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ESA CCI CMUG Integration Meeting , Exeter, UK 2-4 June 2014. - PowerPoint PPT Presentation
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ESA CCI CMUG Integration Meeting , Exeter, UK 2-4 June 2014The importance of observations for understanding the role of glaciers in the Earth climate system-Glaciers_cci contributions to the internationally coordinated glacier monitoring efforts
Michael Zemp
Director WGMS, PD Dr. sc. nat.
World Glacier Monitoring Service,Department of Geography, University of Zurich,Switzerland
Fiddlers Ferry coal fired power station near Liverpool, England Photograph: Phil Noble/Reuters Global climate is changing
1862Findelengletscher, Switzerland, at its Little Ice Age maximum extentso are glaciers around the globeVisualization of Findelengletscher, Zermatt, by P. Rastner
1894F.-A. Forel (1841-1912) initiates internationally coordinated glacier observations in 1894 so are glaciers around the globeVisualization of Findelengletscher, Zermatt, by P. Rastner
2010ESA Glaciers_cci Phase 1so are glaciers around the globeVisualization of Findelengletscher, Zermatt, by P. Rastner
impacts of glaciers changes on hazards, run-off, and sea levelPhotos by J. Alean.Photos by Focus Online and J. Alean.Thames Barrier. Photo from Wikimedia Commons.Male, Maledives. Photo from photos4travel.
Huss et al. (2014)intro glacier distribution glacier changes conclusionObservations are essential for- setting initial model conditions- comparing scenario ensembles with real development
Climate-glacier processes
Glacier distribution
Glacier change rates
Secondary impacts
Grand challenges in climate-glacier researchintro glacier distribution glacier changes conclusion
Internationally coordinated glacier monitoringwww.wgms.ch www.nsidc.org www.glims.org www.gtn-g.org
intro glacier distribution glacier changes conclusion
intro glacier distribution glacier changes conclusion
c. 1,000 pages of documentationbutnot (yet) much data products!
Randolph Glacier Inventoryintro glacier distribution glacier changes conclusion
Randolph Dataset 2.0
Randolph Dataset by A. Arendt et al. (2012) from different source main purpose: global SLR modelling vector outlines of different levels of detail and quality limited meta-data (e.g., time stamp, elevation range, length, classification)
How to bridge to last mile to GLIMS database?
intro glacier distribution glacier changes conclusion
How (fast) are glaciers changing? Gardner et al. (2013)intro glacier distribution glacier changes conclusion
Data sources: WGMSintro glacier distribution glacier changes conclusion
Data sources: WGMSintro glacier distribution glacier changes conclusion
Data sources: WGMS, Jacob et al. 2012intro glacier distribution glacier changes conclusion
Elevation changes from ICESat Gardner et al. (2013)intro glacier distribution glacier changes conclusion
Kb et al. (2013)Elevation changes from ICESat intro glacier distribution glacier changes conclusion
www.dlr.deFloricioiu, Jaber and Rott (2012)Opportunities:High spatial resolutionCovering entire mountain rangesChallenges:Mountain topographyHow bridging the last mile?intro glacier distribution glacier changes conclusion
Glaciers observations are a fundamental requirement for assessing climate change impacts on glacier hazards, runoff, and global sea level rise.
Growing number of remote sensing data have a great potential for boosting glacier monitoring but requires additional capacities at the international data centers to tap the full potential of these data and to truly link traditional methods with new technologies.
Thereto, the explicit focus of ESAs Glaciers_cci on monitoring is highly appreciated.
Phase 2 hopefully will produce less documentation but more data products!
intro glacier distribution glacier changes conclusion
Hintergrund: vollerz Zyklus zwischen zwei Interglazialen ca. 100,000 a fr die letzen 700,000 a; davor nur ca. 40,000 a*AR5 to be published in 2014*Changes in (a) glacier area, (b) annual runoff, (c) runoff hydrographs based on different assumitions of initial ice volume (+/-30%). Relative changes compared to glacier area in 2007 and mean runoff 1962-2010 are given in % for the year 2075.***AR5 to be published in 2014*