Strong volcanic-induced climatic shocks on historical Moselle wine production

<p>In central and southern Europe, grapevine is a climate-sensitive agricultural product of great economic importance, both in historical times and today. We systematically investigated the climatic impact, focusing on volcanic-forced abrupt cooling, on two long annual records of wine producti...

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Main Authors: F. C. Ljungqvist, B. Christiansen, L. Schneider, P. Thejll
Format: Article
Language:English
Published: Copernicus Publications 2025-02-01
Series:Climate of the Past
Online Access:https://cp.copernicus.org/articles/21/327/2025/cp-21-327-2025.pdf
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author F. C. Ljungqvist
F. C. Ljungqvist
F. C. Ljungqvist
B. Christiansen
L. Schneider
L. Schneider
P. Thejll
author_facet F. C. Ljungqvist
F. C. Ljungqvist
F. C. Ljungqvist
B. Christiansen
L. Schneider
L. Schneider
P. Thejll
author_sort F. C. Ljungqvist
collection DOAJ
description <p>In central and southern Europe, grapevine is a climate-sensitive agricultural product of great economic importance, both in historical times and today. We systematically investigated the climatic impact, focusing on volcanic-forced abrupt cooling, on two long annual records of wine production quantity (spanning 1444–1786) from the Moselle Valley in present-day Luxembourg, close to the northern limit of viticulture in Europe. We present a consistent picture of the impact of volcanic eruptions on wine production through climate. To this end, we applied superposed epoch analysis – an appropriate method for detecting episodic signals in non-stationary time series – in combination with a bootstrap procedure to estimate the statistical significance. We also assessed the long-term relationship between different annual and seasonal climate parameters and wine production in the Moselle Valley. Robust and highly significant wine production declines occurred in the years immediately following major volcanic events. Warmer and, to a lesser extent, drier climate conditions had a moderately strong, but persistent, positive effect on wine production. We also find a volcanic cooling signature in spring and summer in temperature reconstructions. However, the detected volcanic signature in the Moselle Valley wine production is considerably stronger than the one found for central Europe in tree-ring-based reconstructions and is instead more akin to the strong volcanic signature present in Fennoscandian tree-ring series. On the basis of our findings, we encourage further compilation, publication, and analyses of additional wine production series containing unique biological and climatic information.</p>
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spelling doaj-art-b1216f1885b042d6bf230ff611aa9e4d2025-02-03T05:11:38ZengCopernicus PublicationsClimate of the Past1814-93241814-93322025-02-012132734210.5194/cp-21-327-2025Strong volcanic-induced climatic shocks on historical Moselle wine productionF. C. Ljungqvist0F. C. Ljungqvist1F. C. Ljungqvist2B. Christiansen3L. Schneider4L. Schneider5P. Thejll6Department of History, Stockholm University, 106 91 Stockholm, SwedenBolin Centre for Climate Research, Stockholm University, 106 91 Stockholm, SwedenSwedish Collegium for Advanced Study, Linneanum, Villavägen 6c, 752 36 Uppsala, SwedenDanish Meteorological Institute, Sankt Kjelds Plads 11, 2100 Copenhagen Ø, DenmarkDepartment of Geography, Justus-Liebig-University, 35390 Giessen, GermanyCenter for international Development and Environmental Research, Justus-Liebig-University, 35390 Giessen, GermanyDanish Meteorological Institute, Sankt Kjelds Plads 11, 2100 Copenhagen Ø, Denmark<p>In central and southern Europe, grapevine is a climate-sensitive agricultural product of great economic importance, both in historical times and today. We systematically investigated the climatic impact, focusing on volcanic-forced abrupt cooling, on two long annual records of wine production quantity (spanning 1444–1786) from the Moselle Valley in present-day Luxembourg, close to the northern limit of viticulture in Europe. We present a consistent picture of the impact of volcanic eruptions on wine production through climate. To this end, we applied superposed epoch analysis – an appropriate method for detecting episodic signals in non-stationary time series – in combination with a bootstrap procedure to estimate the statistical significance. We also assessed the long-term relationship between different annual and seasonal climate parameters and wine production in the Moselle Valley. Robust and highly significant wine production declines occurred in the years immediately following major volcanic events. Warmer and, to a lesser extent, drier climate conditions had a moderately strong, but persistent, positive effect on wine production. We also find a volcanic cooling signature in spring and summer in temperature reconstructions. However, the detected volcanic signature in the Moselle Valley wine production is considerably stronger than the one found for central Europe in tree-ring-based reconstructions and is instead more akin to the strong volcanic signature present in Fennoscandian tree-ring series. On the basis of our findings, we encourage further compilation, publication, and analyses of additional wine production series containing unique biological and climatic information.</p>https://cp.copernicus.org/articles/21/327/2025/cp-21-327-2025.pdf
spellingShingle F. C. Ljungqvist
F. C. Ljungqvist
F. C. Ljungqvist
B. Christiansen
L. Schneider
L. Schneider
P. Thejll
Strong volcanic-induced climatic shocks on historical Moselle wine production
Climate of the Past
title Strong volcanic-induced climatic shocks on historical Moselle wine production
title_full Strong volcanic-induced climatic shocks on historical Moselle wine production
title_fullStr Strong volcanic-induced climatic shocks on historical Moselle wine production
title_full_unstemmed Strong volcanic-induced climatic shocks on historical Moselle wine production
title_short Strong volcanic-induced climatic shocks on historical Moselle wine production
title_sort strong volcanic induced climatic shocks on historical moselle wine production
url https://cp.copernicus.org/articles/21/327/2025/cp-21-327-2025.pdf
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