ClimateSearch

Thị Trấn Thuận Châu, Sơn La Province

Vietnam · 153k people · 599 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 high69°F (21°C)74°F (23°C)80°F (27°C)83°F (29°C)85°F (29°C)84°F (29°C)83°F (28°C)83°F (28°C)82°F (28°C)79°F (26°C)75°F (24°C)69°F (21°C)
Average low54°F (12°C)56°F (13°C)62°F (17°C)67°F (19°C)70°F (21°C)72°F (22°C)72°F (22°C)71°F (22°C)70°F (21°C)66°F (19°C)60°F (16°C)54°F (12°C)
Dew point53°F (12°C)56°F (13°C)61°F (16°C)67°F (19°C)70°F (21°C)73°F (23°C)73°F (23°C)73°F (23°C)71°F (22°C)66°F (19°C)59°F (15°C)54°F (12°C)
Rainfall1.8 in (46 mm)1.5 in (38 mm)3 in (75 mm)4.9 in (124 mm)8.8 in (224 mm)14.5 in (368 mm)17.4 in (443 mm)14.7 in (373 mm)7.7 in (196 mm)2.8 in (70 mm)1.5 in (39 mm)1.5 in (39 mm)
Rainy days88121622272827201067
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)
Sunshine220 h232 h279 h286 h281 h235 h225 h246 h270 h276 h242 h229 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

+1.5°F (+0.9°C)

Models range from +1.0°F (+0.6°C) to +2.0°F (+1.1°C)

Days above 90°F (32°C) a year

14 28

About 2.0× as many

Warming by month
  • January: +1.9°F (+1.1°C)
  • February: +1.5°F (+0.9°C)
  • March: +1.4°F (+0.8°C)
  • April: +2.9°F (+1.6°C)
  • May: +2.6°F (+1.4°C)
  • June: +2.1°F (+1.2°C)
  • July: +1.6°F (+0.9°C)
  • August: +1.0°F (+0.5°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.7°F (+0.9°C)
  • November: +1.4°F (+0.8°C)
  • December: +1.7°F (+1.0°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.