ClimateSearch

Santiago de los Caballeros, Santiago Province

Dominican Republic · 1.2M people · 216 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 high85°F (29°C)86°F (30°C)88°F (31°C)89°F (32°C)90°F (32°C)92°F (34°C)92°F (34°C)93°F (34°C)93°F (34°C)92°F (33°C)88°F (31°C)86°F (30°C)
Average low64°F (18°C)65°F (18°C)66°F (19°C)68°F (20°C)70°F (21°C)71°F (22°C)72°F (22°C)72°F (22°C)71°F (22°C)71°F (22°C)68°F (20°C)66°F (19°C)
Dew point64°F (18°C)64°F (18°C)64°F (18°C)66°F (19°C)68°F (20°C)69°F (21°C)69°F (21°C)70°F (21°C)70°F (21°C)70°F (21°C)68°F (20°C)66°F (19°C)
Rainfall2.9 in (73 mm)2.5 in (63 mm)2.7 in (69 mm)3.9 in (100 mm)5.2 in (131 mm)2.5 in (64 mm)2.5 in (63 mm)3.2 in (82 mm)4 in (101 mm)4 in (101 mm)6.2 in (159 mm)4.3 in (109 mm)
Rainy days65681144678107
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)
Sunshine223 h220 h248 h245 h224 h234 h251 h235 h208 h207 h203 h222 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 (+1.1°C)

Models range from +1.3°F (+0.7°C) to +3.2°F (+1.8°C)

Days above 90°F (32°C) a year

100 → 146

About 1.5× as many

Warming by month
  • January: +1.7°F (+0.9°C)
  • February: +1.3°F (+0.7°C)
  • March: +1.7°F (+0.9°C)
  • April: +2.4°F (+1.3°C)
  • May: +1.6°F (+0.9°C)
  • June: +1.4°F (+0.8°C)
  • July: +1.9°F (+1.1°C)
  • August: +2.4°F (+1.3°C)
  • September: +2.2°F (+1.2°C)
  • October: +2.1°F (+1.2°C)
  • November: +1.7°F (+1.0°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.