ClimateSearch

Lhoka, Tibet

China · 354k people · 3559 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 high40°F (5°C)44°F (7°C)49°F (9°C)55°F (13°C)62°F (17°C)68°F (20°C)68°F (20°C)67°F (19°C)64°F (18°C)57°F (14°C)46°F (8°C)43°F (6°C)
Average low19°F (-7°C)22°F (-5°C)27°F (-3°C)33°F (0°C)41°F (5°C)49°F (10°C)52°F (11°C)51°F (11°C)48°F (9°C)37°F (3°C)26°F (-3°C)22°F (-5°C)
Dew point4°F (-15°C)7°F (-14°C)15°F (-10°C)24°F (-5°C)33°F (1°C)44°F (7°C)49°F (9°C)48°F (9°C)44°F (7°C)30°F (-1°C)17°F (-8°C)9°F (-13°C)
Rainfall0.2 in (4 mm)0.2 in (5 mm)0.6 in (16 mm)1.4 in (36 mm)2.2 in (56 mm)3.7 in (94 mm)5.5 in (139 mm)5 in (126 mm)3.1 in (80 mm)1.2 in (30 mm)0.4 in (10 mm)0.1 in (4 mm)
Rainy days125111419242318731
Snowfall1.5 in (3.7 cm)1.8 in (4.5 cm)4.1 in (10.5 cm)6 in (15.2 cm)4.3 in (10.8 cm)0.6 in (1.5 cm)0 in (0.1 cm)0.1 in (0.2 cm)0.4 in (1 cm)4.1 in (10.3 cm)2.7 in (6.8 cm)1.3 in (3.2 cm)
Sunshine308 h297 h355 h354 h386 h362 h320 h314 h324 h334 h311 h307 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

+2.7°F (+1.5°C)

Models range from +1.7°F (+1.0°C) to +3.2°F (+1.8°C)

Days above 90°F (32°C) a year

0 0

Warming by month
  • January: +3.8°F (+2.1°C)
  • February: +2.7°F (+1.5°C)
  • March: +2.9°F (+1.6°C)
  • April: +2.1°F (+1.1°C)
  • May: +1.7°F (+0.9°C)
  • June: +2.7°F (+1.5°C)
  • July: +2.6°F (+1.4°C)
  • August: +2.7°F (+1.5°C)
  • September: +1.9°F (+1.1°C)
  • October: +3.0°F (+1.7°C)
  • November: +2.8°F (+1.6°C)
  • December: +3.0°F (+1.6°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.