Design and Evaluation of a Retrofittable Electric Snow Melting System for Pavements

Gemstone Team SnowMelt

Marine snow studies in the Northeast Atlantic Ocean: distribution, composition and role as a food source for migrating plankton

During a 25 d Lagrangian study in May and June 1990 in the Northeast Atlantic Ocean, marine snow aggregates were collected using a novel water bottle, and the composition was determined microscopically. The aggregates contained a characteristic signature of a matrix of bacteria, cyanobacteria and autotrophic picoplankton with inter alia inclusions of the tintiniid Dictyocysta elegans and large pennate diatoms. The concentration of bacteria and cyanobacteria was much greater on the aggregates than when free-living by factors of 100 to 6000 and 3000 to 2 500 000, respectively, depending on depth. Various species of crustacean plankton and micronekton were collected, and the faecal pellets produced after capture were examined. These often contained the marine snow signature, indicating that these organisms had been consuming marine snow. In some cases, marine snow material appeared to dominate the diet. This implies a food-chain short cut wherby material, normally too small to be consumed by the mesozooplankton, and considered to constitute the diet of the microplankton can become part of the diet of organisms higher in the food-chain. The micronekton was dominated by the amphipod Themisto compressa, whose pellets also contained the marine snow signature. Shipboard incubation experiments with this species indicated that (1) it does consume marine snow, and (2) its gut-passage time is sufficiently long for material it has eaten in the upper water to be defecated at its day-time depth of several hundred meters. Plankton and micronekton were collected with nets to examine their vertical distribution and diel migration and to put into context the significance of the flux of material in the guts of migrants. “Gut flux” for the T. compressa population was calculated to be up to 2% of the flux measured simultaneously by drifting sediment traps and <5% when all migrants are considered. The in situ abundance and distribution of marine snow aggregates (>0.6 mm) was examined photographically. A sharp concentration peak was usually encountered in the depth range 40 to 80 m which was not associated with peaks of in situ fluorescence or attenuation but was just below or at the base of the upper mixed layer. The feeding behaviour of zooplankton and nekton may influence these concentration gradients to a considerable extent, and hence affect the flux due to passive settling of marine snow aggregates.

Coastal storm snow event : November 20-22, 2006 open-file report

This report describes climatologically, the snow storm that occurred from November 20-22, 2006.

A Meteorological and Snow observational data set from Snoqualmie Pass (921 m), Washington Cascades, U.S.

We introduce a quality controlled observational atmospheric, snow, and soil data set from Snoqualmie Pass, Washington, U.S.A., to enable testing of hydrometeorological and snow process representations within a rain-snow transitional climate where existing observations are sparse and limited. Continuous meteorological forcing (including air temperature, total precipitation, wind speed, specific humidity, air pressure, short- and longwave irradiance) are provided at hourly intervals for a 24-year historical period (water years 1989-2012) and at half-hourly intervals for a more-recent period (water years 2013-2015), separated based on the availability of observations. Additional observations include 40-years of snow board new snow accumulation, multiple measurements of total snow depth, and manual snow pits, while more recent years include sub-daily surface temperature, snowpack drainage, soil moisture and temperature profiles, and eddy co-variance derived turbulent heat flux. This data set is ideal for testing hypotheses about energy balance, soil and snow processes in the rain-snow transition zone. Plots of live data can be found here: http://depts.washington.edu/mtnhydr/cgi/plot.cgi

Pamela Snow, Piano Recital, April 9, 1970

Concert Program for Pamela Snow, Piano Recital, April 9, 1970

Ice and Snow, Niagara Falls, U.S.A.

The description of the image reads "514-a-A fairy-land of ice and snow, Niagara Falls, U.S.A.".

An Empirical Comparison of SNoW and SVMs for Face Detection

Impressive claims have been made for the performance of the SNoW algorithm on face detection tasks by Yang et. al. [7]. In particular, by looking at both their results and those of Heisele et. al. [3], one could infer that the SNoW system performed substantially better than an SVM-based system, even when the SVM used a polynomial kernel and the SNoW system used a particularly simplistic 'primitive' linear representation. We evaluated the two approaches in a controlled experiment, looking directly at performance on a simple, fixed-sized test set, isolating out 'infrastructure' issues related to detecting faces at various scales in large images. We found that SNoW performed about as well as linear SVMs, and substantially worse than polynomial SVMs.

Snow white hen.

Cumple con los requisitos del currículo de Inglaterra, Gales y Escocia aportando los conocimientos básicos relacionados con el aprendizaje de la lectura y la escritura en niños de seis y siete años. El texto sirve de base para conocer e identificar los sonidos en las palabras. En esta historia, se trata la rima'en', y en ella vemos cómo la gallina huye del corral y pone los huevos en otro lugar.

The snow queen.

El objetivo de esta serie es desarrollar en los niños las habilidades para la lectura y la comprensión de textos, a lo largo de doce niveles y mediante la narración de una historia distinta en cada uno de los libros que la componen. Se refuerza el vocabulario relacionado con el contenido de la historia y se acompaña de distintas actividades. En ésta, se narra el cuento de la Reina de las Nieves, y se incluye en el nivel doce.

Snow White and the seven dwarfs.

La malvada Reina es muy vanidosa y está decidida a ser la mujer más hermosa sobre la tierra, pero su espejo mágico le desvela que la más bella es la princesa Blancanieves que trabaja de criada en el palacio. Pero nadie puede interponerse en su camino como descubre la hermosa Blancanieves.

Elmer in the snow.

Una mañana, Elmer el elefante mosaico, pregunta a un grupo de elefantes de que se quejan, y éstos le responden que tienen más frío que de costumbre. Elmer les contesta que en la selva no hace frío y para que comparen les lleva hasta las montañas heladas, donde comprueban lo que realmente es pasar frío, pero también se divierten retozando en la nieve y el hielo.

Village in the snow.

Material didáctico como guía de lectura, comprensión y reconocimiento de palabras. Para trabajar: patrones de ortografía comunes para cada fonema, para leer textos y familiarizarse con ritmo y expresión. Aplicación fonológica del vocabulario para deletrear palabras con precisión. Mrs Mary les cuenta a los niños una historia sobre una aldea en las montañas. Los niños van a la habitación de Biff y quieren una aventura. Biff recoge la llave mágica.