ClimateSearch

Sóc Trăng, Can Tho City

Vietnam · 221k people · 9 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 high84°F (29°C)86°F (30°C)89°F (32°C)90°F (32°C)89°F (32°C)87°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)85°F (29°C)84°F (29°C)83°F (29°C)
Average low73°F (23°C)74°F (23°C)76°F (24°C)77°F (25°C)78°F (25°C)77°F (25°C)76°F (25°C)76°F (25°C)76°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)
Dew point70°F (21°C)70°F (21°C)72°F (22°C)74°F (24°C)76°F (24°C)76°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)71°F (22°C)
Rainfall0.9 in (22 mm)0.3 in (9 mm)1.2 in (31 mm)2.7 in (68 mm)8.1 in (206 mm)10 in (253 mm)10 in (254 mm)9.8 in (248 mm)11.2 in (284 mm)12.2 in (310 mm)6.3 in (159 mm)3.4 in (87 mm)
Rainy days425132628302929281911
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)
Sunshine326 h316 h359 h346 h317 h274 h286 h294 h262 h264 h286 h295 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 +1.2°F (+0.7°C) to +1.9°F (+1.0°C)

Days above 90°F (32°C) a year

38 66

About 1.7× as many

Warming by month
  • January: +0.9°F (+0.5°C)
  • February: +0.9°F (+0.5°C)
  • March: +0.9°F (+0.5°C)
  • April: +1.4°F (+0.8°C)
  • May: +1.4°F (+0.8°C)
  • June: +1.6°F (+0.9°C)
  • July: +1.5°F (+0.8°C)
  • August: +1.7°F (+0.9°C)
  • September: +1.7°F (+1.0°C)
  • October: +1.8°F (+1.0°C)
  • November: +1.5°F (+0.8°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.