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 high67°F (20°C)71°F (22°C)77°F (25°C)84°F (29°C)88°F (31°C)90°F (32°C)89°F (32°C)89°F (31°C)87°F (30°C)83°F (28°C)77°F (25°C)70°F (21°C)
Average low57°F (14°C)60°F (16°C)66°F (19°C)72°F (22°C)76°F (24°C)78°F (26°C)78°F (26°C)78°F (25°C)76°F (24°C)71°F (22°C)65°F (18°C)58°F (15°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)
Rainfall2.1 in (53 mm)1.7 in (43 mm)2.9 in (74 mm)4.5 in (114 mm)10.3 in (261 mm)14.3 in (362 mm)14.3 in (364 mm)14.1 in (357 mm)8 in (203 mm)3.9 in (99 mm)2.5 in (62 mm)1.6 in (40 mm)
Rainy days1111131420232525181188
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)
Sunshine118 h112 h118 h175 h235 h233 h242 h248 h262 h263 h212 h174 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.