The "little ice age" and its geomorphological consequences in Mediterranean Europe

The "little ice age" and its geomorphological consequences in Mediterranean Europe

Alpine glacier advances in the "Little lee Age" took place in the decades around 1320, 1600, 1700 and 1810. They were the outcome of snowier winters and cooler summers than those of the twentieth century.

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Bibliographische Detailangaben
Veröffentlicht in:Climatic change 2001-01, Vol.48 (1), p.121-136
1. Verfasser: Grove, A T
Format: Artikel
Sprache:eng
Schlagworte:
Climate change
Floods
Glaciers
Ice ages
Middle Ages
Soil erosion
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Beschreibung
Zusammenfassung:Alpine glacier advances in the "Little lee Age" took place in the decades around 1320, 1600, 1700 and 1810. They were the outcome of snowier winters and cooler summers than those of the twentieth century.
ISSN:0165-0009
1573-1480
DOI:10.1023/A:1005610804390