ClimateSearch

Ba Đồn, Quang Tri

Vietnam · 106k people · 5 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 high73°F (23°C)74°F (24°C)79°F (26°C)86°F (30°C)90°F (32°C)93°F (34°C)92°F (33°C)91°F (33°C)88°F (31°C)84°F (29°C)80°F (27°C)75°F (24°C)
Average low62°F (17°C)65°F (18°C)69°F (20°C)73°F (23°C)77°F (25°C)80°F (27°C)79°F (26°C)78°F (26°C)76°F (25°C)73°F (23°C)69°F (21°C)65°F (18°C)
Dew point62°F (17°C)64°F (18°C)69°F (20°C)73°F (23°C)75°F (24°C)74°F (24°C)74°F (23°C)74°F (24°C)75°F (24°C)72°F (22°C)68°F (20°C)63°F (17°C)
Rainfall4.4 in (113 mm)2.6 in (67 mm)2.6 in (66 mm)3 in (75 mm)4.1 in (104 mm)2.1 in (52 mm)6.2 in (157 mm)5.2 in (133 mm)19.4 in (494 mm)21.2 in (539 mm)14.9 in (378 mm)7.3 in (186 mm)
Rainy days10765737716171413
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)
Sunshine73 h89 h140 h173 h177 h155 h151 h140 h125 h125 h97 h56 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

+1.7°F (+1.0°C)

Models range from +1.5°F (+0.9°C) to +1.9°F (+1.1°C)

Days above 90°F (32°C) a year

81 → 112

About 1.4× as many

Warming by month
  • January: +1.5°F (+0.8°C)
  • February: +1.2°F (+0.6°C)
  • March: +1.6°F (+0.9°C)
  • April: +2.4°F (+1.3°C)
  • May: +1.9°F (+1.1°C)
  • June: +2.1°F (+1.2°C)
  • July: +1.5°F (+0.8°C)
  • August: +1.6°F (+0.9°C)
  • September: +1.7°F (+0.9°C)
  • October: +1.7°F (+0.9°C)
  • November: +1.9°F (+1.1°C)
  • December: +1.7°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.