The Fertile Crescent, its hilly flanks and surrounding drylands has been a critical region for studying how climate has influenced societal change, and this review focuses on the region over the last 20,000 years. The complex social, economic, and environmental landscapes in the region today are not new phenomena and understanding their interactions requires a nuanced, multidisciplinary understanding of the past. This review builds on a history of collaboration between the social and natural palaeoscience disciplines. We provide a multidisciplinary, multiscalar perspective on the relevance of past climate, environmental, and archaeological research in assessing present day vulnerabilities and risks for the populations of southwest Asia. We discuss the complexity of palaeoclimatic data interpretation, particularly in relation to hydrology, and provide an overview of key time periods of palaeoclimatic interest. We discuss the critical role that vegetation plays in the human–climate–environment nexus and discuss the implications of the available palaeoclimate and archaeological data, and their interpretation, for palaeonarratives of the region, both climatically and socially. We also provide an overview of how modelling can improve our understanding of past climate impacts and associated change in risk to societies. We conclude by looking to future work, and identify themes of “scale” and “seasonality” as still requiring further focus. We suggest that by appreciating a given locale's place in the regional hydroscape, be it an archaeological site or palaeoenvironmental archive, more robust links to climate can be made where appropriate and interpretations drawn will demand the resolution of factors acting across multiple scales. This article is categorized under: Human Water > Water as Imagined and Represented Science of Water > Water and Environmental Change Water and Life > Nature of Freshwater Ecosystems

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The groundwater hydrochemical characteristics of theAzraq Basin were investigated and evaluated statistically. The presence of an underground saline water body in the Qa' Al-Azraq area has made this specific part of the basin. 38 samples from 38 GW wells were collected to understand the GW hydrochemistry of the Azraq unconfined aquifer that is mainly composed of marl, evaporites, limestone and clay formations. The PCA analysis indicates that Na, Mg, Cl, Ca, and K contribute the variance in the chemical composition of the GW samples. Piper, Durov and Wilcox diagrams indicated that the water types are mainly earth alkaline with prevailing SO4 and Cl, and alkaline water with prevailing SO4 and Cl. The main processes in the basin are dissolution or mixing and reverse ion exchange in which Na and Cl are prevailing. The GW is mainly oversaturated concerning aragonite, calcite and dolomite as indicated by the excess input of Mg and Ca ions from the rock-water interactions, while anhydrite (CaSO4), halite (NaCl), and gypsum (CaSO4.2H2O) are generally undersaturated. The effect of the agricultural activities in the study area is reflected by the positive correlation between NO3 and PC2. Wilcox diagram indicates that the samples are in the medium to very high salinity slots with the majority in the high salinity slot and in the low and medium alkali hazard zone, while few samples show high to very high alkali hazards. The simulated salinity for the next 30 years shows alarming danger and requires immediate attention as the Qa' area is expected to become saline with TDS values of 2500 to 4600 mg/l, unsuitable to use for domestic and/or agricultural purposes.

Groundwater is an essential source of freshwater for the severely water-deprived country of Jordan. Thus, understanding abstracted amounts of the ground water is essential for sustaining this resource. More than 50% of the annual abstracted groundwater is used for irrigation, indicating the need to correctly estimate this usage and minimize the uncertainties. Thus, this study aims to assess actual groundwater abstraction in North Jordan by implementing a new geographic information system–remote sensing multi-method approach. The results are promising and show that the announced GW abstraction volumes provided by the Water Authority of Jordan and the Ministry of Water and Irrigation are not particularly accurate, especially for areas where extensive agricultural practices are present. This fact may explain the discrepancies between official reports on declining groundwater levels and the results of several studies that assessed North Jordan groundwater abstraction. This study showed that irrigation is a crucial factor that affects this discrepancy and that the crop water requirements are generally higher than what is reported by the governmental sector. The results showed a 31 MCM discrepancy between the official recorded groundwater abstraction volumes and the actual (crop-based) water consumption. Increasing the irrigation efficiency by 20% will aid in sustaining the groundwater in the study area, maintaining the current groundwater wells and save the farmers money.