Titlebook: Water, Environment and Society in Times of Climatic Change; Contributions from a Arie S. Issar,Neville Brown Book 1998 Springer Science+Bus

駭人

The Impact of Climate Changes on Groundwater Regimes and Resources in Russia,d near the Pliocene/Pleistocene boundary (.. 2 million years BP). Millions of square kilometers were then affected by glacial erosion or deposition. Successive advances or retreats of sheet ice repeatedly altered the hydrological network around this time and, of course, subsequently. The accumulatio

喧鬧

Middle to Late Holocene (6,500 Yr. Period) Paleoclimate in the Eastern Mediterranean Region from Stterranean region during the last 25,000 years (Bar-Matthews .., 1997a) and 58,000 years (Bar-Matthews .., 1997b). These studies indicate that the isotopic compositions of speleothems that are older than about 6,500 BP are significantly different from those of present-day speleothems; and that about

總

幼稚

Early to Mid-Holocene Environmental Changes and Their Impact on Human Communities in Southeastern A zones, and has had a history of settlement throughout the Holocene which is characterized by fluctuations between simple village farming communities and complexly organized cities and towns. Archaeologically it is a region where there have been major fluctuations in population, some perhaps related

CAMEO

Antecedent

Some Considerations on Climatic Changes, Water Resources and Water Needs in the Italian Region Soutecipitation, temperature, evaporation, ..), one can expect variations in the frequency of exceptional events, and also in the hydrological regime. There maybe major consequences in terms of economy and quality of life. This has often occurred in the past, and it would be strange if does not happen a

創(chuàng)造性

ASSET

defeatist

Euphonious

Aspects of Climate Variability and the UNESCO International Hydrological Programme,IGBP-BAHC, GEWEX) under the umbrella of WCP-Water (World Climate Programme-Water). To achieve this objective, this short contribution will select some of the cross-cutting issues which link some of findings from the paleoclimatic studies, with the problems of using outputs from atmospheric General C