0.6°C)
  • October: +1.2°F (+0.7°C)
  • November: +0.7°F (+0.4°C)
  • December: +0.8°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.