229 research outputs found

    BUILDING INTEREST AND KNOWLEDGE IN GEOSCIENCES THROUGH PLACE- & FIELD-BASED TEACHER PROFESSIONAL LEARNING PROGRAMS: A COMPARATIVE MULTI-CASE STUDY

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    The focus of this study was to develop and evaluate a geoscience professional development model that would improve K-12 teachers’ capacity to effectively build geoscience literacy and interests in students from a variety of settings and cultural groups. The research compared the application of a geoscience professional development model realized through multiple case studies of varying settings and scales. The study investigated the capacity of each approach in improving teachers’ geoscience background knowledge, awareness of local geologically and culturally significant examples, and ability to integrate place-based, field investigations into standards-based curricula. By using both qualitative and quantitative methodologies, the study not only measured the successfulness of each approach but also identified the underlying reasons for specific outcomes. Cross-case study comparisons were made to identify emergent patterns utilized to improve the geoscience teacher professional development model. The outcome is a refined professional development model that can be universally applied to a diverse range of K-12 school communities. The ultimate aim of this work is to improve geoscience literacy, to develop a society with greater capacity to make informed decisions and to sustainably manage natural resources in the 21st century

    Nueva Normalidad en las Micro Unidades Económicas Turísticas de la Sierra Norte de Puebla

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    La actividad turística, una de las más dañadas en la Sierra Norte del Estado de Puebla (México) por la crisis del coronavirus COVID-19 provocó el cierre parcial o total de decenas de Micro Unidades Económicas (MUE), poblaciones como Cuetzalan del Progreso y Chignahuapan donde se realizó el presente estudio, reconocen que deberán adaptarse a las nuevas circunstancias, tanto en espacio, capacitación y difusión para mantener su presencia en los consumidores a través de sus servicios; de ahí que los giros empresariales como Hoteles, Tours, Restaurantes entre otros, deberán mantener una comunicación continua, información oportuna y adaptarse rápidamente a las normas que se dicten oficialmente en la materia con el fin de reinsertarlos a la dinámica económica de la región. Se realizó un análisis metodológico mixto de UE con giros turísticos, de donde se identificaron factores organizacionales externos, internos y de comunicación, cuyos resultados reflejaron numerosas áreas de oportunidad para una toma la de decisiones para diseñar y proponer estrategias de mercadotecnia, adaptadas a las tendencias internacionales que se toman debido a la afectación del SARS CoV2.   The COVID-19 crisis affected a lot of activities in the Sierra Norte of the State of Puebla (Mexico) including tourism activity. This resulted to the partial or total closure of dozens of Micro Economic Units (EUTM). This study was carried out in Cuetzalan del Progreso and Chignahuapan and they realised the need to adapt to the new circumstances both in space, training, and dissemination to maintain their consumers through their services. For this reason, business tours such as hotels and restaurants must maintain a continuous communication, timely information, and adapt quickly to the rules that are officially dictated in this field in order to reinsert them to the economic dynamics of the region. A mixed EU methodological analysis was carried out from which external, internal, and communication organizational factors were identified. This resulted to numerous areas of opportunity for decision-making to design and propose marketing strategies, which are adapted to international trends that are taken due to the involvement of SARS CoV2

    Emissions of BVOC from lodgepole pine in response to mountain pine beetle attack in high and low mortality forest stands

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    In this screening study, biogenic volatile organic compound (BVOC) emissions from intact branches of lodgepole pine (Pinus contorta) trees were measured from trees at two forested sites that have been impacted differently by the mountain pine beetle (MPB), with one having higher mortality and the other with lower mortality. Differences in the amounts and chemical diversity of BVOC between the two sites and from apparently healthy trees versus trees in different stages of MPB attack are presented, as well as (for one site) observed seasonal variability in emissions. A brief comparison is made of geological and climatic characteristics as well as prior disturbances (both natural and man-made) at each site. Trees sampled at the site experiencing high MPB-related tree mortality had lower chemodiversity in terms of monoterpene (MT) emission profiles, while profiles were more diverse at the lower-mortality site. Also at the higher-mortality site, MPB-infested trees in various stages of decline had lower emissions of sesquiterpenes (SQTs) compared to healthy trees, while at the site with lower mortality, MPB-survivors had significantly higher SQT emissions during part of the growing season when compared to both uninfested and newly infested trees. SQT profiles differed between the two sites and, like monoterpene and oxygenated VOC profiles, varied through the season. For the low-mortality site in which repeated measurements were made over the course of the early summer–late fall, higher chemical diversity was observed in early- compared to late-season measurements for all compound classes investigated (MT, oxygenated VOC, and SQT), with the amount of change appearing to correlate to the MPB status of the trees studied. Emissions of 2-methyl-3-buten-2-ol (MBO) had a distinct seasonal signal but were not much different between healthy or infested trees, except in trees with dead needles, from which emissions of this compound were negligible, and in late-season MPB survivors, in which they were higher than in newly infested or uninfested trees. Emissions of SQT were significantly higher in the MPB survivors during both mid- and late-season sampling at the low-mortality site. The changes in emissions could have implications for regional air quality and climate through changes in ozone and aerosol distributions, although this study was designed as a preliminary screening effort and not enough individuals were sampled for all of the observed differences to be statistically demonstrated. Despite this, the compelling differences in emissions observed between the sites and individual trees with differing MPB-infestation statuses and the potential impacts these have on regional atmospheric chemistry argue for further research in this topic

    A meteo-hydrological modelling system for the reconstruction of river runoff: the case of the Ofanto river catchment

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    Abstract. A meteo-hydrological modelling system has been designed for the reconstruction of long time series of rainfall and river runoff events. The modelling chain consists of the mesoscale meteorological model of the Weather Research and Forecasting (WRF), the land surface model NOAH-MP and the hydrology–hydraulics model WRF-Hydro. Two 3-month periods are reconstructed for winter 2011 and autumn 2013, containing heavy rainfall and river flooding events. Several sensitivity tests were performed along with an assessment of which tunable parameters, numerical choices and forcing data most impacted on the modelling performance.The calibration of the experiments highlighted that the infiltration and aquifer coefficients should be considered as seasonally dependent.The WRF precipitation was validated by a comparison with rain gauges in the Ofanto basin. The WRF model was demonstrated to be sensitive to the initialization time and a spin-up of about 1.5 days was needed before the start of the major rainfall events in order to improve the accuracy of the reconstruction. However, this was not sufficient and an optimal interpolation method was developed to correct the precipitation simulation. It is based on an objective analysis (OA) and a least square (LS) melding scheme, collectively named OA+LS. We demonstrated that the OA+LS method is a powerful tool to reduce the precipitation uncertainties and produce a lower error precipitation reconstruction that itself generates a better river discharge time series. The validation of the river streamflow showed promising statistical indices.The final set-up of our meteo-hydrological modelling system was able to realistically reconstruct the local rainfall and the Ofanto hydrograph

    A meteo-hydrological modelling system for the reconstruction of river runoff: the case of the Ofanto river catchment

    Get PDF
    A meteo-hydrological modelling system has been designed for the reconstruction of long time series of rainfall and river runoff events. The modelling chain consists of the mesoscale meteorological model of the Weather Research and Forecasting (WRF), the land surface model NOAH-MP and the hydrology-hydraulics model WRF-Hydro. Two 3-month periods are reconstructed for winter 2011 and autumn 2013, containing heavy rainfall and river flooding events. Several sensitivity tests were performed along with an assessment of which tunable parameters, numerical choices and forcing data most impacted on the modelling performance. The calibration of the experiments highlighted that the infiltration and aquifer coefficients should be considered as seasonally dependent. The WRF precipitation was validated by a comparison with rain gauges in the Ofanto basin. The WRF model was demonstrated to be sensitive to the initialization time and a spin-up of about 1.5 days was needed before the start of the major rainfall events in order to improve the accuracy of the reconstruction. However, this was not sufficient and an optimal interpolation method was developed to correct the precipitation simulation. It is based on an objective analysis (OA) and a least square (LS) melding scheme, collectively named OA+LS. We demonstrated that the OA+LS method is a powerful tool to reduce the precipitation uncertainties and produce a lower error precipitation reconstruction that itself generates a better river discharge time series. The validation of the river streamflow showed promising statistical indices. The final set-up of our meteo-hydrological modelling system was able to realistically reconstruct the local rainfall and the Ofanto hydrograph

    Simulations of the 2004 North American Monsoon: NAMAP2

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    The second phase of the North American Monsoon Experiment (NAME) Model Assessment Project (NAMAP2) was carried out to provide a coordinated set of simulations from global and regional models of the 2004 warm season across the North American monsoon domain. This project follows an earlier assessment, called NAMAP, that preceded the 2004 field season of the North American Monsoon Experiment. Six global and four regional models are all forced with prescribed, time-varying ocean surface temperatures. Metrics for model simulation of warm season precipitation processes developed in NAMAP are examined that pertain to the seasonal progression and diurnal cycle of precipitation, monsoon onset, surface turbulent fluxes, and simulation of the low-level jet circulation over the Gulf of California. Assessment of the metrics is shown to be limited by continuing uncertainties in spatially averaged observations, demonstrating that modeling and observational analysis capabilities need to be developed concurrently. Simulations of the core subregion (CORE) of monsoonal precipitation in global models have improved since NAMAP, despite the lack of a proper low-level jet circulation in these simulations. Some regional models run at higher resolution still exhibit the tendency observed in NAMAP to overestimate precipitation in the CORE subregion; this is shown to involve both convective and resolved components of the total precipitation. The variability of precipitation in the Arizona/New Mexico (AZNM) subregion is simulated much better by the regional models compared with the global models, illustrating the importance of transient circulation anomalies (prescribed as lateral boundary conditions) for simulating precipitation in the northern part of the monsoon domain. This suggests that seasonal predictability derivable from lower boundary conditions may be limited in the AZNM subregion.open131
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