ClimateSearch

Kēng Tung, Shan State

Myanmar · 172k people · 697 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 high76°F (25°C)82°F (28°C)88°F (31°C)90°F (32°C)88°F (31°C)85°F (30°C)83°F (28°C)83°F (28°C)83°F (28°C)81°F (27°C)78°F (26°C)74°F (24°C)
Average low55°F (13°C)57°F (14°C)63°F (17°C)68°F (20°C)71°F (21°C)72°F (22°C)71°F (22°C)71°F (22°C)70°F (21°C)67°F (19°C)61°F (16°C)56°F (13°C)
Dew point54°F (12°C)52°F (11°C)55°F (13°C)62°F (17°C)69°F (21°C)72°F (22°C)72°F (22°C)72°F (22°C)71°F (22°C)68°F (20°C)62°F (17°C)56°F (14°C)
Rainfall0.8 in (21 mm)0.4 in (11 mm)0.8 in (20 mm)1.8 in (47 mm)5 in (128 mm)7.4 in (188 mm)12.7 in (322 mm)12.5 in (316 mm)7.5 in (192 mm)3.9 in (98 mm)1.5 in (37 mm)0.7 in (19 mm)
Rainy days324817252929231564
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)
Sunshine307 h296 h331 h338 h316 h260 h204 h217 h247 h275 h265 h285 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 +1.4°F (+0.8°C) to +1.9°F (+1.1°C)

Days above 90°F (32°C) a year

43 65

About 1.5× as many

Warming by month
  • January: +1.9°F (+1.1°C)
  • February: +1.4°F (+0.8°C)
  • March: +0.9°F (+0.5°C)
  • April: +2.6°F (+1.4°C)
  • May: +2.7°F (+1.5°C)
  • June: +2.3°F (+1.3°C)
  • July: +1.5°F (+0.8°C)
  • August: +1.1°F (+0.6°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.5°F (+0.8°C)
  • November: +0.9°F (+0.5°C)
  • December: +1.2°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.