ClimateSearch

Nkayi, Bouenza

Republic of the Congo · 103k people · 183 m elevation · Southern 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 high89°F (31°C)90°F (32°C)91°F (33°C)90°F (32°C)88°F (31°C)83°F (28°C)81°F (27°C)83°F (28°C)86°F (30°C)89°F (32°C)89°F (32°C)88°F (31°C)
Average low73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)69°F (21°C)66°F (19°C)67°F (20°C)70°F (21°C)72°F (22°C)73°F (23°C)73°F (23°C)
Dew point73°F (23°C)73°F (23°C)74°F (23°C)74°F (23°C)73°F (23°C)68°F (20°C)65°F (18°C)65°F (18°C)67°F (20°C)70°F (21°C)72°F (22°C)73°F (23°C)
Rainfall4.7 in (118 mm)4.4 in (111 mm)6.8 in (173 mm)8.6 in (217 mm)3.5 in (88 mm)0 in (1 mm)0 in (0 mm)0 in (0 mm)0.4 in (11 mm)5.9 in (151 mm)9.1 in (231 mm)7.5 in (190 mm)
Rainy days1110141680001111817
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)
Sunshine131 h117 h133 h127 h135 h121 h121 h89 h86 h125 h127 h124 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

+1.0°F (+0.5°C)

Models range from +0.7°F (+0.4°C) to +1.4°F (+0.8°C)

Days above 90°F (32°C) a year

29 → 51

About 1.7× as many

Warming by month
  • January: +1.0°F (+0.5°C)
  • February: +1.0°F (+0.6°C)
  • March: +1.3°F (+0.7°C)
  • April: +1.6°F (+0.9°C)
  • May: +1.7°F (+0.9°C)
  • June: +1.2°F (+0.6°C)
  • July: +0.3°F (+0.2°C)
  • August: +0.2°F (+0.1°C)
  • September: +0.5°F (+0.3°C)
  • October: +0.6°F (+0.3°C)
  • November: +0.8°F (+0.4°C)
  • December: +0.9°F (+0.5°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.