Calcareous tufa as indicators of climatic variability: a case study from southern Tuscany (Italy)

2010 ◽  
Vol 336 (1) ◽  
pp. 263-281 ◽  
Author(s):  
Enrico Capezzuoli ◽  
Anna Gandin ◽  
Fabio Sandrelli
2016 ◽  
Author(s):  
John Gowing ◽  
Geoff Parkin ◽  
Nathan Forsythe ◽  
David Walker ◽  
Alemseged Tamiru Haile ◽  
...  

Abstract. There is a need for an evidence-based approach to identify how best to support development of groundwater for small scale irrigation in sub-Saharan Africa (SSA). We argue that it is important to focus this effort on shallow groundwater resources which are most likely to be used by poor rural communities in SSA. However, it is important to consider constraints, since shallow groundwater resources are likely to be vulnerable to over-exploitation and climatic variability. We examine here the opportunities and constraints and draw upon evidence from Ethiopia. We present a methodology for assessing and interpreting available shallow groundwater resources and argue that participatory monitoring of local water resources is desirable and feasible. We consider possib le models for developing distributed small-scale irrigation and assess its technical feasibility. Because of power limits on water lifting and also because of available technology for well construction, groundwater at depths of 50 m or 60 m cannot be regarded as easily accessible for small-scale irrigation. We therefore adopt a working definition of shallow groundwater as < 20 m depth. This detailed case study in the Dangila woreda in Ethiopia explores the feasibility of exploiting shallow groundwater for small-scale irrigation over a range of rainfall conditions. Variability of rainfall over the study period (9 % to 96 % probability of non-exceedance) does not translate into equivalent variability in groundwater levels and river baseflow. Groundwater levels, monitored by local communities, persist into the dry season to at least the end of December in most shallow wells, indicating that groundwater is available for irrigation use after the cessation of the wet season. Arguments historically put forward against the promotion of groundwater use for agriculture in SSA on the basis that aquifers are unproductive and irrigation will have unacceptable impacts on wetlands and other groundwater-dependent ecosystems appear exaggerated. It would be unwise to generalise from this case study to the whole of SSA, but useful insights into the wider issues are revealed by the case study approach. We believe there is a case for arguing that shallow groundwater in sub-Saharan Africa represents a neglected opportunity for sustainable intensification of small-scale agriculture.


Author(s):  
Alessandro Pucci ◽  
Hélder S. Sousa ◽  
José C. Matos

<p>Planet Earth is naturally subject to climatic variability, but over the recent decades extreme deviations have been observed. Climate change, as a manmade-induced process, is mainly due to the increase of greenhouse gasses emission. Global warming consequences drive also to an intensification of hydrological cycles, leading to more frequent and severe precipitations. In parallel, several bridges have collapsed in the last years due to extreme rainfalls. Although the impacts of climate change on built environment do not always present a direct cause-effect relation, analysis on specific parameters (as rain volume) that are inputs in bridge design, can clarify some aspects of this interaction. In this paper, the peak discharge variation of different rivers located in the northwest of Italy, within the last 100 years, is analyzed. A cluster analysis was performed to understand if the hydraulic design loads should be considered with a different intensity if the bridge had been built with reference to an up-to-date database, or if in the last decades, when the majority of these structures were built. The rainfall data was analyzed through classical techniques, such as the frequency-based statistical method, but without the stationary time hypothesis. In this case, the extreme value theory was used for the estimation of intensity-duration curve parameters. By introducing a second-order analysis, where random variables can change over time, an increase-trend of rainfall height was found, and the peak discharge was determined accordingly. The relevant parameters on the case-study area were preliminarily obtained through geographic information systems. The results evidenced that nowadays-floods parameters are significantly different from those of the past, and this behavior is escalated when high return period values are assumed. Furthermore, although hydraulic design loads are increasing, many existing bridges are not properly maintained, leading to an increased number of collapses.</p>


2018 ◽  
Vol 07 (02) ◽  
Author(s):  
Vega YL ◽  
Paulo LB ◽  
Acosta BH ◽  
Valdes OR ◽  
Borroto SG ◽  
...  

Water ◽  
2010 ◽  
Vol 2 (4) ◽  
pp. 773-787 ◽  
Author(s):  
Silvia Terzago ◽  
Claudio Cassardo ◽  
Roberto Cremonini ◽  
Simona Fratianni

2020 ◽  
Author(s):  
Aparna Bera ◽  
Suraj Kumar Singh

Abstract The effects of climate change are causing large scale human displacements all over the World over past few decades and climate refugees are putting biggest challenges to the geophysical biological and social system. This paper attempts to assess the vulnerability of both the refugee and regular settlers of selected mouzas of Sagar Island, south 24parganas, India where people are witnessing their lands vanishing under their feet in these constantly sinking and shrinking deltaic estuaries. Findings of LVI and LVI-IPCC analysis indicate that the climate induced migrant communities are more exposed to climatic variability due to poor adaptive capacity. Poor access to food, water, health facilities are making them extremely vulnerable with lower resilience as these mouzas are facing frequent flooding, severe coastal erosion, embankment breaching and higher storm surges on an annual basis. The outcomes of this study could be beneficial for effective on site risk management, adaptation strategies and further planning propositions.


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