ClimateSearch

Wellington, New Zealand

215k people · 29 m elevation · Köppen Cfb · 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 high64°F (18°C)65°F (18°C)63°F (17°C)60°F (16°C)57°F (14°C)54°F (12°C)52°F (11°C)53°F (11°C)54°F (12°C)56°F (14°C)59°F (15°C)62°F (17°C)
Average low58°F (15°C)59°F (15°C)57°F (14°C)54°F (12°C)52°F (11°C)49°F (9°C)47°F (9°C)47°F (9°C)49°F (9°C)51°F (10°C)53°F (12°C)56°F (13°C)
Dew point55°F (13°C)55°F (13°C)53°F (12°C)51°F (10°C)48°F (9°C)44°F (7°C)43°F (6°C)44°F (6°C)45°F (7°C)47°F (8°C)49°F (9°C)53°F (11°C)
Rainfall2.2 in (57 mm)2.3 in (58 mm)2.4 in (61 mm)2.8 in (72 mm)2.8 in (72 mm)3.6 in (91 mm)3.4 in (86 mm)3.3 in (83 mm)3.1 in (78 mm)3.5 in (90 mm)3 in (75 mm)2.7 in (69 mm)
Rainy days878101112121312121111
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 (0.1 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)
Sunshine385 h323 h318 h264 h235 h203 h218 h254 h283 h324 h355 h376 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

+1.3°F (+0.7°C)

Models range from +0.9°F (+0.5°C) to +1.6°F (+0.9°C)

Days above 90°F (32°C) a year

0 0

Warming by month
  • January: +1.1°F (+0.6°C)
  • February: +1.4°F (+0.8°C)
  • March: +1.6°F (+0.9°C)
  • April: +1.6°F (+0.9°C)
  • May: +1.4°F (+0.8°C)
  • June: +1.4°F (+0.8°C)
  • July: +1.3°F (+0.7°C)
  • August: +1.0°F (+0.6°C)
  • September: +1.2°F (+0.7°C)
  • October: +1.4°F (+0.8°C)
  • November: +1.7°F (+0.9°C)
  • December: +1.4°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.