Publication

Numerical simulation of Rhonegletscher from 1874 to 2100

Jacques Rappaz, Marco Picasso, Guillaume Jouvet, Heinz Blatter
2009
Journal Articles

Abstract

Due to climatic change, many Alpine glaciers have significantly retreated during the last century. In this study we perform the numerical simulation of the temporal and spatial change of Rhonegletscher, Swiss Alps, from 1874 to 2007, and from 2007 to 2100.

Official source

https://infoscience.epfl.ch/entities/publication/dc65c38e-7cb2-4529-a533-cbbd4c8856e3

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Jacques Rappaz, Marco Picasso, Guillaume Jouvet, Heinz Blatter
2009
Journal Articles

Abstract

Official source

https://infoscience.epfl.ch/entities/publication/dc65c38e-7cb2-4529-a533-cbbd4c8856e3

About this result

Related concepts (19)

Alps

The Alps (ælps) are the highest and most extensive mountain range that is entirely in Europe, stretching approximately across eight Alpine countries (from west to east): Monaco, France, Switzerland, Italy, Liechtenstein, Germany, Slovenia, and Austria. The Alpine arch extends from Nice on the western Mediterranean to Trieste on the Adriatic and Vienna at the beginning of the Pannonian Basin. The mountains were formed over tens of millions of years as the African and Eurasian tectonic plates collided.

Swiss Alps

The Alpine region of Switzerland, conventionally referred to as the Swiss Alps (Schweizer Alpen, Alpes suisses, Alpi svizzere, Alps svizras), represents a major natural feature of the country and is, along with the Swiss Plateau and the Swiss portion of the Jura Mountains, one of its three main physiographic regions. The Swiss Alps extend over both the Western Alps and the Eastern Alps, encompassing an area sometimes called Central Alps.

Glacier

A glacier (USpronˈɡleɪʃər; UKˈɡlæsiər,_ˈgleɪsiər) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords.

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