ClimateSearch

Ô Môn, Can Tho City

Vietnam · 130k people · 6 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 high85°F (30°C)88°F (31°C)91°F (33°C)92°F (33°C)90°F (32°C)87°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)85°F (29°C)
Average low72°F (22°C)73°F (23°C)75°F (24°C)77°F (25°C)77°F (25°C)77°F (25°C)76°F (25°C)76°F (25°C)76°F (24°C)75°F (24°C)74°F (23°C)73°F (23°C)
Dew point70°F (21°C)69°F (21°C)71°F (22°C)73°F (23°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)73°F (23°C)71°F (21°C)
Rainfall1 in (26 mm)0.5 in (12 mm)1.6 in (40 mm)3.2 in (82 mm)8.1 in (207 mm)9.6 in (243 mm)10.2 in (259 mm)9.9 in (252 mm)11.1 in (283 mm)11.8 in (301 mm)5.6 in (142 mm)2.8 in (72 mm)
Rainy days426122627292928281810
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)
Sunshine323 h312 h354 h337 h302 h258 h262 h268 h239 h251 h281 h296 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

+2.6°F (+1.5°C)

Models range from +1.5°F (+0.8°C) to +5.4°F (+3.0°C)

Days above 90°F (32°C) a year

67 124

About 1.8× as many

Warming by month
  • January: +1.5°F (+0.8°C)
  • February: +1.5°F (+0.8°C)
  • March: +1.5°F (+0.8°C)
  • April: +2.8°F (+1.6°C)
  • May: +2.4°F (+1.3°C)
  • June: +2.6°F (+1.4°C)
  • July: +2.7°F (+1.5°C)
  • August: +2.6°F (+1.4°C)
  • September: +2.6°F (+1.4°C)
  • October: +2.3°F (+1.3°C)
  • November: +1.9°F (+1.1°C)
  • December: +1.9°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.