The Zambezi River Basin 2017
DOI: 10.4324/9781315282053-4
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Climate change vulnerability and risk

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Cited by 9 publications
(15 citation statements)
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“…Water stress is one of the significant causes for crop losses worldwide, reducing average yields to 50 percent or even more; furthermore, possible global climate change scenario suggests a future upsurge in drought stress [10,11]. Therefore, breeding crop varieties for improved water use efficiency is of utmost importance [12].…”
Section: Introductionmentioning
confidence: 99%
“…Water stress is one of the significant causes for crop losses worldwide, reducing average yields to 50 percent or even more; furthermore, possible global climate change scenario suggests a future upsurge in drought stress [10,11]. Therefore, breeding crop varieties for improved water use efficiency is of utmost importance [12].…”
Section: Introductionmentioning
confidence: 99%
“…Figure ), sometimes starting as early as October and extending well into April (Torrance, ). Rainfall is mainly dependent on the orientation and behaviour of the InterTropical Convergence Zone (ITCZ) , which is influenced by the change in pressure patterns to the north and south of the country (Beilfuss, ). Rainfall is also dependent on the passage of the upper westerly waves of mid‐latitude origin which enhance the intensity of rainfall during a given wet period.…”
Section: Introductionmentioning
confidence: 99%
“…varies from more than 1600 mm/year in several far northern highland areas to less than 600 mm/year in the water-stressed southern portion of the basin (Fig. 8d-f;Beilfuss, 2012). Our experiments shows that key hydrological parameters such are precipitation, evapotranspiration and runoff are highly variable across the basin, from year to year.…”
Section: The Gpr Model As a Topical Machine Learning Algorithm In Reg...mentioning
confidence: 57%
“…8a), the annual variability of TWS dynamics over the study region is represented by a variance of 24.755%. It can therefore be deduced that the strongest annual variability occurred over the central portion of the Zambezi Basin, which consists of notable sub-basins such as the Kabompo, Barotse, Kariba, Mupata, and Kafue, whose combined area is 546,251 km 2 (Beilfuss, 2012).…”
Section: The Influence Of River Discharge and Surface Water Estimates...mentioning
confidence: 99%