ClimateSearch

Manas, Jalal-Abad Region

Kyrgyzstan · 123k people · 786 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 high39°F (4°C)44°F (6°C)55°F (13°C)66°F (19°C)73°F (23°C)82°F (28°C)88°F (31°C)87°F (31°C)79°F (26°C)66°F (19°C)53°F (12°C)42°F (6°C)
Average low18°F (-8°C)22°F (-6°C)33°F (0°C)43°F (6°C)51°F (10°C)57°F (14°C)63°F (17°C)62°F (17°C)54°F (12°C)43°F (6°C)33°F (0°C)23°F (-5°C)
Dew point20°F (-7°C)24°F (-4°C)34°F (1°C)43°F (6°C)50°F (10°C)53°F (12°C)53°F (12°C)51°F (11°C)44°F (7°C)38°F (4°C)32°F (0°C)24°F (-5°C)
Rainfall1.9 in (48 mm)2.8 in (71 mm)3.9 in (99 mm)4.9 in (124 mm)4.7 in (120 mm)2.5 in (64 mm)1.2 in (30 mm)0.8 in (20 mm)1.1 in (27 mm)2.3 in (60 mm)2.8 in (70 mm)2.7 in (69 mm)
Rainy days8101313139445799
Snowfall10.4 in (26.5 cm)11.3 in (28.7 cm)5.3 in (13.5 cm)1.1 in (2.7 cm)0.1 in (0.2 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0.6 in (1.6 cm)4.4 in (11.3 cm)11.7 in (29.8 cm)
Sunshine212 h210 h263 h299 h361 h393 h421 h395 h342 h277 h221 h194 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

+3.2°F (+1.8°C)

Models range from +2.7°F (+1.5°C) to +4.1°F (+2.3°C)

Days above 90°F (32°C) a year

25 39

About 1.5× as many

Warming by month
  • January: +1.3°F (+0.7°C)
  • February: +2.4°F (+1.3°C)
  • March: +2.2°F (+1.2°C)
  • April: +1.6°F (+0.9°C)
  • May: +2.1°F (+1.2°C)
  • June: +3.6°F (+2.0°C)
  • July: +3.0°F (+1.7°C)
  • August: +3.0°F (+1.7°C)
  • September: +3.0°F (+1.7°C)
  • October: +2.3°F (+1.3°C)
  • November: +3.0°F (+1.7°C)
  • December: +2.5°F (+1.4°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.