ClimateSearch

San Pedro de Macorís, San Pedro de Macorís

Dominican Republic · 218k people · 6 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 high87°F (31°C)89°F (32°C)90°F (32°C)90°F (32°C)91°F (33°C)92°F (33°C)92°F (34°C)92°F (34°C)92°F (33°C)91°F (33°C)89°F (32°C)88°F (31°C)
Average low66°F (19°C)67°F (19°C)68°F (20°C)69°F (21°C)72°F (22°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)72°F (22°C)70°F (21°C)68°F (20°C)
Dew point68°F (20°C)67°F (19°C)67°F (19°C)69°F (21°C)71°F (22°C)73°F (23°C)73°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)71°F (22°C)69°F (21°C)
Rainfall1.2 in (31 mm)1 in (25 mm)1.3 in (33 mm)2.3 in (59 mm)4.6 in (116 mm)3.4 in (88 mm)4.1 in (105 mm)5.4 in (137 mm)6.3 in (160 mm)5.1 in (130 mm)3.6 in (90 mm)2 in (50 mm)
Rainy days2234867810963
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)
Sunshine254 h245 h272 h263 h240 h236 h251 h232 h202 h210 h221 h250 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

+1.6°F (+0.9°C)

Models range from +1.3°F (+0.7°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

10 → 32

About 3.2× as many

Warming by month
  • January: +1.7°F (+1.0°C)
  • February: +1.7°F (+1.0°C)
  • March: +1.6°F (+0.9°C)
  • April: +2.1°F (+1.1°C)
  • May: +1.4°F (+0.8°C)
  • June: +1.3°F (+0.7°C)
  • July: +1.6°F (+0.9°C)
  • August: +1.9°F (+1.1°C)
  • September: +2.0°F (+1.1°C)
  • October: +2.1°F (+1.2°C)
  • November: +1.7°F (+0.9°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.