ClimateSearch

Rosario, Santa Fe

Argentina · 948k people · 36 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 high86°F (30°C)83°F (28°C)80°F (27°C)73°F (23°C)66°F (19°C)61°F (16°C)60°F (15°C)65°F (18°C)69°F (20°C)74°F (23°C)79°F (26°C)84°F (29°C)
Average low68°F (20°C)67°F (19°C)64°F (18°C)57°F (14°C)52°F (11°C)47°F (8°C)44°F (7°C)47°F (8°C)50°F (10°C)56°F (13°C)60°F (16°C)65°F (18°C)
Dew point63°F (17°C)63°F (17°C)61°F (16°C)56°F (13°C)51°F (11°C)47°F (8°C)44°F (7°C)45°F (7°C)47°F (9°C)53°F (12°C)56°F (14°C)60°F (16°C)
Rainfall4 in (102 mm)4.4 in (111 mm)4.9 in (125 mm)4.1 in (104 mm)2.7 in (68 mm)1.6 in (40 mm)1.4 in (36 mm)2.2 in (55 mm)2.5 in (64 mm)4.5 in (115 mm)4.5 in (113 mm)4.2 in (107 mm)
Rainy days8888655561089
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)
Sunshine376 h309 h312 h246 h232 h214 h235 h264 h287 h306 h343 h372 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

+2.1°F (+1.2°C)

Models range from +0.8°F (+0.4°C) to +3.7°F (+2.0°C)

Days above 90°F (32°C) a year

20 32

About 1.6× as many

Warming by month
  • January: +1.7°F (+0.9°C)
  • February: +1.9°F (+1.0°C)
  • March: +2.6°F (+1.5°C)
  • April: +2.7°F (+1.5°C)
  • May: +1.8°F (+1.0°C)
  • June: +1.7°F (+0.9°C)
  • July: +2.2°F (+1.2°C)
  • August: +1.9°F (+1.1°C)
  • September: +1.9°F (+1.0°C)
  • October: +2.7°F (+1.5°C)
  • November: +2.6°F (+1.4°C)
  • December: +2.8°F (+1.6°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.