An ~1899 glacier inventory for Nordland, northern Norway, produced from historical maps

Glaciers depicted on old maps reveal their historical extents, before the advent of aerial and satellite remote sensing. Digital glacier inventories produced from these maps can be employed in assessments of centennial-scale glacier change. This study reconstructs the ~1899 (covering the period 1882...

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Main Authors: Paul Weber, Liss M. Andreassen, Clare M. Boston, Harold Lovell, Sidsel Kvarteig
Format: Article
Language:English
Published: Cambridge University Press 2020-04-01
Series:Journal of Glaciology
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S0022143020000039/type/journal_article
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author Paul Weber
Liss M. Andreassen
Clare M. Boston
Harold Lovell
Sidsel Kvarteig
author_facet Paul Weber
Liss M. Andreassen
Clare M. Boston
Harold Lovell
Sidsel Kvarteig
author_sort Paul Weber
collection DOAJ
description Glaciers depicted on old maps reveal their historical extents, before the advent of aerial and satellite remote sensing. Digital glacier inventories produced from these maps can be employed in assessments of centennial-scale glacier change. This study reconstructs the ~1899 (covering the period 1882–1916) glacier extent in Nordland, northern Norway, from historical gradteigskart maps, with an emphasis on examining the accuracy of the mapped glaciers. Glacier outlines were digitised from georectified scans of the analogue maps in a raster graphics editor and were subsequently inventoried in a GIS. The accuracy of the historical glacier extent was established from written descriptions and landscape photographs created during the original field surveys, and further validated against independent glacier outlines of (1) the maximum Little Ice Age extent derived from geomorphological evidence, and (2) the 1945 extent derived from vertical aerial photographs. An overall uncertainty of ±17% is associated with our inventory. Nordland's glaciers covered an area of 1712 ± 291 km2 in 1899. By 2000, total ice cover had decreased by 47% (807 ± 137 km2) at a rate of 6% 10 a−1 (80 ± 14 km2 10 a−1). The approach presented here may serve as a blueprint for future studies intending to derive glacier inventories from historical maps.
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spelling doaj.art-12ad0a377b7245bbada02477e79db4dc2023-03-09T12:40:52ZengCambridge University PressJournal of Glaciology0022-14301727-56522020-04-016625927710.1017/jog.2020.3An ~1899 glacier inventory for Nordland, northern Norway, produced from historical mapsPaul Weber0https://orcid.org/0000-0002-1623-9126Liss M. Andreassen1https://orcid.org/0000-0001-6494-4252Clare M. Boston2Harold Lovell3Sidsel Kvarteig4University of Portsmouth, School of the Environment, Geography and Geosciences, Buckingham Building, Lion Terrace, PortsmouthPO1 3HE, UK Norwegian Water Resources and Energy Directorate (NVE), Oslo, NorwayNorwegian Water Resources and Energy Directorate (NVE), Oslo, NorwayUniversity of Portsmouth, School of the Environment, Geography and Geosciences, Buckingham Building, Lion Terrace, PortsmouthPO1 3HE, UKUniversity of Portsmouth, School of the Environment, Geography and Geosciences, Buckingham Building, Lion Terrace, PortsmouthPO1 3HE, UKNorwegian Mapping Authority (Kartverket), Hønefoss, NorwayGlaciers depicted on old maps reveal their historical extents, before the advent of aerial and satellite remote sensing. Digital glacier inventories produced from these maps can be employed in assessments of centennial-scale glacier change. This study reconstructs the ~1899 (covering the period 1882–1916) glacier extent in Nordland, northern Norway, from historical gradteigskart maps, with an emphasis on examining the accuracy of the mapped glaciers. Glacier outlines were digitised from georectified scans of the analogue maps in a raster graphics editor and were subsequently inventoried in a GIS. The accuracy of the historical glacier extent was established from written descriptions and landscape photographs created during the original field surveys, and further validated against independent glacier outlines of (1) the maximum Little Ice Age extent derived from geomorphological evidence, and (2) the 1945 extent derived from vertical aerial photographs. An overall uncertainty of ±17% is associated with our inventory. Nordland's glaciers covered an area of 1712 ± 291 km2 in 1899. By 2000, total ice cover had decreased by 47% (807 ± 137 km2) at a rate of 6% 10 a−1 (80 ± 14 km2 10 a−1). The approach presented here may serve as a blueprint for future studies intending to derive glacier inventories from historical maps.https://www.cambridge.org/core/product/identifier/S0022143020000039/type/journal_articleGlacier changeglacier inventoryhistorical mapsLittle Ice Agemap accuracyNordlandNorway
spellingShingle Paul Weber
Liss M. Andreassen
Clare M. Boston
Harold Lovell
Sidsel Kvarteig
An ~1899 glacier inventory for Nordland, northern Norway, produced from historical maps
Journal of Glaciology
Glacier change
glacier inventory
historical maps
Little Ice Age
map accuracy
Nordland
Norway
title An ~1899 glacier inventory for Nordland, northern Norway, produced from historical maps
title_full An ~1899 glacier inventory for Nordland, northern Norway, produced from historical maps
title_fullStr An ~1899 glacier inventory for Nordland, northern Norway, produced from historical maps
title_full_unstemmed An ~1899 glacier inventory for Nordland, northern Norway, produced from historical maps
title_short An ~1899 glacier inventory for Nordland, northern Norway, produced from historical maps
title_sort 1899 glacier inventory for nordland northern norway produced from historical maps
topic Glacier change
glacier inventory
historical maps
Little Ice Age
map accuracy
Nordland
Norway
url https://www.cambridge.org/core/product/identifier/S0022143020000039/type/journal_article
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