ClimateSearch

Jaraguá do Sul, Santa Catarina

Brazil · 200k people · 27 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 high83°F (28°C)83°F (28°C)81°F (27°C)78°F (26°C)73°F (23°C)70°F (21°C)69°F (21°C)71°F (22°C)72°F (22°C)75°F (24°C)78°F (25°C)82°F (28°C)
Average low70°F (21°C)71°F (21°C)69°F (21°C)65°F (19°C)60°F (15°C)56°F (14°C)55°F (13°C)56°F (14°C)59°F (15°C)63°F (17°C)65°F (18°C)68°F (20°C)
Dew point71°F (21°C)71°F (22°C)69°F (21°C)65°F (19°C)60°F (16°C)58°F (14°C)56°F (13°C)58°F (14°C)60°F (15°C)63°F (17°C)65°F (18°C)68°F (20°C)
Rainfall9.3 in (237 mm)9.1 in (232 mm)6.5 in (166 mm)4 in (101 mm)4.2 in (107 mm)4.4 in (112 mm)3.6 in (93 mm)3.7 in (93 mm)6 in (152 mm)5.9 in (150 mm)6.1 in (156 mm)6.7 in (169 mm)
Rainy days2422211311910914161820
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)
Sunshine289 h261 h271 h250 h231 h209 h220 h237 h198 h211 h248 h285 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 +1.1°F (+0.6°C) to +1.7°F (+0.9°C)

Days above 90°F (32°C) a year

13 18

About 1.4× as many

Warming by month
  • January: +1.4°F (+0.8°C)
  • February: +1.0°F (+0.6°C)
  • March: +1.2°F (+0.7°C)
  • April: +1.2°F (+0.7°C)
  • May: +1.0°F (+0.6°C)
  • June: +1.3°F (+0.7°C)
  • July: +1.8°F (+1.0°C)
  • August: +1.4°F (+0.8°C)
  • September: +1.0°F (+0.6°C)
  • October: +1.3°F (+0.7°C)
  • November: +1.0°F (+0.6°C)
  • December: +1.8°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.