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Bar-Matthews, M., Ayalon, A. and Kaufman, A. (1998) Middle to Late Holocene (6,500 yr. Period) Paleoclimate in the Eastern Mediterranean Region from Stable Isotopic Composition of Speleothems from Soreq Cave, Israel. In: Issar, A.S. and Brown, N., Eds., Water, Environment and Society in Times of Climatic Change, Volume 31 of the Series Water Science and Technology Library, Springer, Berlin, 203-214.

has been cited by the following article:

• TITLE: Was the 4.2 ka Event an Anthropogenic Disaster?

  AUTHORS: Tomasz Jarosław Szczęsny

  KEYWORDS: Holocene Climatic Optimum, Walker Circulation, Monsoon, Green Sahara Period, 4.2 ka Event

  JOURNAL NAME: Open Journal of Ecology, Vol.6 No.10, September 27, 2016

  ABSTRACT: The article describes a possible impact of demographic explosion during the Neolith on local ecosystems and on the global climate as well as the role of this explosion in aggravating the course of 4.2 ka cooling event. A possible role of human activity in changing the pattern of mid-latitudes westerlies, monsoons and Walker circulation throughout the Holocene is analyzed. It is explained why during the Holocene Climatic Optimum (HCO) monsoons could have been weaker than today, not stronger, as it is commonly stated. It is described how during the HCO the humid Tibetan Plateau could have repelled the Indian monsoon to the west and the East Asian monsoon to the north. The explanation for weaker El Niño-Southern Oscillation (ENSO) during HCO is proposed.