Climatology
This page presents Kyrgyz Republic's climate context for the current climatology, 1991-2020, derived from observed, historical data. Information should be used to build a strong understanding of current climate conditions in order to appreciate future climate scenarios and projected change. You can visualize data for the current climatology through spatial variation, the seasonal cycle, or as a time series. Analysis is available for both annual and seasonal data. Data presentation defaults to national-scale aggregation, however sub-national data aggregations can be accessed by clicking within a country, on a sub-national unit. Other historical climatologies can be selected from the Time Period dropdown list.
Observed, historical data is produced by the Climatic Research Unit (CRU) of University of East Anglia. Data is presented at a 0.5º x 0.5º (50km x 50km) resolution.
The climate in the Kyrgyz Republic is as varied as the country’s topography and can be classified into four major zones, each with distinctive characteristics. The valley-sub-mountain zone (from 900-1,200 m) experiences hot summers, snowless and temperate winters, and almost zero precipitation. The mountain zone (from 900–1,200 to 2,000–2,200 m) is characterized by a temperate climate, which has warm summers and cold, snowy winters. The high-mountain zone (from 2,000–2,200 to 3,000–3,500 m) is cooler in the summer and has relatively cold, snowless winters, with temperatures ranging from well below zero to 16°C. The nival belt zone (from 3,500 m and higher) has a polar climate and is covered by numerous snowfields and glaciers. Temperature has a seasonal nature – February being the coldest month with average temperature -3.7°C and July being the warmest with +17.4°C.