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  1. #Glims logo update#
  2. #Glims logo manual#

  • Discuss and propose a way to implement a sustainable release cycle for the various RGI products, which will depend on long-term institutional funding.
  • Automate the process of glacier attribute generation and data formatting, so that future RGI versions can be generated semi-automatically.
  • Develop tools in GLIMS to allow outline selection by date and possibly other attributes (e.g.
  • glims logo

  • Make GLIMS the single entry point to access future RGI versions.
  • The WG will have the following general objectives:

    #Glims logo update#

    In this WG, we strive to continuously improve and update the RGI, as well as to lay out a long-term plan for sustainable continuation of the RGI beyond the end of this WG. from the mid-1980s or earlier) to facilitate validation of glacier evolution models or transient mass balance calculations. Additionally, there is also a demand for consistent historic glacier outlines (e.g. Examples include data quality (wrong/outdated outlines, ice divides) but also the quality and availability of glacier attributes (hypsometry, glacier type…). Furthermore, the RGI (as of version 6) needs further improvements to remain useful to the wider scientific community. One of the main objectives of the WG is to automate this process as much as possible by incorporating RGI generation tools into the Global Land Ice Measurements from Space ( GLIMS) database.

    #Glims logo manual#

    In the past, the RGI was produced with an ad-hoc manual process, which was effective but labor-intensive. The latest RGI version (V6) was released in July 2017. After its creation in 2012, the dataset’s further development has been coordinated by an earlier IACS Working Group. It has become a pillar of glaciological research at global and regional scales, for estimates of recent and future glacier changes, glacier mass balance, and glacier contribution to sea-level rise. It was created with limited resources to meet the needs of the assessment reports of the Intergovernmental Panel on Climate Change (IPCC). The Randolph Glacier Inventory (RGI) is a globally complete collection of digital glacier outlines, excluding the polar ice sheets.

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    Har Amrit Singh Sandhu, Iestyn Barr, Etienne Berthier, Wilson Cheung, Luke Copland, Bethan Davies, Amaury Dehecq, Ankur Dixit, Kaian Fernandes, Caitlyn Florentine, Romain Hugonnet, Sam Herreid, Eñaut Izagirre, Mylène Jacquemart, Tatiana Khromova, Russia, Peter Kirchner, Jack Kohler, Lukas Krieger, Will Kochtitzky, Rohit Kumar, Johannes Landmann, Kirsty Langley, Robert McNabb, Emilio Mateo, Dan McGrath, Francisco Navarro, Ben Roberts-Pierel, Dirk Scherler, Christoph Schneider, Levan Tielidze, Hendrik Wulf Background Liss Andreassen (Norway), Tobias Bolch (UK), Nicolas Champollion (France), Matthias Dusch (Austria), Koji Fujita (Japan), Ajanta Goswami (India), Matthias Huss (Switzerland), James M Lea (UK), Akiko Sakai (Japan), Antoine Rabatel (France), David Rounce (US), David Shean (US), Thorsten Seehaus (Germany) WG contributors Michael Zemp, World Glacier Monitoring Service, Zurich, Switzerland WG members Philipp Rastner, University of Zurich, Zurich, Switzerlandīruce Raup, National Snow and Ice Data Center, Boulder, USA Regine Hock, University of Alaska Fairbanks, USA Steering Committeeįrank Paul, University of Zurich, Zurich, Switzerland Follow this wild mountain stream through the entire Val Sagliains until you reach the forest road again above the Vereina car transport station, which leads you back to Lavin via the Aua da Sagliains.Randolph Glacier Inventory (RGI) and its role in future glacier monitoring and GLIMSįabien Maussion, University of Innsbruck, Austria A small footbridge leads to the other side of the Aua da Sagliains. On the other side of the Fuorcla there is a short descent into the Val Sagliains. Between this and the Piz Glims further to the left, you can already make out the Fuorcla da Glims crossing, the highest point of the hike. Directly after the uppermost lakes, the summit of Piz Linard begins. The lakes are located in the middle of an alpine landscape and are ideal for a lunch break. The trail continues up to the Glims lakes, partly following the outflow stream of the lakes. The hut is open during the summer months. With the mighty Piz Linard, the highest peak of the Silvretta, in view, the path climbs in a pleasant gradient up to the Chamonna dal Linard. If desired, a cab can be reserved to Plan dal Bügl (see further information). The footpath crosses the forest road several times before reaching the Plan dal Bügl viewpoint. Shortly after leaving the village, a sparse forest begins. From Lavin follow the signs in the direction of Chamonna dal Linard.










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