ClimateSearch

Coronel, Biobio

Chile · 108k people · 3 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 high75°F (24°C)74°F (23°C)71°F (22°C)65°F (18°C)60°F (15°C)56°F (13°C)55°F (13°C)56°F (14°C)59°F (15°C)62°F (17°C)67°F (19°C)71°F (22°C)
Average low57°F (14°C)57°F (14°C)55°F (13°C)51°F (10°C)48°F (9°C)45°F (7°C)43°F (6°C)44°F (6°C)45°F (7°C)48°F (9°C)51°F (11°C)55°F (13°C)
Dew point54°F (12°C)55°F (13°C)54°F (12°C)51°F (10°C)49°F (10°C)47°F (8°C)45°F (7°C)45°F (7°C)46°F (8°C)48°F (9°C)50°F (10°C)53°F (11°C)
Rainfall0.3 in (8 mm)0.6 in (14 mm)0.9 in (23 mm)2.6 in (65 mm)6.7 in (170 mm)9.2 in (234 mm)7.1 in (180 mm)6.2 in (158 mm)3.3 in (85 mm)2.4 in (60 mm)1.2 in (30 mm)0.9 in (22 mm)
Rainy days1236111413128743
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)
Sunshine424 h359 h350 h276 h220 h188 h218 h240 h293 h354 h382 h421 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

+1.8°F (+1.0°C)

Models range from +1.2°F (+0.6°C) to +2.5°F (+1.4°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +1.9°F (+1.1°C)
  • February: +1.8°F (+1.0°C)
  • March: +1.2°F (+0.7°C)
  • April: +1.6°F (+0.9°C)
  • May: +1.1°F (+0.6°C)
  • June: +0.8°F (+0.5°C)
  • July: +1.0°F (+0.5°C)
  • August: +0.7°F (+0.4°C)
  • September: +0.7°F (+0.4°C)
  • October: +1.1°F (+0.6°C)
  • November: +1.8°F (+1.0°C)
  • December: +1.7°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.