956 resultados para Rocky Shores


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Rock mass classification systems are widely used tools for assessing the stability of rock slopes. Their calculation requires the prior quantification of several parameters during conventional fieldwork campaigns, such as the orientation of the discontinuity sets, the main properties of the existing discontinuities and the geo-mechanical characterization of the intact rock mass, which can be time-consuming and an often risky task. Conversely, the use of relatively new remote sensing data for modelling the rock mass surface by means of 3D point clouds is changing the current investigation strategies in different rock slope engineering applications. In this paper, the main practical issues affecting the application of Slope Mass Rating (SMR) for the characterization of rock slopes from 3D point clouds are reviewed, using three case studies from an end-user point of view. To this end, the SMR adjustment factors, which were calculated from different sources of information and processes, using the different softwares, are compared with those calculated using conventional fieldwork data. In the presented analysis, special attention is paid to the differences between the SMR indexes derived from the 3D point cloud and conventional field work approaches, the main factors that determine the quality of the data and some recognized practical issues. Finally, the reliability of Slope Mass Rating for the characterization of rocky slopes is highlighted.

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At the June 2015 European Council, European leaders were meant to come to an agreement in order to help Italy and Greece cope with the increasing number of migrants and asylum seekers arriving on their shores. They were invited to give their agreement on a proposal from the European Commission to set up a mandatory relocation scheme, i.e. a scheme defining the precise number of asylum seekers that should be relocated to each member state over the next two years.

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The March 2016 EU Summit was yet another attempt to make progress on managing the EU’s migration/refugee crisis. In this post-summit analysis, Janis A. Emmanouilidis argues that the EU-Turkey deal, which foresees a return of migrants from Greece to Turkey and a direct resettlement of Syrians from Turkey to the EU on the grounds of a ‘1-for-1’ scheme, is a key and necessary element in a very complex puzzle trying to stop ‘irregular routes’ of migration. The ultimate success of this agreement is by no means certain, but it has the chance to reduce the number of people arriving at the shores of Europe. However, this would neither settle the crisis nor will it provide an adequate response to those in need of international protection. The ‘humanitarian imperative’ requires that the EU-Turkey deal is complemented by a much more ambitious direct resettlement scheme and other long-term measures as part of a comprehensive plan aiming to balance ‘solidarity and security’ in an effort to sustainably overcome the crisis.

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Um destino de sol e praia, nos dias de hoje, trava uma luta constante para manter ou criar atributos que sejam capazes de atrair turistas às suas costas; torna-se por isso importante conhecer o que permite deixar todos esses turistas “agarrados” ao destino promovendo a volta ao mesmo, tantas vezes quantas as possíveis. Explorar os níveis de lealdade apresentados por (Oliver, 1999) num destino como o Algarve numa tentativa de perceber a persistência deste tipo de destinos, focando neste caso os turistas não residentes, pela importância que este tipo de mercados representa para a sustentabilidade do destino. Pretende-se perceber o que influencia a duração da estadia e a relação do turista com o destino – compromisso - e como se relacionam com aquelas construções teóricas, recorrendo à Análise de Equações Estruturais para a sua concretização, tentando contribuir desta forma para a compreensão das dinâmicas que continuam a promover a escolha destes destinos nos dias de hoje.

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Macrofossil series from mountainous and polar areas such as the Alps, the Scandes, and the Rocky Mountains provide useful information about the late Quaternary course of treelines. Reconstructions of past treeline positions and compositions after the Ice Age can be used to infer paleoclimatic information or to study treeline ecosystem responses to (rapid) climatic change. Both approaches are illustrated by study cases. In addition to these paleoclimatic and paleoecological issues, macrofossil records can be used to validate dynamic treeline vegetation models. An example from the Alps shows the high potential of such a procedure towards applying forest-succession models for assessing future vegetation dynamics at treeline.

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Volumes of Holocene (10 000 years) terrigenous sediments and annnal sediment supply in the Laptev Sea were evaluated from average thickness of the Holocene veneer. Volumes of deposits supplied from various sediment sourees and by different proeesses (abrasion of hinterland and island shores, river discharge, eolian input, drifting ice) were diseriminating of deposition in the eoastal zone, at river/sea barrier, and in the shelf basin itself. Accumulation by drifting iee and the role of local sea bottom erosion were also considered. Total amount of sediments transported from the Laptev Sea shelf to Amundsen and Nansen Basins of the Aretie Ocean was compared with other Russian Aretie seas.

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A method was developed to extract adenine nucleotides AMP, ADP, and ATP from marine macroalgal tissue to gain information on the cellular energy charge. Quantification was carried out by high performance liquid chromatography (HPLC). Three species from the rocky shore of the island of Helgoland (German Bight) were examined: Laminaria saccharina (Phaeophyta), Chondrus crispus (Rhodophyta), and Ulva lactuca (Chlorophyta). In L. saccharina and C. crispus, the adenylate energy charge (AEC) was determined in different thallus regions. AEC varied in relation to tissue age and function. Higher AEC values typically occurred in thallus regions with meristematic activity. Furthermore, L. saccharina and U. lactuca were exposed to UV-A and elevated UV-B radiation. The AEC was calculated and the maximal quantum yield of photosystem II (Fv/Fm) was determined as indicators for UV stress. In both species, the AEC remained at high values (0.72 ± 0.04), while Fv/Fm dropped rapidly. The results show that the photosynthesis of the phaeophyte is more resistant to UV radiation than the chlorophyte.

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Includes bibliographical references.

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A mathematical model for long-term, three-dimensional shoreline evolution is developed. The combined effects of variations of sea level; wave refraction and diffraction; loss of sand by density currents during storms, by rip currents, and by wind; bluff erosion and berm accretion; effects of manmade structures such as long groin or navigational structures; and beach nourishment are all taken into account. A computer program is developed with various subroutines which permit modification as the state-of-the-art progresses. The program is applied to a test case at Holland Harbor, Michigan. (Author).

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Beach profile lines at 21 near-evenly spaced intervals along Holden Beach, North Carolina, between Lockwoods Folly and Shallotte Inlets, were measured from November 1970 to December 1974. These have been analyzed to determine the spatial and temporal variabilities on long-term, seasonal, and short-term scales. Profile lines near the inlets showed the greatest variability in mean sea level (MSL) position, above MSL volume, foreshore slope, and profile envelope. This variability near Lockwoods Folly Inlet was partly enhanced by artificial nourishment at profile line 2. Temporary, low-cost shore protection devices (e.g., sandbag groins) were constructed near that inlet during part of the study. No other modifications or activities that affected beach processes were known to occur during the study period. The central part of Holden Beach was studied separately because of the high variability of the inlet sections at either end of the island. Foreshore slopes along this reach increased from an average of 1:30 at the east end to 1:17 at the west. A seasonal change in above MSL volume indicates loss of sand during autumn and winter, and gain during spring and summer. Changes in MSL shoreline intercept and above MSL volume were highly variable during the study.

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Federal Highway Administration, Washington, D.C.

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Federal Highway Administration, Washington, D.C.

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National Highway Traffic Safety Administration, Washington, D.C.

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Papers from the 11th Wildland Shrub Symposium, held at the Bringham Young University Conference Center, Provo, Utah, June 13-15, 2000.