ClimateSearch

Kuala Krai, Kelantan

Malaysia · 105k people · 36 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)85°F (30°C)88°F (31°C)90°F (32°C)89°F (32°C)88°F (31°C)88°F (31°C)88°F (31°C)88°F (31°C)86°F (30°C)83°F (28°C)82°F (28°C)
Average low71°F (22°C)72°F (22°C)73°F (23°C)74°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)74°F (23°C)74°F (23°C)73°F (23°C)73°F (23°C)72°F (22°C)
Dew point72°F (22°C)72°F (22°C)73°F (23°C)75°F (24°C)76°F (24°C)76°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)73°F (23°C)
Rainfall8.1 in (205 mm)4.1 in (105 mm)6.4 in (162 mm)7.6 in (193 mm)8.8 in (223 mm)7.9 in (200 mm)7.8 in (198 mm)8.9 in (225 mm)10.2 in (260 mm)13.7 in (348 mm)15.2 in (387 mm)15 in (381 mm)
Rainy days221517222725252528292827
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)
Sunshine287 h291 h325 h325 h324 h305 h315 h315 h301 h279 h242 h237 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

+1.5°F (+0.8°C)

Models range from +1.1°F (+0.6°C) to +2.2°F (+1.2°C)

Days above 90°F (32°C) a year

50 87

About 1.7× as many

Warming by month
  • January: +1.2°F (+0.7°C)
  • February: +1.3°F (+0.7°C)
  • March: +1.5°F (+0.8°C)
  • April: +1.6°F (+0.9°C)
  • May: +1.4°F (+0.8°C)
  • June: +1.5°F (+0.8°C)
  • July: +1.5°F (+0.8°C)
  • August: +1.6°F (+0.9°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.3°F (+0.7°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.