467 resultados para Beaches.


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Geophysical surveying and geoelectricalmethods are effective to study permafrost distribution and conditions in polar environments. Geoelectrical methods are particularly suited to study the spatial distribution of permafrost because of its high electrical resistivity in comparison with that of soil or rock above 0 °C. In the South Shetland Islands permafrost is considered to be discontinuous up to elevations of 20–40ma.s.l., changing to continuous at higher altitudes. There are no specific data about the distribution of permafrost in Byers Peninsula, in Livingston Island, which is the largest ice-free area in the South Shetland Islands. With the purpose of better understanding the occurrence of permanent frozen conditions in this area, a geophysical survey using an electrical resistivity tomography (ERT)methodologywas conducted during the January 2015 field season, combined with geomorphological and ecological studies. Three overlapping electrical resistivity tomographies of 78meach were done along the same profile which ran from the coast to the highest raised beaches. The three electrical resistivity tomographies are combined in an electrical resistivitymodel which represents the distribution of the electrical resistivity of the ground to depths of about 13malong 158m. Several patches of high electrical resistivity were found, and interpreted as patches of sporadic permafrost. The lower limits of sporadic to discontinuous permafrost in the area are confirmed by the presence of permafrost-related landforms nearby. There is a close correspondence between moss patches and permafrost patches along the geoelectrical transect.

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En los últimos años, la modificación que el medio urbano ejerce sobre el clima regional a una escala local, la llamada isla de calor urbana, ha sido uno de los fenómenos más estudiados, dado que tiene una relación directa con el confort y la calidad de vida de la población. Es por ello que el presente trabajo tiene por objeto presentar los primeros resultados de la estimación la isla de calor urbana en Santa Teresita, una localidad balnearia ubicada en el centro este de la provincia de Buenos Aires, a los 33º 33´ 00´´ S y 56º 41´ 00´´ O. La ciudad ha nacido y crecido con un fin turístico asociado al clima templado oceánico y a sus atractivas playas. Se efectuaron mediciones de temperatura del aire y humedad relativa a través de la ciudad para determinar la forma y la intensidad de la isla de calor urbano utilizando estaciones móviles e información de una estación meteorológica fija y datos del Servicio Meteorológico Nacional. La ciudad presenta una variación climática generada por las edificaciones, la incidencia del mar y de la vegetación, diferente a lo largo del día.Palabras Clave: Isla de calor urbana – Temperatura - Humedad relativa - Santa Teresita, ArgentinaAbstracIn the last years, the modification that the urban way exercises on the regional climate to a local scale, the so called urban heat island, has been one of the most studied phenomena ast it has a direct relation with the comfort and quality of life of the population. It is for it that the present work takes as an object present the initial results of estimating the urban heat island in Santa Teresita, a touristic locality located in the central eastern province of Buenos Aires, the 33º 3 ‘00 “ S and 56º40‘00 “ W. The city was born and grew up with a tourism associated with the moderate oceanic climate and with their attractive beaches. There were effected measurements of temperature of the air and relative dampness across the city to determine the form and the intensity of the urban heat island using mobile stations and information from a wheater station data sets and the Meteorological National Service. The city has a diverged climate generated by the buildings, the incident of the sea and of the vegetation, different throughout the day.Key words: Urban heat island - Temperature - Relative dampness - Santa Teresita, Argentina.