ClimateSearch

Tebingtinggi, North Sumatra

Indonesia · 118k people · 28 m elevation · Northern 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 (29°C)84°F (29°C)85°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)85°F (29°C)84°F (29°C)83°F (28°C)83°F (28°C)
Average low73°F (23°C)73°F (23°C)74°F (23°C)74°F (24°C)75°F (24°C)75°F (24°C)74°F (24°C)74°F (23°C)74°F (23°C)74°F (23°C)73°F (23°C)73°F (23°C)
Dew point73°F (23°C)74°F (23°C)74°F (24°C)75°F (24°C)76°F (24°C)75°F (24°C)75°F (24°C)74°F (24°C)75°F (24°C)74°F (24°C)74°F (24°C)74°F (23°C)
Rainfall7.4 in (189 mm)5.7 in (145 mm)6.7 in (169 mm)8 in (203 mm)8.5 in (217 mm)5.9 in (151 mm)6.1 in (156 mm)7 in (177 mm)10.1 in (256 mm)11.8 in (300 mm)12.6 in (321 mm)11.1 in (283 mm)
Rainy days242123272622212328292927
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)
Sunshine295 h286 h302 h285 h295 h297 h303 h298 h281 h265 h240 h254 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

+0.9°F (+0.5°C)

Models range from +0.0°F (+0.0°C) to +1.3°F (+0.7°C)

Days above 90°F (32°C) a year

4 5

About 1.3× as many

Warming by month
  • January: +0.9°F (+0.5°C)
  • February: +1.1°F (+0.6°C)
  • March: +0.9°F (+0.5°C)
  • April: +1.1°F (+0.6°C)
  • May: +0.8°F (+0.5°C)
  • June: +0.7°F (+0.4°C)
  • July: +0.8°F (+0.5°C)
  • August: +1.1°F (+0.6°C)
  • September: +1.0°F (+0.5°C)
  • October: +1.3°F (+0.7°C)
  • November: +1.3°F (+0.7°C)
  • December: +1.5°F (+0.8°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.