ClimateSearch

Manukau City, Auckland

New Zealand · 362k people · 35 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 high76°F (25°C)77°F (25°C)74°F (24°C)70°F (21°C)64°F (18°C)60°F (15°C)59°F (15°C)60°F (16°C)63°F (17°C)66°F (19°C)69°F (21°C)74°F (23°C)
Average low60°F (15°C)60°F (16°C)57°F (14°C)53°F (12°C)50°F (10°C)46°F (8°C)44°F (7°C)45°F (7°C)48°F (9°C)51°F (10°C)54°F (12°C)58°F (14°C)
Dew point58°F (14°C)59°F (15°C)57°F (14°C)54°F (12°C)51°F (11°C)48°F (9°C)47°F (8°C)47°F (8°C)48°F (9°C)50°F (10°C)52°F (11°C)56°F (13°C)
Rainfall3.9 in (99 mm)3.6 in (93 mm)4 in (101 mm)4.1 in (105 mm)5 in (127 mm)4.7 in (120 mm)5.9 in (150 mm)4.9 in (125 mm)4.1 in (104 mm)3.4 in (86 mm)3.5 in (88 mm)4.6 in (116 mm)
Rainy days767810111314121199
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)
Sunshine239 h201 h210 h177 h163 h143 h148 h173 h180 h199 h210 h215 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

+1.4°F (+0.8°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: +1.2°F (+0.7°C)
  • February: +1.5°F (+0.8°C)
  • March: +1.5°F (+0.9°C)
  • April: +1.5°F (+0.8°C)
  • May: +1.3°F (+0.7°C)
  • June: +1.4°F (+0.8°C)
  • July: +1.4°F (+0.8°C)
  • August: +1.0°F (+0.6°C)
  • September: +1.3°F (+0.7°C)
  • October: +1.4°F (+0.8°C)
  • November: +1.7°F (+1.0°C)
  • December: +1.6°F (+0.9°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.