ClimateSearch

Labuan Bajo, East Nusa Tenggara

Indonesia · 189k people · 58 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 high82°F (28°C)82°F (28°C)83°F (28°C)83°F (29°C)84°F (29°C)83°F (28°C)83°F (28°C)83°F (28°C)84°F (29°C)85°F (29°C)85°F (29°C)83°F (28°C)
Average low76°F (24°C)76°F (24°C)76°F (25°C)77°F (25°C)76°F (25°C)75°F (24°C)74°F (23°C)74°F (23°C)75°F (24°C)76°F (25°C)77°F (25°C)77°F (25°C)
Dew point75°F (24°C)75°F (24°C)75°F (24°C)74°F (24°C)73°F (23°C)71°F (22°C)69°F (21°C)69°F (20°C)71°F (21°C)73°F (23°C)75°F (24°C)75°F (24°C)
Rainfall16.8 in (428 mm)15.6 in (396 mm)12.5 in (318 mm)9 in (229 mm)3.5 in (89 mm)2.1 in (53 mm)1.3 in (32 mm)0.7 in (17 mm)1.9 in (48 mm)5.3 in (134 mm)8.8 in (223 mm)13.3 in (338 mm)
Rainy days30272721117436152328
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)
Sunshine293 h271 h321 h327 h348 h334 h352 h361 h355 h365 h346 h306 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

+1.4°F (+0.8°C)

Models range from +1.2°F (+0.7°C) to +1.5°F (+0.8°C)

Days above 90°F (32°C) a year

0 0

About 2.0× as many

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