Differential denudation across the Judea Range, Israel, suggests the persistence of a rain-shadow since mid Miocene

U. Ryb; A. Matmon; Y. Erel; I. Haviv; L. C. Benedetti

Differential denudation across the Judea Range, Israel, suggests the persistence of a rain-shadow since mid Miocene

U. Ryb, A. Matmon, Y. Erel, I. Haviv, L. C. Benedetti

Department of Earth and Environmental sciences

Ben-Gurion University of the Negev

Research output: Contribution to journal › Meeting Abstract

Abstract

The Judea Range which is composed of a thick sequence of Cretaceous marine carbonate rises up to ~1000 m between the Mediterranean Sea and the Dead Sea basins. The western flank of the range faces predominant winds which deliver humidity from the Mediterranean and thus maintains a sub-humid Mediterranean climate (Mean Annual Precipitation (MAP) of 500-700 mm). Over the eastern, leeward side, rain-shadow orographic effect imposes a climatic gradient from Mediterranean near the water divide to hyper-arid near the Dead Sea rift escarpment (MAP

Original language	American English
Journal	Geophysical Research Abstracts
Volume	41
State	Published - 1 Dec 2013

Keywords

1039 GEOCHEMISTRY Alteration and weathering processes
1625 GLOBAL CHANGE Geomorphology and weathering

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http://adsabs.harvard.edu/abs/2013AGUFMEP41C0811R

Cite this

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title = "Differential denudation across the Judea Range, Israel, suggests the persistence of a rain-shadow since mid Miocene",

abstract = "The Judea Range which is composed of a thick sequence of Cretaceous marine carbonate rises up to ~1000 m between the Mediterranean Sea and the Dead Sea basins. The western flank of the range faces predominant winds which deliver humidity from the Mediterranean and thus maintains a sub-humid Mediterranean climate (Mean Annual Precipitation (MAP) of 500-700 mm). Over the eastern, leeward side, rain-shadow orographic effect imposes a climatic gradient from Mediterranean near the water divide to hyper-arid near the Dead Sea rift escarpment (MAP",

keywords = "1039 GEOCHEMISTRY Alteration and weathering processes, 1625 GLOBAL CHANGE Geomorphology and weathering",

author = "U. Ryb and A. Matmon and Y. Erel and I. Haviv and Benedetti, {L. C.}",

year = "2013",

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language = "American English",

volume = "41",

journal = "Geophysical Research Abstracts",

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T1 - Differential denudation across the Judea Range, Israel, suggests the persistence of a rain-shadow since mid Miocene

AU - Ryb, U.

AU - Matmon, A.

AU - Erel, Y.

AU - Haviv, I.

AU - Benedetti, L. C.

PY - 2013/12/1

Y1 - 2013/12/1

N2 - The Judea Range which is composed of a thick sequence of Cretaceous marine carbonate rises up to ~1000 m between the Mediterranean Sea and the Dead Sea basins. The western flank of the range faces predominant winds which deliver humidity from the Mediterranean and thus maintains a sub-humid Mediterranean climate (Mean Annual Precipitation (MAP) of 500-700 mm). Over the eastern, leeward side, rain-shadow orographic effect imposes a climatic gradient from Mediterranean near the water divide to hyper-arid near the Dead Sea rift escarpment (MAP

AB - The Judea Range which is composed of a thick sequence of Cretaceous marine carbonate rises up to ~1000 m between the Mediterranean Sea and the Dead Sea basins. The western flank of the range faces predominant winds which deliver humidity from the Mediterranean and thus maintains a sub-humid Mediterranean climate (Mean Annual Precipitation (MAP) of 500-700 mm). Over the eastern, leeward side, rain-shadow orographic effect imposes a climatic gradient from Mediterranean near the water divide to hyper-arid near the Dead Sea rift escarpment (MAP

KW - 1039 GEOCHEMISTRY Alteration and weathering processes

KW - 1625 GLOBAL CHANGE Geomorphology and weathering

M3 - Meeting Abstract

SN - 1029-7006

VL - 41

JO - Geophysical Research Abstracts

JF - Geophysical Research Abstracts

ER -

Differential denudation across the Judea Range, Israel, suggests the persistence of a rain-shadow since mid Miocene

Abstract

Keywords

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