Western European climate, and Pinot noir grape harvest dates in Burgundy, France, since the 17th century

Time-series of growing season air temperature anomalies in the Parisian region and of Pinot noir grape harvest dates (GHD) in Burgundy (1676-2004) are analyzed in the frequency domain. Variability of both time-series display 3 significant frequency-bands (peaks significant at the 5% level): (1) a lo...

Full description

Bibliographic Details
Main Authors: Tourre, Y. M., Rousseau, D., Jarlan, Lionel, Ladurie, E. L., Daux, V.
Format: Text
Language:English
Published: 2011
Subjects:
GHD
Online Access:http://www.documentation.ird.fr/hor/fdi:010053571
id ftird:oai:ird.fr:fdi:010053571
record_format openpolar
spelling ftird:oai:ird.fr:fdi:010053571 2023-05-15T17:35:34+02:00 Western European climate, and Pinot noir grape harvest dates in Burgundy, France, since the 17th century Tourre, Y. M. Rousseau, D. Jarlan, Lionel Ladurie, E. L. Daux, V. 2011 http://www.documentation.ird.fr/hor/fdi:010053571 EN eng http://www.documentation.ird.fr/hor/fdi:010053571 oai:ird.fr:fdi:010053571 Tourre Y. M., Rousseau D., Jarlan Lionel, Ladurie E. L., Daux V. Western European climate, and Pinot noir grape harvest dates in Burgundy, France, since the 17th century. Climate Research, 2011, 46 (3), p. 243-253. Western European climate variability Climate change Grape harvest dates Pinot noir Burgundy GHD text 2011 ftird 2020-08-21T06:56:20Z Time-series of growing season air temperature anomalies in the Parisian region and of Pinot noir grape harvest dates (GHD) in Burgundy (1676-2004) are analyzed in the frequency domain. Variability of both time-series display 3 significant frequency-bands (peaks significant at the 5% level): (1) a low-frequency-band (multi-decadal) with a 25 yr peak period, (2) a 3 to 8 yr band period (inter-annual) with a 3.1 yr peak period, and (3) a 2 to 3 yr band period (quasi-biennial) with a 2.4 yr peak period. Joint sea surface temperature/sea level pressure (SST/SLP) EOF analyses based on data from the 20th century along with spatio-temporal patterns for the above frequency-bands, are presented. SST anomalies were found to display early significant spatial SST patterns in the north Atlantic ocean (air temperature lagging by 6 mo) similar to those obtained from EOF analyses. It is proposed that the robust power spectra for the above frequency-bands are linked with Atlantic climate variability modulating western European climate: (1) the global Multi-Decadal Oscillation (MDO) with its Atlantic Multi-decadal Oscillation (AMO) footprint, (2) the Atlantic Inter-Annual (IA) fluctuations, and (3) the Atlantic Quasi-Biennial (QB) fluctuations. Moreover these specific western European climate signals are perceived as contributors to the timing of GHD in Burgundy. Thus, advance knowledge on the evolution and phasing of the above climate fluctuations become important elements for viticulture and wine industry management, since anthropogenic effects could have modified time-series patterns, particularly since the mid-1980s. Text North Atlantic 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 Western European climate variability
Climate change
Grape harvest
dates
Pinot noir
Burgundy
GHD
spellingShingle Western European climate variability
Climate change
Grape harvest
dates
Pinot noir
Burgundy
GHD
Tourre, Y. M.
Rousseau, D.
Jarlan, Lionel
Ladurie, E. L.
Daux, V.
Western European climate, and Pinot noir grape harvest dates in Burgundy, France, since the 17th century
topic_facet Western European climate variability
Climate change
Grape harvest
dates
Pinot noir
Burgundy
GHD
description Time-series of growing season air temperature anomalies in the Parisian region and of Pinot noir grape harvest dates (GHD) in Burgundy (1676-2004) are analyzed in the frequency domain. Variability of both time-series display 3 significant frequency-bands (peaks significant at the 5% level): (1) a low-frequency-band (multi-decadal) with a 25 yr peak period, (2) a 3 to 8 yr band period (inter-annual) with a 3.1 yr peak period, and (3) a 2 to 3 yr band period (quasi-biennial) with a 2.4 yr peak period. Joint sea surface temperature/sea level pressure (SST/SLP) EOF analyses based on data from the 20th century along with spatio-temporal patterns for the above frequency-bands, are presented. SST anomalies were found to display early significant spatial SST patterns in the north Atlantic ocean (air temperature lagging by 6 mo) similar to those obtained from EOF analyses. It is proposed that the robust power spectra for the above frequency-bands are linked with Atlantic climate variability modulating western European climate: (1) the global Multi-Decadal Oscillation (MDO) with its Atlantic Multi-decadal Oscillation (AMO) footprint, (2) the Atlantic Inter-Annual (IA) fluctuations, and (3) the Atlantic Quasi-Biennial (QB) fluctuations. Moreover these specific western European climate signals are perceived as contributors to the timing of GHD in Burgundy. Thus, advance knowledge on the evolution and phasing of the above climate fluctuations become important elements for viticulture and wine industry management, since anthropogenic effects could have modified time-series patterns, particularly since the mid-1980s.
format Text
author Tourre, Y. M.
Rousseau, D.
Jarlan, Lionel
Ladurie, E. L.
Daux, V.
author_facet Tourre, Y. M.
Rousseau, D.
Jarlan, Lionel
Ladurie, E. L.
Daux, V.
author_sort Tourre, Y. M.
title Western European climate, and Pinot noir grape harvest dates in Burgundy, France, since the 17th century
title_short Western European climate, and Pinot noir grape harvest dates in Burgundy, France, since the 17th century
title_full Western European climate, and Pinot noir grape harvest dates in Burgundy, France, since the 17th century
title_fullStr Western European climate, and Pinot noir grape harvest dates in Burgundy, France, since the 17th century
title_full_unstemmed Western European climate, and Pinot noir grape harvest dates in Burgundy, France, since the 17th century
title_sort western european climate, and pinot noir grape harvest dates in burgundy, france, since the 17th century
publishDate 2011
url http://www.documentation.ird.fr/hor/fdi:010053571
genre North Atlantic
genre_facet North Atlantic
op_relation http://www.documentation.ird.fr/hor/fdi:010053571
oai:ird.fr:fdi:010053571
Tourre Y. M., Rousseau D., Jarlan Lionel, Ladurie E. L., Daux V. Western European climate, and Pinot noir grape harvest dates in Burgundy, France, since the 17th century. Climate Research, 2011, 46 (3), p. 243-253.
_version_ 1766134765349502976