ClimateSearch

San Pedro de la Paz, Biobio

Chile · 122k people · 12 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)73°F (23°C)70°F (21°C)65°F (18°C)60°F (16°C)56°F (14°C)55°F (13°C)56°F (14°C)60°F (15°C)63°F (17°C)68°F (20°C)72°F (22°C)
Average low53°F (11°C)51°F (11°C)49°F (10°C)46°F (8°C)45°F (7°C)44°F (7°C)42°F (6°C)42°F (6°C)43°F (6°C)45°F (7°C)48°F (9°C)51°F (10°C)
Dew point54°F (12°C)54°F (12°C)53°F (12°C)50°F (10°C)49°F (9°C)46°F (8°C)44°F (7°C)45°F (7°C)46°F (8°C)47°F (9°C)50°F (10°C)52°F (11°C)
Rainfall0.5 in (12 mm)0.6 in (15 mm)1.2 in (31 mm)2.7 in (69 mm)5.9 in (151 mm)10 in (255 mm)6.9 in (176 mm)6.7 in (169 mm)3.8 in (96 mm)2.3 in (58 mm)1.3 in (34 mm)1.1 in (28 mm)
Rainy days1135101412127633
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)
Sunshine354 h297 h275 h197 h135 h111 h138 h154 h200 h251 h289 h335 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

+1.7°F (+0.9°C)

Models range from +1.2°F (+0.6°C) to +2.2°F (+1.2°C)

Days above 90°F (32°C) a year

0 → 0

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