ClimateSearch

Taungoo, Bago Region

Myanmar · 107k people · 51 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 (31°C)94°F (35°C)98°F (37°C)101°F (38°C)96°F (35°C)89°F (32°C)88°F (31°C)87°F (31°C)89°F (32°C)91°F (33°C)92°F (33°C)89°F (32°C)
Average low60°F (16°C)62°F (17°C)69°F (21°C)76°F (25°C)77°F (25°C)76°F (24°C)76°F (24°C)76°F (24°C)75°F (24°C)75°F (24°C)70°F (21°C)63°F (17°C)
Dew point59°F (15°C)56°F (14°C)58°F (15°C)65°F (18°C)73°F (23°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (24°C)69°F (21°C)62°F (17°C)
Rainfall0.3 in (8 mm)0 in (1 mm)0.3 in (8 mm)17.5 in (445 mm)7.5 in (191 mm)13.5 in (343 mm)16 in (407 mm)16.2 in (410 mm)11.6 in (295 mm)5.8 in (147 mm)1.2 in (30 mm)0.4 in (10 mm)
Rainy days10151323252518921
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)
Sunshine270 h266 h297 h280 h179 h68 h48 h50 h98 h185 h235 h263 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

+1.3°F (+0.7°C)

Models range from +0.7°F (+0.4°C) to +2.2°F (+1.2°C)

Days above 90°F (32°C) a year

95 → 119

About 1.2× as many

Warming by month
  • January: +1.4°F (+0.8°C)
  • February: +1.4°F (+0.8°C)
  • March: +0.9°F (+0.5°C)
  • April: +2.0°F (+1.1°C)
  • May: +2.2°F (+1.2°C)
  • June: +1.8°F (+1.0°C)
  • July: +1.1°F (+0.6°C)
  • August: +1.0°F (+0.6°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.0°F (+0.6°C)
  • November: +0.8°F (+0.4°C)
  • December: +1.1°F (+0.6°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.