ClimateSearch

San Cristóbal, San Cristóbal

Dominican Republic · 154k people · 37 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)83°F (28°C)83°F (29°C)84°F (29°C)85°F (29°C)85°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)85°F (29°C)83°F (29°C)82°F (28°C)
Average low69°F (21°C)69°F (21°C)69°F (21°C)71°F (22°C)72°F (22°C)73°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 point66°F (19°C)66°F (19°C)66°F (19°C)68°F (20°C)71°F (22°C)72°F (22°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)
Rainfall1.4 in (36 mm)1.3 in (32 mm)1.6 in (41 mm)2.6 in (65 mm)5 in (128 mm)4.4 in (111 mm)4.4 in (113 mm)5.4 in (136 mm)5.1 in (129 mm)4.8 in (121 mm)3.1 in (79 mm)1.7 in (42 mm)
Rainy days121113162222222221221712
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 h357 h353 h359 h353 h359 h346 h312 h317 h312 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 +2.1°F (+1.2°C)

Days above 90°F (32°C) a year

4 18

About 5.0× as many

Warming by month
  • January: +1.5°F (+0.8°C)
  • February: +1.4°F (+0.8°C)
  • March: +1.4°F (+0.8°C)
  • April: +2.0°F (+1.1°C)
  • May: +1.8°F (+1.0°C)
  • June: +1.6°F (+0.9°C)
  • July: +1.9°F (+1.1°C)
  • August: +2.0°F (+1.1°C)
  • September: +2.2°F (+1.2°C)
  • October: +2.1°F (+1.2°C)
  • November: +1.5°F (+0.8°C)
  • December: +1.8°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.