ClimateSearch

Bento Gonçalves, Rio Grande do Sul

Brazil · 128k people · 669 m elevation · Southern 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 high79°F (26°C)78°F (26°C)76°F (24°C)71°F (22°C)65°F (18°C)62°F (17°C)62°F (17°C)66°F (19°C)68°F (20°C)71°F (22°C)74°F (23°C)78°F (26°C)
Average low63°F (17°C)63°F (17°C)60°F (16°C)56°F (13°C)50°F (10°C)47°F (9°C)46°F (8°C)48°F (9°C)50°F (10°C)54°F (12°C)56°F (14°C)61°F (16°C)
Dew point64°F (18°C)64°F (18°C)61°F (16°C)57°F (14°C)52°F (11°C)49°F (10°C)47°F (9°C)49°F (10°C)52°F (11°C)56°F (13°C)58°F (14°C)61°F (16°C)
Rainfall7.9 in (202 mm)7.2 in (184 mm)6 in (152 mm)5.6 in (142 mm)5.4 in (137 mm)5.6 in (142 mm)7 in (178 mm)5.5 in (139 mm)6.7 in (171 mm)8.4 in (213 mm)6.3 in (161 mm)7.3 in (186 mm)
Rainy days181716121111111113151416
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)
Sunshine332 h294 h296 h254 h231 h202 h217 h249 h234 h260 h304 h335 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 (+0.9°C)

Models range from +1.3°F (+0.7°C) to +2.1°F (+1.1°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +1.5°F (+0.9°C)
  • February: +1.3°F (+0.7°C)
  • March: +1.3°F (+0.7°C)
  • April: +1.4°F (+0.8°C)
  • May: +1.5°F (+0.8°C)
  • June: +1.3°F (+0.7°C)
  • July: +1.7°F (+0.9°C)
  • August: +1.5°F (+0.8°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.5°F (+0.8°C)
  • November: +1.5°F (+0.8°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.