3,125 research outputs found

    Ensemble Modeling Informs Hypoxia Management In The Northern Gulf Of Mexico

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    A large region of low-dissolved-oxygen bottom waters (hypoxia) forms nearly every summer in the northern Gulf of Mexico because of nutrient inputs from theMississippi River Basin andwater column stratification. Policymakers developed goals to reduce the area of hypoxic extent because of its ecological, economic, and commercial fisheries impacts. However, the goals remain elusive after 30 y of research and monitoring and 15 y of goal-setting and assessment because there has been little change in river nitrogen concentrations. An intergovernmental Task Force recently extended to 2035 the deadline for achieving the goal of a 5,000-km(2) 5-y average hypoxic zone and set an interim load target of a 20% reduction of the spring nitrogen loading from the Mississippi River by 2025 as part of their adaptive management process. The Task Force has asked modelers to reassess the loading reduction required to achieve the 2035 goal and to determine the effect of the 20% interim load reduction. Here, we address both questions using a probabilistic ensemble of four substantially different hypoxia models. Our results indicate that, under typical weather conditions, a 59% reduction in Mississippi River nitrogen load is required to reduce hypoxic area to 5,000 km(2). The interim goal of a 20% load reduction is expected to produce an 18% reduction in hypoxic area over the long term. However, due to substantial interannual variability, a 25% load reduction is required before there is 95% certainty of observing any hypoxic area reduction between consecutive 5-y assessment periods

    Genome Sequence of Magnetospirillum magnetotacticum Strain MS-1

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    Here, we report the genome sequence of Magnetospirillum magnetotacticum strain MS-1, which consists of of 36 contigs and 4,136 protein-coding genes

    Ensemble modeling informs hypoxia management in the northern Gulf of Mexico

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    A large region of low-dissolved-oxygen bottom waters (hypoxia) forms nearly every summer in the northern Gulf of Mexico because of nutrient inputs from theMississippi River Basin andwater column stratification. Policymakers developed goals to reduce the area of hypoxic extent because of its ecological, economic, and commercial fisheries impacts. However, the goals remain elusive after 30 y of research and monitoring and 15 y of goal-setting and assessment because there has been little change in river nitrogen concentrations. An intergovernmental Task Force recently extended to 2035 the deadline for achieving the goal of a 5,000-km(2) 5-y average hypoxic zone and set an interim load target of a 20% reduction of the spring nitrogen loading from the Mississippi River by 2025 as part of their adaptive management process. The Task Force has asked modelers to reassess the loading reduction required to achieve the 2035 goal and to determine the effect of the 20% interim load reduction. Here, we address both questions using a probabilistic ensemble of four substantially different hypoxia models. Our results indicate that, under typical weather conditions, a 59% reduction in Mississippi River nitrogen load is required to reduce hypoxic area to 5,000 km(2). The interim goal of a 20% load reduction is expected to produce an 18% reduction in hypoxic area over the long term. However, due to substantial interannual variability, a 25% load reduction is required before there is 95% certainty of observing any hypoxic area reduction between consecutive 5-y assessment periods

    Advanced 3D modeling versus Building Information Modeling: the case study of Palazzo Ettoreo in Sacile (Italy)

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    This paper presents an experience of 3D modeling starting from laser scanning data and following two alternative approaches: the first one, called \u201cAdvanced 3D modeling\u201d, based on an original meshing algorithm, while the second make use of Revit BIM software. The case study in Palace Ettoreo in Sacile (Pordenone, Italy), constructed in Renaissance Venetian style in the 16th century: it has a trapezoid plan and is developed on three floors, with the ground one endowing a portico on two fa\ue7ades. The palace has been surveyed by two terrestrial laser scanners: a Riegl Z420i for 5 external scans and a FARO Photon 120 for 53 internal scans; also a topographic surveying of 270 targets have been carried out. The final TLS cloud has 1,4 billions of points. The Advanced 3D modeling has produced a \u201csmart\u201d mesh, allowing also to model the elements with deformations (out of plumb, bulges and troughs). Moreover, this model drastically reduce the stored data: the whole palace is modeled by 111.496 polygons only. The modeling with Revit follows the classical flowchart where the principal architectonical elements are gradually composed: this HBIM process has required a strong manual work in exploiting the available parametric objects and/or in the definition of new objects. Comparing the two models with respect the points cloud, both have evidenced advantages and limitations: therefore, the best solution is a process involving their combination. At the beginning, the Advanced 3D modeling is performed onto the points cloud, so well exploiting the segmentation tools and the smart meshing of the surfaces preserving any geometrical irregularity. Such obtained model allows metrical and morphological evaluation on the various structural and architectonical elements. Afterwards, this very light model becomes the entry data for the modeling in BIM environment, where also the shape of irregular elements are so imported

    Draft Genome Sequence of Beneficial Rice Rhizosphere Isolate Pseudomonas aeruginosa PUPa3.

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    Published onlinePseudomonas aeruginosa PUPa3 is a rhizosphere-colonizing and plant growth-promoting strain isolated from the rhizosphere of rice. This strain has, however, been shown to be pathogenic in two nonmammalian infection models. Here we report the draft genome sequence of P. aeruginosa PUPa3.G.U. and M.K. were funded by the Ministry of Education, Science and Technological Development, Republic of Serbia (grant no. 173019). G.U. is also the beneficiary of FEMS Research Fellowship 2014-1. The laboratory of V.V. was financed by ICGEB core funding

    A Novel Approach for an Integrated Straw tube-Microstrip Detector

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    We report on a novel concept of silicon microstrips and straw tubes detector, where integration is accomplished by a straw module with straws not subjected to mechanical tension in a Rohacell ®^{\circledR} lattice and carbon fiber reinforced plastic shell. Results on mechanical and test beam performances are reported on as well.Comment: Accepted by Transactions on Nuclear Science (2005). 11 pages, 9 figures, uses lnfprep.st

    High-resolution tracking in a GEM-Emulsion detector

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    SHiP (Search for Hidden Particles) is a beam dump experiment proposed at the CERN SPS aiming at the observation of long lived particles very weakly coupled with ordinary matter mostly produced in the decay of charmed hadrons. The beam dump facility of SHiP is also a copious factory of neutrinos of all three kinds and therefore a dedicated neutrino detector is foreseen in the SHiP apparatus. The neutrino detector exploits the Emulsion Cloud Chamber technique with a modular structure, alternating walls of target units and planes of electronic detectors providing the time stamp to the event. GEM detectors are one of the possible choices for this task. This paper reports the results of the first exposure to a muon beam at CERN of a new hybrid chamber, obtained by coupling a GEM chamber and an emulsion detector. Thanks to the micrometric accuracy of the emulsion detector, the position resolution of the GEM chamber as a function of the particle inclination was evaluated in two configurations, with and without the magnetic fiel

    Reconstrucción histórica de glaciares en la Cordillera del Viento (Neuquén, Argentina)

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    En las últimas décadas, los estudios hidrológicos han trascendido por el rol que desempeñan en la gestión de los recursos hídricos, para el desarrollo sostenible y la adaptación a los cambios de las condiciones climáticas y medioambientales. En referencia a ello, los glaciares ocupan un lugar destacado a nivel mundial como indicadores de cambios climáticos. Las condiciones naturales propicias para formación de glaciares, generalmente se dan en áreas con terreno complejo y difícil acceso, por lo que hay baja disponibilidad de datos. Ello propició, la utilización de sensores remotos para estudios glaciológicos alrededor del mundo. En el norte de la Patagonia argentina, la Cordillera del Viento constituye una reserva de agua dulce, donde el estudio, monitoreo y protección de los cuerpos de hielo es necesaria. Este trabajo realizó la primera reconstrucción histórica de glaciares existentes en dicha región para el año 1963, para evaluar el estado de los cuerpos de hielo y sentar bases precedentes a la puesta en órbita de satélites de mediana/alta resolución. Se pretendió a su vez, una contribución a los diversos estudios glaciológicos que se están desarrollando actualmente en el territorio nacional. Se llevó a cabo un proceso de georreferenciación y ortorectificación de 38 fotografías aéreas analógicas de la Cordillera del Viento (120.0 km de longitud), con modernas técnicas fotogramétricas digitales. Posteriormente se analizaron parámetros morfométricos de los glaciares, siguiendo lineamientos definidos a nivel internacional. La reconstrucción definió la existencia en 1963 de 151 glaciares (5.94 km²), con morfologías propias de cuerpos estacionarios o en retroceso. Se identificaron 139 glaciares (4.33 km²) con una superficie de 0.01 a 0.1 km², 10 glaciares (1.20 km²) de 0.1 a 0.2 km² y 2 glaciares (0.40 km²) mayores a 0.2 km². Fueron desestimados del estudio previamente 31 cuerpos al considerarse bancos de nieve, mientras que otros 128 cuerpos (0.61 km²) no se consideraron sistemáticamente al no respetar la superficie mínima glaciar (mayor a 0.01 km²). Los cuerpos existentes en el Vn. Domuyo tampoco fueron considerados.Eje: Ciencias Hidrológicas y Criósfera.Facultad de Ciencias Astronómicas y Geofísica
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