ClimateSearch

Miyakonojō, Miyazaki

Japan · 161k people · 148 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 high54°F (12°C)57°F (14°C)62°F (17°C)71°F (21°C)77°F (25°C)81°F (27°C)88°F (31°C)89°F (32°C)84°F (29°C)76°F (25°C)67°F (20°C)57°F (14°C)
Average low34°F (1°C)37°F (3°C)42°F (6°C)51°F (10°C)59°F (15°C)67°F (19°C)74°F (23°C)74°F (24°C)69°F (21°C)59°F (15°C)48°F (9°C)37°F (3°C)
Dew point36°F (2°C)38°F (3°C)44°F (6°C)51°F (11°C)60°F (15°C)68°F (20°C)74°F (24°C)75°F (24°C)70°F (21°C)60°F (15°C)50°F (10°C)40°F (4°C)
Rainfall2.7 in (68 mm)3.9 in (100 mm)5.6 in (143 mm)7.8 in (197 mm)8.8 in (224 mm)19.6 in (497 mm)14.7 in (372 mm)11.5 in (293 mm)10.9 in (277 mm)5.6 in (143 mm)4.3 in (109 mm)3 in (77 mm)
Rainy days7812111017141311886
Snowfall0.4 in (1.1 cm)0.2 in (0.4 cm)0 in (0.1 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)0.1 in (0.2 cm)
Sunshine169 h153 h147 h148 h138 h83 h148 h187 h155 h173 h162 h173 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 +1.9°F (+1.1°C) to +2.4°F (+1.3°C)

Days above 90°F (32°C) a year

9 → 22

About 2.5× as many

Warming by month
  • January: +2.3°F (+1.3°C)
  • February: +1.9°F (+1.0°C)
  • March: +1.7°F (+1.0°C)
  • April: +2.2°F (+1.2°C)
  • May: +1.8°F (+1.0°C)
  • June: +2.0°F (+1.1°C)
  • July: +2.4°F (+1.4°C)
  • August: +2.1°F (+1.2°C)
  • September: +2.4°F (+1.3°C)
  • October: +2.5°F (+1.4°C)
  • November: +2.3°F (+1.3°C)
  • December: +2.5°F (+1.4°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.