Term for a relatively long-lasting climatic phenomenon from 1450 to 1850 that occurred worldwide with regional and temporal focal points in Europe, North America, Russia and China. Prior to this, there had been a pronounced temperature high between 900 and 1350, mainly in Europe, which was referred to as the Medieval Warm Period. At that time, the wine-growing frontier was much further north along the southern Baltic coast.
Around the year 1450, the climate began to deteriorate significantly again. Particularly cold periods stretched from 1570 to 1630 and from 1675 to 1715, accompanied by a worldwide expansion of the glaciers. The greatest expansion of the ice occurred around 1700, after which the glaciers slowly retreated again. This retreat is still continuing and many glaciers in the Alps have already melted completely.
![]()
wein.plus is a handy, efficient guide to a quick overview of the colourful world of wines, winegrowers and grape varieties. In Wine lexicon, the most comprehensive of its kind in the world, you will find around 26,000 keywords on the subject of grape varieties, wineries, wine-growing regions and much more.
Roman Horvath MW
Domäne Wachau (Wachau)