ClimateSearch

Việt Trì, Phu Tho

Vietnam · 415k people · 26 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 (19°C)70°F (21°C)76°F (25°C)84°F (29°C)88°F (31°C)90°F (32°C)89°F (32°C)88°F (31°C)86°F (30°C)82°F (28°C)76°F (25°C)69°F (21°C)
Average low57°F (14°C)60°F (15°C)65°F (18°C)71°F (22°C)76°F (24°C)78°F (26°C)78°F (26°C)78°F (25°C)76°F (24°C)72°F (22°C)65°F (19°C)58°F (15°C)
Dew point54°F (12°C)58°F (14°C)63°F (17°C)70°F (21°C)74°F (24°C)77°F (25°C)78°F (25°C)77°F (25°C)75°F (24°C)69°F (21°C)63°F (17°C)55°F (13°C)
Rainfall1.7 in (43 mm)1.1 in (28 mm)2 in (52 mm)3.4 in (86 mm)8.1 in (207 mm)9 in (230 mm)10.3 in (263 mm)12.2 in (310 mm)8.5 in (217 mm)4.4 in (111 mm)2 in (52 mm)1.3 in (32 mm)
Rainy days98111117192122181177
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)
Sunshine122 h119 h133 h196 h249 h245 h248 h243 h249 h257 h214 h175 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 +2.1°F (+1.2°C)

Days above 90°F (32°C) a year

60 95

About 1.6× as many

Warming by month
  • January: +2.3°F (+1.3°C)
  • February: +1.5°F (+0.9°C)
  • March: +1.7°F (+1.0°C)
  • April: +3.0°F (+1.7°C)
  • May: +2.4°F (+1.4°C)
  • June: +1.9°F (+1.1°C)
  • July: +1.6°F (+0.9°C)
  • August: +1.4°F (+0.8°C)
  • September: +1.8°F (+1.0°C)
  • October: +2.1°F (+1.2°C)
  • November: +2.3°F (+1.3°C)
  • December: +2.2°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.