Many studies show the sensitivity of our environment to manmade changes, especially the anthropogenic impact on atmospheric and hydrological processes. The effect on Solid Earth processes such as subsidence is less straightforward. Subsidence is usually slow and relates to the interplay of complex hydro-mechanical processes, thus making relations to atmospheric changes difficult to observe. In the Dead Sea (DS) region, however, climatic forcing is strong and over-use of fresh water is massive. An observation period of 3 years was thus sufficient to link the high evaporation (97 cm/year) and the subsequent drop of the Dead Sea lake level (− 110 cm/year), with high subsidence rates of the Earth’s surface (− 15 cm...
Sediment cores recovered by the Dead Sea Deep Drilling Project (DSDDP) from the deepest basin of the...
This paper is not subject to U.S. copyright. The definitive version was published in Journal of Geo...
of late glacial Lake Lisan and fan delta surfaces between 280 and 365m bmsl (meters below mean sea l...
Many studies show the sensitivity of our environment to manmade changes, especially the anthropogeni...
The deepest point on Earth, the Dead Sea level, has been dropping alarmingly since 1978 by 0.7 m/a o...
From the 1970s, the Dead Sea experienced severe halo-karstification and anthropogenic modifications....
Based on geomorphic observations, we discuss lake-level fluctuations, alluvial deposition and river ...
The modern hydrological regime of the Dead Sea is strongly affected by anthropogenic activity. The n...
Delta margins are subject to relatively high rates of land subsidence and have the potential to sign...
The Dead Sea (DS) area is one of the best examples of the significant impact that the uncontrolled e...
Changes in the level of closed lakes such as the glacial Lake Lisan/Near East, that occupied the Jor...
The lake level of the Dead Sea, Southern Levant, has fluctuated with an amplitude of ∼250 m in respo...
The Dead Sea is a terminal lake of one of the largest hydrological systems in the Levant and may thu...
Since the mid-1980s the coast of the Dead Sea is affected by sinkholes occurring over and around the...
peer reviewedSubaqueous mass failures that comprise slides, slumps and debris flows are a major proc...
Sediment cores recovered by the Dead Sea Deep Drilling Project (DSDDP) from the deepest basin of the...
This paper is not subject to U.S. copyright. The definitive version was published in Journal of Geo...
of late glacial Lake Lisan and fan delta surfaces between 280 and 365m bmsl (meters below mean sea l...
Many studies show the sensitivity of our environment to manmade changes, especially the anthropogeni...
The deepest point on Earth, the Dead Sea level, has been dropping alarmingly since 1978 by 0.7 m/a o...
From the 1970s, the Dead Sea experienced severe halo-karstification and anthropogenic modifications....
Based on geomorphic observations, we discuss lake-level fluctuations, alluvial deposition and river ...
The modern hydrological regime of the Dead Sea is strongly affected by anthropogenic activity. The n...
Delta margins are subject to relatively high rates of land subsidence and have the potential to sign...
The Dead Sea (DS) area is one of the best examples of the significant impact that the uncontrolled e...
Changes in the level of closed lakes such as the glacial Lake Lisan/Near East, that occupied the Jor...
The lake level of the Dead Sea, Southern Levant, has fluctuated with an amplitude of ∼250 m in respo...
The Dead Sea is a terminal lake of one of the largest hydrological systems in the Levant and may thu...
Since the mid-1980s the coast of the Dead Sea is affected by sinkholes occurring over and around the...
peer reviewedSubaqueous mass failures that comprise slides, slumps and debris flows are a major proc...
Sediment cores recovered by the Dead Sea Deep Drilling Project (DSDDP) from the deepest basin of the...
This paper is not subject to U.S. copyright. The definitive version was published in Journal of Geo...
of late glacial Lake Lisan and fan delta surfaces between 280 and 365m bmsl (meters below mean sea l...