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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Approaching the Medieval Optimum, 212 to 1000 AD,oks, Ellsworth Huntington, Hubert Lamb.... Historians have tended thus far to be either blankly indifferent or somewhat scornful. Some notable exceptions are to be found among the community of French historians associated with ., a journal founded in 1929 and committed to forging links with other su

Loathe

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Innovative

Climate Change and History during the Holocene in the Eastern Mediterranean Region, us to reconstruct quite comprehensively and with high definition the climate changes which have occurred in the Mediterranean region during the last 10,000 years. One may start with indicators not influenced by human activity, like isotope ratios, or ancient Mediterranean and Dead Sea levels; proce

Gum-Disease

interference

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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Frequency of Extreme Hydroclimatically-Induced Events as a Key to Understanding Environmental Changt interpretations of sediments, landforms and parallel biotic changes. These sources of information point to episodes with higher or lower frequency of extreme events, and indicate that some of these occurred under wetter and cooler conditions that permitted higher water storage (.. Starkel, 1983).

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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