Abstract
Abstract. The Dead Sea desertification-threatened region is affected by continual lake level decline and occasional but life-endangering flash floods. Climate change has aggravated such issues in the past decades. In this study, the impact on local conditions leading to heavy precipitation from the changing conditions of the Dead Sea is investigated. Idealized sensitivity simulations with the high-resolution COSMO-CLM (COnsortium for Small-scale MOdelling and Climate Limited-area Modelling) and several numerical weather prediction (NWP) runs on an event timescale are performed on the Dead Sea area. The simulations are idealized in the sense that the Dead Sea model representation does not accurately represent the real conditions but those given by an external dataset. A reference or Dead Sea simulation covering the 2003–2013 period and a twin sensitivity or bare soil simulation in which the Dead Sea is set to bare soil are compared. NWP simulations focus on heavy precipitation events exhibiting relevant differences between the Dead Sea and the bare soil decadal realization to assess the impact on the underlying convection-related processes. The change in the conditions of the Dead Sea is seen to affect the atmospheric conditions leading to convection in two ways. (a) The local decrease in evaporation reduces moisture availability in the lower boundary layer locally and in the neighbouring regions, directly affecting atmospheric stability. Weaker updraughts characterize the drier and more stable atmosphere of the simulations in which the Dead Sea has been dried out. (b) Thermally driven wind system circulations and resulting divergence/convergence fields are altered, preventing in many occasions the initiation of convection because of the omission of convergence lines. On a decadal scale, the difference between the simulations suggests a weak decrease in evaporation, higher air temperatures and less precipitation (less than 0.5 %).
Highlights
The Eastern Mediterranean and the Middle East is a sensitive climate change area (Smiatek et al, 2011)
We examine the evolution of specific humidity (Qv2 m) and temperature at 2 m (T2 m), as well as total column integrated water vapour (IWV) and equivalent low-boundary-layer (
This process has been related to significant local climate changes which affect the Dead Sea valley and neighbouring regions
Summary
The Eastern Mediterranean and the Middle East is a sensitive climate change area (Smiatek et al, 2011). The anticipated warming in the 21st century combined with the general drying tendency suggests important regional impacts of climate change which should be investigated to assess and mitigate local effects on society and ecosystems. The complex topography of the area favours the combined occurrence of several wind regimes in addition to the general synoptic systems, namely valley and slope winds, Mediterranean breezes, and local lake breezes Shafir and Alpert, 2011) These wind systems are of great importance for the living conditions in the region since they influence visibility and the air quality
Sign-in/Register to view highlights & summary Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
