The paleoclimate of Jordan during the Pleisto- cene as a possible indicator for future climate change: an overview
نویسنده
چکیده
Present-day climate cannot account for the presence of such lakes in the arid to semi arid area of Jordan. Therefore more intense and wetter Mediterranean cyclones in winter coupled with Arabian monsoon or even ArabianIndian monsoon in summer would have affected major parts of Jordan up to latitude 31° 32 ́ during the warmer periods of the Pleistocene and brought more rain to establish and sustain such lakes.
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