ClimateSearch

Rondonópolis, Mato Grosso

Brazil · 264k people · 229 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 high89°F (32°C)89°F (32°C)89°F (32°C)89°F (32°C)87°F (30°C)85°F (30°C)85°F (29°C)89°F (32°C)92°F (34°C)93°F (34°C)91°F (33°C)89°F (32°C)
Average low69°F (21°C)69°F (20°C)69°F (20°C)67°F (19°C)62°F (17°C)58°F (14°C)56°F (13°C)59°F (15°C)65°F (19°C)68°F (20°C)69°F (20°C)69°F (20°C)
Dew point73°F (23°C)73°F (23°C)73°F (23°C)71°F (21°C)65°F (18°C)61°F (16°C)57°F (14°C)56°F (14°C)62°F (17°C)70°F (21°C)72°F (22°C)73°F (23°C)
Rainfall11.3 in (288 mm)10.2 in (259 mm)7.9 in (201 mm)4.2 in (107 mm)1.5 in (38 mm)0.5 in (12 mm)0.4 in (10 mm)0.3 in (9 mm)1.4 in (37 mm)5.7 in (145 mm)7.8 in (199 mm)9.3 in (237 mm)
Rainy days191716831114111518
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)
Sunshine148 h142 h175 h202 h223 h236 h259 h263 h231 h204 h176 h158 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

+1.6°F (+0.9°C)

Models range from +1.3°F (+0.7°C) to +1.9°F (+1.1°C)

Days above 90°F (32°C) a year

124 → 187

About 1.5× as many

Warming by month
  • January: +1.8°F (+1.0°C)
  • February: +1.2°F (+0.7°C)
  • March: +1.6°F (+0.9°C)
  • April: +1.6°F (+0.9°C)
  • May: +1.6°F (+0.9°C)
  • June: +2.4°F (+1.3°C)
  • July: +2.9°F (+1.6°C)
  • August: +2.9°F (+1.6°C)
  • September: +4.0°F (+2.2°C)
  • October: +3.7°F (+2.0°C)
  • November: +3.0°F (+1.7°C)
  • December: +1.7°F (+1.0°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.