XIONIA / GLACIERS

Tajikistan glaciers: map, annual measurements & history

Explore 180 distinct glaciers in the available WGMS monitoring sample for Tajikistan. The combined record spans 1870–2025; coverage and gaps differ for each glacier. Examples in the record include RAMA, MUSHKETOV, MAZARSKIY.

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.

180glaciers with observation series
5with mass-balance measurements
1870–2025year range across available series
EAST ZULMART (GLACIER NO 139) · 7-day forecast

Loading forecast…

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 · EAST ZULMART (GLACIER NO 139)

38.8628°, 73.0033°

Link to this pointFull point forecast
Enter coordinates

Loading forecast…

Detailed forecast and model comparison · EAST ZULMART (GLACIER NO 139)

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 · EAST ZULMART (GLACIER NO 139)

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 · EAST ZULMART (GLACIER NO 139)

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 · EAST ZULMART (GLACIER NO 139)

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 EAST ZULMART (GLACIER NO 139).

EAST ZULMART (GLACIER NO 139)

Measurements and references

Powered by www.xionia.com · WGMS

Glacier catalogue — Tajikistan

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
AKBAYTAL—1960–1990
BAKCHIGIR—1972–1990
BELEULI—1973–1980
BUZ-CHUBEK—1980–1990
CHAKYDZHILGA—1973–1990
DIAKHANDARA—1964–1978
DIDAL—1973–1985
DIKHADANG (NO.314)1983–19851980–1990
DUSAKASAY—1973–1990
DZHAYLYAUKUMSAY—1973–1990
EAST ZULMART (GLACIER NO 139)2019–2025—
FEDCHENKO—1928–1990
GARMO—1972–1985
GEOGRAPHICHESKOGO OBSHCHESTVA—1962–1989
GLACIER NO. 71 (YAKARCHA)2020–2020—
ICHKELSAY—1973–1990
KARA-ART—1973–1990
KHADYRSHA—1977–1990
KIZILGORUM—1940–1985
KRASNOSLOBODTSEV—1973–1990
KYZYLDZHILGA—1980–1990
KYZYLKUL—1975–1980
M. OKTYABRSKIY—1963–1990
MAZARSKIY—1958–1990
MEDVEZHIY—1962–1985
MUSHKETOV—1962–1990
NANKALDY—1980–1990
NICHKEDZHILGA—1973–1990
NO. 457 (NHD)2021–2025—
NO. 676 (GGP)2020–2020—
NO.001.14.03.17—1973–1990
NO.003.14.03.17—1973–1990
NO.005.14.03.17—1973–1990
NO.008.14.03.17—1980–1990
NO.010.14.03.17—1973–1990
NO.012.14.03.17—1980–1990
NO.015.14.03.17—1980–1990
NO.016.14.03.17—1980–1990
NO.030.14.03.17—1980–1990
NO.031.14.03.14—1973–1990
NO.031.14.03.17—1980–1990
NO.034.14.03.17—1980–1990
NO.036.14.03.17—1980–1990
NO.038.14.03.14—1973–1990
NO.039.14.03.14—1973–1990
NO.041.14.03.17—1980–1990
NO.042.14.03.17—1973–1990
NO.044.14.03.14—1973–1990
NO.046.14.03.14—1973–1990
NO.047.14.03.14—1973–1990
NO.052.14.03.14—1973–1990
NO.054.14.03.14—1973–1990
NO.072.14.03.17—1980–1990
NO.083.14.03.14—1973–1990
NO.087.14.03.14—1973–1990
NO.089.14.03.14—1973–1990
NO.093.14.03.14—1973–1990
NO.093.14.03.17—1980–1990
NO.096.14.03.17—1980–1990
NO.100.14.03.14—1973–1990
NO.101.14.03.14—1973–1990
NO.134.14.03.17—1973–1980
NO.136.14.03.17—1973–1990
NO.139.14.03.17—1973–1990
NO.152.14.03.14—1973–1990
NO.155.14.03.14—1973–1990
NO.159.14.03.14—1973–1990
NO.160.14.03.14—1973–1990
NO.161.14.03.14—1973–1990
NO.165.14.03.14—1973–1990
NO.168.14.03.14—1973–1990
NO.169.14.03.14—1973–1990
NO.170.14.03.14—1973–1990
NO.172.14.03.14—1973–1990
NO.173.14.03.14—1973–1990
NO.174.14.03.14—1973–1990
NO.208.14.03.14—1973–1990
NO.239.14.03.17—1973–1990
NO.240.14.03.17—1973–1990
NO.241.14.03.17—1973–1990
NO.242.14.03.17—1973–1990
NO.243.14.03.14—1973–1990
NO.254.14.03.17—1973–1990
NO.257.14.03.17—1980–1990
NO.259.14.03.17—1973–1990
NO.26.14.03.17—1980–1990
NO.260.14.03.17—1980–1990
NO.261.14.03.17—1980–1990
NO.262.14.03.17—1973–1990
NO.263.14.03.17—1973–1990
NO.264.14.03.17—1973–1980
NO.268.14.03.17—1973–1990
NO.269.14.03.17—1973–1990
NO.270.14.03.17—1973–1990
NO.271.14.03.17—1973–1990
NO.273.14.03.14—1973–1990
NO.279.14.03.14—1973–1990
NO.280.14.03.14—1973–1990
NO.281.14.03.14—1973–1990
NO.284.14.03.14—1973–1990
NO.306.14.03.14—1973–1990
NO.314.14.03.08—1973–1990
NO.315.14.03.08—1973–1990
NO.324.14.03.08—1980–1990
NO.329.14.03.14—1973–1990
NO.331.14.03.14—1973–1990
NO.375.14.03.15—1973–1990
NO.385.14.03.15—1973–1990
NO.388.14.03.15—1973–1990
NO.390.14.03.15—1973–1990
NO.394.14.03.15—1973–1990
NO.429.14.03.15—1973–1990
NO.434.14.03.15—1973–1990
NO.446.14.03.13—1980–1990
NO.447.14.03.08—1973–1990
NO.448.14.03.08—1973–1990
NO.449.14.03.08—1973–1990
NO.449.14.03.13—1980–1990
NO.453.14.03.13—1980–1990
NO.464.14.03.08—1973–1990
NO.469.14.03.08—1973–1990
NO.471.14.03.08—1973–1990
NO.473.14.03.08—1973–1990
NO.474.14.03.08—1973–1990
NO.499.14.03.13—1980–1990
NO.503—1974–1989
NO.503.14.03.08—1973–1990
NO.506.14.03.08—1973–1990
NO.507—1975–1985
NO.508.14.03.08—1973–1990
NO.509.14.03.08—1973–1990
NO.512.14.03.08—1973–1990
NO.514.14.03.08—1973–1990
NO.517—1975–1989
NO.519.14.03.08—1973–1990
NO.531.14.03.08—1973–1990
NO.532.14.03.08—1973–1990
NO.541.14.03.08—1973–1990
NO.543.14.03.08—1973–1990
NO.544.14.03.08—1973–1990
NO.549.14.03.08—1973–1990
NO.551.14.03.08—1973–1990
NO.558.14.03.08—1973–1990
NO.572.14.03.08—1973–1990
NO.573.14.03.08—1973–1990
NO.578.14.03.08—1973–1990
NO.579.14.03.08—1973–1990
NO.580.14.03.08—1980–1990
NO.582.14.03.08—1973–1990
NO.586.14.03.08—1973–1990
NO.591.14.03.08—1973–1990
NO.597.14.03.14—1973–1990
NO.598.14.03.14—1980–1990
NO.599.14.03.08—1973–1990
NO.600.14.03.08—1973–1990
NO.605.14.03.08—1973–1990
NO.606.14.03.08—1973–1990
NO.608.14.03.08—1973–1990
NO.612.14.03.08—1973–1990
NO.614.14.03.08—1973–1990
NO.617.14.03.08—1973–1990
NO.622.14.03.08—1973–1990
NO.623.14.03.08—1973–1990
NO.675—1977–1990
RAMA—1870–1990
SEVERNIY DZHAYLYAUKUMSAY—1973–1990
SEVERNIY ZULUMART—1973–1990
SKOGACH—1973–1990
TURO—1980–1990
UNNAMED 23518—1973–1990
URTA-BAKCHIGIR 1—1973–1990
URTA-BAKCHIGIR 2—1973–1990
VOLODARSKIY 1—1973–1990
VOLODARSKIY 2—1973–1990
VOLODARSKIY 3—1973–1990
YUZHNIY KARAKAYSHAN—1973–1990
ZAPADNIY OKTYABRSKIY—1973–1990
ZERAVSHANSKIY—1880–1990
ZORTASHKOL—1980–1990
ZULUMART—1943–2001

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.