ClimateSearch

Tsukuba, Ibaraki

Japan · 242k people · 30 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 high49°F (9°C)50°F (10°C)56°F (13°C)65°F (18°C)72°F (22°C)76°F (25°C)83°F (29°C)86°F (30°C)80°F (26°C)70°F (21°C)61°F (16°C)52°F (11°C)
Average low29°F (-2°C)31°F (0°C)37°F (3°C)47°F (8°C)56°F (13°C)63°F (17°C)70°F (21°C)72°F (22°C)66°F (19°C)55°F (13°C)44°F (6°C)33°F (1°C)
Dew point28°F (-2°C)29°F (-2°C)36°F (2°C)46°F (8°C)55°F (13°C)64°F (18°C)71°F (22°C)72°F (22°C)66°F (19°C)56°F (13°C)45°F (7°C)34°F (1°C)
Rainfall1.6 in (42 mm)2.1 in (55 mm)3.5 in (88 mm)4.2 in (106 mm)4.9 in (125 mm)5.8 in (146 mm)5.9 in (151 mm)5 in (127 mm)6.8 in (173 mm)8.3 in (210 mm)3.1 in (78 mm)2.2 in (57 mm)
Rainy days561010101097101186
Snowfall2.3 in (5.8 cm)3 in (7.7 cm)1.1 in (2.7 cm)0.1 in (0.2 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)0.1 in (0.3 cm)0.3 in (0.7 cm)
Sunshine190 h165 h166 h161 h148 h101 h123 h170 h127 h127 h139 h167 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

+2.2°F (+1.2°C)

Models range from +2.0°F (+1.1°C) to +2.5°F (+1.4°C)

Days above 90°F (32°C) a year

14 → 38

About 2.7× as many

Warming by month
  • January: +2.4°F (+1.3°C)
  • February: +2.3°F (+1.3°C)
  • March: +2.0°F (+1.1°C)
  • April: +2.4°F (+1.3°C)
  • May: +2.3°F (+1.3°C)
  • June: +2.0°F (+1.1°C)
  • July: +2.3°F (+1.3°C)
  • August: +2.4°F (+1.4°C)
  • September: +2.8°F (+1.5°C)
  • October: +2.6°F (+1.4°C)
  • November: +2.5°F (+1.4°C)
  • December: +2.0°F (+1.1°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.