ClimateSearch

Balneário Camboriú, Santa Catarina

Brazil · 139k people · 10 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 high85°F (29°C)84°F (29°C)83°F (29°C)80°F (27°C)74°F (24°C)72°F (22°C)70°F (21°C)71°F (22°C)72°F (22°C)75°F (24°C)78°F (26°C)82°F (28°C)
Average low68°F (20°C)68°F (20°C)66°F (19°C)62°F (16°C)56°F (13°C)54°F (12°C)51°F (11°C)53°F (12°C)57°F (14°C)61°F (16°C)63°F (17°C)66°F (19°C)
Dew point71°F (21°C)71°F (22°C)69°F (21°C)66°F (19°C)61°F (16°C)58°F (14°C)56°F (14°C)57°F (14°C)59°F (15°C)63°F (17°C)64°F (18°C)68°F (20°C)
Rainfall8.8 in (223 mm)9.3 in (237 mm)6.6 in (168 mm)5 in (127 mm)4.4 in (111 mm)3.7 in (95 mm)3 in (77 mm)3.7 in (94 mm)4.9 in (126 mm)5.7 in (144 mm)5.1 in (131 mm)5.8 in (148 mm)
Rainy days1514128887710111111
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)
Sunshine172 h160 h177 h166 h153 h129 h137 h145 h118 h114 h150 h172 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

+1.4°F (+0.8°C)

Models range from +1.2°F (+0.6°C) to +1.7°F (+0.9°C)

Days above 90°F (32°C) a year

2 → 3

About 1.7× as many

Warming by month
  • January: +1.4°F (+0.8°C)
  • February: +1.1°F (+0.6°C)
  • March: +1.1°F (+0.6°C)
  • April: +1.3°F (+0.7°C)
  • May: +1.2°F (+0.7°C)
  • June: +1.3°F (+0.7°C)
  • July: +1.4°F (+0.8°C)
  • August: +1.2°F (+0.7°C)
  • September: +1.1°F (+0.6°C)
  • October: +1.3°F (+0.7°C)
  • November: +1.0°F (+0.6°C)
  • December: +1.6°F (+0.9°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.