Relevant bibliographies by topics / Snow class

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Snow class'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Snow class"

1

Satyawali, P. K., and M. Schneebeli. "Spatial scales of snow texture as indicator for snow class." Annals of Glaciology 51, no. 54 (2010): 55–63. http://dx.doi.org/10.3189/172756410791386544.

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AbstractA method for automated and fast classification of snow texture would be useful for applications where snow structure must be quantified. Large numbers of field measurements were carried out on natural snow in order to investigate small-scale variations of the micro-penetration force. Snow characterization was done for snow from the Himalaya and the Alps, using a high-resolution snow penetrometer (SnowMicroPen). Measurements of snow resistance at equal intervals of 4 μm were geostatistically evaluated. The range parameter (correlation length, or CL) of penetration force was estimated fo
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Verseghy, Diana, Ross Brown, and Libo Wang. "Evaluation of CLASS Snow Simulation over Eastern Canada." Journal of Hydrometeorology 18, no. 5 (2017): 1205–25. http://dx.doi.org/10.1175/jhm-d-16-0153.1.

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Abstract The Canadian Land Surface Scheme (CLASS), version 3.6.1, was run offline for the period 1990–2011 over a domain centered on eastern Canada, driven by atmospheric forcing data dynamically downscaled from ERA-Interim using the Canadian Regional Climate Model. The precipitation inputs were adjusted to replicate the monthly average precipitation reported in the CRU observational database. The simulated fractional snow cover and the surface albedo were evaluated using NOAA Interactive Multisensor Snow and Ice Mapping System and MODIS data, and the snow water equivalent was evaluated using
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MacKay, Murray D. "Preface‐modelling Canadian snow cover with CLASS." Atmosphere-Ocean 44, no. 3 (2006): 1–3. http://dx.doi.org/10.3137/ao.440300.

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Sturm, Matthew, and Jon Holmgren. "Differences in compaction behavior of three climate classes of snow." Annals of Glaciology 26 (1998): 125–30. http://dx.doi.org/10.3189/1998aog26-1-125-130.

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In a recent paper (Sturm and others, 1995), a global seasonal snow-cover classification system was developed with each class defined by snow properties like grain-size and type. Here, characteristic bulk density vs time curves are assigned to three classes using snow-course data from Alaskan and Canadian sites. Within each class, curves have similar slopes and intercepts but between classes they are different. The relationship between slope, intercept and snow rheology has been investigated using a finite-difference model in which snow layers are assumed to behave as viscous fluids. Using obse
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Sturm, Matthew, and Jon Holmgren. "Differences in compaction behavior of three climate classes of snow." Annals of Glaciology 26 (1998): 125–30. http://dx.doi.org/10.1017/s0260305500014683.

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In a recent paper (Sturm and others, 1995), a global seasonal snow-cover classification system was developed with each class defined by snow properties like grain-size and type. Here, characteristic bulk density vs time curves are assigned to three classes using snow-course data from Alaskan and Canadian sites. Within each class, curves have similar slopes and intercepts but between classes they are different. The relationship between slope, intercept and snow rheology has been investigated using a finite-difference model in which snow layers are assumed to behave as viscous fluids. Using obse
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Langlois, A., J. Bergeron, R. Brown, et al. "Evaluation of CLASS 2.7 and 3.5 Simulations of Snow Properties from the Canadian Regional Climate Model (CRCM4) over Québec, Canada*." Journal of Hydrometeorology 15, no. 4 (2014): 1325–43. http://dx.doi.org/10.1175/jhm-d-13-055.1.

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Abstract Snow cover simulations from versions 2.7 and 3.5 of the Canadian Land Surface Scheme (CLASS) coupled to the Canadian Regional Climate Model, version 4 (CRCM4), are evaluated over northern Québec and the larger Québec domain using in situ and remotely sensed datasets. Version 2.7 of CLASS has been used in the operational version of CRCM4 at Ouranos since 2006. Version 3.5 includes a number of improvements to the snow processes as well as a more realistic parameterization of snow thermal conductivity. The evaluation shows that version 3.5 provides improved simulations of snow water equi
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Roy, A., A. Royer, B. Montpetit, P. A. Bartlett, and A. Langlois. "Snow specific surface area simulation using the one-layer snow model in the Canadian LAnd Surface Scheme (CLASS)." Cryosphere 7, no. 3 (2013): 961–75. http://dx.doi.org/10.5194/tc-7-961-2013.

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Abstract. Snow grain size is a key parameter for modeling microwave snow emission properties and the surface energy balance because of its influence on the snow albedo, thermal conductivity and diffusivity. A model of the specific surface area (SSA) of snow was implemented in the one-layer snow model in the Canadian LAnd Surface Scheme (CLASS) version 3.4. This offline multilayer model (CLASS-SSA) simulates the decrease of SSA based on snow age, snow temperature and the temperature gradient under dry snow conditions, while it considers the liquid water content of the snowpack for wet snow meta
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Roy, A., A. Royer, B. Montpetit, P. A. Bartlett, and A. Langlois. "Snow specific surface area simulation using the one-layer snow model in the Canadian LAnd Surface Scheme (CLASS)." Cryosphere Discussions 6, no. 6 (2012): 5255–89. http://dx.doi.org/10.5194/tcd-6-5255-2012.

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Abstract. Snow grain size is a key parameter for modeling microwave snow emission properties and the surface energy balance because of its influence on the snow albedo, thermal conductivity and diffusivity. A model of the specific surface area (SSA) of snow was implemented in the one-layer snow model in the Canadian LAnd Surface Scheme (CLASS) version 3.4. This offline multilayer model (CLASS-SSA) simulates the decrease of SSA based on snow age, snow temperature and the temperature gradient under dry snow conditions, whereas it considers the liquid water content for wet snow metamorphism. We c
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Brown, Ross, Paul Bartlett, Murray MacKay, and Diana Verseghy. "Evaluation of snow cover in CLASS for SnowMIP." Atmosphere-Ocean 44, no. 3 (2006): 223–38. http://dx.doi.org/10.3137/ao.440302.

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Hirayama, Kimiko, and Michinori Sakimoto. "Regeneration of Cryptomeria japonica on a sloping topography in a cool-temperate mixed forest in the snowy region of Japan." Canadian Journal of Forest Research 33, no. 4 (2003): 543–51. http://dx.doi.org/10.1139/x02-190.

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Cryptomeria japonica D. Don shows a limited distribution on and around ridges in its native habitat. To clarify the regeneration process of this species, we analysed spatial patterns among five size classes on a slope extending from a ridge to a valley bottom, and growth patterns of understorey trees related to their slope position, in a cool-temperate old-growth mixed forest in Japan. Although the largest size-class trees ([Formula: see text]20 cm diameter at breast height (DBH)) were confined to the upper part of the slope, understorey size-class trees ([Formula: see text]50 cm stem length a
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Dissertations / Theses on the topic "Snow class"

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Thériault, Nathalie. "Analyse de sensibilité et amélioration des simulations d’albédo de surfaces enneigées dans les zones subarctiques et continentales humides à l’est du Canada avec le schéma de surface CLASS." Mémoire, Université de Sherbrooke, 2015. http://hdl.handle.net/11143/6946.

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Résumé : Le bilan d’énergie de la Terre est largement influencé par la variation de l’albédo de surface (fraction de l'énergie solaire réfléchie par une surface). Ces variations sont modifiées par la présence, l’épaisseur et les propriétés physiques de la neige. Le réchauffement climatique observé a un impact significatif sur l'évolution du couvert nival, ce qui influence grandement l'albédo de surface, et en retour modifie le climat. Malgré l’importance de l’albédo de surface, plusieurs modèles calculent l’albédo de manière empirique, ce qui peut entraîner des biais significatifs entre les si
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Marchand, Nicolas. "Suivi de la température de surface dans les zones de pergélisol arctique par l'utilisation de données de télédétection inversées dans le schéma de surface du modèle climatique canadien (CLASS)." Thèse, Université de Sherbrooke, 2017. http://hdl.handle.net/11143/10591.

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Les régions de haute latitude sont actuellement les plus sensibles aux effets du réchauffement climatique, et avec des élévations de température pouvant atteindre les 3 à 8 ◦C au niveau du pôle sur les 100 prochaines années. Les pergélisols (sols présentant des températures négatives deux années consécutives) sont présents sur 25 % des terres émergées de l’hémisphère nord et contiennent de grandes quantités de carbone « gelé », estimées à 1400 Gt (40 % de la quantité de carbone terrestre global). Des études récentes ont montré qu’une partie non négligeable (50 %) des premiers mètres des pergél
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Laffage-Cosnier, Sébastien. "L’élève accompli. Les innovations scolaires menées à Vanves par le Dr Max Fourestier (1950-1973)." Thesis, Besançon, 2013. http://www.theses.fr/2013BESA1028.

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Les expériences scolaires menées à Vanves par le Docteur Max Fourestier sont un « lieu de mémoire » de l’histoire de l’éducation physique et sportive du milieu du XXe siècle. Ancré dans Les Trente Glorieuses, ce travail heuristique vise à décrire la place et le rôle des pratiques corporelles au sein des diverses expérimentations (mi-temps pédagogique et sportif, classe de neige, classe de sieste, classe de forêt ou encore tiers-temps pédagogique) conçues à l’école Gambetta et, plus généralement, dans les établissements scolaires vanvéens. Croisant des sources variées et originales, l’étude rév
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Books on the topic "Snow class"

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Surovtsov, Vicka Markov. Snow and sand. iUniverse, Inc., 2010.

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Harrison, Derek. Birmingham Snow Hill: A first class return. P. Watts, 1986.

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Phillips, Caryl. In the falling snow. Alfred A. Knopf, 2009.

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Phillips, Caryl. In the falling snow. Alfred A. Knopf, 2009.

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Phillips, Caryl. In the Falling Snow. Knopf Doubleday Publishing Group, 2009.

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Phillips, Caryl. In the falling snow. W F Howes, 2010.

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Dahl, Michael. Claws in the snow. Stone Arch Books, 2009.

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1974-, Vue Tou, ed. Claws in the snow. Raintree, 2009.

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ill, Mortimer Anne, ed. Santa's Snow Kitten. Katherine Tegen Books, 2008.

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Stainton, Sue. Santa's Snow Cat. HarperCollins, 2001.

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Book chapters on the topic "Snow class"

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Wen, Ming, Lu Wang, Lei Wang, Qing Zhuo, and Wenyuan Wang. "Object Class Recognition Using SNoW with a Part Vocabulary." In Lecture Notes in Computer Science. Springer Berlin Heidelberg, 2007. http://dx.doi.org/10.1007/978-3-540-72530-5_63.

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"Chapter Two. James Petras And That ‘Long Petal Of Wine, Sea And Snow’." In Imperialism, Crisis and Class Struggle. BRILL, 2010. http://dx.doi.org/10.1163/ej.9789004184145.i-320.8.

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Henning, Brian G., Joseph Petek, and George Lucas. "Harvard lectures, spring semester 1927." In The Harvard Lectures of Alfred North Whitehead, 1925-1927. Edinburgh University Press, 2021. http://dx.doi.org/10.3366/edinburgh/9781474416931.003.0005.

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Notes taken by George Perrigo Conger, Lester Snow King, Paul Weiss, and George Bosworth Burch during Whitehead’s class ‘Philosophy 3b: Philosophy of Science’. The topics covered in these twenty-seven lectures are wide-ranging, but the focus is largely on metaphysics and the intersection of philosophy and science.
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Henning, Brian G., Joseph Petek, and George Lucas. "Harvard lectures, fall semester 1926." In The Harvard Lectures of Alfred North Whitehead, 1925-1927. Edinburgh University Press, 2021. http://dx.doi.org/10.3366/edinburgh/9781474416931.003.0004.

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Notes taken by George Perrigo Conger, Everett John Nelson, Lester Snow King, Gardner Jackson, and George Bosworth Burch during Whitehead’s class ‘Philosophy 3b: Philosophy of Science’. The topics covered in these thirty-six lectures are wide-ranging, but the focus is largely on metaphysics and the intersection of philosophy and science.
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Ervin, Keona K. "The Legacies of Black Working-Class Women’s Political Leadership." In Gateway to Equality. University Press of Kentucky, 2017. http://dx.doi.org/10.5810/kentucky/9780813168838.003.0008.

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Jean King, a St. Louis transplant from Osceola, Arkansas, and Memphis, Tennessee, in the fall of 1968 spotted a young Andre Smallwood eating a piece of bread he found on the snow-covered ground outside of their Darst public-housing development located just south of downtown. King soon learned that Smallwood’s mother had a monthly welfare check that amounted to less than the newly stipulated rent increase. The contrast between King and Smallwood’s mother could not have been more striking, although both resided in the same housing project. King and her husband, employed and married with one child, had the means to avoid routine visits from caseworkers, fluctuating welfare payments, and rent schedules that continually increased. But negotiating these realities was typical for most other black women, many of whom functioned as their family’s breadwinners. Public-housing tenants had already been meeting regularly to discuss the possibility of conducting a rent strike when King attended a tenants’ meeting at the nearby Blumeyer Housing Project in midtown St. Louis. After King shared the story of her encounter with Smallwood’s mother, tenants elected her president of the Citywide Rent Strike Committee. Like many “organic intellectuals” who emerged as leaders of grassroots social movements, King came out of a local movement that was already organized when the time to strike arrived. King, along with other black women community organizers, went on to spearhead one of the nation’s largest and earliest rent strikes in the postwar era. Women’s militant mass action garnered national attention and later influenced public policy reform. Because of the long and distinguished activism of black working-class women, a groundswell of grassroots organizing on a national scale, and federal action in support of antipoverty ...
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Suding, Katharine N. "Top of the World Collaborations: Lessons from above Treeline." In Long-Term Ecological Research. Oxford University Press, 2016. http://dx.doi.org/10.1093/oso/9780199380213.003.0046.

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My involvement at the Niwot Ridge Long-Term Ecological Research (LTER) site began when I was an undergraduate summer research assistant, and it has extended through a postdoctoral fellowship, a tenured professorship, and now a leadership role in the program. I focus on alpine tundra plant diversity, plant–soil interactions, and how environmental changes may influence community dynamics over time and space. Cross-site synthesis work has been one of the most valuable experiences of my career, enabling me to ask more general questions and produce more influential work than I could have done with a focus at a single site. Such comparative research has allowed me to interact with a fabulous group of scientists that has strongly influenced my professional development. These scientists remain strong role models for me. My experiences in the LTER program have formed my model of education and training, emphasizing experimental and observational approaches, quantitative methods, and data management and sharing. I think it is the best way to approach the difficult and complex ecological questions facing our society today. My involvement in the LTER program started in college, when I decided to study for one semester at the University of Colorado. During that semester, I took a class from Marilyn Walker, who was part of the Niwot Ridge (NWT) LTER program. Marilyn’s class did not go to the tundra or even focus on alpine systems. However, when time came to figure out what to do over the summer, I asked her if I could be her research assistant. She gave me the chance to work at Niwot Ridge (Figure 29.1). I spent the summer before my senior year at 3,500-m elevation, recording point quadrat vegetation data in permanent plots. The snow was late to melt that year, so I spent much of June in the Institute of Alpine and Arctic Research’s loading dock, painting thick black stripes on 2.5-m long PVC poles to be used to measure snow depth. When snow melted enough to allow access on the entrance road, I went up to Niwot Ridge for the first time.
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Maiden, Martin. "The verbs ‘rain’ and ‘snow’ in Gallo-Romance, and other morphological mismatches in diachrony." In Variation and Change in Gallo-Romance Grammar. Oxford University Press, 2020. http://dx.doi.org/10.1093/oso/9780198840176.003.0018.

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The historical morphology of the verb ‘snow’ in Francoprovençal presents a conundrum, in that it is clearly analogically influenced by the verb ‘rain’, for obvious reasons of lexical semantic similarity, but the locus of that influence is not the ‘root’ (the ostensible bearer of lexical meaning) but desinential inflexion-class members, which are in principle independent of any lexical meaning. Similar morphological changes are also identified for other Gallo-Romance verbs. It seems, in effect, that speakers can identify exponents of the lexical meaning of word-forms in linear sequences larger than the apparent ‘morphemic’ composition of those word-forms, even when such a composition may seem prima facie transparent and obvious. It is argued that these facts are inherently incompatible with ‘constructivist’, morpheme-based, models of morphology, and strongly compatible with what have been called ‘abstractivist’ (‘word-and-paradigm’) approaches, which generally take entire word-forms as the primary units of morphological analysis.
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Wohl, Ellen. "November: Beavers to the Rescue." In Saving the Dammed. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780190943523.003.0014.

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By late November, snow covers much of the beaver meadow. I visit on a sunny day well above freezing, but the low-angle light comes with long, long shadows. The meadow is noisy with continuously rushing wind that keeps the bare willow branches swaying and sculpts the snow on the lee side of plants into streamlined mounds. Individual grass stems have traced downwind crescents on the snow surface. Tracks of wind, tracks of animals: the activities of the meadow are once again made visible in the footprints of moose, hare, squirrel, coyote, and birds. The snow is mushy in the warmth and many of the tracks are blurred, but I also cross fresh, sharply defined traces left by four little leaping paws, with just the brush from a long, slender tail behind them. The prints are so delicate that they barely indent the snow, but clearly a mouse was stirring here recently. The fragile tracery of tiny claws in the snow seems vulnerable, but I know the animal is probably better adapted to the cold than I am. The main channel of the creek remains open, the water golden brown between white banks bulbed with ice along the edges. The creek flows quietly, the sound of moving water submerged beneath the wind. The larger side channels also remain open and green with filamentous algae, but I break through the snow-covered thin ice on the smallest side channels. The off-channel ponds are frozen more solidly. Mats of dried algae quiver in the wind on one newly drained pond. Downwind, the snow is dirty with silt blown from the exposed bed. A layer of sticks, sand, and muck floors the pond with a woody carpet created by the beavers. The main beaver lodge is freshly plastered with mud and sticks, but the ice on the surrounding pond remains unbroken and the snow is trackless. Away from the pond, snow into which I sink to mid-calf obscures the details of the ground. The upright stems of willows and aspen trunks dominate the foreground.
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Thomas, Fabien, and Armand Masion. "27Al NMR Study of the Hydrolysis and Condensation of Organically Complexed Aluminum." In Nuclear Magnetic Resonance Spectroscopy in Environment Chemistry. Oxford University Press, 1997. http://dx.doi.org/10.1093/oso/9780195097511.003.0015.

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Aluminum is the most abundant metal of the Earth’s crust, of which it represents approximately 8%, ranking after oxygen and silicon. It exists mainly as oxides. In terrestrial environments, aluminum commonly exists as secondary (authigenic) hydroxide or aluminosilicate minerals, mainly clays. These minerals are highly insoluble at neutral pH. However, aluminum occurs in detectable amounts in natural waters, due to leaching of the soil minerals in acidic conditions. Soil acidity may have a natural origin, such as an acidic (silicic) mother rock, melted snow, dissolved carbonic acid, or biologically generated organic acids. During the past two decades, it has been demonstrated that one of the major origins of increased aluminum mobilization and transport in forested soils is introduction of strong acid through atmospheric sulfur and nitrogen deposition. It has also been shown that aqueous aluminum is the biogeochemical link between atmospheric pollution and damage caused to tree roots and aquatic organisms such as plankton, crustaceans, insects, and fish. Biological studies have shown that the different aluminum species exhibit various toxicities: the most toxic are the monomeric and the polynuclear species; complexation with organic acids results in low toxicity. The significance of aluminum to human health has long been regarded as negligible. There is a possible link between high-level aluminum contamination by renal dialysis or hemodialysis, and neurodegenerative health disorders such as Parkinson’s or Alzheimer’s diseases, but the part played by aluminum is not clear. However, since aluminum salts are used on an industrial level as coagulants and flocculants in water treatment, the aluminum concentration and speciation in drinking water deserve careful monitoring. Because of the specific toxicity of the aluminum species, there has been considerable concern in the past two decades over the speciation of aqueous aluminum present in soils and aquatic systems. To this end, several techniques have been developed in order to partition the aluminum species. The most common among them are chromatographic separation and categorization methods such as timed ferron reaction, and computational methods derived from thermodynamic equilibrium constants. However, significant discrepancies between the results have been noticed, and attributed to the dramatic interference of organic and inorganic anions in the Al fractionation.
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Parini, Jay. "Endings." In The Art of Teaching. Oxford University Press, 2005. http://dx.doi.org/10.1093/oso/9780195169690.003.0008.

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It’s spring in the academic village, with blossoming fruit trees all over campus, the ground smelling of fresh mud, and once again my thoughts turn to summer. I think of those long, delicious months when, without the telephone ringing and student papers sitting on my desk ungraded, without faculty meetings and office hours, without classes to prepare, I’m free again to work exclusively on my own writing. My e-mails will dwindle to communications with a few good friends. Some mornings, I might even sleep in. But spring also brings with it a small feeling of dread. “April is the crudest month,” wrote T. S. Eliot—a memorable line. I think of it again as lawn mowers drone outside the open windows of my classroom, a sweet wind blows papers off my desk, and I begin to anticipate the end of another school year, with the many losses that inevitably attend that moment, marked so vividly by the graduation ceremony, when half a dozen kids I had really come to like, even love, wave to me from the platform as they proceed into their adult life, diplomas in hand. I’m aware that one or two from each class will remain friends forever, but I know as well that there will be many— the majority of those whom I genuinely considered friends—who won’t. It’s not their fault, I tell myself. They will get busy. Soon spouses and children will lay claim to their attention. I’m just a passing figure in their lives; they know this, and I know it. It’s not as bad as it sounds, given the demands I feel myself toward spouse and family, toward a circle of friends that has widened decade by decade. There is only so much attention to go around. I begin to feel this little dread coming on in late March, when the spring snows in Vermont begin to thaw. Huge piles of the stuff grow wet at the edges, melting slowly, so that by the middle of April there are puddles everywhere, and I have for the first time to wear my waders to school.
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Conference papers on the topic "Snow class"

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Bachman, L. Joseph, and James McIntyre. "Snow Traction Performance of Low Rolling Resistance Drive Tires for Class-8 Tractor Trailers." In SAE 2012 Commercial Vehicle Engineering Congress. SAE International, 2012. http://dx.doi.org/10.4271/2012-01-1918.

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Takishita, Hirofumi, Takahiro Onagi, and Ken Takeuchi. "Storage class memory based SSD performance in consideration of error correction capabilities and write/read latencies." In 2016 IEEE Silicon Nanoelectronics Workshop (SNW). IEEE, 2016. http://dx.doi.org/10.1109/snw.2016.7578000.

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Tseng, Yu-Ting, та Jeng-Rern Yang. "A 0.9-GHz fully integrated 45% PAE class-Ε power amplifier fabricated using a 0.18-μm CMOS process for LoRa applications". У 2017 Silicon Nanoelectronics Workshop (SNW). IEEE, 2017. http://dx.doi.org/10.23919/snw.2017.8242325.

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Hesketh, Peter J., Martha A. Gallivan, Surajit Kumar, Christine J. Erdy, and Zhong L. Wang. "Modeling and Characterization of Dielectrophoretic Assembly Process for Nanobelts." In ASME 2005 International Mechanical Engineering Congress and Exposition. ASMEDC, 2005. http://dx.doi.org/10.1115/imece2005-81153.

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Robust manufacturing methods are needed for nanocomponent assembly, and one must understand the physics to optimize the processing and to develop control schemes to deal with the inherent uncertainty. We are studying field induced assembly of a new class of semiconducting metal oxides — nanobelts — that have been demonstrated for chemical sensing. We have demonstrated the integration of nanobelts with electrodes to make sensors by dielectrophoresis (DEP). The SnO2 nanobelts (width ~ 100–300 nm, thickness ~ 30–40 nm) were suspended in ethanol and introduced into a microchannel, and were assembl
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Carroll, Ernest A., and Dan B. Rathbone. "Using an Unmanned Airborne Data Acquisition System (ADAS) for Traffic Surveillance, Monitoring, and Management." In ASME 2002 International Mechanical Engineering Congress and Exposition. ASMEDC, 2002. http://dx.doi.org/10.1115/imece2002-32916.

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This paper presents the history of and current status of a U.S. DOT and NASA sponsored program designed to demonstrate the feasibility of using a small-unmanned airborne data acquisition system (ADAS) for traffic surveillance, monitoring, and management. ADAS is ideally suited for application in monitoring traffic flow, traffic congestion, and supporting ITS assets. GeoData Systems (GDS), Inc., with principal offices at 10565 Lee Highway, Suite 100, Fairfax, VA 22030 has developed a revolutionary new class of airborne data acquisition systems. In this effort, GDS has teamed with traffic expert
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