ClimateSearch

Dessalines, Artibonite

Haiti · 182k people · 23 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 high88°F (31°C)89°F (32°C)89°F (32°C)90°F (32°C)90°F (32°C)92°F (33°C)94°F (34°C)93°F (34°C)91°F (33°C)89°F (32°C)88°F (31°C)88°F (31°C)
Average low69°F (21°C)69°F (21°C)70°F (21°C)72°F (22°C)74°F (24°C)76°F (24°C)76°F (25°C)76°F (25°C)75°F (24°C)74°F (24°C)72°F (22°C)70°F (21°C)
Dew point65°F (19°C)65°F (18°C)65°F (19°C)68°F (20°C)71°F (22°C)73°F (23°C)72°F (22°C)73°F (23°C)74°F (23°C)73°F (23°C)70°F (21°C)67°F (20°C)
Rainfall0.4 in (10 mm)0.5 in (12 mm)0.9 in (24 mm)2.5 in (65 mm)6.6 in (167 mm)5.2 in (132 mm)3.9 in (99 mm)4.6 in (118 mm)5.8 in (149 mm)5 in (128 mm)2 in (50 mm)0.5 in (13 mm)
Rainy days3361220191720221993
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)
Sunshine318 h314 h363 h355 h359 h357 h364 h346 h324 h321 h314 h321 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

+1.7°F (+0.9°C)

Models range from +1.5°F (+0.8°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

187 258

About 1.4× as many

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