ClimateSearch

Santiago de Cuba, Santiago de Cuba Province

Cuba · 556k people · 63 m elevation · Northern 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 high84°F (29°C)85°F (29°C)85°F (29°C)86°F (30°C)86°F (30°C)88°F (31°C)90°F (32°C)89°F (32°C)88°F (31°C)86°F (30°C)85°F (29°C)84°F (29°C)
Average low70°F (21°C)70°F (21°C)70°F (21°C)72°F (22°C)74°F (23°C)76°F (24°C)76°F (25°C)77°F (25°C)76°F (24°C)75°F (24°C)73°F (23°C)71°F (22°C)
Dew point66°F (19°C)65°F (19°C)66°F (19°C)68°F (20°C)71°F (22°C)74°F (23°C)74°F (23°C)74°F (24°C)74°F (24°C)74°F (23°C)71°F (21°C)68°F (20°C)
Rainfall0.5 in (13 mm)0.6 in (16 mm)1.2 in (29 mm)2 in (50 mm)4.9 in (124 mm)3.3 in (84 mm)2.5 in (63 mm)3.5 in (88 mm)4.8 in (121 mm)4.5 in (115 mm)2.4 in (62 mm)1 in (25 mm)
Rainy days336916141316211894
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)
Sunshine322 h307 h356 h353 h345 h342 h368 h351 h325 h314 h301 h307 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 +1.6°F (+0.9°C) to +2.5°F (+1.4°C)

Days above 90°F (32°C) a year

40 79

About 2.0× as many

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