XIONIA / GLACIERS

Switzerland glaciers: map, annual measurements & history

Explore 136 distinct glaciers in the available WGMS monitoring sample for Switzerland. The combined record spans 1833–2025; coverage and gaps differ for each glacier. Examples in the record include TRIENT, RHONE, MORTERATSCH, VADRET DA.

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.

136glaciers with observation series
38with mass-balance measurements
1833–2025year range across available series
RHONE · 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.

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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 · RHONE

46.6200°, 8.4000°

Link to this pointFull point forecast
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Detailed forecast and model comparison · RHONE

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 · RHONE

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 · RHONE

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 · RHONE

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 RHONE.

RHONE

Measurements and references

Powered by www.xionia.com · WGMS

Glacier catalogue — Switzerland

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
ADLER2006–2024—
ALBIGNA1955–19601855–2024
ALLALIN1956–20251881–2020
ALPETLI (KANDER)—1893–2024
ALPHUBEL-S2025–2025—
AMMERTEN—1969–2024
AROLLA (BAS)—1856–2024
BASODINO1992–20251893–2024
BELLA TOLA—1945–2005
BIFERTEN—1883–2024
BIS—1900–2024
BLUEMLISALP—1893–2024
BOVEYRE—1889–2024
BRENEY—1881–2023
BRESCIANA—1896–2023
BRUNEGG—1934–2024
BRUNNI—1882–2024
CALDERAS—1920–2023
CAMBRENA—1888–2024
CAVAGNOLI—1893–2022
CHEILLON—1924–2024
CHESSJEN-NW2025–2025—
CHLI (NO. 91)—2020–2024
CLARIDENFIRN1915–2025—
CORBASSIERE1997–20251889–2023
CORNO—1893–2024
CORVATSCH-S (PART OF E23/18)2014–2025—
CROSLINA GRANDE—1989–2019
DAMMA—1921–2023
DUNGEL—1893–2012
EIGER—1876–2021
EN DARREY—1880–2023
FEE NORTH—1883–2023
FERPECLE—1891–2024
FIESCHER—1891–2023
FINDELEN2005–20251885–2024
FIRNALPELI—1894–2018
FORNO1955–19601833–2024
GAMCHI—1883–2024
GAULI—1882–2024
GELTEN-W—1999–2009
GIETRO1967–20251889–2023
GLAERNISCH—1923–2024
GORNER—1882–2024
GRAND DESERT—1892–2024
GRAND PLAN NEVE—1893–2024
GRIES1962–20251847–2024
GRIESS (KLAUSEN)—1929–2023
GRIESSEN (OBWALDEN)—1894–2023
GROSSER ALETSCH1940–20251870–2024
HINTERSULZFIRN—1912–2024
HOHLAUB1956–20252005–2023
HOHSAAS2025–2025—
HOHWAENG1971–1977—
HUEFI—1882–2010
KALTWASSER—1891–2023
KEHLEN—1893–2024
KESSJEN-E1956–19951928–2023
LAEMMERN (WILDSTRUBEL)—1917–2024
LANG—1888–2023
LAVAZ—1882–2024
LENTA—1895–2018
LIMMERN1948–19851885–2024
LISCHANA—1895–2021
MARTINETS—1894–1992
MITTELALETSCH—1959–2023
MOIRY—1891–2024
MOMING—1879–2023
MONT DURAND—1890–2023
MONT MINE—1956–2023
MORTERATSCH, VADRET DA—1874–2024
MURTEL VADRET DAL2013–2025—
MUTT—1918–2023
OBERAAR2021–20251858–2024
OBERALETSCH—1870–2023
OBERER GRINDELWALD—1879–2024
OFENTAL—1922–1995
ORNY GLACIER D' (NO. 108)2023–20252021–2023
OTEMMA2020–20251881–2023
PALUE—1885–2024
PANEYROSSE—1886–2024
PARADIES—1873–2024
PARADISINO (CAMPO)—1955–2024
PERS, VADRET2020–2025—
PIERREDAR—1923–1995
PIZOL2007–20211893–2024
PLAINE MORTE, GLACIER DE LA2010–2025—
PLAN NEVE2025–2025—
PLATTALVA1948–19891969–2024
PLATTAS GLATSCHER DA-E2025–2025—
PORCHABELLA—1893–2024
PRAPIO—1898–2023
PUNTEGLIAS—1895–2024
RAETZLI (PLAINE MORTE)—1857–2024
RHONE1885–20251879–2024
RIED—1895–2024
ROSEG—1855–2024
ROSENLAUI—1880–1996
ROSSBODEN—1891–2023
ROTFIRN NORD—1956–2017
SALEINA—1878–2024
SANKT ANNA2012–20231867–2024
SARDONA—1895–2020
SCALETTA—1998–2020
SCHWARZ—1924–2015
SCHWARZBACH2013–2021—
SCHWARZBERG1956–20251880–2023
SEEWJINEN—2005–2023
SESVENNA—1956–2024
SEX ROUGE2012–20251898–2023
SILVRETTA1919–20251956–2024
STEIN—1893–2024
STEINLIMMI—1961–2019
SURETTA2010–20111930–2024
TAELLIBODEN—1922–1995
TIATSCHA—1850–2024
TIEFEN—1922–2024
TORTIN GLACIER DE (MONT FORT)2022–20251892–2024
TRIENT—1879–2024
TRIFT (GADMEN)—1891–2024
TSANFLEURON2010–20251884–2024
TSCHIERVA—1934–2023
TSCHINGEL—1893–2024
TSEUDET—1890–2024
TSIDJIORE NOUVE—1880–2024
TURTMANN (WEST)—1885–2024
UNTERAAR—1876–2024
UNTERER GRINDELWALD—1879–2024
VAL TORTA—1970–2011
VALLEGGIA—1971–2024
VALSOREY—1889–2024
VERSTANKLA—1926–2024
VORAB—1882–2024
WALLENBUR—1893–2024
ZINAL—1891–2023
ZMUTT—1892–2023

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.