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AbstractUnderstanding the emotional impact of climate change (CC), its education and communication processes on young people is essential to identify what motivates their engagement in climate action. We have analysed the emotional experiences of secondary school students in the south of Spain (N = 1,050) to develop a tool for exploring the emotional impact of CC, and its relationship to processes of climate education, communication and participation among young people. While there is no clear emotional bias towards CC in the overall sample, significant differences in these experiences depend on the variables listed above. Formal education (educational grade and curricular greening) tends to increase worry, powerlessness and fear, and decrease positive emotions. Frequently, the use of information sources, such as traditional media, specialised sources and social networks is associated with higher emotional intensity. Social networks are a powerful influencer, while traditional media and specialised sources present barriers to access. Participating in climate action (climate movements, climate strikes, environmental groups’ activities and school’s voluntary activities) has a clearly negative emotional footprint among the group studied. [ABSTRACT FROM AUTHOR]

River flooding is one of the most widespread natural disasters. Projections indicate that climate change will increase flood hazard in many areas around the world. In this study, we investigate the individual and combined effects of sea level rise, flow increase and riparian vegetation encroachment on flood hazard in the lower Biobío River, Chile. Results show that each has the potential to individually increase flood hazard in certain areas, and that individual effects can compound. Encroachment of riparian vegetation onto previously sparsely vegetated areas of the floodplain, likely a result of the Chilean megadrought, causes higher flow resistance and increased flooding during large events. Somewhat counterintuitively, drought has therefore led to an increase in flood hazard in the study area. Drought risk for most land areas across the globe is expected to increase with climate change. Potential future vegetation encroachment should therefore be included as a key variable in riverine flood hazard studies. [ABSTRACT FROM AUTHOR]

Hydrological modelling has undergone constant growth with the increase in information processing capabilities. Hydrological models have traditionally been used to study the effects of climate change on management and land-use changes and for water resources planning, among other purposes. The aim of this study was to determine and analyse the advantages of the HBV and HYMOD models, which are commonly used in hydrology on daily and monthly time scales. A regional sensitivity analysis was used to compare the processes that take on greater importance at different time scales in the two models. As a result, it was found that quick precipitation-runoff processes prove to be better represented in the HBV model, while slow, time-aggregated processes are better represented by the HYMOD model. This study confirms that both models are adequate for rain-dominated basins, such as those of the study area. Additionally, the HBV model proved to be more robust in comparison to HYMOD. [ABSTRACT FROM AUTHOR]

We assessed whether ecophysiological requirements are consistent with the environmental traits within the current ranges in a relictual lizard group, Algyroides, composed of four species with restricted and disjunctive distributions. We considered temperature, precipitation and their seasonal profiles, and focused on the preferred body temperature (Tp) and the evaporative water loss (EWL). The ranges of all four species differed in environmental traits. The two geographically more restricted species followed divergent patterns: A. moreoticus inhabits hot and climatically buffered areas, and A. marchi occupies cold seasonal environments. Tp and EWL also differed among species following a geographical grouping: A. nigropunctatus (Slovenia) and A. fitzingeri (Sardinia) selected for lower Tp and lost less water than the southern species A. moreoticus (Peloponnese) and A. marchi (Southern Spain). Tp and EWL were correlated at species level but not at individual level within species. Results suggest that the current distribution of Algyroides species partly reflects their ecophysiology, with water ecology taking precedence over thermal ecology as constraining factor. By unravelling the environmental factors limiting the distribution of species, ecophysiology may provide directions for conservation, predicting the degree of vulnerability to climate change. [ABSTRACT FROM AUTHOR]

In recent years, it has been documented that climatic variability influences hydrological processes; however, these influences, such as hydrologic dynamics, have not yet been incorporated into models, which have been assumed as stationary with regard to climatic conditions. In this study, the temporal variability of hydrological processes and their influence on the water balance of a mountainous and data-sparse catchment in Chile are observed and modeled through the comparison of a stationary (time-invariant parameters) and dynamic (time-variant parameters) model. Since conceptual models are the most adequate option for a data-scarce basin, a conceptual model integrated with the Monte Carlo Analysis Toolbox is used to perform the analyses. Simple analyses aimed at increasing the amount of information obtained from models were used. The General and Dynamic Identifiability Analyses were used to perform stationary and dynamic calibration strategies, respectively. As a result we concluded that the dynamic model is more robust than the stationary one. Additionally, DYNIA helped us to observe the temporal variability of hydrological processes. This analysis contributed to a better understanding of hydrological processes in a data-sparse Andean catchment and thus could potentially help reduce uncertainties in the outputs of hydrological models under scenarios of climate change and/or variability. [ABSTRACT FROM AUTHOR]

The hydrology of scarce-data areas, such as the mountainous area of the Andes, is poorly known mainly owing to the lack of data. Global gridded climatological datasets (GGCDs) are becoming more precise and common, but the utility of these datasets and their applicability to complex hydrological systems are still not yet well determined. In this paper the reliability of a GGCD is evaluated as an alternative source to supply the lacking in situ observations, with the aim of studying the hydrology of a mountainous area in south-central Chile. The GGCDs are found to recover the climate variability in Andean areas, and partially recover the orographic effect caused by the mountains. A finding of practical relevance is that GGCDs could be considered as an adequate source for performing hydrological models and studies under high spatial variability and scarce-data environments such as the Andes. [ABSTRACT FROM AUTHOR]