ClimateSearch

Mu-se, Shan State

Myanmar · 165k people · 826 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 high72°F (22°C)76°F (25°C)83°F (28°C)87°F (30°C)84°F (29°C)81°F (27°C)80°F (27°C)81°F (27°C)81°F (27°C)79°F (26°C)75°F (24°C)72°F (22°C)
Average low50°F (10°C)54°F (12°C)60°F (16°C)65°F (18°C)67°F (20°C)69°F (21°C)69°F (21°C)69°F (21°C)68°F (20°C)65°F (18°C)57°F (14°C)52°F (11°C)
Dew point50°F (10°C)50°F (10°C)52°F (11°C)58°F (15°C)67°F (19°C)71°F (22°C)71°F (22°C)71°F (22°C)70°F (21°C)67°F (19°C)60°F (16°C)54°F (12°C)
Rainfall1.1 in (27 mm)0.8 in (21 mm)1.1 in (28 mm)2.2 in (57 mm)7.5 in (190 mm)11.3 in (287 mm)14.6 in (370 mm)12.7 in (323 mm)8.4 in (213 mm)5.8 in (147 mm)2.1 in (53 mm)0.7 in (17 mm)
Rainy days335920283030251973
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)
Sunshine316 h298 h336 h348 h316 h216 h168 h200 h234 h265 h281 h303 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 +1.0°F (+0.5°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

14 21

About 1.5× as many

Warming by month
  • January: +1.9°F (+1.1°C)
  • February: +1.4°F (+0.8°C)
  • March: +0.8°F (+0.5°C)
  • April: +1.4°F (+0.8°C)
  • May: +2.1°F (+1.2°C)
  • June: +1.7°F (+1.0°C)
  • July: +1.0°F (+0.6°C)
  • August: +1.0°F (+0.6°C)
  • September: +1.2°F (+0.7°C)
  • October: +1.4°F (+0.8°C)
  • November: +1.0°F (+0.6°C)
  • December: +1.3°F (+0.7°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.