Frequency of extreme hydroclimatically induced as a key to understanding environmental changes in the Holocene
Water environment and society in times of climatic change
During the Holocene were identified episodes with higher frequency of extreme events like heavy downpours, continuous rains, rainy phases, rapid decades. All of them are reflected in sedimentary sequences, in relief and biotic changes
Geomorphic response to climatic and environmental changes along a Central Asian transect during the Holocene
Special issue. Geomorphic response of mediterranean and arid areas to climate change
This paper discusses the geomorphic response to late Quaternary climatic changes, and to some extent, human impact, along an Asian transect running from Eastern Siberia via Mongolia and Tibet to India : Khangai Mountains of Mongolia, Darjeeling
To provide characteristics of present-day extreme events which may serve as a key to better recognition of past hydrological changes, the upper Vistula basin was taken as an example. The observations are mainly related to last 100-150 years