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 high82°F (28°C)81°F (27°C)77°F (25°C)68°F (20°C)60°F (16°C)56°F (13°C)55°F (13°C)57°F (14°C)61°F (16°C)66°F (19°C)72°F (22°C)78°F (26°C)
Average low56°F (13°C)56°F (13°C)53°F (12°C)48°F (9°C)44°F (7°C)41°F (5°C)38°F (4°C)40°F (4°C)42°F (5°C)45°F (7°C)49°F (9°C)53°F (12°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)
Rainfall0.4 in (10 mm)1 in (24 mm)0.9 in (23 mm)3 in (75 mm)7.6 in (192 mm)10.4 in (264 mm)7.9 in (200 mm)6.5 in (166 mm)3.8 in (96 mm)2.5 in (63 mm)1.2 in (30 mm)0.9 in (22 mm)
Rainy days1235101411127742
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)
Sunshine426 h360 h355 h284 h227 h185 h217 h237 h287 h349 h383 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

+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.