ClimateSearch

Sacaba, Cochabamba

Bolivia · 181k people · 2699 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 high68°F (20°C)67°F (20°C)67°F (20°C)68°F (20°C)68°F (20°C)67°F (20°C)67°F (19°C)68°F (20°C)69°F (21°C)70°F (21°C)71°F (22°C)70°F (21°C)
Average low54°F (12°C)54°F (12°C)53°F (12°C)51°F (11°C)48°F (9°C)46°F (8°C)45°F (7°C)46°F (8°C)49°F (9°C)52°F (11°C)53°F (12°C)54°F (12°C)
Dew point52°F (11°C)53°F (12°C)52°F (11°C)49°F (10°C)45°F (7°C)42°F (5°C)41°F (5°C)43°F (6°C)46°F (8°C)48°F (9°C)50°F (10°C)52°F (11°C)
Rainfall9 in (228 mm)8 in (204 mm)6.2 in (156 mm)2.9 in (75 mm)1.3 in (32 mm)0.9 in (24 mm)1.2 in (30 mm)1.7 in (44 mm)2.1 in (53 mm)2.8 in (72 mm)4 in (102 mm)6.6 in (169 mm)
Rainy days27252313757913171824
Snowfall0 in (0.1 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0.1 cm)0.1 in (0.2 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)
Sunshine310 h276 h306 h307 h330 h321 h333 h331 h330 h341 h318 h312 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

+2.0°F (+1.1°C)

Models range from +1.7°F (+0.9°C) to +2.3°F (+1.3°C)

Days above 90°F (32°C) a year

0 0

Warming by month
  • January: +1.9°F (+1.0°C)
  • February: +2.0°F (+1.1°C)
  • March: +1.9°F (+1.1°C)
  • April: +1.8°F (+1.0°C)
  • May: +2.2°F (+1.2°C)
  • June: +2.2°F (+1.2°C)
  • July: +2.6°F (+1.4°C)
  • August: +2.6°F (+1.5°C)
  • September: +2.4°F (+1.3°C)
  • October: +2.2°F (+1.2°C)
  • November: +1.9°F (+1.1°C)
  • December: +2.1°F (+1.2°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.