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

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Reverie

Agnosia

Medieval Climatic Anomaly in the Americas,cally, these discussions focus on the temperature departures that might result from continued anthropogenic emission of greenhouse gasses; on the response of the earth’s physical and biotic systems to those departures; and on the socio-economic impacts of those responses. Strong differences of opini

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Paleohydrology of the Northern Negev: Comparative Evaluation of Two Catchments,habitation. Permanent water sources in the region are scarce, making runoff the dominant source for both domestic use and agriculture (Evenari .., 1971). The technology of collecting the runoff to cisterns and cultivated plots was practiced in the northern Negev during several periods, climaxing in

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Nebulizer

Application of a Global Volcanicity Time-Series on High-Resolution Paleoclimatic Modeling of the Eaead and O’Shea (1989:1) phrase it: “human communities have developed an impressive array of cultural mechanisms for buffering variability. The diversity of these mechanisms, however, should not mask the fact that an effective strategy must match, in both capacity and scale, the variability with whic

OATH

Population Growth and Decline in the Northern Part of Eretz-Israel during the Historical Period as ansition zone between the Euroasian and African continents, and between the Mediterranean and the arid climatic zones (Map 7.1). The historical-geographical name Eretz-Israel applies to the region between the Mediterranean Sea to the Jordan River and the Dead Sea Rift Valley, which includes the Stat

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,Settlement, Agriculture and Paleoclimate in ?Uvda Valley, Southern Negev Desert, 6th–3rd Millennia mm annual average, with an annual evaporation rate of 4,000 mm. The significance of these figures is more apparent when compared with those of the Negev Highland desert, 100 km to the north, with 100 mm average annual precipitation and 2,000 mm evaporation potential. Obviously, the water balance of