ClimateSearch

Manta, Manabí

Ecuador · 264k people · 32 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 high83°F (28°C)83°F (28°C)83°F (29°C)83°F (29°C)83°F (28°C)82°F (28°C)81°F (27°C)81°F (27°C)82°F (28°C)82°F (28°C)82°F (28°C)83°F (28°C)
Average low74°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)73°F (23°C)71°F (22°C)71°F (22°C)71°F (21°C)71°F (22°C)71°F (22°C)73°F (23°C)
Dew point71°F (22°C)73°F (23°C)73°F (23°C)72°F (22°C)71°F (22°C)69°F (21°C)68°F (20°C)67°F (19°C)67°F (19°C)67°F (19°C)67°F (20°C)69°F (20°C)
Rainfall2.9 in (74 mm)5.8 in (148 mm)4.7 in (119 mm)3.1 in (80 mm)1.4 in (35 mm)0.6 in (14 mm)0.3 in (8 mm)0.2 in (6 mm)0.3 in (9 mm)0.4 in (9 mm)0.5 in (13 mm)1.3 in (33 mm)
Rainy days1217161284212236
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)
Sunshine273 h237 h286 h288 h290 h271 h271 h283 h275 h288 h297 h299 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

+1.1°F (+0.6°C)

Models range from +0.3°F (+0.2°C) to +1.7°F (+0.9°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +0.9°F (+0.5°C)
  • February: +1.7°F (+0.9°C)
  • March: +1.6°F (+0.9°C)
  • April: +1.7°F (+1.0°C)
  • May: +1.9°F (+1.1°C)
  • June: +2.0°F (+1.1°C)
  • July: +1.7°F (+1.0°C)
  • August: +1.7°F (+1.0°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.5°F (+0.8°C)
  • November: +1.3°F (+0.7°C)
  • December: +0.8°F (+0.4°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.