ClimateSearch

Ladysmith, KwaZulu-Natal

South Africa · 143k people · 1010 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 high82°F (28°C)82°F (28°C)80°F (27°C)75°F (24°C)71°F (22°C)67°F (19°C)67°F (19°C)72°F (22°C)78°F (26°C)80°F (26°C)81°F (27°C)82°F (28°C)
Average low62°F (17°C)62°F (17°C)59°F (15°C)53°F (12°C)46°F (8°C)40°F (5°C)39°F (4°C)44°F (7°C)50°F (10°C)54°F (12°C)57°F (14°C)60°F (16°C)
Dew point59°F (15°C)60°F (15°C)57°F (14°C)51°F (10°C)42°F (6°C)35°F (2°C)33°F (1°C)37°F (3°C)42°F (6°C)50°F (10°C)54°F (12°C)58°F (14°C)
Rainfall6.6 in (167 mm)5.4 in (136 mm)4.5 in (114 mm)2.1 in (53 mm)0.8 in (20 mm)0.6 in (14 mm)0.6 in (16 mm)1.1 in (27 mm)1.5 in (37 mm)3.8 in (97 mm)5.2 in (133 mm)6.6 in (167 mm)
Rainy days191413743247131619
Snowfall0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0.1 cm)0.2 in (0.4 cm)0 in (0 cm)0.1 in (0.2 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)
Sunshine327 h293 h313 h289 h295 h286 h295 h302 h305 h301 h304 h330 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

+1.9°F (+1.1°C)

Models range from +0.8°F (+0.4°C) to +2.9°F (+1.6°C)

Days above 90°F (32°C) a year

27 56

About 2.1× as many

Warming by month
  • January: +1.7°F (+1.0°C)
  • February: +2.3°F (+1.3°C)
  • March: +2.3°F (+1.3°C)
  • April: +2.0°F (+1.1°C)
  • May: +1.7°F (+1.0°C)
  • June: +2.2°F (+1.2°C)
  • July: +2.1°F (+1.2°C)
  • August: +2.3°F (+1.3°C)
  • September: +3.1°F (+1.7°C)
  • October: +3.7°F (+2.1°C)
  • November: +2.7°F (+1.5°C)
  • December: +1.7°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.