Little Ice Age glacier extension and retreat in Spitsbergen Island (High Arctic, Svalbard Archipelago)

The influence of the Little Ice Age on the glaciers of Spitsbergen has been well documented by many investigations since long time. This paper studies, measures and presents new data on the Little Ice Age maximum glacier extension and retreat by aerial photo interpretation and Geographic Information...

Full description

Bibliographic Details
Published in:Cuadernos de Investigación Geográfica
Main Authors: Martín-Moreno, Raúl, Allende-Álvarez, Fernando
Format: Article in Journal/Newspaper
Language:English
Published: Universidad de La Rioja 2016
Subjects:
GIS
SIG
Online Access:https://publicaciones.unirioja.es/ojs/index.php/cig/article/view/2919
https://doi.org/10.18172/cig.2919
id ftunivriojaojs:oai:ojs.www.unirioja.es:article/2919
record_format openpolar
spelling ftunivriojaojs:oai:ojs.www.unirioja.es:article/2919 2023-05-15T14:29:03+02:00 Little Ice Age glacier extension and retreat in Spitsbergen Island (High Arctic, Svalbard Archipelago) Extensión y retroceso glaciar durante la Pequeña Edad del Hielo en Spitsbergen (Alto Ártico, archipiélago de Svalbard) Martín-Moreno, Raúl Allende-Álvarez, Fernando 2016-09-13 application/pdf https://publicaciones.unirioja.es/ojs/index.php/cig/article/view/2919 https://doi.org/10.18172/cig.2919 eng eng Universidad de La Rioja https://publicaciones.unirioja.es/ojs/index.php/cig/article/view/2919/2700 https://publicaciones.unirioja.es/ojs/index.php/cig/article/view/2919 doi:10.18172/cig.2919 Copyright (c) 2016 Raúl Martín-Moreno, Fernando Allende-Álvarez https://creativecommons.org/licenses/by/4.0 CC-BY Cuadernos de Investigación Geográfica; Vol. 42, Núm. 2 (2016); 383-398 1697-9540 0211-6820 10.18172/cig.vol42iss2 glacier retreat aerial photo interpretation GIS Little Ice Age Spitsbergen retroceso glaciar fotointerpretación SIG Pequeña Edad del Hielo info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2016 ftunivriojaojs https://doi.org/10.18172/cig.2919 https://doi.org/10.18172/cig.vol42iss2 2022-08-25T09:49:05Z The influence of the Little Ice Age on the glaciers of Spitsbergen has been well documented by many investigations since long time. This paper studies, measures and presents new data on the Little Ice Age maximum glacier extension and retreat by aerial photo interpretation and Geographic Information Systems (GIS) tools use. It also elaborates cartography where all the results are expressed in greater detail. During the LIA maximum the Island of Spitsbergen was covered with a 7.34% more of ice than today. After the Little Ice Age, the total glacier area loss was 13.84%, which means a total of 2769.8 Km2 over the 20,008.7 Km2 of the total glaciated in the current context. The analysis of the maximum Little Ice Age glacier extension in the major drainage basins brings important differences among them; hardly 100 years ago some basin drainage increased the glacier area more than 24% (in the western and central region of Spitsbergen), while others less than 5% (in the northeast region of the Island). The greatest retreats are found in the tidewater glaciers that extend into the sea, which we explain due to different factors: their glacier front beds are found below the sea level, the intense ablation of the calving process, the fact that their tidewater fronts are thin and temperate (which make them more dynamic and very sensitive to climate fluctuations), and that the advances of these glaciers may correspond with surges, which means that the rapid retreats are motivated by the post-surging phases as well. The conclusions of the present research point out a very important ice loss in the whole Island since the Little Ice Age, and the high vulnerability of this Arctic Archipelago to global warming. El alcance de la Pequeña Edad del Hielo (PEH) en los glaciares de Spitsbergen ha sido bien documentada desde antiguo por numerosas investigaciones. El presente artículo estudia, cuantifica, y presenta nuevos datos sobre la extensión máxima y retroceso glaciar desde la Pequeña Edad del Hielo a partir del uso de ... Article in Journal/Newspaper Arctic Archipelago Arctic glacier Global warming Svalbard Tidewater Spitsbergen Portal de Revistas de la Universidad de La Rioja Arctic Hielo ENVELOPE(-58.133,-58.133,-62.083,-62.083) Pequeña ENVELOPE(-61.455,-61.455,-64.012,-64.012) Svalbard Svalbard Archipelago Cuadernos de Investigación Geográfica 42 2 383 398
institution Open Polar
collection Portal de Revistas de la Universidad de La Rioja
op_collection_id ftunivriojaojs
language English
topic glacier retreat
aerial photo interpretation
GIS
Little Ice Age
Spitsbergen
retroceso glaciar
fotointerpretación
SIG
Pequeña Edad del Hielo
spellingShingle glacier retreat
aerial photo interpretation
GIS
Little Ice Age
Spitsbergen
retroceso glaciar
fotointerpretación
SIG
Pequeña Edad del Hielo
Martín-Moreno, Raúl
Allende-Álvarez, Fernando
Little Ice Age glacier extension and retreat in Spitsbergen Island (High Arctic, Svalbard Archipelago)
topic_facet glacier retreat
aerial photo interpretation
GIS
Little Ice Age
Spitsbergen
retroceso glaciar
fotointerpretación
SIG
Pequeña Edad del Hielo
description The influence of the Little Ice Age on the glaciers of Spitsbergen has been well documented by many investigations since long time. This paper studies, measures and presents new data on the Little Ice Age maximum glacier extension and retreat by aerial photo interpretation and Geographic Information Systems (GIS) tools use. It also elaborates cartography where all the results are expressed in greater detail. During the LIA maximum the Island of Spitsbergen was covered with a 7.34% more of ice than today. After the Little Ice Age, the total glacier area loss was 13.84%, which means a total of 2769.8 Km2 over the 20,008.7 Km2 of the total glaciated in the current context. The analysis of the maximum Little Ice Age glacier extension in the major drainage basins brings important differences among them; hardly 100 years ago some basin drainage increased the glacier area more than 24% (in the western and central region of Spitsbergen), while others less than 5% (in the northeast region of the Island). The greatest retreats are found in the tidewater glaciers that extend into the sea, which we explain due to different factors: their glacier front beds are found below the sea level, the intense ablation of the calving process, the fact that their tidewater fronts are thin and temperate (which make them more dynamic and very sensitive to climate fluctuations), and that the advances of these glaciers may correspond with surges, which means that the rapid retreats are motivated by the post-surging phases as well. The conclusions of the present research point out a very important ice loss in the whole Island since the Little Ice Age, and the high vulnerability of this Arctic Archipelago to global warming. El alcance de la Pequeña Edad del Hielo (PEH) en los glaciares de Spitsbergen ha sido bien documentada desde antiguo por numerosas investigaciones. El presente artículo estudia, cuantifica, y presenta nuevos datos sobre la extensión máxima y retroceso glaciar desde la Pequeña Edad del Hielo a partir del uso de ...
format Article in Journal/Newspaper
author Martín-Moreno, Raúl
Allende-Álvarez, Fernando
author_facet Martín-Moreno, Raúl
Allende-Álvarez, Fernando
author_sort Martín-Moreno, Raúl
title Little Ice Age glacier extension and retreat in Spitsbergen Island (High Arctic, Svalbard Archipelago)
title_short Little Ice Age glacier extension and retreat in Spitsbergen Island (High Arctic, Svalbard Archipelago)
title_full Little Ice Age glacier extension and retreat in Spitsbergen Island (High Arctic, Svalbard Archipelago)
title_fullStr Little Ice Age glacier extension and retreat in Spitsbergen Island (High Arctic, Svalbard Archipelago)
title_full_unstemmed Little Ice Age glacier extension and retreat in Spitsbergen Island (High Arctic, Svalbard Archipelago)
title_sort little ice age glacier extension and retreat in spitsbergen island (high arctic, svalbard archipelago)
publisher Universidad de La Rioja
publishDate 2016
url https://publicaciones.unirioja.es/ojs/index.php/cig/article/view/2919
https://doi.org/10.18172/cig.2919
long_lat ENVELOPE(-58.133,-58.133,-62.083,-62.083)
ENVELOPE(-61.455,-61.455,-64.012,-64.012)
geographic Arctic
Hielo
Pequeña
Svalbard
Svalbard Archipelago
geographic_facet Arctic
Hielo
Pequeña
Svalbard
Svalbard Archipelago
genre Arctic Archipelago
Arctic
glacier
Global warming
Svalbard
Tidewater
Spitsbergen
genre_facet Arctic Archipelago
Arctic
glacier
Global warming
Svalbard
Tidewater
Spitsbergen
op_source Cuadernos de Investigación Geográfica; Vol. 42, Núm. 2 (2016); 383-398
1697-9540
0211-6820
10.18172/cig.vol42iss2
op_relation https://publicaciones.unirioja.es/ojs/index.php/cig/article/view/2919/2700
https://publicaciones.unirioja.es/ojs/index.php/cig/article/view/2919
doi:10.18172/cig.2919
op_rights Copyright (c) 2016 Raúl Martín-Moreno, Fernando Allende-Álvarez
https://creativecommons.org/licenses/by/4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.18172/cig.2919
https://doi.org/10.18172/cig.vol42iss2
container_title Cuadernos de Investigación Geográfica
container_volume 42
container_issue 2
container_start_page 383
op_container_end_page 398
_version_ 1766303146786684928