How accurate are estimates of glacier ice thickness? Results from ITMIX, the Ice Thickness Models Intercomparison eXperiment
-
Published:2017-04-18
Issue:2
Volume:11
Page:949-970
-
ISSN:1994-0424
-
Container-title:The Cryosphere
-
language:en
-
Short-container-title:The Cryosphere
Author:
Farinotti DanielORCID, Brinkerhoff Douglas J., Clarke Garry K. C., Fürst Johannes J.ORCID, Frey Holger, Gantayat Prateek, Gillet-Chaulet Fabien, Girard Claire, Huss MatthiasORCID, Leclercq Paul W., Linsbauer AndreasORCID, Machguth HorstORCID, Martin CarlosORCID, Maussion FabienORCID, Morlighem MathieuORCID, Mosbeux Cyrille, Pandit Ankur, Portmann Andrea, Rabatel Antoine, Ramsankaran RAAJ, Reerink Thomas J., Sanchez Olivier, Stentoft Peter A., Singh Kumari Sangita, van Pelt Ward J. J.ORCID, Anderson Brian, Benham Toby, Binder Daniel, Dowdeswell Julian A.ORCID, Fischer Andrea, Helfricht KayORCID, Kutuzov StanislavORCID, Lavrentiev IvanORCID, McNabb RobertORCID, Gudmundsson G. HilmarORCID, Li Huilin, Andreassen Liss M.
Abstract
Abstract. Knowledge of the ice thickness distribution of glaciers and ice caps is an important prerequisite for many glaciological and hydrological investigations. A wealth of approaches has recently been presented for inferring ice thickness from characteristics of the surface. With the Ice Thickness Models Intercomparison eXperiment (ITMIX) we performed the first coordinated assessment quantifying individual model performance. A set of 17 different models showed that individual ice thickness estimates can differ considerably – locally by a spread comparable to the observed thickness. Averaging the results of multiple models, however, significantly improved the results: on average over the 21 considered test cases, comparison against direct ice thickness measurements revealed deviations on the order of 10 ± 24 % of the mean ice thickness (1σ estimate). Models relying on multiple data sets – such as surface ice velocity fields, surface mass balance, or rates of ice thickness change – showed high sensitivity to input data quality. Together with the requirement of being able to handle large regions in an automated fashion, the capacity of better accounting for uncertainties in the input data will be a key for an improved next generation of ice thickness estimation approaches.
Publisher
Copernicus GmbH
Subject
Earth-Surface Processes,Water Science and Technology
Reference86 articles.
1. Anderson, B. M., Mackintosh, A. N., Stumm, D., George, L., Kerr, T., Winter-Billington, A., and Fitzsimons, S. J.: Climate sensitivity of a high-precipitation glacier in New Zealand, J. Glaciol., 56, 114–128, https://doi.org/10.3189/002214310791190929, 2010. 2. Anderton, P. W.: Tasman Glacier 1971-73, Hydrological Research: Annual Report 33., Published by the Ministry of Works and Development for the National Water and Soil Conservation Organization of New Zealand, 1975. 3. Andreassen, L. M., Paul, F., Kääb, A., and Hausberg, J. E.: Landsat-derived glacier inventory for Jotunheimen, Norway, and deduced glacier changes since the 1930s, The Cryosphere, 2, 131–145, https://doi.org/10.5194/tc-2-131-2008, 2008. 4. Andreassen, L. M., Huss, M., Melvold, K., Elvehøy, H., and Winsvold, S. H.: Ice thickness measurements and volume estimates for glaciers in Norway, J. Glaciol., 61, 763–775, https://doi.org/10.3189/2015JoG14J161, 2015. 5. Andreassen, L. M., Elvehøy, H., Kjøllmoen, B., and Engeset, R. V.: Reanalysis of long-term series of glaciological and geodetic mass balance for 10 Norwegian glaciers, The Cryosphere, 10, 535–552, https://doi.org/10.5194/tc-10-535-2016, 2016.
Cited by
178 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
|
|