ClimateSearch

Nizāmābād, Telangana

India · 311k people · 389 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)92°F (33°C)98°F (37°C)103°F (39°C)107°F (42°C)97°F (36°C)87°F (31°C)87°F (30°C)87°F (31°C)89°F (32°C)87°F (31°C)86°F (30°C)
Average low60°F (16°C)65°F (18°C)71°F (22°C)78°F (25°C)83°F (28°C)78°F (26°C)74°F (24°C)74°F (23°C)73°F (23°C)70°F (21°C)63°F (17°C)59°F (15°C)
Dew point52°F (11°C)52°F (11°C)53°F (12°C)56°F (13°C)58°F (14°C)69°F (20°C)71°F (22°C)71°F (22°C)71°F (22°C)67°F (19°C)59°F (15°C)53°F (12°C)
Rainfall0.2 in (5 mm)0.2 in (5 mm)0.8 in (20 mm)0.8 in (20 mm)0.5 in (12 mm)6.7 in (171 mm)14.1 in (358 mm)12.8 in (326 mm)9.5 in (242 mm)2.8 in (71 mm)0.5 in (14 mm)0.1 in (3 mm)
Rainy days1122110161412621
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 h262 h301 h291 h291 h147 h81 h85 h133 h215 h245 h258 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 +1.3°F (+0.7°C) to +1.5°F (+0.9°C)

Days above 90°F (32°C) a year

130 → 142

About 1.1× as many

Warming by month
  • January: +0.1°F (+0.1°C)
  • February: +0.1°F (+0.1°C)
  • March: −0.2°F (−0.1°C)
  • April: −0.3°F (−0.2°C)
  • May: +0.9°F (+0.5°C)
  • June: +2.0°F (+1.1°C)
  • July: +1.1°F (+0.6°C)
  • August: +1.2°F (+0.7°C)
  • September: +1.3°F (+0.7°C)
  • October: +1.2°F (+0.6°C)
  • November: +0.7°F (+0.4°C)
  • December: +0.3°F (+0.2°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.