ClimateSearch

Palma Soriano, Santiago de Cuba Province

Cuba · 103k people · 151 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)86°F (30°C)87°F (30°C)88°F (31°C)88°F (31°C)89°F (32°C)91°F (33°C)91°F (33°C)88°F (31°C)86°F (30°C)84°F (29°C)83°F (29°C)
Average low67°F (19°C)67°F (19°C)68°F (20°C)70°F (21°C)72°F (22°C)74°F (23°C)74°F (23°C)74°F (24°C)74°F (23°C)73°F (23°C)70°F (21°C)68°F (20°C)
Dew point65°F (18°C)64°F (18°C)64°F (18°C)67°F (19°C)70°F (21°C)73°F (23°C)73°F (23°C)73°F (23°C)74°F (23°C)73°F (23°C)70°F (21°C)67°F (19°C)
Rainfall0.6 in (15 mm)0.6 in (16 mm)1.2 in (30 mm)1.9 in (48 mm)5 in (126 mm)4.3 in (108 mm)3.7 in (93 mm)4.1 in (104 mm)5.3 in (135 mm)4.4 in (112 mm)2.2 in (57 mm)1 in (26 mm)
Rainy days4469181919212220115
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)
Sunshine317 h304 h351 h352 h343 h340 h367 h350 h325 h312 h298 h303 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

82 139

About 1.7× as many

Warming by month
  • January: +2.0°F (+1.1°C)
  • February: +1.9°F (+1.1°C)
  • March: +2.0°F (+1.1°C)
  • April: +2.3°F (+1.3°C)
  • May: +2.1°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: +2.1°F (+1.2°C)
  • October: +2.2°F (+1.2°C)
  • November: +1.5°F (+0.8°C)
  • December: +1.9°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.