ClimateSearch

Pucallpa, Ucayali

Peru · 326k people · 157 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 high90°F (32°C)90°F (32°C)90°F (32°C)90°F (32°C)89°F (32°C)89°F (32°C)90°F (32°C)92°F (33°C)92°F (34°C)91°F (33°C)91°F (33°C)91°F (33°C)
Average low72°F (22°C)71°F (22°C)71°F (22°C)71°F (22°C)70°F (21°C)69°F (21°C)68°F (20°C)69°F (20°C)70°F (21°C)71°F (22°C)71°F (22°C)72°F (22°C)
Dew point74°F (24°C)74°F (24°C)74°F (24°C)74°F (24°C)73°F (23°C)73°F (23°C)72°F (22°C)72°F (22°C)74°F (23°C)74°F (24°C)74°F (24°C)74°F (24°C)
Rainfall6.4 in (163 mm)7.2 in (184 mm)9.4 in (238 mm)7.4 in (189 mm)4.9 in (125 mm)3.3 in (84 mm)2.5 in (64 mm)2.6 in (67 mm)4.3 in (108 mm)6.7 in (171 mm)8 in (202 mm)6.9 in (175 mm)
Rainy days15151916117569141616
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)
Sunshine135 h104 h111 h131 h171 h178 h206 h227 h189 h151 h128 h134 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

+1.5°F (+0.9°C)

Models range from +1.2°F (+0.7°C) to +2.0°F (+1.1°C)

Days above 90°F (32°C) a year

32 → 95

About 3.0× as many

Warming by month
  • January: +1.4°F (+0.8°C)
  • February: +1.6°F (+0.9°C)
  • March: +1.6°F (+0.9°C)
  • April: +1.7°F (+0.9°C)
  • May: +1.9°F (+1.0°C)
  • June: +1.9°F (+1.0°C)
  • July: +2.5°F (+1.4°C)
  • August: +2.6°F (+1.5°C)
  • September: +2.5°F (+1.4°C)
  • October: +2.4°F (+1.3°C)
  • November: +1.7°F (+0.9°C)
  • December: +1.7°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.