ClimateSearch

Sucre, Chuquisaca Department

Bolivia · 225k people · 2783 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)74°F (23°C)74°F (23°C)74°F (23°C)73°F (23°C)73°F (23°C)72°F (22°C)75°F (24°C)77°F (25°C)77°F (25°C)79°F (26°C)78°F (25°C)
Average low54°F (12°C)53°F (12°C)52°F (11°C)49°F (10°C)46°F (8°C)44°F (7°C)43°F (6°C)44°F (7°C)47°F (9°C)52°F (11°C)52°F (11°C)53°F (12°C)
Dew point51°F (11°C)51°F (11°C)51°F (10°C)48°F (9°C)42°F (6°C)37°F (3°C)36°F (2°C)38°F (3°C)41°F (5°C)45°F (7°C)48°F (9°C)50°F (10°C)
Rainfall5.5 in (140 mm)4.9 in (125 mm)4.1 in (103 mm)1.1 in (27 mm)0.2 in (5 mm)0.1 in (2 mm)0.1 in (3 mm)0.4 in (10 mm)1 in (26 mm)2 in (50 mm)2.1 in (54 mm)3.9 in (100 mm)
Rainy days211917610125101117
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)
Sunshine159 h140 h160 h179 h219 h229 h242 h238 h219 h201 h170 h159 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

+1.9°F (+1.0°C)

Models range from +1.6°F (+0.9°C) to +2.2°F (+1.2°C)

Days above 90°F (32°C) a year

0 → 0

Warming by month
  • January: +1.9°F (+1.0°C)
  • February: +1.7°F (+0.9°C)
  • March: +1.9°F (+1.1°C)
  • April: +1.6°F (+0.9°C)
  • May: +1.7°F (+1.0°C)
  • June: +2.1°F (+1.2°C)
  • July: +2.5°F (+1.4°C)
  • August: +2.3°F (+1.3°C)
  • September: +2.4°F (+1.4°C)
  • October: +2.7°F (+1.5°C)
  • November: +2.3°F (+1.3°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.