Climate variability during the last 1000 years inferred from Andean ice cores : a review of methodology and recent results

Andean ice core investigations began approximately 30 years ago. Today, 10 drilling sites, from 0 degrees to 52 degrees S, have been explored for paleoclimate reconstructions. Most of the ice cores reaching the bedrock cover the last 20,000 years with seasonal resolution over the last few centuries...

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Main Authors: Vimeux, Françoise, Ginot, Patrick, Schwikowski, M., Vuille, M., Hoffmann, G., Thompson, L. G., Schotterer, U.
Format: Text
Language:English
Published: 2009
Subjects:
Online Access:http://www.documentation.ird.fr/hor/fdi:010048376
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spelling ftird:oai:ird.fr:fdi:010048376 2023-05-15T16:39:13+02:00 Climate variability during the last 1000 years inferred from Andean ice cores : a review of methodology and recent results Vimeux, Françoise Ginot, Patrick Schwikowski, M. Vuille, M. Hoffmann, G. Thompson, L. G. Schotterer, U. 2009 http://www.documentation.ird.fr/hor/fdi:010048376 EN eng http://www.documentation.ird.fr/hor/fdi:010048376 oai:ird.fr:fdi:010048376 Vimeux Françoise, Ginot Patrick, Schwikowski M., Vuille M., Hoffmann G., Thompson L. G., Schotterer U. Climate variability during the last 1000 years inferred from Andean ice cores : a review of methodology and recent results. Palaeogeography Palaeoclimatology Palaeoecology, 2009, 281 (3-4), p. 229-241. Andean ice cores South American high-altitude climate Last millennium Andean Isotopic Index Little Ice Age ENSO text 2009 ftird 2020-08-21T06:57:50Z Andean ice core investigations began approximately 30 years ago. Today, 10 drilling sites, from 0 degrees to 52 degrees S, have been explored for paleoclimate reconstructions. Most of the ice cores reaching the bedrock cover the last 20,000 years with seasonal resolution over the last few centuries to the last 1000 years for the Quelccaya site. We discuss both the potential and the limitations of tropical ice cores as climate archives with regard to the collaborative effort to reconstruct past climate variations in South America over the last 1000 years. We point out the uniqueness of South American ice cores, due to their location at high altitude, and also their two main limitations, which are related to (i) the interpretation of certain proxies in terms of climate and (ii) the relatively poordating when seasonal cycles are no longer resolved. In addition, we present an overview of the proxies that have been used so far to analyze tropical climate dynamics. Finally we discuss records of ENSO, the Little Ice Age and the 20th century decadal variability including the anthropogenic period, which are all preserved in ice cores. Text ice core IRD (Institute de recherche pour le développement): Horizon
institution Open Polar
collection IRD (Institute de recherche pour le développement): Horizon
op_collection_id ftird
language English
topic Andean ice cores
South American high-altitude climate
Last millennium
Andean Isotopic Index
Little Ice Age
ENSO
spellingShingle Andean ice cores
South American high-altitude climate
Last millennium
Andean Isotopic Index
Little Ice Age
ENSO
Vimeux, Françoise
Ginot, Patrick
Schwikowski, M.
Vuille, M.
Hoffmann, G.
Thompson, L. G.
Schotterer, U.
Climate variability during the last 1000 years inferred from Andean ice cores : a review of methodology and recent results
topic_facet Andean ice cores
South American high-altitude climate
Last millennium
Andean Isotopic Index
Little Ice Age
ENSO
description Andean ice core investigations began approximately 30 years ago. Today, 10 drilling sites, from 0 degrees to 52 degrees S, have been explored for paleoclimate reconstructions. Most of the ice cores reaching the bedrock cover the last 20,000 years with seasonal resolution over the last few centuries to the last 1000 years for the Quelccaya site. We discuss both the potential and the limitations of tropical ice cores as climate archives with regard to the collaborative effort to reconstruct past climate variations in South America over the last 1000 years. We point out the uniqueness of South American ice cores, due to their location at high altitude, and also their two main limitations, which are related to (i) the interpretation of certain proxies in terms of climate and (ii) the relatively poordating when seasonal cycles are no longer resolved. In addition, we present an overview of the proxies that have been used so far to analyze tropical climate dynamics. Finally we discuss records of ENSO, the Little Ice Age and the 20th century decadal variability including the anthropogenic period, which are all preserved in ice cores.
format Text
author Vimeux, Françoise
Ginot, Patrick
Schwikowski, M.
Vuille, M.
Hoffmann, G.
Thompson, L. G.
Schotterer, U.
author_facet Vimeux, Françoise
Ginot, Patrick
Schwikowski, M.
Vuille, M.
Hoffmann, G.
Thompson, L. G.
Schotterer, U.
author_sort Vimeux, Françoise
title Climate variability during the last 1000 years inferred from Andean ice cores : a review of methodology and recent results
title_short Climate variability during the last 1000 years inferred from Andean ice cores : a review of methodology and recent results
title_full Climate variability during the last 1000 years inferred from Andean ice cores : a review of methodology and recent results
title_fullStr Climate variability during the last 1000 years inferred from Andean ice cores : a review of methodology and recent results
title_full_unstemmed Climate variability during the last 1000 years inferred from Andean ice cores : a review of methodology and recent results
title_sort climate variability during the last 1000 years inferred from andean ice cores : a review of methodology and recent results
publishDate 2009
url http://www.documentation.ird.fr/hor/fdi:010048376
genre ice core
genre_facet ice core
op_relation http://www.documentation.ird.fr/hor/fdi:010048376
oai:ird.fr:fdi:010048376
Vimeux Françoise, Ginot Patrick, Schwikowski M., Vuille M., Hoffmann G., Thompson L. G., Schotterer U. Climate variability during the last 1000 years inferred from Andean ice cores : a review of methodology and recent results. Palaeogeography Palaeoclimatology Palaeoecology, 2009, 281 (3-4), p. 229-241.
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