ClimateSearch

Santo Domingo de los Colorados, Santo Domingo de los Tsáchilas

Ecuador · 459k people · 550 m elevation · Southern 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 high80°F (27°C)81°F (27°C)83°F (28°C)82°F (28°C)81°F (27°C)79°F (26°C)79°F (26°C)79°F (26°C)80°F (26°C)79°F (26°C)78°F (26°C)80°F (27°C)
Average low66°F (19°C)66°F (19°C)67°F (19°C)67°F (19°C)67°F (20°C)66°F (19°C)65°F (18°C)64°F (18°C)65°F (18°C)65°F (18°C)64°F (18°C)66°F (19°C)
Dew point68°F (20°C)68°F (20°C)69°F (20°C)69°F (20°C)69°F (20°C)67°F (20°C)66°F (19°C)66°F (19°C)66°F (19°C)67°F (19°C)67°F (19°C)67°F (20°C)
Rainfall15.6 in (397 mm)18.8 in (479 mm)19.6 in (497 mm)18.8 in (478 mm)9.8 in (249 mm)6.2 in (157 mm)2.2 in (55 mm)1.7 in (43 mm)2.9 in (74 mm)2.6 in (65 mm)2 in (51 mm)5.8 in (146 mm)
Rainy days2625272520145486413
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)
Sunshine87 h78 h88 h95 h100 h97 h101 h97 h81 h81 h85 h91 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

+1.5°F (+0.8°C)

Models range from +1.0°F (+0.6°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

0 → 0

Warming by month
  • January: +1.4°F (+0.8°C)
  • February: +1.5°F (+0.8°C)
  • March: +1.7°F (+1.0°C)
  • April: +1.9°F (+1.1°C)
  • May: +1.8°F (+1.0°C)
  • June: +2.0°F (+1.1°C)
  • July: +1.6°F (+0.9°C)
  • August: +1.6°F (+0.9°C)
  • September: +1.6°F (+0.9°C)
  • October: +1.3°F (+0.7°C)
  • November: +1.4°F (+0.8°C)
  • December: +1.6°F (+0.9°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.