ClimateSearch

Osorno, Los Lagos Region

Chile · 136k people · 36 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 high71°F (22°C)71°F (22°C)67°F (20°C)60°F (16°C)56°F (13°C)51°F (11°C)50°F (10°C)52°F (11°C)55°F (13°C)58°F (15°C)62°F (17°C)67°F (19°C)
Average low52°F (11°C)52°F (11°C)49°F (10°C)45°F (7°C)43°F (6°C)40°F (5°C)38°F (3°C)39°F (4°C)40°F (5°C)43°F (6°C)46°F (8°C)49°F (10°C)
Dew point50°F (10°C)50°F (10°C)49°F (10°C)47°F (8°C)45°F (7°C)42°F (6°C)40°F (5°C)41°F (5°C)42°F (6°C)44°F (7°C)46°F (8°C)48°F (9°C)
Rainfall1.5 in (39 mm)1.7 in (43 mm)2.6 in (67 mm)4.4 in (112 mm)7.5 in (191 mm)9.7 in (246 mm)8.9 in (227 mm)8.1 in (207 mm)4.9 in (123 mm)4.4 in (111 mm)3 in (76 mm)2.6 in (67 mm)
Rainy days76912151918181414118
Snowfall0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0.1 cm)0.2 in (0.4 cm)0.1 in (0.3 cm)0 in (0.1 cm)0.1 in (0.2 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)
Sunshine388 h327 h308 h231 h183 h147 h173 h196 h249 h302 h328 h374 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

+2.8°F (+1.5°C)

Models range from +2.1°F (+1.2°C) to +3.3°F (+1.9°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +2.5°F (+1.4°C)
  • February: +3.6°F (+2.0°C)
  • March: +2.2°F (+1.2°C)
  • April: +1.8°F (+1.0°C)
  • May: +1.4°F (+0.8°C)
  • June: +1.1°F (+0.6°C)
  • July: +1.0°F (+0.5°C)
  • August: +0.9°F (+0.5°C)
  • September: +1.0°F (+0.5°C)
  • October: +1.3°F (+0.7°C)
  • November: +2.0°F (+1.1°C)
  • December: +2.3°F (+1.3°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.