ClimateSearch

Ādilābād, Telangana

India · 119k people · 255 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 high87°F (31°C)93°F (34°C)100°F (38°C)106°F (41°C)111°F (44°C)101°F (38°C)89°F (32°C)88°F (31°C)89°F (32°C)90°F (32°C)88°F (31°C)86°F (30°C)
Average low59°F (15°C)64°F (18°C)71°F (22°C)78°F (26°C)84°F (29°C)80°F (27°C)76°F (24°C)75°F (24°C)74°F (24°C)71°F (21°C)63°F (17°C)58°F (15°C)
Dew point52°F (11°C)52°F (11°C)53°F (11°C)54°F (12°C)57°F (14°C)69°F (21°C)73°F (23°C)73°F (23°C)73°F (23°C)67°F (20°C)59°F (15°C)53°F (11°C)
Rainfall0.1 in (3 mm)0.3 in (8 mm)1.1 in (27 mm)0.5 in (14 mm)0.4 in (9 mm)7.7 in (196 mm)14.4 in (365 mm)11.3 in (287 mm)9.6 in (244 mm)2.1 in (53 mm)0.5 in (12 mm)0.1 in (3 mm)
Rainy days1132110171412511
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)
Sunshine260 h261 h302 h292 h298 h149 h75 h77 h133 h227 h253 h263 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

+1.5°F (+0.9°C)

Models range from +1.4°F (+0.8°C) to +1.7°F (+0.9°C)

Days above 90°F (32°C) a year

143 → 160

About 1.1× as many

Warming by month
  • January: −0.1°F (+0.0°C)
  • February: +0.0°F (+0.0°C)
  • March: −0.3°F (−0.1°C)
  • April: −0.4°F (−0.2°C)
  • May: +0.8°F (+0.4°C)
  • June: +2.3°F (+1.3°C)
  • July: +1.2°F (+0.7°C)
  • August: +1.1°F (+0.6°C)
  • September: +1.3°F (+0.7°C)
  • October: +1.0°F (+0.6°C)
  • November: +0.6°F (+0.4°C)
  • December: +0.0°F (+0.0°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.