ClimateSearch

Mawlamyine, Mon

Myanmar · 439k people · 40 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 high91°F (33°C)93°F (34°C)95°F (35°C)96°F (36°C)91°F (33°C)85°F (30°C)83°F (29°C)83°F (29°C)85°F (30°C)89°F (32°C)91°F (33°C)90°F (32°C)
Average low64°F (18°C)67°F (19°C)72°F (22°C)76°F (24°C)76°F (24°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)72°F (22°C)67°F (20°C)
Dew point65°F (18°C)66°F (19°C)71°F (21°C)74°F (24°C)76°F (25°C)76°F (25°C)76°F (24°C)75°F (24°C)76°F (24°C)75°F (24°C)71°F (22°C)65°F (18°C)
Rainfall0.1 in (3 mm)0.1 in (4 mm)0.5 in (13 mm)3.2 in (81 mm)19 in (484 mm)35.9 in (911 mm)52.2 in (1325 mm)46.8 in (1188 mm)29.9 in (761 mm)7.7 in (196 mm)1.3 in (33 mm)0.5 in (13 mm)
Rainy days001522293030271421
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)
Sunshine255 h247 h265 h243 h121 h50 h33 h29 h78 h177 h229 h253 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

+1.6°F (+0.9°C)

Models range from +1.1°F (+0.6°C) to +2.3°F (+1.3°C)

Days above 90°F (32°C) a year

90 → 120

About 1.3× as many

Warming by month
  • January: +1.3°F (+0.7°C)
  • February: +1.5°F (+0.8°C)
  • March: +1.0°F (+0.5°C)
  • April: +1.9°F (+1.1°C)
  • May: +2.1°F (+1.2°C)
  • June: +1.9°F (+1.1°C)
  • July: +1.4°F (+0.8°C)
  • August: +1.4°F (+0.8°C)
  • September: +1.3°F (+0.7°C)
  • October: +1.4°F (+0.8°C)
  • November: +1.1°F (+0.6°C)
  • December: +1.4°F (+0.8°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.