ClimateSearch

Tegucigalpa, Francisco Morazán Department

Honduras · 851k people · 941 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 high79°F (26°C)83°F (28°C)86°F (30°C)89°F (31°C)85°F (29°C)81°F (27°C)81°F (27°C)82°F (28°C)81°F (27°C)79°F (26°C)78°F (25°C)78°F (26°C)
Average low62°F (17°C)63°F (17°C)64°F (18°C)67°F (20°C)68°F (20°C)68°F (20°C)67°F (19°C)67°F (20°C)67°F (20°C)66°F (19°C)64°F (18°C)63°F (17°C)
Dew point59°F (15°C)58°F (14°C)58°F (14°C)60°F (16°C)65°F (18°C)67°F (20°C)66°F (19°C)66°F (19°C)67°F (20°C)67°F (19°C)64°F (18°C)61°F (16°C)
Rainfall0.3 in (8 mm)0.2 in (6 mm)0.6 in (17 mm)2.3 in (58 mm)10.3 in (263 mm)9.5 in (240 mm)4.9 in (124 mm)7.4 in (188 mm)10.6 in (269 mm)9.4 in (239 mm)1.9 in (47 mm)0.4 in (11 mm)
Rainy days323922241822262293
Snowfall0 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 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)
Sunshine336 h320 h363 h349 h326 h310 h349 h344 h307 h300 h312 h328 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 +1.7°F (+0.9°C) to +4.0°F (+2.2°C)

Days above 90°F (32°C) a year

20 43

About 2.2× as many

Warming by month
  • January: +1.9°F (+1.0°C)
  • February: +2.1°F (+1.2°C)
  • March: +2.3°F (+1.3°C)
  • April: +2.6°F (+1.5°C)
  • May: +1.7°F (+0.9°C)
  • June: +2.4°F (+1.4°C)
  • July: +2.5°F (+1.4°C)
  • August: +2.4°F (+1.3°C)
  • September: +2.4°F (+1.4°C)
  • October: +1.8°F (+1.0°C)
  • November: +1.4°F (+0.8°C)
  • December: +1.9°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.