ClimateSearch

Peñalolén, Santiago Metropolitan

Chile · 242k people · 704 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)84°F (29°C)80°F (27°C)73°F (23°C)65°F (18°C)58°F (14°C)58°F (14°C)61°F (16°C)66°F (19°C)71°F (22°C)78°F (26°C)83°F (28°C)
Average low58°F (15°C)56°F (13°C)52°F (11°C)48°F (9°C)44°F (6°C)39°F (4°C)38°F (3°C)40°F (5°C)43°F (6°C)48°F (9°C)51°F (11°C)55°F (13°C)
Dew point50°F (10°C)50°F (10°C)48°F (9°C)43°F (6°C)38°F (3°C)33°F (1°C)32°F (0°C)35°F (2°C)40°F (4°C)44°F (6°C)46°F (8°C)48°F (9°C)
Rainfall0.1 in (3 mm)0.2 in (5 mm)0.3 in (9 mm)1.1 in (27 mm)3.3 in (84 mm)4.3 in (110 mm)2.6 in (67 mm)3.4 in (87 mm)1.4 in (35 mm)1 in (24 mm)0.4 in (11 mm)0.2 in (4 mm)
Rainy days012378776520
Snowfall0 in (0 cm)0 in (0 cm)0 in (0 cm)0.6 in (1.5 cm)3.5 in (8.9 cm)12.1 in (30.7 cm)11 in (28 cm)9.9 in (25.2 cm)5.3 in (13.4 cm)2.4 in (6.1 cm)0.4 in (1 cm)0.1 in (0.2 cm)
Sunshine361 h313 h306 h232 h176 h143 h166 h187 h204 h255 h299 h354 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

+2.3°F (+1.3°C)

Models range from +2.1°F (+1.2°C) to +2.6°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: +2.1°F (+1.2°C)
  • February: +2.3°F (+1.3°C)
  • March: +1.8°F (+1.0°C)
  • April: +3.1°F (+1.7°C)
  • May: +2.1°F (+1.2°C)
  • June: +2.0°F (+1.1°C)
  • July: +2.2°F (+1.2°C)
  • August: +2.1°F (+1.2°C)
  • September: +2.2°F (+1.2°C)
  • October: +2.3°F (+1.3°C)
  • November: +2.8°F (+1.5°C)
  • December: +2.5°F (+1.4°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.