ClimateSearch

Georgetown, Demerara-Mahaica

Guyana · 235k people · 3 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 (30°C)86°F (30°C)86°F (30°C)87°F (31°C)86°F (30°C)86°F (30°C)87°F (31°C)88°F (31°C)89°F (32°C)90°F (32°C)89°F (31°C)87°F (30°C)
Average low75°F (24°C)75°F (24°C)76°F (24°C)76°F (25°C)76°F (24°C)75°F (24°C)74°F (24°C)75°F (24°C)76°F (25°C)76°F (25°C)76°F (24°C)75°F (24°C)
Dew point72°F (22°C)71°F (22°C)72°F (22°C)73°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (24°C)74°F (24°C)74°F (24°C)74°F (24°C)73°F (23°C)
Rainfall7.4 in (187 mm)3.6 in (91 mm)3.9 in (100 mm)4.4 in (112 mm)10.2 in (259 mm)10.5 in (267 mm)9.3 in (237 mm)5.8 in (148 mm)3.3 in (83 mm)3.4 in (87 mm)5.6 in (142 mm)10.1 in (257 mm)
Rainy days1377819232415891419
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)
Sunshine209 h200 h223 h196 h164 h148 h195 h229 h231 h216 h186 h195 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 (+0.9°C) to +1.7°F (+1.0°C)

Days above 90°F (32°C) a year

0 → 0

Warming by month
  • January: +1.4°F (+0.8°C)
  • February: +1.5°F (+0.8°C)
  • March: +1.6°F (+0.9°C)
  • April: +1.7°F (+0.9°C)
  • May: +1.9°F (+1.1°C)
  • June: +1.6°F (+0.9°C)
  • July: +1.7°F (+0.9°C)
  • August: +1.7°F (+0.9°C)
  • September: +1.7°F (+1.0°C)
  • October: +1.7°F (+0.9°C)
  • November: +1.8°F (+1.0°C)
  • December: +1.5°F (+0.8°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.