ClimateSearch

Yichang, Hubei

China · 1.4M people · 63 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)53°F (12°C)61°F (16°C)72°F (22°C)79°F (26°C)84°F (29°C)88°F (31°C)87°F (31°C)80°F (27°C)71°F (22°C)62°F (17°C)52°F (11°C)
Average low35°F (2°C)38°F (4°C)45°F (7°C)55°F (13°C)64°F (18°C)71°F (22°C)76°F (25°C)75°F (24°C)67°F (20°C)58°F (14°C)48°F (9°C)38°F (4°C)
Dew point32°F (0°C)36°F (2°C)44°F (7°C)54°F (12°C)62°F (17°C)70°F (21°C)75°F (24°C)74°F (23°C)65°F (19°C)56°F (13°C)46°F (8°C)36°F (2°C)
Rainfall1.3 in (32 mm)1.5 in (37 mm)2.5 in (64 mm)3.4 in (85 mm)5 in (127 mm)7.6 in (192 mm)9.4 in (238 mm)6.5 in (166 mm)4 in (102 mm)3.2 in (81 mm)2.1 in (54 mm)1 in (26 mm)
Rainy days6711111313191611986
Snowfall2.9 in (7.4 cm)1.5 in (3.7 cm)0.7 in (1.9 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)0.2 in (0.5 cm)0.9 in (2.3 cm)
Sunshine207 h185 h209 h231 h249 h251 h278 h285 h217 h208 h193 h198 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 +1.6°F (+0.9°C) to +2.8°F (+1.6°C)

Days above 90°F (32°C) a year

28 49

About 1.7× as many

Warming by month
  • January: +2.9°F (+1.6°C)
  • February: +2.3°F (+1.3°C)
  • March: +2.2°F (+1.2°C)
  • April: +2.3°F (+1.3°C)
  • May: +1.8°F (+1.0°C)
  • June: +2.7°F (+1.5°C)
  • July: +1.8°F (+1.0°C)
  • August: +2.1°F (+1.1°C)
  • September: +2.7°F (+1.5°C)
  • October: +2.0°F (+1.1°C)
  • November: +2.3°F (+1.3°C)
  • December: +2.7°F (+1.5°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.