XIONIA / GLACIERS

Russia glaciers: map, annual measurements & history

Explore 113 distinct glaciers in the available WGMS monitoring sample for Russia. The combined record spans 1604–2025; coverage and gaps differ for each glacier. Examples in the record include TSEYA, SKAZKA, DJANKUAT.

Find the glacier pin and map temperatures, a forecast for up to 14 days and the hourly meteogram. Compare 850 hPa and precipitation ensembles, inspect weather satellite imagery and explore the WGMS observation history.

113glaciers with observation series
32with mass-balance measurements
1604–2025year range across available series
DJANKUAT · 7-day forecast

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Glacier map, coordinates and temperatures

Dots mark WGMS monitoring locations. Select a glacier or click another map point: the widget, detailed forecast, meteogram, ensembles and satellite update for those same coordinates.

Loading catalogue… The catalogue and sources are also available below.

Temperatures apply to the selected forecast point. Day choices appear only where numeric data are available, up to 14 days.

FORECAST AT YOUR COORDINATES

Weather and 14-day forecast · DJANKUAT

43.1944°, 42.7612°

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Detailed forecast and model comparison · DJANKUAT

Daily temperature, 850 hPa, precipitation, snow, wind and pressure at the selected point. The combination uses the available models from the same forecast; missing values stay missing.

Hourly glacier meteogram · DJANKUAT

Follow 2 m and 850 hPa temperature, rain, snow and wind over the next 72 hours. Change models, range and variables, select an hour on the chart or open full screen.

Ensembles 850 hPa & precipitation · DJANKUAT

Each ensemble model calculates many possible outcomes from slightly different initial conditions. Thin lines represent its members and the stronger line their mean. A wider spread indicates greater uncertainty. Compare direct NOAA GEFS/AIGEFS, ECMWF IFS ENS/AIFS ENS and ECCC GEPS data when the corresponding downloads have completed.

The first visit to a new point may require collection time. This section shows the actual status and available range, without inventing members or values.

Weather satellite at the glacier · DJANKUAT

Inspect cloud cover using available visible and infrared channels. Image times and geographic coverage depend on the satellite; not every geostationary satellite covers polar regions. Cloud images do not measure glacier thickness.

Open satellite and radar · Powered by www.xionia.com

Glacier history and WGMS observations

Historical observations belong to DJANKUAT.

DJANKUAT

Measurements and references

Powered by www.xionia.com · WGMS

Glacier catalogue — Russia

Counts cover glaciers with mass-balance or observed front-variation records in this archive. They are not the total glacier population of a country.

WGMS observation series
GlacierMass balanceFront variation
ALIBEKSKIY1875–1995
ANUTSINA1913–2010
ARKHANGELSKOLGU1992–2010
BEZENGI1960–19741888–1998
BIRDZHALYCHIRAN1887–2007
BITYUKTYUBE1887–2007
BOLSHOY ABYL-OYUK1850–1962
BOLSHOY AZAU1849–2010
BOLSHOY MAASHEY1924–1990
BROUNOVE1913–2010
BUNGE1871–2011
CHACHI1964–2014
CHAEVA1992–2010
CHERNYSHEVA1992–2010
CHUNGURCHATCHIRAN1887–2007
DJANKUAT1968–20251887–2024
DYKH-SU1850–2000
DZHELO1936–2005
FISHT1905–1990
GARABASHI1984–20251887–2025
GEBLER (KATUNSKY)1835–1989
GRECHISHKIN1979–1979
IGAN1958–19811958–1981
INOSTRANZEVA1913–2010
IRIK1887–2007
IRIKCHAT1887–2007
KARACHAUL1887–2007
KARBASNIKOV1913–2006
KASHKATASH1839–2010
KAYARTA1964–1977
KELBASHI1966–1970
KHAKEL1974–19791888–2000
KOIAVGAN1968–1974
KORUMDU1936–2005
KORYTO1960–20001604–2000
KOZELSKIY1973–19971948–2000
KOZITSITI1888–2000
KRAYNIY 11992–2010
KRAYNIY21992–2010
KRIVOSHEINA1992–2010
KROPOTKIN1985–19851986–2000
KROPOTKINA1992–2010
KULAK NIZHNIY1970–1998
KYUKYURTLYU1887–2007
LEVIY AKTRU1977–20251975–2025
LEVIY KARAGEMSKIY1850–2005
MAKA1913–2010
MALIY AKTRU1962–20121911–2009
MALIY AZAU1887–2010
MARUKHSKIY1967–19821888–2000
MGU1953–1981
MIKELCHIRAN2025–20251887–2025
MIZHIRGICHIRAN1888–1998
MOSHNIY1992–2010
MURKAR1964–1985
MUTNOVSKIY NE1980–19841995–2000
MUTNOVSKIY SW1980–19841997–1999
NALLI1992–2010
NIIGA1992–2010
NO.311957–1969
OBRUCHEV1958–19811953–1981
PAVLOV1913–2011
PERVENETS1988–1988
PETERSEN (NOVZEM)1871–2011
PRAVIY AKTRU1980–19901936–1980
PRAVIY KARAGEMSKIY1850–2005
RODZEVICH1850–1995
ROZE1992–2010
ROZHDESTVENSKOGO1992–2010
RYKACHEVA1913–2010
SEDOV1958–1958
SHOKALSKIY (NOVAYA ZEMLYA)1958–19691913–2010
SHURY 11992–2010
SHURY 21992–2010
SKAZKA1890–2000
SOFIYSKIY1988–19991898–2001
SREDNIY1992–2010
STAGER1977–1977
TAISIYA 11992–2010
TAISIYA 21992–2010
TERSKOL1887–2007
TIKHITSAR1850–1988
TSEYA1960–19701890–2000
UILPATA1890–1990
ULLUCHIRAN1887–2007
ULLUKAM1870–2009
ULLUKOL1887–2007
ULLUMALIENDERKU1887–2007
UNIVERSITET (NO. 122)1985–1995
UNNAMED 11992–2010
UNNAMED 21992–2010
UNNAMED 31992–2010
UNNAMED 41992–2010
UNNAMED 51992–2010
UNNAMED 61992–2010
UNNAMED 71992–2010
VAVILOV ICE CAP (NO. 104)1975–19881985–1990
VEL'KENA1913–2010
VERA1913–2011
VERSHINSKOGO1992–2010
VIATAU1968–1974
VIL'KITSKOGO (NORTHERN)1992–2010
VIL'KITSKOGO (SOUTHERN)1992–2010
VISYACHIY1968–1974
VIZE1913–2010
VODOPADNIY (NO.125)1977–20121985–2009
VOEYKOVA1992–2010
VOSTOCHNYI KLUHORSKIY (NO. 762)1890–1990
VYLKI 11992–2010
VYLKI 21992–2010
YUGO-VOSTOCHNIY1959–2000
YUNOM1977–1977
YUZHNIY1862–2000

Glaciers by country and territory

Antarctica299 in the sample · 1940–2025Argentina40 in the sample · 1660–2025Austria160 in the sample · 1620–2025Bhutan3 in the sample · 1984–2021Bolivia4 in the sample · 1963–2024Canada102 in the sample · 1720–2025Chile180 in the sample · 1628–2025China76 in the sample · 1900–2025Colombia46 in the sample · 1945–2025DR Congo1 in the sample · 1906–2005Ecuador1 in the sample · 1956–2025France17 in the sample · 1730–2025Georgia40 in the sample · 1810–2025Germany2 in the sample · 1896–1968Greenland99 in the sample · 1811–2025Heard and McDonald Islands21 in the sample · 1947–2019Iceland91 in the sample · 1740–2025India69 in the sample · 1780–2025Indonesia3 in the sample · 1825–1990Italy413 in the sample · 1833–2025Japan1 in the sample · 1968–2025Kazakhstan33 in the sample · 1850–2025Kenya13 in the sample · 1893–2014Kyrgyzstan45 in the sample · 1850–2025Mexico2 in the sample · 1921–1999Nepal23 in the sample · 1910–2025New Zealand95 in the sample · 1865–2025Norway97 in the sample · 1600–2025Pakistan17 in the sample · 1850–2010Peru17 in the sample · 1932–2025Poland4 in the sample · 1978–2016Russia113 in the sample · 1604–2025South Georgia and South Sandwich Islands6 in the sample · 1882–2003Spain30 in the sample · 1825–2025Svalbard and Jan Mayen42 in the sample · 1861–2025Sweden21 in the sample · 1896–2025Switzerland136 in the sample · 1833–2025Tajikistan180 in the sample · 1870–2025Türkiye1 in the sample · 1902–2008Uganda1 in the sample · 1906–2003United States223 in the sample · 1670–2025Uzbekistan11 in the sample · 1961–2025

Why glaciers matter: water, climate and changing mountains

A glacier is a body of snow and ice that flows over land. Snow accumulation adds mass; melting and ice loss remove it. A snowy week is therefore only one part of a much longer balance. NSIDC: glaciers.

Glacier melt contributes to river flow and freshwater supply. Ice stored on land also matters for sea level when it reaches the ocean. Changing ice affects mountain landscapes and the ecosystems connected to meltwater. NSIDC: why glaciers matter.

Use the country pages to move from a broad view to an individual observation record. Then open nearby mountain or ski-resort forecasts to examine temperature, precipitation and wind. These forecasts describe short-term weather; the glacier history describes measured change over years.

How to read glacier mass balance and retreat

Annual mass balance, m w.e. A positive value means net mass gain during the reported hydrological year; a negative value means net loss. Metres of water equivalent express the mass as an equivalent water layer. They are not a direct measurement of metres of ice thickness at one point. WGMS: mass-balance units.

Front variation, metres. This measures movement of the glacier terminus between the stated dates. Negative values mean retreat, positive values advance. A measurement interval may span several years: the chart preserves the interval and does not invent annual values.

Missing years and different methods. Gaps remain gaps. Winter and summer balances are displayed only when reported. Glacier outlines are dated observations of shape, while a mass-balance series measures change; combining them does not turn the map into a live ice forecast.

Planning a mountain visit. Links to nearby destinations show approximate straight-line distances, not routes across ice. Check the destination’s forecast and current local operating information before choosing a ski area or mountain itinerary.

Sources, coverage and updates

Location catalogue: public WGMS service, retrieved 2026-09-14. Historical series are requested from WGMS when you select a glacier, with a seven-day cache. Each series displays its edition and retrieval time. Cached copies are clearly marked when the source is unavailable.

Forecast and meteogram: available weather models via Open-Meteo or direct NOAA, ECMWF and ECCC/GEM feeds, with source selection. Ensembles use direct official feeds. Weather models and meteorological maps · Embeddable weather widgets.