Using a Web Map Service to map Little Ice Age glacier extents at regional scales

Abstract Extending the record of glacier area changes into the past improves our understanding of climate change impacts. Although analogue maps showing historic glacier extents are abundant, digital outlines from before the satellite era are sparse as the digitisation of moraines and trimlines on f...

Full description

Bibliographic Details
Published in:Annals of Glaciology
Main Authors: Reinthaler, Johannes, Paul, Frank
Other Authors: European Space Agency, Horizon 2020 Framework Programme
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2023
Subjects:
Online Access:http://dx.doi.org/10.1017/aog.2023.39
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305523000393
Description
Summary:Abstract Extending the record of glacier area changes into the past improves our understanding of climate change impacts. Although analogue maps showing historic glacier extents are abundant, digital outlines from before the satellite era are sparse as the digitisation of moraines and trimlines on freely available satellite images is challenging. With the now available very high-resolution images provided by Web Map Services (WMS), new doors are open for the precise digitisation. Here, we used the ESRI WMS to digitise Little Ice Age (LIA) glacier extents and present area changes since the LIA in four selected regions along with a detailed uncertainty analysis. We used modern glacier outlines as a starting point and additionally consulted Sentinel-2 images, the ArcticDEM and historic maps for interpretation. Dating records from the literature allowed calculating area change rates. In total, 493 LIA glaciers (4640 km 2 , now 891 ice bodies with 3590 km 2 ) were digitised, yielding relative area changes of −20% (−0.14% a −1 ), −15% (−0.10% a −1 ), −26% (−0.16% a −1 ) and −61% (−0.19% a −1 ) for Alaska, Baffin Island, Novaya Zemlya and the tropics, respectively. The ESRI WMS images are a great asset to precisely map moraines and trimlines, but information about the timing of the related extents requires further sources.