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The modern and Last Glacial Maximum hydrological cycles of the Eastern Mediterranean and the Levant from a water isotope perspective
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文摘
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We present a methodology for interpreting modern and paleo-isotopic data.

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Using modern data we model the Eastern Mediterranean isotopic hydrological cycle.

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Sea-land temperature gradient is an important control on the isotopic composition.

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We model the full Last Glacial Maximum paleohydrological isotopic cycle of the Eastern Mediterranean.

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Last Glacial Maximum moisture transport, humidity and distillation shifts altered rainfall composition.

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