ClimateSearch

Curitiba, Paraná

Brazil · 1.9M people · 922 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 high77°F (25°C)77°F (25°C)75°F (24°C)72°F (22°C)67°F (19°C)65°F (18°C)65°F (18°C)68°F (20°C)69°F (21°C)72°F (22°C)73°F (23°C)76°F (25°C)
Average low64°F (18°C)64°F (18°C)63°F (17°C)59°F (15°C)54°F (12°C)51°F (11°C)50°F (10°C)51°F (11°C)54°F (12°C)57°F (14°C)59°F (15°C)62°F (17°C)
Dew point65°F (18°C)65°F (18°C)63°F (17°C)60°F (15°C)55°F (13°C)53°F (11°C)51°F (11°C)52°F (11°C)55°F (13°C)58°F (15°C)60°F (15°C)63°F (17°C)
Rainfall8.7 in (222 mm)7.6 in (192 mm)5 in (127 mm)2.9 in (73 mm)3.7 in (94 mm)4.1 in (103 mm)3.6 in (93 mm)3.2 in (81 mm)5.3 in (134 mm)5.4 in (137 mm)5 in (126 mm)6.4 in (162 mm)
Rainy days232118111098811151619
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)
Sunshine285 h260 h272 h251 h225 h210 h230 h252 h212 h222 h254 h290 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 +1.3°F (+0.7°C) to +2.1°F (+1.2°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +1.6°F (+0.9°C)
  • February: +1.2°F (+0.7°C)
  • March: +1.3°F (+0.7°C)
  • April: +1.4°F (+0.8°C)
  • May: +1.2°F (+0.7°C)
  • June: +1.5°F (+0.8°C)
  • July: +2.1°F (+1.2°C)
  • August: +1.7°F (+1.0°C)
  • September: +1.2°F (+0.7°C)
  • October: +1.6°F (+0.9°C)
  • November: +1.3°F (+0.7°C)
  • December: +2.0°F (+1.1°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.