ClimateSearch

Chillán, Ñuble

Chile · 150k people · 122 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 (29°C)77°F (25°C)67°F (20°C)59°F (15°C)54°F (12°C)53°F (12°C)56°F (14°C)62°F (16°C)67°F (19°C)74°F (23°C)80°F (27°C)
Average low53°F (12°C)51°F (11°C)49°F (9°C)45°F (7°C)42°F (6°C)41°F (5°C)38°F (4°C)39°F (4°C)41°F (5°C)44°F (7°C)47°F (9°C)51°F (11°C)
Dew point51°F (11°C)52°F (11°C)51°F (10°C)48°F (9°C)46°F (8°C)43°F (6°C)41°F (5°C)42°F (5°C)44°F (7°C)46°F (8°C)48°F (9°C)49°F (10°C)
Rainfall0.7 in (18 mm)0.9 in (24 mm)1.1 in (28 mm)2.3 in (59 mm)6.3 in (161 mm)9 in (228 mm)7.5 in (190 mm)6.8 in (172 mm)3.5 in (88 mm)2.4 in (60 mm)1.5 in (37 mm)1.4 in (35 mm)
Rainy days122591311116733
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)
Sunshine362 h305 h287 h206 h142 h107 h137 h151 h195 h245 h292 h340 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

+2.6°F (+1.5°C)

Models range from +2.2°F (+1.2°C) to +2.8°F (+1.6°C)

Days above 90°F (32°C) a year

3 → 6

About 1.8× as many

Warming by month
  • January: +2.4°F (+1.3°C)
  • February: +2.7°F (+1.5°C)
  • March: +2.0°F (+1.1°C)
  • April: +2.7°F (+1.5°C)
  • May: +1.4°F (+0.8°C)
  • June: +1.3°F (+0.7°C)
  • July: +1.2°F (+0.7°C)
  • August: +0.9°F (+0.5°C)
  • September: +1.1°F (+0.6°C)
  • October: +1.7°F (+1.0°C)
  • November: +3.0°F (+1.7°C)
  • December: +2.7°F (+1.5°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.