Abstract
Climatically, Jordan shows close affinity to its neighbours. Summers are hot, especially on the plateau and in the Jordan Valleys, where temperatures up to 48 °C have been recorded. Winters are fairly cold, and on the plateau frost and some snow are usual, though not in the lower Jordan Valley. The significant element of the climate of Jordan is rainfall. In the higher parts (i.e. the uplands of Samaria and Judaea and the hills overlooking the eastern Jordan Valley) 370 to 620 mm of rainfall occur, enough for agriculture; but elsewhere as little as 200 mm or less may fall, and pastoral nomadism is the only possible way of life. Only about 25% of the total area of Jordan is sufficiently humid for cultivation.
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Bibliography
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© 1970 Dr. W. Junk N.V., Publishers, The Hague
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Oedekoven, K.H. (1970). Jordan. In: Kaul, R.N. (eds) Afforestation in Arid Zones. Monographiae Biologicae, vol 20. Springer, Dordrecht. https://doi.org/10.1007/978-94-010-3350-3_7
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DOI: https://doi.org/10.1007/978-94-010-3350-3_7
Publisher Name: Springer, Dordrecht
Print ISBN: 978-94-010-3352-7
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