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• W2314277830 abstract "CR Climate Research Contact the journal Facebook Twitter RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout the JournalEditorsSpecials CR 46:243-253 (2011) - DOI: https://doi.org/10.3354/cr00991 Western European climate, and Pinot noir grape harvest dates in Burgundy, France, since the 17th century Yves M. Tourre1,2,*, Daniel Rousseau3, Lionel Jarlan4, Emmanuel Le Roy Ladurie5, Valérie Daux6 1Météo-France, 31057 Toulouse, France 2Lamont-Doherty Earth Observatory (LDEO) of Columbia University, 10964-1707 Palisades, New York, USA 3Conseil Supérieur de la Météorologie, 31057 Toulouse, France 4Institut de Recherches pour le Développement/Centre d’Etudes Spatiales de la BIOsphère (IRD/CESBIO), 31401 Toulouse, France 5Collège de France, 75005 Paris, France 6Laboratoire des Sciences du Climat et de l’Environnement (LSCE), 91191 Gif-sur-Yvette, France *Email: yvestourre@aol.com ABSTRACT: 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. KEY WORDS: Western European climate variability · Climate change · Grape harvest dates · Pinot noir · Burgundy · GHD Full text in pdf format PreviousNextCite this article as: Tourre YM, Rousseau D, Jarlan L, Le Roy Ladurie E, Daux V (2011) Western European climate, and Pinot noir grape harvest dates in Burgundy, France, since the 17th century. Clim Res 46:243-253. https://doi.org/10.3354/cr00991 Export citation RSS - Facebook - Tweet - linkedIn Cited by Published in CR Vol. 46, No. 3. Online publication date: April 28, 2011 Print ISSN: 0936-577X; Online ISSN: 1616-1572 Copyright © 2011 Inter-Research." @default.
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