ClimateSearch

Myeik, Tanintharyi Region

Myanmar · 173k people · 17 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 high89°F (32°C)90°F (32°C)90°F (32°C)90°F (32°C)86°F (30°C)84°F (29°C)83°F (28°C)82°F (28°C)83°F (28°C)85°F (29°C)87°F (31°C)88°F (31°C)
Average low72°F (22°C)73°F (23°C)75°F (24°C)77°F (25°C)77°F (25°C)76°F (25°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)72°F (22°C)
Dew point69°F (20°C)70°F (21°C)73°F (23°C)76°F (24°C)77°F (25°C)76°F (25°C)76°F (24°C)76°F (24°C)75°F (24°C)75°F (24°C)73°F (23°C)68°F (20°C)
Rainfall1.1 in (29 mm)1.4 in (35 mm)3.8 in (96 mm)6 in (151 mm)16.9 in (430 mm)22.4 in (569 mm)25.3 in (644 mm)25.6 in (651 mm)23.2 in (589 mm)14.1 in (358 mm)3.1 in (80 mm)0.9 in (23 mm)
Rainy days461319293031313027114
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)
Sunshine334 h309 h336 h327 h271 h223 h204 h185 h200 h265 h307 h329 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

+1.9°F (+1.1°C)

Models range from +1.6°F (+0.9°C) to +2.6°F (+1.5°C)

Days above 90°F (32°C) a year

71 103

About 1.4× as many

Warming by month
  • January: +1.4°F (+0.8°C)
  • February: +1.3°F (+0.7°C)
  • March: +1.0°F (+0.6°C)
  • April: +1.9°F (+1.1°C)
  • May: +2.0°F (+1.1°C)
  • June: +2.0°F (+1.1°C)
  • July: +1.8°F (+1.0°C)
  • August: +1.9°F (+1.1°C)
  • September: +2.1°F (+1.2°C)
  • October: +1.8°F (+1.0°C)
  • November: +1.6°F (+0.9°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.