ClimateSearch

Thị Trấn Đại Từ, Thai Nguyen

Vietnam · 179k people · 65 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 high65°F (19°C)69°F (21°C)72°F (22°C)80°F (27°C)88°F (31°C)91°F (33°C)90°F (32°C)90°F (32°C)88°F (31°C)84°F (29°C)78°F (26°C)71°F (22°C)
Average low54°F (12°C)58°F (15°C)63°F (17°C)69°F (20°C)74°F (24°C)77°F (25°C)77°F (25°C)77°F (25°C)74°F (23°C)69°F (21°C)63°F (17°C)57°F (14°C)
Dew point55°F (13°C)58°F (15°C)64°F (18°C)71°F (22°C)75°F (24°C)78°F (26°C)79°F (26°C)78°F (26°C)75°F (24°C)69°F (21°C)62°F (17°C)55°F (13°C)
Rainfall0.7 in (18 mm)1.2 in (31 mm)1.9 in (48 mm)2.9 in (74 mm)7.5 in (191 mm)10.9 in (277 mm)14.6 in (371 mm)14.1 in (357 mm)7.7 in (196 mm)2.6 in (66 mm)1.4 in (36 mm)1.2 in (31 mm)
Rainy days24451316191812534
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)
Sunshine51 h47 h46 h81 h112 h96 h103 h116 h147 h169 h132 h98 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 +1.1°F (+0.6°C) to +2.1°F (+1.1°C)

Days above 90°F (32°C) a year

62 → 95

About 1.5× as many

Warming by month
  • January: +2.2°F (+1.2°C)
  • February: +1.5°F (+0.9°C)
  • March: +1.7°F (+0.9°C)
  • April: +3.0°F (+1.7°C)
  • May: +2.3°F (+1.3°C)
  • June: +1.9°F (+1.1°C)
  • July: +1.5°F (+0.9°C)
  • August: +1.4°F (+0.8°C)
  • September: +1.7°F (+0.9°C)
  • October: +1.9°F (+1.1°C)
  • November: +2.2°F (+1.2°C)
  • December: +2.1°F (+1.2°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.