ClimateSearch

Santo Domingo, Nacional

Dominican Republic · 2.2M people · 24 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 high82°F (28°C)82°F (28°C)83°F (29°C)84°F (29°C)85°F (29°C)86°F (30°C)87°F (30°C)87°F (30°C)86°F (30°C)85°F (29°C)83°F (28°C)82°F (28°C)
Average low69°F (21°C)69°F (20°C)69°F (21°C)71°F (22°C)73°F (23°C)74°F (23°C)74°F (23°C)74°F (24°C)74°F (23°C)73°F (23°C)72°F (22°C)70°F (21°C)
Dew point67°F (19°C)66°F (19°C)66°F (19°C)68°F (20°C)71°F (22°C)73°F (23°C)72°F (22°C)73°F (23°C)73°F (23°C)73°F (23°C)70°F (21°C)68°F (20°C)
Rainfall1.3 in (33 mm)1.2 in (31 mm)1.6 in (40 mm)2.5 in (63 mm)4.7 in (120 mm)4.3 in (109 mm)4.4 in (111 mm)5.2 in (131 mm)5 in (128 mm)4.6 in (117 mm)3 in (77 mm)1.6 in (42 mm)
Rainy days121112162122222221221612
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)
Sunshine323 h312 h355 h352 h359 h353 h358 h344 h312 h317 h311 h329 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

+1.8°F (+1.0°C)

Models range from +1.6°F (+0.9°C) to +1.9°F (+1.1°C)

Days above 90°F (32°C) a year

4 11

About 2.9× as many

Warming by month
  • January: +1.4°F (+0.8°C)
  • February: +1.6°F (+0.9°C)
  • March: +1.6°F (+0.9°C)
  • April: +2.1°F (+1.2°C)
  • May: +1.5°F (+0.8°C)
  • June: +1.7°F (+0.9°C)
  • July: +1.8°F (+1.0°C)
  • August: +2.0°F (+1.1°C)
  • September: +2.1°F (+1.2°C)
  • October: +2.1°F (+1.2°C)
  • November: +1.4°F (+0.8°C)
  • December: +1.7°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.