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 high87°F (31°C)87°F (31°C)87°F (31°C)87°F (31°C)86°F (30°C)86°F (30°C)87°F (31°C)91°F (33°C)94°F (34°C)92°F (33°C)89°F (31°C)87°F (31°C)
Average low74°F (23°C)74°F (23°C)73°F (23°C)72°F (22°C)68°F (20°C)65°F (19°C)64°F (18°C)67°F (20°C)72°F (22°C)74°F (24°C)74°F (23°C)74°F (23°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)
Rainfall10.4 in (265 mm)8.7 in (220 mm)6.8 in (174 mm)2.6 in (67 mm)1 in (24 mm)0.4 in (10 mm)0.3 in (6 mm)0.3 in (7 mm)1.6 in (42 mm)4.4 in (111 mm)6.9 in (175 mm)9.7 in (247 mm)
Rainy days2522221141126172125
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)
Sunshine294 h272 h308 h305 h313 h308 h323 h331 h313 h326 h312 h307 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.