TY - CHAP
T1 - The Quaternary Climate of Israel
AU - Torfstein, Adi
N1 - Publisher Copyright: © The Author(s), under exclusive license to Springer Nature Switzerland AG 2024.
PY - 2024
Y1 - 2024
N2 - Israel is located in the southern sector of the LevantLevant, spanning the climatic transition between the hyperarid Sahara Desert in the south and the moderate Mediterranean climate in the north. Past changes in the locus of this climatic transition zone have been recorded at numerous sites in Israel and its surroundings, reflecting major Quaternary climateQuaternary climate changes that have impacted regional fauna, flora, and hominid migration patterns, and influenced the cultural history of this region. Importantly, two uniquely resolved, continuous and long records—the Dead Sea sediments and concomitant cave deposits—serve as globally prominent archives of subtropical continental climate, which together with numerous additional regional climate reconstructions provide a highly detailed record of Quaternary climateQuaternary climate change in the Levant. In this chapter, the main archives and observations that provide the basis for regional climate reconstruction are described, and used to provide an overview of climate patterns in the southern LevantLevant throughout the Quaternary.
AB - Israel is located in the southern sector of the LevantLevant, spanning the climatic transition between the hyperarid Sahara Desert in the south and the moderate Mediterranean climate in the north. Past changes in the locus of this climatic transition zone have been recorded at numerous sites in Israel and its surroundings, reflecting major Quaternary climateQuaternary climate changes that have impacted regional fauna, flora, and hominid migration patterns, and influenced the cultural history of this region. Importantly, two uniquely resolved, continuous and long records—the Dead Sea sediments and concomitant cave deposits—serve as globally prominent archives of subtropical continental climate, which together with numerous additional regional climate reconstructions provide a highly detailed record of Quaternary climateQuaternary climate change in the Levant. In this chapter, the main archives and observations that provide the basis for regional climate reconstruction are described, and used to provide an overview of climate patterns in the southern LevantLevant throughout the Quaternary.
KW - Glacial–interglacial cycles
KW - Levant
KW - Quaternary climate
UR - http://www.scopus.com/inward/record.url?scp=85188943635&partnerID=8YFLogxK
U2 - 10.1007/978-3-031-44764-8_4
DO - 10.1007/978-3-031-44764-8_4
M3 - فصل
T3 - World Geomorphological Landscapes
SP - 49
EP - 71
BT - World Geomorphological Landscapes
ER -