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 high82°F (28°C)88°F (31°C)95°F (35°C)99°F (37°C)94°F (34°C)87°F (31°C)85°F (30°C)85°F (29°C)86°F (30°C)86°F (30°C)84°F (29°C)81°F (27°C)
Average low58°F (15°C)62°F (17°C)69°F (21°C)76°F (25°C)77°F (25°C)76°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)73°F (23°C)67°F (20°C)61°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 (6 mm)0.1 in (1 mm)0.2 in (6 mm)0.9 in (23 mm)4.8 in (122 mm)5.2 in (132 mm)5.6 in (143 mm)7.5 in (190 mm)7.9 in (200 mm)6.3 in (160 mm)1.6 in (42 mm)0.4 in (11 mm)
Rainy days101516212326232261
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)
Sunshine325 h309 h355 h358 h347 h280 h252 h249 h261 h296 h306 h322 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.