ClimateSearch

Standerton, Mpumalanga

South Africa · 101k people · 1567 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 high77°F (25°C)77°F (25°C)75°F (24°C)71°F (22°C)67°F (20°C)63°F (17°C)63°F (17°C)69°F (20°C)76°F (24°C)77°F (25°C)76°F (25°C)77°F (25°C)
Average low58°F (15°C)58°F (15°C)55°F (13°C)50°F (10°C)43°F (6°C)37°F (3°C)36°F (2°C)41°F (5°C)48°F (9°C)52°F (11°C)55°F (13°C)57°F (14°C)
Dew point57°F (14°C)56°F (13°C)53°F (12°C)47°F (8°C)38°F (3°C)31°F (0°C)29°F (-2°C)31°F (0°C)36°F (2°C)45°F (7°C)51°F (11°C)55°F (13°C)
Rainfall4.8 in (122 mm)3.6 in (91 mm)3.1 in (79 mm)1.5 in (38 mm)0.6 in (15 mm)0.3 in (8 mm)0.3 in (7 mm)0.5 in (13 mm)0.9 in (23 mm)3.5 in (88 mm)4.3 in (110 mm)5.8 in (149 mm)
Rainy days161311631124101518
Snowfall0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0.1 in (0.2 cm)0.3 in (0.7 cm)0 in (0.1 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)
Sunshine343 h306 h316 h296 h296 h289 h301 h315 h326 h331 h323 h349 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

+2.4°F (+1.3°C)

Models range from +1.3°F (+0.7°C) to +3.5°F (+2.0°C)

Days above 90°F (32°C) a year

2 6

About 2.4× as many

Warming by month
  • January: +2.2°F (+1.2°C)
  • February: +2.9°F (+1.6°C)
  • March: +2.8°F (+1.6°C)
  • April: +2.2°F (+1.2°C)
  • May: +2.0°F (+1.1°C)
  • June: +2.3°F (+1.3°C)
  • July: +2.3°F (+1.3°C)
  • August: +2.1°F (+1.2°C)
  • September: +3.3°F (+1.8°C)
  • October: +4.2°F (+2.3°C)
  • November: +3.1°F (+1.7°C)
  • December: +2.1°F (+1.2°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.