ClimateSearch

Hayward, California

United States · 158k people · 32 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 high60°F (15°C)63°F (17°C)66°F (19°C)70°F (21°C)73°F (23°C)78°F (26°C)80°F (27°C)81°F (27°C)81°F (27°C)77°F (25°C)67°F (20°C)60°F (16°C)
Average low43°F (6°C)45°F (7°C)47°F (8°C)48°F (9°C)52°F (11°C)55°F (13°C)57°F (14°C)57°F (14°C)56°F (13°C)52°F (11°C)47°F (8°C)42°F (6°C)
Dew point43°F (6°C)44°F (7°C)46°F (8°C)46°F (8°C)49°F (9°C)51°F (11°C)54°F (12°C)55°F (13°C)54°F (12°C)50°F (10°C)46°F (8°C)42°F (6°C)
Rainfall3.4 in (87 mm)3.2 in (81 mm)2.4 in (62 mm)1.3 in (33 mm)0.5 in (13 mm)0.2 in (4 mm)0 in (1 mm)0 in (1 mm)0.1 in (2 mm)1 in (26 mm)1.8 in (47 mm)3 in (77 mm)
Rainy days988431000358
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)
Sunshine143 h155 h200 h241 h288 h318 h337 h314 h282 h238 h176 h146 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

+1.7°F (+0.9°C)

Models range from +0.9°F (+0.5°C) to +2.4°F (+1.4°C)

Days above 90°F (32°C) a year

10 → 15

About 1.5× as many

Warming by month
  • January: +1.3°F (+0.7°C)
  • February: +1.4°F (+0.8°C)
  • March: +1.3°F (+0.7°C)
  • April: +1.5°F (+0.8°C)
  • May: +1.9°F (+1.1°C)
  • June: +2.0°F (+1.1°C)
  • July: +1.3°F (+0.7°C)
  • August: +1.8°F (+1.0°C)
  • September: +1.9°F (+1.1°C)
  • October: +2.8°F (+1.6°C)
  • November: +2.8°F (+1.6°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.