ClimateSearch

Sunggal, North Sumatra

Indonesia · 158k people · 32 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 high88°F (31°C)90°F (32°C)91°F (33°C)91°F (33°C)91°F (33°C)91°F (33°C)90°F (32°C)89°F (32°C)89°F (32°C)89°F (31°C)88°F (31°C)88°F (31°C)
Average low72°F (22°C)72°F (22°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)72°F (22°C)72°F (22°C)72°F (22°C)72°F (22°C)72°F (22°C)72°F (22°C)
Dew point73°F (23°C)73°F (23°C)74°F (23°C)74°F (24°C)75°F (24°C)74°F (24°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)73°F (23°C)
Rainfall6.3 in (161 mm)4.6 in (118 mm)6.1 in (155 mm)7.9 in (200 mm)9 in (230 mm)7.3 in (186 mm)7 in (177 mm)8.5 in (215 mm)11.7 in (297 mm)13.3 in (337 mm)11.3 in (287 mm)9.3 in (236 mm)
Rainy days151115202016161923252420
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)
Sunshine138 h147 h151 h129 h131 h147 h150 h136 h121 h103 h87 h95 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

+1.3°F (+0.7°C)

Models range from +0.9°F (+0.5°C) to +1.7°F (+1.0°C)

Days above 90°F (32°C) a year

7 → 12

About 1.8× as many

Warming by month
  • January: +1.1°F (+0.6°C)
  • February: +1.2°F (+0.7°C)
  • March: +1.1°F (+0.6°C)
  • April: +1.4°F (+0.8°C)
  • May: +1.2°F (+0.7°C)
  • June: +1.1°F (+0.6°C)
  • July: +1.1°F (+0.6°C)
  • August: +1.5°F (+0.9°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.7°F (+0.9°C)
  • November: +1.5°F (+0.8°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.