2024
600 years of wine must quality and April to August temperatures in western Europe 1420-2019
PFISTER, Christian, Stefan BRÖNNIMANN, Andres ALTWEGG, Rudolf BRÁZDIL, Laurent LITZENBURGER et. al.Základní údaje
Originální název
600 years of wine must quality and April to August temperatures in western Europe 1420-2019
Autoři
PFISTER, Christian, Stefan BRÖNNIMANN, Andres ALTWEGG, Rudolf BRÁZDIL (203 Česká republika, domácí), Laurent LITZENBURGER, Daniele LORUSSO a Thomas PLIEMON
Vydání
Climate of the Past, Copernicus Publications, 2024, 1814-9324
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10510 Climatic research
Stát vydavatele
Německo
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 4.300 v roce 2022
Organizační jednotka
Přírodovědecká fakulta
UT WoS
001255272400001
Klíčová slova česky
kvalita vinného moštu; vinobaní; proxy letních teplot; synoptický typ; historická klimatologie; západní Evropa
Klíčová slova anglicky
wine must quality; grape harvest; summer temperature proxy; weather type; historical climatology; Western Europe
Štítky
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 30. 8. 2024 11:33, Mgr. Marie Šípková, DiS.
Anotace
V originále
This study investigates the validity of wine must quality as an April-to-August temperature proxy between 1420 and 2019 based on expert ratings and quality measurements from Germany, Luxembourg, eastern France, and the Swiss Plateau. This is highly relevant as uncertainties remain on past climate variations during this period. The evidence was reviewed according to the best practice of historical climatology. Expert ratings tended to agree with Oechsle density measurements that gradually replaced them from the 1840s. A statistical model calibrated to predict wine must quality from climate data explains 75 % of the variance, underlining the potential value of wine must quality as a climate proxy. Premium crops were collected in years of early harvest involving high insolation during maturation, while poor crops resulted from very late harvests in cold and wet summers. An analysis of daily weather types for high- and low-quality years after 1763 shows marked differences. On a decadal timescale, the average quality was highest from 1470 to 1479, from 1536 to 1545, and from 1945 to 1954. Poor crops were collected in periods with prevailing cold and wet summers such as 1453 to 1466, 1485 to 1494, 1585 to 1614, 1685 to 1703, 1812 to 1821, and 1876 to 1936. In the period of enhanced warming after 1990, high quality became the rule.