ClimateSearch

Pátra, West Greece

Greece · 168k people · 11 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 high53°F (12°C)54°F (12°C)59°F (15°C)65°F (19°C)74°F (23°C)83°F (28°C)89°F (31°C)89°F (32°C)80°F (27°C)72°F (22°C)63°F (17°C)55°F (13°C)
Average low42°F (5°C)42°F (5°C)45°F (7°C)50°F (10°C)57°F (14°C)65°F (18°C)70°F (21°C)71°F (22°C)65°F (18°C)58°F (15°C)51°F (11°C)45°F (7°C)
Dew point41°F (5°C)41°F (5°C)44°F (7°C)48°F (9°C)55°F (13°C)60°F (16°C)62°F (17°C)63°F (17°C)60°F (16°C)56°F (13°C)50°F (10°C)44°F (7°C)
Rainfall4.8 in (121 mm)4.5 in (115 mm)4 in (101 mm)2.8 in (72 mm)2.1 in (53 mm)0.9 in (24 mm)0.5 in (13 mm)0.5 in (13 mm)2 in (51 mm)3 in (76 mm)5 in (127 mm)5.2 in (132 mm)
Rainy days121212109433781113
Snowfall0.4 in (0.9 cm)0.5 in (1.2 cm)0.1 in (0.3 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)0.2 in (0.4 cm)
Sunshine231 h234 h302 h339 h376 h408 h421 h399 h330 h292 h227 h214 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

+2.7°F (+1.5°C)

Models range from +1.7°F (+0.9°C) to +4.0°F (+2.2°C)

Days above 90°F (32°C) a year

34 47

About 1.4× as many

Warming by month
  • January: +2.1°F (+1.1°C)
  • February: +1.6°F (+0.9°C)
  • March: +2.6°F (+1.5°C)
  • April: +2.4°F (+1.3°C)
  • May: +2.3°F (+1.3°C)
  • June: +2.8°F (+1.6°C)
  • July: +2.4°F (+1.3°C)
  • August: +2.7°F (+1.5°C)
  • September: +3.4°F (+1.9°C)
  • October: +1.6°F (+0.9°C)
  • November: +1.7°F (+0.9°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.