ClimateSearch

Fernando de la Mora, Central Department

Paraguay · 120k people · 128 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 high90°F (32°C)88°F (31°C)86°F (30°C)81°F (27°C)74°F (23°C)71°F (22°C)71°F (22°C)76°F (24°C)80°F (26°C)83°F (28°C)85°F (29°C)88°F (31°C)
Average low75°F (24°C)74°F (23°C)71°F (22°C)67°F (19°C)61°F (16°C)58°F (15°C)56°F (13°C)59°F (15°C)62°F (17°C)67°F (19°C)69°F (20°C)73°F (23°C)
Dew point71°F (21°C)70°F (21°C)68°F (20°C)65°F (18°C)59°F (15°C)57°F (14°C)54°F (12°C)55°F (13°C)58°F (14°C)64°F (18°C)65°F (19°C)69°F (21°C)
Rainfall4.9 in (123 mm)5.5 in (141 mm)4.8 in (121 mm)6.1 in (155 mm)5.5 in (139 mm)4.1 in (105 mm)3.1 in (80 mm)2.6 in (67 mm)4.4 in (112 mm)7.9 in (200 mm)7.6 in (193 mm)6.5 in (165 mm)
Rainy days131311999879121113
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)
Sunshine357 h294 h314 h271 h242 h218 h239 h270 h275 h305 h320 h351 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

+2.0°F (+1.1°C)

Models range from +1.7°F (+1.0°C) to +2.4°F (+1.3°C)

Days above 90°F (32°C) a year

67 105

About 1.6× as many

Warming by month
  • January: +1.8°F (+1.0°C)
  • February: +1.8°F (+1.0°C)
  • March: +2.1°F (+1.2°C)
  • April: +1.4°F (+0.8°C)
  • May: +1.8°F (+1.0°C)
  • June: +1.5°F (+0.9°C)
  • July: +2.4°F (+1.4°C)
  • August: +2.4°F (+1.4°C)
  • September: +2.3°F (+1.3°C)
  • October: +2.2°F (+1.2°C)
  • November: +2.0°F (+1.1°C)
  • December: +2.3°F (+1.3°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.