Academic literature on the topic 'Melting of snow'

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Journal articles on the topic "Melting of snow"

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Torpy, Janet M. "Melting Snow." JAMA 303, no. 12 (2010): 1123. http://dx.doi.org/10.1001/jama.2010.182.

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OKUMA, Takashi, Hiroaki YONAI, Isao ONODA, and Yuji KOBAYASHI. "Snow-melting capacity and standard-design methods of snow-melting-gutter systems." Doboku Gakkai Ronbunshu, no. 371 (1986): 107–14. http://dx.doi.org/10.2208/jscej.1986.371_107.

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Ivanova, Anastasia, Sergey Pavlov, Luka Akimov, and Lidya Zakharova. "Zoning of the territory with snow removal using snow melting plants." MATEC Web of Conferences 170 (2018): 02023. http://dx.doi.org/10.1051/matecconf/201817002023.

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In this paper, the issue of clearing the territory of snow with the use of snow melting units is being considered. The operating principle of the snow-melting stations is based on sewage heat) melting the snow collected in the snow collection chambers. Snow melt water mixed with wastewater is discharged into the collectors and transported to have a full treatment cycle at the wastewater treatment plant. Three problems of urban snow-melting process are considered. The solution of three problems is proposed: compiling a list of signs of mandatory snow removal zones; the allocation of the main zones corresponding to the proposed features; method of determining the amount of snow that is mandatory for export from the territory of the zone.
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Monastersky, R. "Greenhouse Snow: Melting the Preconceptions." Science News 140, no. 8 (1991): 119. http://dx.doi.org/10.2307/3976105.

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Aoki, Kazuo, Masaru Hattori, and Nobuyuki Ishikawa. "Characteristic of Heat Exchanger Operating with Snow Melting. (1st Report, Melting of Piled Snow)." Transactions of the Japan Society of Mechanical Engineers Series B 60, no. 571 (1994): 1022–27. http://dx.doi.org/10.1299/kikaib.60.1022.

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Ishikawa, Nobuyuki, Kazuo Aoki, Masaru Hattori, and Makoto Usui. "Characteristics of Heat Exchanger Operating with Snow Melting. 2nd Report, Melting of Falling Snow." Transactions of the Japan Society of Mechanical Engineers Series B 60, no. 573 (1994): 1765–69. http://dx.doi.org/10.1299/kikaib.60.1765.

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Kantor, P., Z. Karl, F. Šach, and V. Černohous. "Analysis of snow accumulation and snow melting in a young mountain spruce and beech stand in the Orlické hory Mts., Czech Republic." Journal of Forest Science 55, No. 10 (2009): 437–51. http://dx.doi.org/10.17221/121/2008-jfs.

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The paper evaluates snow accumulation and the intensity of snow melting in a young spruce and beech stand. The study was carried out at the Deštné field research station in the Orlické hory Mts. (altitude 900 m, WSW aspect) in winter seasons 2005/2006, 2006/2007 and 2007/2008. The process of snow accumulation and melting was markedly affected or disturbed by the nearly total damage to the spruce stand by top breakage due to the extreme load of wet snow. Winter 2005/2006 was characterized by extreme parameters of snowpack (maximum depth of snow in spruce 157 cm, in beech 164 cm, maximum snow water equivalent in spruce 819 mm, in beech 833 mm). From the aspect of the snow cover duration, winter 2006/2007 was below the average, winter 2007/2008 was average. With respect to the significant reduction of the spruce crown biomass after snow breakage in winter 2005/2006, no significant differences were noted either in snow depth or in snow water equivalent in the spruce and beech stands. The rate of snow melting in the spruce and beech stands was never higher than 50 mm per day. If the spring final stage of snow melting is not accompanied by intensive rainstorms, mountain coniferous and broadleaved forest ecosystems reduce the danger of stormflows and floods within the required degree.
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Mensah, Kwesi, and Jong Min Choi. "Peak and Annual Snow Load Pattern for Effective Snow Melting System Design in Republic of Korea." International Journal of Air-Conditioning and Refrigeration 23, no. 04 (2015): 1550031. http://dx.doi.org/10.1142/s2010132515500315.

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Snowstorm, slippery pedestrian walkways, ice and snow on pavement and roofs of structures continue to serve as a threat to life and infrastructure in many low temperature nations. Owing to these menaces coupled with an increase in the demand and cost of energy globally, engineers and planners are tasked to design effective and efficient green technologies to counterbalance these demands. Snow melting systems are gradually gaining widespread application in the areas of bridge, pavements and roofs of buildings. Snow melting loads are an integral part in the design of snow melting systems. This paper developed snow melting and roof snow building load for the Republic of Korea. Annual averages and frequency distribution methods were used in the analysis of a 10-year period weather data. Monthly total as well as peak snowfall rate values were used to generate annual and peak snow melting load values, respectively. It was observed that the annual-average approach is more conservative for most climatic conditions than the frequency analysis method. Minimum flat roof snow building loads were presented to aid in the structural analysis of structures within the Republic of Korea. The developed database in this paper will provide the database for designing a snow melting system and for analyzing the building structural interpretation considering snow weight.
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Zhou, Jian, Jing Li, Guoqiang Liu, Tao Yang, and Yongli Zhao. "Long-Term Performance and Deicing Effect of Sustained-Release Snow Melting Asphalt Mixture." Advances in Civil Engineering 2019 (June 11, 2019): 1–12. http://dx.doi.org/10.1155/2019/1940692.

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To accelerate snow and ice melting, traditional chloride-based salts are spreaded on asphalt pavement surface, causing serious environmental pollution and infrastructure corrosion. For sustained-release snow melting asphalt mixture, the snow melting agent of Mafilon is directly added to asphalt mixture by replacing partial mineral powder to develop a new type of functional asphalt mixture. In this paper, through the Marshall test, immersion Marshall test, rutting test, trabecular bending test, and Cantabro test, the effects of Mafilon addition on asphalt pavement performance is systematically analysed. Meanwhile, salt precipitation rate is measured by conductimetry to estimate effective deicing period of the pavement. Finally, a new experimental device is designed to quantitatively evaluate snow melting effect of sustained-release snow melting asphalt pavement. The experimental results show that replacing 70% of the mineral powder with Mafilon by volume can achieve satisfactory snow melting effect without affecting usability of asphalt pavement.
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Zawadzki, I., W. Szyrmer, C. Bell, and F. Fabry. "Modeling of the Melting Layer. Part III: The Density Effect." Journal of the Atmospheric Sciences 62, no. 10 (2005): 3705–23. http://dx.doi.org/10.1175/jas3563.1.

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Abstract A model of the melting snow and its radar reflectivity is presented here. The main addition to previous description of the melting layer is the explicit introduction of snow density as a variable. The model is validated with radar observations. Differences in brightband intensity for comparable precipitation rates are related here to the coexistence of supercooled cloud water (SCW) with snow above the melting level leading to riming and change in snow density. Cases where riming was suspected were selected according to the characteristics of the vertical profile of reflectivity flux above the melting layer and vertical Doppler velocities faster than expected from low-density snow. For stratiform precipitation with a melting layer, high snow-to-rain velocity ratio indicates high-density snow and consequently a small peak-to-rain reflectivity difference is expected. This relationship was computed from the model and confirmed with vertically pointing radar observations. In spite of the complexity of the physical processes present in the melting layer the model appears to capture the essential elements.
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Dissertations / Theses on the topic "Melting of snow"

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Harrington, Robert Franklin 1955. "Release of meltwater and ionic solute from melting snow." Diss., The University of Arizona, 1997. http://hdl.handle.net/10150/191224.

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The release of ionic solute from melting seasonal snow produces an influx of ion laden water into hydrologic systems at the start of spring snowmelt. The spatial and temporal variability of meltwater and solute release from melting snow was investigated at different spatial scales to assess the magnitude and variability of this process. Four laboratory experiments were performed where an 0.4 m³ volume of snow was placed in a plexiglass box and melted from above. NaCl and dye tracer experiments revealed contemporaneous areas of concentrated dye and dilute meltwater in flow fingers, indicating that meltwater in preferential flow paths is diluted by low concentration water from the top of the snowpack. Meltwater discharge and meltwater electrical conductivity were measured in snow lysimeters, and snow accumulation and electrical conductivity of samples from snowpits were measured over four snowmelt seasons at an alpine field site. Peak snow-water equivalent ranged from 0.57 to 2.92 m, and lysimeter discharges ranged from 20 to 205% of the mean flow; however mean lysimeter flow was representative of snow ablation observed in snow pits. The electrical conductivity in snowpit samples and lysimeter meltwater averaged 2-3 μS cm⁻¹. Peak meltwater electrical conductivity ranged from 6 to 14 times that of the bulk premelt snowpack. The highest conductivities were observed during the first few days following the onset of flow, and the lysimeters that began flowing earliest tended to have the highest conductivities at the onset of flow. A mathematical model for solute transport in snow was developed that includes the effects of mass transfer between mobile and immobile liquid phases, advection, hydrodynamic dispersion, and melt—freeze episodes. The ability of the model to accurately simulate solute movement and release depends on the validity of the assumption of one—dimensional flow and on the accuracy of modeling the snowpack energy balance. This model is preferable to the empirical models of solute elution currently in use for investigations of watershed hydrogeochemical response because it has the ability to respond directly to changes in snow accumulation or meteorlogical conditions.
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Viklander, Maria. "Melting of urban snow deposits : a water quality study." Licentiate thesis, Luleå tekniska universitet, Arkitektur och vatten, 1994. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-26557.

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McLeod, Kari S. "Melting snow, a re-examination of Dr. John Snow, his dot-map and the 1854 Broad Street cholera outbreak." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk2/tape17/PQDD_0002/MQ32371.pdf.

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Fortner, Sarah Kathryn. "The geochemistry of glacier snow and melt the Oregon Cascades and the Taylor Valley, Antarctica /." Columbus, Ohio : Ohio State University, 2008. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1228255773.

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Matthijsse, Mathilde. "Melting snow : the changing roles of Iqaluit women in family, work and society." Thesis, Durham University, 2010. http://etheses.dur.ac.uk/279/.

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My thesis is a detailed anthropological study of the experiences of women as a result of their changing gender roles in Inuit families, in the labour market and in Inuit society more broadly. Although McElroy reported as early as 1975 that ‘a higher percentage of the total population of women than of men are employed [in Frobisher Bay and Pangnirtung]’ (McElroy 1975:679) the effects of this have never been systematically researched. This thesis is the first to use theoretical constructs from Bourdieu’s toolkit, including the capitals (social, cultural, symbolic), the habitus and the cultural arbitrary as well as theories of empowerment, to analyse how women have constructed and negotiated meaning in their new roles as financial provider for their families. It draws on data collected during ten months of fieldwork in Iqaluit, Canada, using a mix of qualitative methods including in-depth interviews, group discussions and participant observation. My findings show that different ideologies, values, ways of life and habitus shape and are shaped by life experiences of women in contemporary Iqaluit. These differences find their basis in women’s upbringing, ranging from traditional, to transitional, to contemporary; women’s experiences with education; and their interactions with incoming institutions with different cultural origins. Social negotiations characterise the process in which women create roles and identities for themselves, combining these different influences. Women’s access to financial and cultural capital in some cases impacts on and is a consequence of women’s empowerment, and their ability to challenge the cultural arbitrary. However, whilst empowerment is generally seen as a positive development, it can upset the balance between partners or other family members, who may struggle to appropriate economic, cultural and social change to the same extent. For that reason, it is important that the people of Nunavut, both men and women, work together to create for themselves a place in their family, community and society in which they can provide a meaningful contribution.
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Mahat, Vinod. "Effect of Vegetation on the Accumulation and Melting of Snow at the TW Daniels Experimental Forest." DigitalCommons@USU, 2011. https://digitalcommons.usu.edu/etd/1078.

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Snow melt is an important component of Western US water resources, accounting for about 50-80% of the annual runoff. Prediction of runoff from snowmelt in heterogeneous watersheds requires the quantification of physical processes accounting for the effects of forest canopy on snow accumulation, melt and sublimation. The forest canopy intercepts snowfall that resulting in smaller snow accumulations in forest area than in open area. The forest canopy also modifies the energy exchange between snow surface and the atmosphere, and alters the sublimation and melting of sub-canopy snow relative to open area. This dissertation has examined ways to improve snowmelt modeling capability to better account for canopy effects and has presented enhancements to an energy balance model that include i) an improved representation of the transmission of radiation through the canopy, ii) an improved representation of the atmospheric transport of heat and water vapor between the snow on the ground, in the canopy and the atmosphere above, and iii) an improved representation of the processes of canopy snow interception and unloading. These enhancements were evaluated against 4 years of field data (2006-2010) collected at the TW Daniels Experimental Forest (TWDEF) located 30 miles N-E of Logan. Observations included continuous automated climate and snow depth measurements supported by periodic field measurements of snow water equivalent and temperature in four different vegetation classes (grass, shrubs, coniferous forest, deciduous forest). The enhanced canopy components were included into the Utah Energy Balance Snowmelt model and provide improved capability to predict the surface water input and runoff from snowmelt in heterogeneous watersheds using a parsimonious approach that can be used with practically available information.
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Bhattacharya, Indrajit. "ANALYSIS OF SURFACE MELTING AND SNOW ACCUMULATION OVER THE GREENLAND ICE SHEET FROM SPACEBORNE MICROWAVE SENSORS." The Ohio State University, 2010. http://rave.ohiolink.edu/etdc/view?acc_num=osu1276621670.

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Gari, Abdullatif Abdulhadi. "Analysis of conjugate heat transfer in tube-in-block heat exchangers for some engineering applications." [Tampa, Fla] : University of South Florida, 2006. http://purl.fcla.edu/usf/dc/et/SFE0001716.

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Guventurk, Abdulkadir. "Impacts Of Climate Change On Water Resources On Eastern Mountainous Region Of Turkey." Master's thesis, METU, 2013. http://etd.lib.metu.edu.tr/upload/12615706/index.pdf.

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Temperature and precipitation are the most important indicators of climate change. Especially for the basins fed by snow, the shifts of melting to earlier times, affects the streamflow. Increase in temperature causes to shifts of melting of snow to shift to earlier times so that hydrologic regime of the river system changes, and leads to changes in climatic conditions of the region. In this study the shifts of snow melting times are analyzed for the selected 15 streamflow stations located in Euphrates, Tigris, Aras, and &Ccedil<br>oruh basins in Eastern Anatolia of Turkey along with period from 1970 to 2010. The shifts in snowmelt runoff are determined by Center Time (CT) method. Meteorological stations representing the stream gauge stations regarding the basin characteristics are also selected to be used in the analyses. In order to relate CT shifts to temperature and precipitation changes, trend analysis are applied to temperature, precipitation and streamflow data. In addition to these, days with daily average temperature less than freezing and wet days below freezing until CT for each station pair between stream gauge and meteorological stations and each year are also analyzed. These days till CT within a year for each station pair can be indirectly linked to snowy days and accumulated snow amount. Complete analyses show significant warming at each station in the region and no important trends in annual precipitation. However at a few stations meaningful seasonal changes in precipitation are observed. Regional warming and associated changes in precipitation and snowmelt runoff cause significant shifts to earlier times of snowmelt runoff. In the region eight out of fifteen stream gauge stations in Euphrates, Tigris and Aras basins showed significant time shifts according to statistical trend tests.
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Bouron, Gaël. "Mécanismes et effets de la fonte des accumulations neigeuses sur le fonctionnement hydrologique du Lignon du Forez, Massif Central, France." Phd thesis, Ecole Nationale Supérieure des Mines de Saint-Etienne, 2013. http://tel.archives-ouvertes.fr/tel-00937095.

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Ce travail de thèse propose une méthodologie d'instrumentation reposant sur plusieurs outils hydrologiques, géophysiques et géochimiques afin de quantifier l'apport nival dans les débits du Lignon. Cette instrumentation consiste en un suivi des échanges aux différents compartiments/interfaces hydrologiques que forment l'atmosphère, la neige, le sol et les cours d'eau au cours des saisons. La neige, et surtout l'équivalent en eau liquide qu'elle représente, est fondamentale pour la compréhension du fonctionnement des sources du Lignon, situées à l'aval direct d'une congère de grand volume. Ce volume d'eau est stocké durant la saison froide pour être restitué lors de la fonte printanière. Cette restitution est loin d'être homogène dans le Haut Lignon, en raison de la forte variabilité spatio-temporelle des paramètres qui la pilotent.L'infiltration de l'eau alors produite est une étape clef dans le comportement hydrologique du Lignon au printemps. La structure du sol à proximité des sources explique également la forte dépendance des sources du Lignon par rapport aux précipitations neigeuses. Cette dépendance est particulièrement visible lors de la fonte de la neige, qui modifie à très court terme les débits aux sources. Cette relation neige-pluie-débit met en évidence une alimentation superficielle pluvio-neigeuse prépondérante par rapport aux débits issus d'eau plus profonde, mais variable au cours de l'année.La méthode d'instrumentation employée, adaptée à l'hydrologie locale employée, permet de corroborer les résultats obtenus avec une précision appréciable, tout en ouvrant de nouvelles perspectives d'application à d'autres bassins versants d'altitude.
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Books on the topic "Melting of snow"

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Melting snow: An Irishman in Moscow. Appletree Press, 1991.

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Richard, Michele, and Lindsey Gray. Melting the Snow. Renaissance Romance Publishing, 2013.

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Melting The Snow On Hester Street. HarperCollins Publishers, 2013.

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Melting the snow on Hester Street. 2013.

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Melting The Snow On Hester Street. HarperCollins Publishers, 2013.

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(Illustrator), Arlene Adams, ed. Oxford Reading Tree: Stage 3: Snapdragons: Melting Snow. Oxford University Press, 2004.

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D, Hewitt Alan, Colbeck Samuel C, and Cold Regions Research and Engineering Laboratory (U.S.), eds. Elution of ions from melting snow: Chromatographic versus metamorphic mechanisms. U.S. Army Corps of Engineers, Cold Regions Research & Engineering Laboratory, 1993.

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Silverman, Buffy. On a Snow-Melting Day: Seeking Signs of Spring. Lerner Publishing Group, 2020.

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Szeto, Kit Kong. Mesoscale circulations forced by the melting of snow in the atmosphere. 1986.

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Snow Melting in a Silver Bowl: A Book of Active Meditations. Red Wheel, 2004.

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Book chapters on the topic "Melting of snow"

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Tedesco, Marco, Thomas Mote, Konrad Steffen, Dorothy K. Hall, and Waleed Abdalati. "Remote sensing of melting snow and ice." In Remote Sensing of the Cryosphere. John Wiley & Sons, Ltd, 2014. http://dx.doi.org/10.1002/9781118368909.ch6.

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Nielsen, Anker. "Sensitivity Analysis of Melting and Freezing of Snow on Roofs." In Springer Proceedings in Energy. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-030-00662-4_86.

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Zhao, Wenke, Yaning Zhang, Lei Li, Wentao Su, Bingxi Li, and Zhongbin Fu. "Experimental Investigation of a Ground Source Heat Pump Based Snow Melting System: Control Optimization." In Springer Proceedings in Energy. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-38804-1_14.

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Ho, I.-Hsuan. "Numerical Modeling of Heat Production for a Snow-Melting System Using Geothermal Energy in North Dakota." In Advancement in the Design and Performance of Sustainable Asphalt Pavements. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-61908-8_17.

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Rühland, Kathleen, Netajirao R. Phadtare, Rajendra K. Pant, Satish J. Sangode, and John P. Smol. "Accelerated Melting of Himalayan Snow and Ice Triggers Pronounced Changes in a Valley Peatland from Northern India." In Collected Reprint Series. American Geophysical Union, 2014. http://dx.doi.org/10.1002/9781118782033.ch5.

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Ahbari, Abdellatif, Laila Stour, and Ali Agoumi. "Impacts of Climate Change on the Hydro-Climatology and Performances of Bin El Ouidane Reservoir: Morocco, Africa." In African Handbook of Climate Change Adaptation. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-45106-6_245.

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AbstractIn arid and humid contexts, dams’ reservoirs play a crucial role in water regulation and flood control. Under the projected climate change (CC) effects, even a preoptimized management approach (MA) of a reservoir needs to be assessed in this projected climate. This chapter aims to assess the impacts of CC on the Hydroclimatic (HC) variables of the basin upstream the reservoir of Bin El Ouidane (Morocco), and the effects on the performances of its preoptimized MA. The applied Top-Down assessment procedure included CORDEX climate projections, hydrological, siltation, evaporation, and management models. Concerning the HC variables, the results obtained concord with those reported in the literature in terms of trend, but not always in terms of intensity of change. On the other hand, the projections expected a decrease in the performances of the reservoir, except for criterion allocations’ standard deviation, calibrated during the optimization. Also, interesting conclusions have been found like: the change in precipitation dominant form, the accentuation of the pluvial hydrological regime, the advanced snow melting due to the temperature increase. This chapter presents a typical case study on how to use climate projections for reservoir MA adaptation, without being highly and negatively influenced by the climate model uncertainties.
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Ho, I.-Hsuan. "Assessment of Direct Use of Geothermal Hot Water for Snow-Melting Pavements in Western North Dakota Using Finite Element Method." In Proceedings of GeoShanghai 2018 International Conference: Transportation Geotechnics and Pavement Engineering. Springer Singapore, 2018. http://dx.doi.org/10.1007/978-981-13-0011-0_8.

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Diaz, Henry F., Jon K. Eischeid, Chris Duncan, and Raymond S. Bradley. "Variability of Freezing Levels, Melting Season Indicators, and Snow Cover for Selected High-Elevation and Continental Regions in the Last 50 Years." In Advances in Global Change Research. Springer Netherlands, 2003. http://dx.doi.org/10.1007/978-94-015-1252-7_3.

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Kayastha, Rijan B., Yutaka Ageta, and Koji Fujita. "Use of Positive Degree-Day Methods for Calculating Snow and Ice Melting and Discharge in Glacierized Basins in the Langtang Valley, Central Nepal." In Climate and Hydrology in Mountain Areas. John Wiley & Sons, Ltd, 2006. http://dx.doi.org/10.1002/0470858249.ch2.

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Xue, Binxia, Weiguang Li, and Xiaofei Kang. "Study on the Continuous Running Automation Control Mode of the Double-Layer Subsurface-Flow Snow Melting System Based on the Interaction Mechanism of Electronic Sensor." In Advances in Mechanical and Electronic Engineering. Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-31516-9_32.

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Conference papers on the topic "Melting of snow"

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Aoki. "Skid preventing and snow-melting properties of a two-layer structure snow melting agent." In 2003. 3rd International Symposium on Environmentally Conscious Design and Inverse Manufacturing - EcoDesign'03. IEEE, 2003. http://dx.doi.org/10.1109/ecodim.2003.1322709.

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Aoki, H. "Skid preventing and snow-melting properties of a two-layer structure snow melting agent." In 2003 IEEE 58th Vehicular Technology Conference. VTC 2003-Fall (IEEE Cat. No.03CH37484). IEEE, 2003. http://dx.doi.org/10.1109/vetecf.2003.239929.

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Wu, Yuhui, Chengyu Wan, and Jiliang Wang. "Applicability of Highway Snow-Melting Agents." In Third International Conference on Transportation Engineering (ICTE). American Society of Civil Engineers, 2011. http://dx.doi.org/10.1061/41184(419)493.

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Zhang, Wei, Erkki Salonen, and Seppo Karhu. "Evaluation of Attenuations for Melting Snow and the Melting Layer." In 20th European Microwave Conference, 1990. IEEE, 1990. http://dx.doi.org/10.1109/euma.1990.336271.

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Huang, Yong, Qing Gao, Yan Liu, and Y. Y. Yan. "Investigation of Thermal Characteristics on Simultaneous Snow and Melt in Road." In ASME 2010 International Mechanical Engineering Congress and Exposition. ASMEDC, 2010. http://dx.doi.org/10.1115/imece2010-40041.

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An automatically controlled hydronic ice-snow melting (HISM) technology in road coupled with slab solar collection (SSC) and underground thermal energy storage (UTES) has become an increasingly sustainable and important measure in road engineering and heat engineering An experiment on the hydronic snow melting system with coil pipe imbedded in road was implemented to investigate the thermal characteristics of simultaneous snow and melt in road. Research focused on the active sync process of road snow melting in the different pitch pipe, snow melt patterns, surface temperature, unit area heat consumption and unit length temperature difference, etc, and explored factors of impact characteristics, and recognized a synchronous process. The result shows that the smaller pipe pitch of dense arrangement is, the higher snow free area ratio is and the effect of snow removal is better. Actually the short duration of snow melting needs big heat load and heat consumption. The arrangement of small pitch can support big heating intensity. In the simultaneous snow and melt, a short duration of snow melting and timely melting must be fulfilled as quickly as possible and it can significantly shorten the lifetime of snow accumulated on road. But a big heating system will be required and it leads to a large initial investment.
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Xiaonan Ji, Yan Chen, Ling Tong, Mingquan Jia, Longfei Tan, and Shaokai Fan. "Area retrieval of melting snow in alpine areas." In IGARSS 2014 - 2014 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2014. http://dx.doi.org/10.1109/igarss.2014.6947360.

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Wu, Yuhui. "Performance Comparison of Different Highway Snow-Melting Agents." In Second International Conference on Transportation Information and Safety. American Society of Civil Engineers, 2013. http://dx.doi.org/10.1061/9780784413036.079.

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Nagai, Niro, Kensuke Suzuki, Yoshikazu Maegawa, and Haruki Taniguchi. "Snow Melting System Around Steel Top of Underground Fire Cistern Using Heat Pipe BACH." In ASME/JSME 2011 8th Thermal Engineering Joint Conference. ASMEDC, 2011. http://dx.doi.org/10.1115/ajtec2011-44256.

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This research aims to develop snow melting system around steel top of underground fire cistern by using Bubble Actuated Circulating Heat pipe (BACH). Water in afire cistern installed underground is heated by underground heat source, 10∼15 °C Heat is transported by BACH from water to snow melting panel near the surface, which contains the steel top, resulting in snow melting around the top. The experimental results show that this system can melt the snow on the snow melting panel in winter season preferably, and has enough anti-freezing ability around the steel top. The numerical simulation program was found to predict temperature variations of the whole system preferably. From a thermal point of view, BACH showed better results compared to those of a conventional thermosiphon heat pipe.
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9

Paloscia, S., P. Pampaloni, S. Pettinato, E. Santi, and L. Cara. "The Detection of Melting Snow and Analysis of Melting-Refreezing Cycles using Microwave Radiometry." In IGARSS 2018 - 2018 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2018. http://dx.doi.org/10.1109/igarss.2018.8519153.

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10

Pan, Jinmei, Lingmei Jiang, Lixin Zhang, et al. "Simulation of emission properties and snow-soil system status of a melting thin snow pack." In IGARSS 2011 - 2011 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2011. http://dx.doi.org/10.1109/igarss.2011.6049899.

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Reports on the topic "Melting of snow"

1

Hamill, Daniel D., Jeremy J. Giovando, Chandler S. Engel, Travis A. Dahl, and Michael D. Bartles. Application of a Radiation-Derived Temperature Index Model to the Willow Creek Watershed in Idaho, USA. U.S. Army Engineer Research and Development Center, 2021. http://dx.doi.org/10.21079/11681/41360.

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The ability to simulate snow accumulation and melting processes is fundamental to developing real-time hydrological models in watersheds with a snowmelt-dominated flow regime. A primary source of uncertainty with this model development approach is the subjectivity related to which historical periods to use and how to combine parameters from multiple calibration events. The Hydrologic Engineering Center, Hydrological Modeling System, has recently implemented a hybrid temperature index (TI) snow module that has not been extensively tested. This study evaluates a radiatative temperature index (RTI) model’s performance relative to the traditional air TI model. The TI model for Willow Creek performed reasonably well in both the calibration and validation years. The results of the RTI calibration and validation simulations resulted in additional questions related to how best to parameterize this snow model. An RTI parameter sensitivity analysis indicates that the choice of calibration years will have a substantial impact on the parameters and thus the streamflow results. Based on the analysis completed in this study, further refinement and verification of the RTI model calculations are required before an objective comparison with the TI model can be completed.
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