Soil, snow, weather, and sub-surface storage data from a mountain catchment in the rain-snow transition zone

A comprehensive hydroclimatic data set is presented for the 2011 water year to improve understanding of hydrologic processes in the rain-snow transition zone. This type of dataset is extremely rare in scientific literature because of the quality and quantity of soil depth, soil texture, soil moisture, and soil temperature data. Standard meteorological and snow cover data for the entire 2011 water year are included, which include several rain-on-snow events. Surface soil textures and soil depths from 57 points are presented as well as soil texture profiles from 14 points. Meteorological data include continuous hourly shielded, unshielded, and wind corrected precipitation, wind speed, air temperature, relative humidity, dew point temperature, and incoming solar and thermal radiation data. Sub-surface data included are hourly soil moisture data from multiple depths from 7 soil profiles within the catchment, and soil temperatures from multiple depths from 2 soil profiles. Hydrologic response data include hourly stream discharge from the catchment outlet weir, continuous snow depths from one location, intermittent snow depths from 5 locations, and snow depth and density data from ten weekly snow surveys. Though it represents only a single water year, the presentation of both above and below ground hydrologic condition makes it one of the most detailed and complete hydro-climatic datasets from the climatically sensitive rain-snow transition zone for a wide range of modeling and descriptive studies.

Pollen records from two outcrop profiles in the Kakitu Mountain of Tibet

There is a great similarity between pollen types which occur in the early Holocene NE Tibetan pollen spectra and those which are commonly considered to be typical for the Würm Late Glacial period in Central Europe and for the Würm Pleniglacial period in Southern Europe. Evidently, this similarity is due to a remarkable general conformity of plant taxa growing in cold-arid regions of the northern hemisphere. The improvement of the climate and the retreat of the glaciers that commenced at the end of the Würm period had already terminated definitely before 9500 BP. In addition, the climatic situation as well as the vegetation belts must have remained rather constant during the following 3000 yr, i.e. through most parts of the climatic optimum of the Holocene.

Palabra y construcción de la identidad en Harry Potter and the Philosopher's Stone

En Harry Potter and the Philosopher's Stone, texto inaugural del ciclo novelístico de J. K. Rowling, aparecen diversos elementos y situaciones que inscriben el relato dentro del género bildungsroman (o novela de formación) y que a su vez son constitutivos del monomito estudiado por Joseph Campbell. Dentro de ese marco, el presente trabajo analizará la función que desempeña la palabra en el desarrollo del protagonista de la novela. Se sostendrá que la adquisición y el dominio pleno de una palabra permiten construir la subjetividad del personaje, quien valiéndose de esta herramienta se volverá capaz de disipar sus inquietudes frente a lo desconocido y al peso de la voz popular. El estudio se centrará en el nombre del antagonista, Lord Voldemort, su influencia en la saga y en cuán importante es que Harry sea capaz de nombrarlo por ese apelativo. Para este abordaje se utilizarán algunos conceptos de diversas disciplinas que nos permitirán advertir la injerencia de la palabra en la novela seminal de esta serie literaria y en el tránsito del personaje por la compleja senda del héroe