Titlebook: Standing up to Climate Change; Creating Prospects f Shahrooz Mohajeri,Lena Horlemann,Wolf Raber Book 2020 Springer Nature Switzerland AG 20

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Returning Periods of Drought and Climate Change in the Zayandeh Rud River Basinmmon disasters in all kinds of climate regimes (Chen et al. 2013). Unlike other natural disasters, the effects of drought appear gradually over time, typically on the order of several months to several years. Drought analysis usually involves estimating one of the drought indices and then calculatin

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Hydrological Modeling of Spatial and Temporal Changes of Blue and Green Water Resources in the Zayanrategic importance of the Zayandeh Rud river basin as the only water supply of central Iran, not enough work has been initiated to study the spatial and temporal changes of water resources components in the basin. Therefore, the main objective of this chapter is to survey and discuss the spatial var

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Dust Production Crisis Following the Recent Droughts in the Eastern Part of the Zayandeh Rud River Bhe world’s land surface is covered by these natural ecosystems and has several significant benefits for human society including the improvement of water quality, flood reduction biodiversity conservation, and the storage of water (Cui et al. 2009). In recent decades, the consequences of fast populat

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Participatory Development of Strategies for the Transformation of Agriculture in the Zayandeh Rud Rial rainfall and the volume of upstream water reservoirs over the last 10–20 years. Severe droughts have led to drastic changes in surface water supply for all stakeholders in the basin, and to an unpredictable irrigation water supply for agriculture. A factor adding to problems in water availability

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Adaptive Land and Water Management: A Regional Action Plan for Roodasht to Cope with Climate Change conditions (Gohari et al. 2013; Torfe et al. 2017; Salemi and Murray-Rust 2002). In the closed basin, where every drop of water is used multiple times, the basin-wide problems are magnified in the agricultural areas at the tail end of the river course (Molle and Mamanpoush 2012).