ClimateSearch

Lárisa, Thessaly

Greece · 147k people · 76 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 high50°F (10°C)53°F (12°C)59°F (15°C)67°F (20°C)78°F (25°C)87°F (31°C)91°F (33°C)91°F (33°C)82°F (28°C)71°F (22°C)60°F (16°C)51°F (11°C)
Average low35°F (2°C)37°F (3°C)41°F (5°C)48°F (9°C)57°F (14°C)66°F (19°C)71°F (22°C)71°F (22°C)63°F (17°C)55°F (13°C)46°F (8°C)38°F (3°C)
Dew point34°F (1°C)36°F (2°C)40°F (4°C)45°F (7°C)51°F (10°C)54°F (12°C)56°F (14°C)57°F (14°C)55°F (13°C)51°F (11°C)45°F (7°C)37°F (3°C)
Rainfall2.8 in (71 mm)2.5 in (64 mm)2.5 in (65 mm)2 in (50 mm)1.8 in (47 mm)1 in (26 mm)1 in (26 mm)0.8 in (19 mm)1.9 in (49 mm)2.4 in (61 mm)2.7 in (68 mm)3.3 in (83 mm)
Rainy days99118754457810
Snowfall3.1 in (8 cm)3.5 in (8.8 cm)1.7 in (4.3 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 (0.1 cm)2.7 in (6.8 cm)
Sunshine205 h213 h273 h324 h369 h413 h421 h397 h321 h263 h204 h188 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

+2.4°F (+1.4°C)

Models range from +1.3°F (+0.7°C) to +4.1°F (+2.3°C)

Days above 90°F (32°C) a year

52 66

About 1.3× as many

Warming by month
  • January: +2.4°F (+1.3°C)
  • February: +1.4°F (+0.8°C)
  • March: +2.8°F (+1.5°C)
  • April: +2.5°F (+1.4°C)
  • May: +1.4°F (+0.8°C)
  • June: +2.7°F (+1.5°C)
  • July: +2.3°F (+1.3°C)
  • August: +2.3°F (+1.3°C)
  • September: +3.0°F (+1.7°C)
  • October: +1.5°F (+0.9°C)
  • November: +1.9°F (+1.0°C)
  • December: +2.2°F (+1.2°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.