Multi-century tree-ring based reconstruction of the Neuquén River streamflow, northern Patagonia, Argentina

In most cases, gauged river flow records in southern South America extend for only a few decades, hampering the detection of long-term, decadal to centennial-scale cycles and trends. Long streamflow series can be reconstructed from tree-ring records, offering the opportunity of extending the limited...

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Main Authors: I. A. Mundo, M. H. Masiokas, R. Villalba, M. S. Morales, R. Neukom, C. Le Quesne, R. B. Urrutia, A. Lara
Format: Article
Language:English
Published: Copernicus Publications 2012-04-01
Series:Climate of the Past
Online Access:http://www.clim-past.net/8/815/2012/cp-8-815-2012.pdf
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author I. A. Mundo
M. H. Masiokas
R. Villalba
M. S. Morales
R. Neukom
C. Le Quesne
R. B. Urrutia
A. Lara
author_facet I. A. Mundo
M. H. Masiokas
R. Villalba
M. S. Morales
R. Neukom
C. Le Quesne
R. B. Urrutia
A. Lara
author_sort I. A. Mundo
collection DOAJ
description In most cases, gauged river flow records in southern South America extend for only a few decades, hampering the detection of long-term, decadal to centennial-scale cycles and trends. Long streamflow series can be reconstructed from tree-ring records, offering the opportunity of extending the limited hydrological instrumental data to several centuries. In northern Patagonia, Argentina, the Neuquén River has great importance for local and national socio-economic activities such as hydroelectric power generation, agriculture and tourism. In this study, new and updated tree-ring chronologies from <i>Araucaria araucana</i> and <i>Austrocedrus chilensis</i> are used to reconstruct the October–June mean streamflow for the Neuquén River and place the period of gauged flows (1903–2009), in a long-term, multi-century context. The reconstruction covers the period 1346–2000 AD and was developed from a network of 43 tree-ring chronologies, grouped in composite series, using a nested principal component regression approach. Analyses of the frequency, intensity, and duration of droughts and pluvial events indicate that the 20th century contains some of the driest and wettest annual to decadal-scale events in the last 654 yr, but longer and more severe events were recorded in previous centuries. Blackman-Tukey and singular spectral analyses identified quasiperiodic oscillations from 3.5 to 17.5 yr. A dominant 6.8-yr cycle explains ca. 23.6% of the total variance in the Neuquén River streamflow reconstruction. Correlation analyses showed that discharges of the Neuquén River are related to variations in the Southern Annular Mode (SAM), a measure of air mass exchanges between middle and high latitudes in the Southern Hemisphere. This association is consistent with previous studies that indicate a strong correlation between rainfall in northern Patagonia and SAM variations.
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spelling doaj.art-7b60492e1af747a2a2b6f6b0304660fc2022-12-21T21:01:00ZengCopernicus PublicationsClimate of the Past1814-93241814-93322012-04-018281582910.5194/cp-8-815-2012Multi-century tree-ring based reconstruction of the Neuquén River streamflow, northern Patagonia, ArgentinaI. A. MundoM. H. MasiokasR. VillalbaM. S. MoralesR. NeukomC. Le QuesneR. B. UrrutiaA. LaraIn most cases, gauged river flow records in southern South America extend for only a few decades, hampering the detection of long-term, decadal to centennial-scale cycles and trends. Long streamflow series can be reconstructed from tree-ring records, offering the opportunity of extending the limited hydrological instrumental data to several centuries. In northern Patagonia, Argentina, the Neuquén River has great importance for local and national socio-economic activities such as hydroelectric power generation, agriculture and tourism. In this study, new and updated tree-ring chronologies from <i>Araucaria araucana</i> and <i>Austrocedrus chilensis</i> are used to reconstruct the October–June mean streamflow for the Neuquén River and place the period of gauged flows (1903–2009), in a long-term, multi-century context. The reconstruction covers the period 1346–2000 AD and was developed from a network of 43 tree-ring chronologies, grouped in composite series, using a nested principal component regression approach. Analyses of the frequency, intensity, and duration of droughts and pluvial events indicate that the 20th century contains some of the driest and wettest annual to decadal-scale events in the last 654 yr, but longer and more severe events were recorded in previous centuries. Blackman-Tukey and singular spectral analyses identified quasiperiodic oscillations from 3.5 to 17.5 yr. A dominant 6.8-yr cycle explains ca. 23.6% of the total variance in the Neuquén River streamflow reconstruction. Correlation analyses showed that discharges of the Neuquén River are related to variations in the Southern Annular Mode (SAM), a measure of air mass exchanges between middle and high latitudes in the Southern Hemisphere. This association is consistent with previous studies that indicate a strong correlation between rainfall in northern Patagonia and SAM variations.http://www.clim-past.net/8/815/2012/cp-8-815-2012.pdf
spellingShingle I. A. Mundo
M. H. Masiokas
R. Villalba
M. S. Morales
R. Neukom
C. Le Quesne
R. B. Urrutia
A. Lara
Multi-century tree-ring based reconstruction of the Neuquén River streamflow, northern Patagonia, Argentina
Climate of the Past
title Multi-century tree-ring based reconstruction of the Neuquén River streamflow, northern Patagonia, Argentina
title_full Multi-century tree-ring based reconstruction of the Neuquén River streamflow, northern Patagonia, Argentina
title_fullStr Multi-century tree-ring based reconstruction of the Neuquén River streamflow, northern Patagonia, Argentina
title_full_unstemmed Multi-century tree-ring based reconstruction of the Neuquén River streamflow, northern Patagonia, Argentina
title_short Multi-century tree-ring based reconstruction of the Neuquén River streamflow, northern Patagonia, Argentina
title_sort multi century tree ring based reconstruction of the neuquen river streamflow northern patagonia argentina
url http://www.clim-past.net/8/815/2012/cp-8-815-2012.pdf
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