An idealized model sensitivity study on Dead Sea desertification with a focus on the impact on convection

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 %).

A Vision on a UNESCO Global Geopark at the Southeastern Dead Sea in Jordan—Geosites and Conceptual Approach

“…In the last decades, however, the human and natural impact has accelerated the changes in the natural system, leading to a rapid decline in the water level of the lake (Figure 2, based on satellite images from [28,29]). The shorelines of the lake suffer from an increase in natural hazards related to desertification and erosion, such as sinkholes, landslides, salt storms and flash floods, all of these are prominent examples that caused life and economic loss [23,[30][31][32][33][34][35][36] recently. The sad highlight in this context is the flash floods of Wadi Ma'in and Wadi Musa that caused high death tolls in Jordan in October 2018 [37].…”

Modelling of the Discharge Response to Climate Change under RCP8.5 Scenario in the Alata River Basin (Mersin, SE Turkey)

“…Curiously, the projected precipitation in the beginning (in April-May) and middle (in January-March) of the century did not differ significantly from the baseline values (Figure 8c). This can be explained by the increase in convective precipitation caused by the regional neighbouring synoptic weather patterns (such as the Cyprus low, recognised as responsible for a large part of the annual rainfall in the Levant region) of the Mediterranean region, resulting in short and heavy rainfall events in the ARB (e.g., [92][93][94].…”