Coastal lagoons and their watersheds as GWDE: a case study in the southwest coast of Portugal

The study of groundwater dependent ecosystems opened the opportunity to involve specialists of different areas of knowledge in order to obtain answers for complex interrelations between groundwater and the associated ecosystems. The actual study, carried out in two coastal lagoons of the Portuguese SW coast, showed the high dependency of the marine life and vegetation of the lagoons and associated streams discharging in the lagoons on the fresh water supply of these two lagoons and the high contribution they receive from groundwater in the dry period, which corresponds to more than half of each hydrologic year. Every year, the lagoons are artificially opened to the ocean for a few days to a few weeks, which dramatically changes the inside salinity. The sensitivity of these ecological niches is demonstrated by the strong dependence that some species that are more sensitive to high salinity waters show in relation to the entrance of freshwater resultant from the discharge of the phreatic aquifer of Sines sedimentary Basin. The great biodiversity of these lagoons and its precarious balance is only possible to preserve if the aquifer continue to act as a regulatory factor of the lagoon’s salinity. The equilibrium can be changed in the event of overexploitation of the phreatic aquifer, which is not at risk in the near future. In a scenario of climate change the lagoons will benefit from a slow increase in groundwater contribution, due to the rise of sea level, which will be accompanied by a rise in groundwater levels in the aquifer near the sea.

TECTONIC CONTROLS ON FLUVIAL LANDSCAPE DEVELOPMENT IN CENTRAL-EASTERN PORTUGAL: INSIGHTS FROM LONG PROFILE TRIBUTARY STREAM ANALYSES

This study examines the long profiles of tributaries of the Tejo (Tagus) and Zêzere rivers in central eastern Portugal (West Iberia) in order to provide new insights into the patterns, timing and controls on drainage development during the Pleistocene to Holocene incision stage. The long profiles were extracted from lower order tributary streams associated with the trunk drainage of the Tejo River and one main tributary, the Zêzere River (Fig. 1). These streams flow through a landscape strongly influenced by variations in bedrock lithology (mainly granites and metasediments), fault structures delimiting crustal blocks with distinct uplift rates, and a base-level lowering history (tectonic uplift / eustatic). The long profiles of the tributaries of the Tejo and Zêzere rivers record a series of transient and permanent knickpoints. The permanent knickpoints have direct correlation with the bedrock strength, corresponding to the outcropping of very hard quartzites or to the transition from softer (slates/metagreywaques) to harder (granite) basement. The analyzed streams/rivers record also an older transient knickpoint/knickzone separating: a) an upstream relict graded profile, with lower steepness and higher concavity, that reflects a long period of quasi-equilibrium conditions reached after the beginning of the incision stage; and b) a downstream reach displaying a rejuvenated long profile, with steeper gradient and lower concavity, particularly for the final segment, which is often convex (Fig. 2). The rejuvenated reaches testify the upstream propagation of several incision waves that are the response of each stream to continuous or increasing crustal uplift and dominant periods of base-level lowering by the trunk drainages, coeval of low sea level conditions. The long profiles and their morphological configurations enabled spatial and relative temporal patterns of incision to be quantified for each individual tributary stream. The incision values of streams flowing in uplifted blocks of the Portuguese Central Range (PCR) (ca.380-280 m) indicate differential uplift and are higher than the incision values of streams flowing on the adjacent South Portugal planation surface – the Meseta (ca. 200 m). The normalized steepness index, calculated using the method of Wobus et al. (2006), proved to be sensitive to active tectonics, as lower ksn values were found in relict graded profiles of streams located in less uplifted blocks, (e.g. Sertã stream in the PCR), or in those flowing through tectonic depressions. Fig. 1 – Geological map of the study area. 1 – fluvial terraces (Pleistocene); 2 – sedimentary cover (Paleogene and Neogene); 3 – slates and metasandstones (Devonian); 4 – slates and quartzites (Silurian); 5 – quartzites (Ordovician); 6 – slates and metagreywackes (Precambrian to Cambrian); 7 – slates, metagreywackes and limestones (Precambrian); 8 – granites and ortogneisses; 9 – diorites and gabros; 10 - fault. SFf – Sobreira Formosa fault; Sf – Sertã fault; Pf – Ponsul fault; Gf – Grade fault. The differential uplift indicated by the distribution of the ksn values and by the fluvial incision was likely accumulated on a few major faults, as the Sobreira Formosa fault (SFf), thus corroborating the tectonic activity of these faults. Due to the fact that the relict graded profiles can be correlated with other geomorphic references documented in the study area, namely the T1 terrace of the Tagus River (with an age of ca. 1 Myr), the following incision rates can be estimated: a) for the studied streams located in uplifted blocks of the PCR, 0.38 m/kyr to 0.28 m/kyr; b) for the streams flowing on the South Portugal planation surface, 0.20 m/kyr. The differential uplift inferred between crustal blocks in the study area corroborates the neotectonic activity of the bordering faults, which has been proposed in previous studies based upon less robust data. Fig. 2 – Longitudinal profile of the Nisa stream a tributary of the Tejo River. Note the equilibrium relict profile upstream the older transient knickpoint (hatched line) and the downstream rejuvenated profile (continuous line). Legend: tKP – transient knickpoint; rKp – resistant knickpoint; Mt – schist and phyllite; Gr – granite; Hf – hornfels; Og – orthogneisse. In the inset Distance – Slope plots, fill circles correspond to the relict graded profile, crosses correspond to the rejuvenated profile located downstream the older transient knickpoint (tKP).

Spirituality in the Undergraduate Curricula of Nursing Schools in Portugal and São Paulo-Brazil

Spirituality is considered a dimension of nursing care, which is often recognized as being neglected, mainly due to a lack of education. Several studies have addressed nursing students’ perceptions and skills for providing spiritual care, but there is little evidence on how spirituality is addressed in undergraduate nursing curricula. This study comprised Portuguese and Brazilian nursing schools (from São Paulo) and describes how spirituality is addressed in undergraduate nursing curricula. It is descriptive and the survey research was performed in 2014–2015. The questionnaire was composed of closed and open-ended questions and was sent by e-mail. A total of 129 answers were obtained, mostly from Portugal. Results indicated that several curricular units include spirituality, although having different contents. The learning outcomes are consistent with improving nursing students’ integral education, developing the clinical reasoning regarding spirituality, and improving the assessment of the patient across the life span. Nevertheless, it seems that spirituality is poorly addressed in clinical practice. Few nursing schools have courses or curricular units specifically dealing with spirituality, but they do provide some form of teaching on the subject. No standard curriculum exists, but teachers believe that it is a very important subject that should be included in the courses taught.

DNI Measurements in the South of Portugal: Long Term Results through Direct Comparison with Global and Diffuse Radiation Measurements and Existing Time Series

The present work describes the measurement effort for direct normal irradiance (DNI) evaluation in the sunny south of Portugal, with a network of eight radiation measurement stations in several locations (including Évora) providing a good coverage of the region. This new initiative for DNI measurement will still need many years (typically 10 or more) to produce a time series which can claim having long term statistical value. This problem can, however, be temporarily mitigated by measuring DNI at the same time as GHI and DHI, in a place where long term series dating back, already exist for those two. It so happens that a long term series (20 years) of global and diffuse solar irradiation exists for the location Évora. So the expectation is to establish correlations with the goal of attributing at least some long term statistical significance to the short and recent DNI series. The paper describes the setup of the measuring stations and presents the preliminary measurements obtained. It further presents the first correlations of monthly averages between normal beam (DNI), global and diffuse radiation. It then uses these correlations, admittedly without acceptable statistical significance (short series of less than one year of measured data), to exemplify how to get a prediction of long term DNI for Évora. This preliminary obtained value is compared to that predicted by the commercial data from Meteonorm.

Tectonic and lithological controls on fluvial landscape development in central-eastern Portugal: Insights from long profile tributary stream analyses

This study examines the long profiles of tributaries of the Tagus and Zêzere rivers in Portugal (West Iberia) in order to provide new insights into patterns, timing, and controls on drainage development during the Quaternary incision stage. The studied streams are incised into a relict culminant fluvial surface, abandoned at the beginning of the incision stage. The streams flow through a landscape with bedrock variations in lithology (mainly granites and metasediments) and faulted blocks with distinct uplift rates. The long profiles of the analyzed streams record an older transitory knickpoint/knickzone separating (1) an upstream relict graded profile, with lower steepness and higher concavity, that reflects a long period of quasi-equilibrium conditions reached after the beginning of the incision stage, and (2) a downstream rejuvenated long profile, with steeper gradient and lower concavity, particularly for the final reach, which is often convex. The rejuvenated reaches testify to the upstream propagation of several incision waves, interpreted as the response of each stream to increasing crustal uplift and prolonged periods of base-level lowering by the trunk drainages, coeval with low sea level conditions. The morphological configurations of the long profiles enabled spatial and relative temporal patterns of incisions to be quantified. The incision values of streams flowing on the Portuguese Central Range (PCR; ca. 380–150 m) are variable but generally higher than the incision values of streams flowing on the adjacent South Portugal Planation Surface (SPPS; ca. 220–110 m), corroborating differential uplift of the PCR relative to the SPPS. Owing to the fact that the relict graded profiles can be correlated with the Tagus River T1 terrace (1.1–0.9 My) present in the study area, incision rates can be estimated (1) for the streams located in the PCR, 0.38–0.15 m/ky and (2) for the streams flowing on the SPPS, 0.22–0.12 m/ky. The differential uplift inferred in the study area supports the neotectonic activity of the bordering faults, as proposed in previous studies based upon other geological evidence.

Contribution to the diffuse radiation modelling in Évora, Portugal

Solar radiation data is crucial for the design of energy systems based on the solar resource. Since diffuse radiation measurements are not always available in the archive data series, either due to the inexistence of measuring equipment, shading device misplacement or missing data, models to generate these data are needed. In this work, one year of hourly and daily horizontal solar global and diffuse irradiation measurements in Évora are used to establish a new relation between the diffuse radiation and the clearness index. The proposed model includes a fitting parameter, which was adjusted through a simple optimization procedure to minimize the Least Square Error as compared to measurements. A comparison against several other fitting models presented in the literature was also carried out using the Root Mean Square Error as statistical indicator, and it was found that the present model is more accurate than the previous fitting models for the diffuse radiation data in Évora.

Annual Average Value of Solar Radiation and its Variability in Portugal

Solar resource assessment is essential for the different phases of solar energy projects, such as preliminary design engineering, financing including due diligence and, later, insurance phases. An important aspect is the long term resource estimation. This kind of estimation can only be obtained through the statistical analysis of long-term data series of solar radiation measurements, preferably ground measurements. This paper is a first step in this direction, with an initial statistical analysis performed over the radiation data from a national measurement network, consisting of eighty-nine meteorological stations. These preliminary results are presented in figures that represent the annual average values of Global Horizontal Irradiation (GHI) and its Variability in the Portuguese continental territory. These results show that the South of Portugal is the most suitable area for the implementation of medium to large scale solar plants.

Inversion of ambient seismic noise HVSR to evaluate velocity and structural models of the Lower Tagus Basin, Portugal

During its history, several significant earthquakes have shaken the Lower Tagus Valley (Portugal). These earthquakes were destructive; some strong earthquakes were produced by large ruptures in offshore structures located southwest of the Portuguese coastline, and other moderate earthquakes were produced by local faults. In recent years, several studies have successfully obtained strong-ground motion syntheses for the Lower Tagus Valley using the finite difference method. To confirm the velocity model of this sedimentary basin obtained from geophysical and geological data, we analysed the ambient seismic noise measurements by applying the horizontal to vertical spectral ratio (HVSR) method. This study reveals the dependence of the frequency and amplitude of the low-frequency (HVSR) peaks (0.2–2 Hz) on the sediment thickness. We have obtained the depth of the Cenozoic basement along a profile transversal to the basin by the inversion of these ratios, imposing constraints from seismic reflection, boreholes, seismic sounding and gravimetric and magnetic potentials. This technique enables us to improve the existing three-dimensional model of the Lower Tagus Valley structure. The improved model will be decisive for the improvement of strong motion predictions in the earthquake hazard analysis of this highly populated basin. The methodology discussed can be applied to any other sedimentary basin.

Estudo da sismicidade em Portugal no período 1300-2014: mapa de intensidade máxima observada (IMO).

O estudo da sismicidade em Portugal ao longo de várias centenas de anos é essencial para uma melhor avaliação do risco sísmico ao qual o continente está sujeito. Neste trabalho, a organização de diversas fontes históricas e atuais numa base de dados possibilita validar facilmente a ocorrência de eventos sísmicos no período desde 1300 a 2014. A construção de um mapa de intensidades máximas observadas neste período permite mostrar que todo o território Português esteve sujeito a sismos com Io≥V. Existem também registos de grandes eventos sísmicos, concentrados em pequenas áreas, que causaram danos consideráveis. De destacar ainda o impacto dos sismos com epicentro no mar, nas cidades costeiras, no Centro e Sul do país.

Intensidades máximas observadas nos Açores (Portugal): resultados preliminares.

O Arquipélago dos Açores é uma região sismicamente activa. Desde o seu povoamento no séc. XV o arquipélago foi afectado por 33 sismos de intensidade máxima (Io) ≥ VII. O obejctivo é apresentar o primeiro mapa de intensidades máximas observadas (IMO) do arquipélago dos Açores. A elaboração do IMO visa identificar as áreas afectadas no passado por eventos de grande magnitude. Do catálogo sísmico (1915-2003) foram selecionados as intensidades máxima dos eventos ≥ V. Foram adicionados 14 sismos históricos com Io ≥ VII que ocorreram entre 1522 e 1912. Os clusters sísmicos associados a erupções vulcânicas (1957/58 e 1964) assim como réplicas foram removidos para evitar o enviesamento dos resultados. Utilizou-se o método de krigagem ([1], [2]) para fazer a interpolação para obter os valores de intensidade dos pontos desconhecidos com base dos pontos e intensidades conhecidas. O mapa IMO mostra que a parte oriental das ilhas de São Jorge e Graciosa têm os valores de intensidade mais elevados, XI e IX, respectivamente. Nas ilhas da Terceira e Pico as IMO, com intensidades VIII e VII, respectivamente, estão limitadas aos extremos oriental e ocidental. No Faial, uma faixa com direcção NW-SE apresenta os valores de intensidade (X) mais elevada. Em S. Miguel as IMO (VII e X) estão localizadas na parte ocidental, sudeste e norte da ilha. Por fim, só a parte oriental da ilha de Santa Maria apresenta os valores mais elevados de IMO (VI). Não apresentamos resultados para as ilhas Flores e Corvo, devido à reduzida sismicidade que não preenche os critérios estabelecidos para a selecção de sismos com Io ≥ V. Os mapas IMO não têm capacidade para descriminar os efeitos de sítio, apesar de mostrarem as áreas com elevado movimento do solo.

Solar and thermal radiative effects during the 2011 extreme desert dust episode over Portugal

This paper analyses the influence of the extreme Saharan desert dust (DD) event on shortwave (SW) and longwave (LW) radiation at the EARLINET/AERONET Évora station (Southern Portugal) from 4 up to 7 April 2011. There was also some cloud occurrence in the period. In this context, it is essential to quantify the effect of cloud presence on aerosol radiative forcing. A radiative transfer model was initialized with aerosol optical properties, cloud vertical properties and meteorological atmospheric vertical profiles. The intercomparison between the instantaneous TOA shortwave and longwave fluxes derived using CERES and those calculated using SBDART, which was fed with aerosol extinction coefficients derived from the CALIPSO and lidar-PAOLI observations, varying OPAC dataset parameters, was reasonably acceptable within the standard deviations. The dust aerosol type that yields the best fit was found to be the mineral accumulation mode. Therefore, SBDART model constrained with the CERES observations can be used to reliably determine aerosol radiative forcing and heating rates. Aerosol radiative forcings and heating rates were derived in the SW (ARFSw, AHRSw) and LW (ARFLw, AHRLw) spectral ranges, considering a cloud-aerosol free reference atmosphere. We found that AOD at 440 nm increased by a factor of 5 on 6 April with respect to the lower dust load on 4 April. It was responsible by a strong cooling radiative effect pointed out by the ARFSw value (−99 W/m2 for a solar zenith angle of 60°) offset by a warming radiative effect according to ARFLw value (+21.9 W/m2) at the surface. Overall, about 24% and 12% of the dust solar radiative cooling effect is compensated by its longwave warming effect at the surface and at the top of the atmosphere, respectively. Hence, larger aerosol loads could enhance the response between the absorption and re-emission processes increasing the ARFLw with respect to those associated with moderate and low aerosol loads. The unprecedented results derived from this work complement the findings in other regions on the modifications of radiative energy budget by the dust aerosols, which could have relevant influences on the regional climate and will be topics for future investigations.

EFEITOS DE CENÁRIOS DE USO DO SOLO NA VAZÃO E PRODUÇÃO DE SEDIMENTOS NA BACIA DO RIO COBRES, PORTUGAL

Introdução Caracterização da área de estudo Materiais e métodos O modelo SWAT Dados de chuva, vazão e produção de sedimentos Tipos de solos e determinação dos parâmetros do SWAT Análises Estatísticas Cenários de Uso do Solo Resultados e discussões Estimativa da Vazão Estimativa da produção de sedimentos Modelagem Hidrossedimentológica em Diferentes Cenários Conclusões Referências bibliográficas RESUMO – A erosão dos solos é um dos mais graves problemas ambientais em todo o mundo, principalmente em regiões semiáridas que sofrem com a variabilidade espaço-temporal da precipitação. Este artigo analisou os processos hidrossedimentológicos na Bacia do Rio Cobres, localizada na porção semiárida de Portugal, utilizando o modelo SWAT. Neste estudo foram utilizados dados diários de precipitação, temperatura, umidade do ar, vazão e produção de sedimentos, para o período de 1960 a 2000, mapas digitais de elevação do terreno com resolução espacial de 90 m, uso e ocupação do solo e tipos de solo da bacia. Os resultados demonstraram a eficácia do modelo na calibração da vazão, com Coeficiente de Determinação (R²) = 0,81 e Coeficiente de Nash-Sutcliffe (NS) = 0,63, e também para produção de sedimentos com R² = 0,62 e NS = 0,47. O Cenário 3 (Mata) apresentou o maior decréscimo na vazão média, em relação aos Cenários 1 (Real) e 2 (Pastagem). Conclui-se que o modelo SWAT acoplado ao SIG é uma ferramenta poderosa na análise espaço-temporal do comportamento dos processos hidrossedimentológicos. Palavas-chave: SIG, modelo hidrossedimentológico, erosão ABSTRACT – Effects of Scenarios of Land Use on Runoff and Sediment Yield for Cobres River Basin, Portugal. Soil erosion is a major environmental problem worldwide, mainly in semiarid regions that suffer with rainfall spatial and temporal variability. Thus, this paper analysed the runoff-erosion process at the Cobres River Basin, located in semiarid portion of Portugal, using the SWAT model. In this paper, rainfall, temperature and humidity data from 1960 to 2000, and digital maps of land cover, terrain digital elevation model with spatial resolution of 90 m, soil types were used. The results showed the effectiveness of the model for the runoff calibration, with R² = 0.81 and NS = 0.63, and also for sediment yield with R² = 0.62 and NS = 0.47. Scenario 1 (Forest) had the highest decrease in average streamflow, in relation to the Scenarios 1 (Real) and 2 (Pasture) scenarios. It is concluded that the SWAT model coupled to GIS is a powerful tool in the analysis of temporal and spatial behaviour of runoff-erosion processes.

As rotas Jacobeias em Portugal : estudo e divulgação do caso alentejano. Proposta de valorização - criação de um museu virtual e de um centro de interpretação

As peregrinações, entre elas a Santiago de Compostela, marcaram profundamente a sociedade europeia. Além das questões religiosas, os caminhos de Santiago originaram a criação de uma rede de infraestruturas que permitiu o desenvolvimento de regiões e aglomerados urbanos. Para provar a importância desses caminhos no distrito de Évora partimos de uma abordagem aos testemunhos patrimoniais evocando S. Tiago (móveis e imóveis, materiais e imateriais), procurando, como objectivo da Dissertação de Mestrado, conceber um projecto para divulgação da informação recolhida. Assim, sabendo que a sociedade actual exige mais informação visual na compreensão do legado cultural, optámos pela criação de um Museu Virtual e de um Centro de Interpretação. Se os Museus Virtuais oferecem inúmeras possibilidades de acesso às manifestações culturais, possibilitando ainda a formação através de tecnologias aplicadas na educação, os Centros de Interpretação criam condições de acolhimento e visita adequadas, fornecendo informações essenciais na compreensão e valorização dos legados patrimoniais. ABSTRACT: The pilgrimages, among them Santiago de Compostela, profoundly marked European society. ln addition to religious matters, the Way of Saint James led to the creation of a network infrastructure that enabled the development of regions and urban areas. To prove the importance of these pathways in the district of Évora part of an asset with reference to testimonies S. James (movable and immovable, tangible and intangible), for such purpose the master's thesis, designing a project to disseminate the information collected. So, knowing that society is demanding more visual information to understand the cultural legacy, we decided to create a Virtual Museum and an Interpretation Center. lf the Virtual Museums offer many opportunities for access to cultural events and can therefore training through technologies applied to education, the Centers for Interpretation create conditions for the reception and visit appropriate, providing key information in understanding and appreciation of legacies.

Study of Atlantic chub mackerel's (Scomber colias, Gmelin, 1789) landings evolution in Portugal: importance for purse seine fleet

The Portuguese purse seine fishery could be sustainable if measures to promote multi-specify catches are placed. Chub mackerel is one of the top three species landed by purse seine and landings have been increasing, which could be partly explained by Docapesca’s campaign promoting chub mackerel consumption. Therefore, it is necessary to understand if chub mackerel could represent a sustainable alternative. Results point to overexploitation levels, already exceeding estimated Maximum Sustainable Yield (MSY). The break point was registered in 2011, when chub mackerel landings surpassed 30 thousand tonnes landed, which is far beyond MSY estimates by Schaefer’s (24 703 ton), Gulland’s (21 750 ton) and Cadima’s (23 250 ton) models. Chub mackerel could represent an alternative to purse seine fisheries if: (i) a catch limit is established; (ii) measures to promote a regulated market on supply and demand laws are placed; (iii) research investment is augmented; Estudo da evolução dos desembarques de cavala (Scomber colias, Gmelin, 1782) em Portugal: sua importância para a pesca de cerco. Resumo: A pesca de cerco em Portugal poderá ser sustentável se forem implementadas medidas para a sua diversificação. A cavala é uma das três espécies mais capturadas pelo cerco, tendo-se observado um aumento dos desembarques nos últimos anos, parte explicado pela campanha focada no seu consumo, promovida pela Docapesa. Torna-se necessário compreender se a cavala poderá constituir uma alternativa sustentável. Os resultados apontam para níveis de exploração acima do Rendimento Máximo Sustentável (RMS) estimado, atingido em 2011, quando os desembarques de cavala ultrapassaram as 30 mil toneladas, acima do RMS estimado de acordo com Schaefer (24 703 ton), Gulland (21 750 ton) e Cadima (23 250 ton), mantendo-se a tendência de sobre-exploração. A cavala poderá ser uma alternativa para o cerco se: (i) estabelecido um limite de captura; (ii) criadas medidas de promoção de um mercado regulado pela lei da oferta e da procura (iii) aumentar o investimento em investigação.

The Impacts of Climate Change on Irrigated Agriculture in Southern Portugal

Climate change projections point to increasing air temperature and reduced precipitation in southern Portugal, which would affect farming systems. This study aims to assess the impacts of climate change on irrigated agriculture in southern Portugal. These impacts were assessed by combining climate model data with a soil water balance model and a numerical model for the design of irrigation systems. Meteorological data from two weather stations were used along with three climate models (HadRM3P, HIRHAMh and HIRHAMhh; 2071–2100). The crop rotations studied included sugar beet–maize–tomato–wheat and sunflower–wheat–barley. Two adaptation measures were considered: (i) maintaining the current crop varieties; (ii) using new crop varieties. The results from the considered climate change scenarios indicated that the impacts of climate change on irrigation requirements depend on the adopted adaptation measures. On average, the seasonal irrigation requirements increased by 13–70% when new crop varieties were used and by −13 to 7% when the current crop varieties were maintained. The impacts of climate change on irrigation system design were considerable, with the design flow rate increasing by 5–24%.