ClimateSearch

San Francisco De Borja, Lima region

Peru · 105k people · 169 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 high76°F (24°C)77°F (25°C)77°F (25°C)74°F (23°C)71°F (22°C)68°F (20°C)66°F (19°C)66°F (19°C)67°F (19°C)68°F (20°C)70°F (21°C)73°F (23°C)
Average low67°F (19°C)68°F (20°C)68°F (20°C)65°F (18°C)62°F (17°C)60°F (15°C)58°F (14°C)57°F (14°C)58°F (14°C)59°F (15°C)61°F (16°C)64°F (18°C)
Dew point65°F (19°C)67°F (20°C)67°F (19°C)64°F (18°C)60°F (16°C)58°F (14°C)56°F (13°C)55°F (13°C)56°F (13°C)57°F (14°C)59°F (15°C)62°F (17°C)
Rainfall0.6 in (15 mm)1 in (26 mm)0.8 in (21 mm)0.2 in (6 mm)0.1 in (2 mm)0 in (1 mm)0 in (1 mm)0 in (1 mm)0.1 in (2 mm)0.1 in (3 mm)0.1 in (2 mm)0.2 in (6 mm)
Rainy days587200000112
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)
Sunshine341 h295 h326 h334 h341 h321 h336 h343 h347 h360 h344 h341 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

+1.6°F (+0.9°C)

Models range from +1.3°F (+0.7°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

0 0

Warming by month
  • January: +1.5°F (+0.8°C)
  • February: +1.7°F (+0.9°C)
  • March: +1.6°F (+0.9°C)
  • April: +1.9°F (+1.0°C)
  • May: +2.1°F (+1.1°C)
  • June: +1.9°F (+1.1°C)
  • July: +2.2°F (+1.2°C)
  • August: +2.2°F (+1.2°C)
  • September: +1.8°F (+1.0°C)
  • October: +2.0°F (+1.1°C)
  • November: +1.7°F (+1.0°C)
  • December: +1.8°F (+1.0°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.