Gotowe bibliografie tematyczne / Ice

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Gotowa bibliografia na temat „Ice”

Autor: Grafiati

Data publikacji: 4 czerwca 2021

Data aktualizacji: 28 września 2024

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Artykuły w czasopismach na temat "Ice"

Kokkinakis E, N., A. Fragkiadakis G, H. Ioakeimidi S, B. Giankoulof I i N. Kokkinaki A. "Microbiological quality of ice cream after HACCP implementation: a factory case study". Czech Journal of Food Sciences 26, No. 5 (31.10.2008): 383–91. http://dx.doi.org/10.17221/1126-cjfs.

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The microbiological quality of the final product and the safety of the production procedures were screened in an ice cream factory, after implementation of a Hazard Analysis Critical Control Points (HACCP) system. We analysed 30 vanilla (IC1), 30 strawberry (IC2), and 30 chocolate flavoured (IC3) samples of ice cream; 30 of water; 90 of personnel’s hands flora; 150 of plastic ice cream containers flora; 50 of sanitised equipment-surfaces flora. After HACCP introduction, Staphylococcus aureus was not further detectable in ice cream and Escherichia coli was mostly less than 10 CFU/g, while the spoilage markers (total coliforms – TC, aerobic plate counts – APC) in ice cream and the environment were reduced by 20–35%. Mean log CFU/g, for IC1: TC from 2.20 reduced to 1.57, APC from 4.58 reduced to 3.62. For IC2: TC from 2.29 reduced to 1.65, APC from 4.61 reduced to 3.49. For IC3: TC from 2.67 reduced to 1.76, APC from 5.08 reduced to 3.81.

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Commissariat, Tushna. "Ice ice baby". Physics World 34, nr 8 (1.09.2021): 23. http://dx.doi.org/10.1088/2058-7058/34/08/26.

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Geli, Norma. "Ice, Ice Baby". ASHA Leader 21, nr 6 (czerwiec 2016): 8. http://dx.doi.org/10.1044/leader.gl.21062016.8.

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Armstrong, Gavin. "Ice ice maybe". Nature Chemistry 2, nr 4 (kwiecień 2010): 256. http://dx.doi.org/10.1038/nchem.608.

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Toliver, Richard. "Ice Is Ice?" Journal of the IEST 31, nr 3 (1.05.1988): 31–33. http://dx.doi.org/10.17764/jiet.1.31.3.y1421304rgg67121.

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MIL-STD-810D, Method 521.0, "Icing/Freezing Rain," contains guidance for testing equipment exposed to freezing rain. This method was developed around a narrow set of meteorological conditions resulting in the buildup of clear glaze ice. The icing procedures described in Method 521.0 can be applied to a wide range of equipment and will help to predict equipment operations during natural freezing rain. However, the procedures do not give any indication of the operation of equipment during exposure to rime ice. The physical properties of rime and glaze ice differ significantly, as do their effects on equipment. Until MIL-STD-810D is modified to include rime icing, program managers and environmental test engineers will find no guidance or procedures in MIL-STD-810D for half of the icing (rime vs. glaze) that equipment can be exposed to in nature.

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Fei, Xie, Lu Peng, Cheng Bin, Yang Qian i Li Zhijun. "Magical spherical ice (ice balls, ice eggs)". Journal of Lake Sciences 34, nr 2 (2022): 695–98. http://dx.doi.org/10.18307/2022.0228.

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Bradley, David. "No ice, ice, baby". Materials Today 36 (czerwiec 2020): 4. http://dx.doi.org/10.1016/j.mattod.2020.04.022.

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Schulson, Erland M., i Andrew L. Fortt. "Friction of ice on ice". Journal of Geophysical Research: Solid Earth 117, B12 (grudzień 2012): n/a. http://dx.doi.org/10.1029/2012jb009219.

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Guizzo, E. "Into deep ice [ice monitoring]". IEEE Spectrum 42, nr 12 (grudzień 2005): 28–35. http://dx.doi.org/10.1109/mspec.2005.1549779.

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Moore, John. "Ice blisters and ice dolines". Journal of Glaciology 39, nr 133 (1993): 714–16. http://dx.doi.org/10.1017/s002214300001666x.

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Rozprawy doktorskie na temat "Ice"

Sukhorukov, Sergiy. "Ice-Ice and Ice-Steel Friction in Field and in Laboratory". Doctoral thesis, Norges teknisk-naturvitenskapelige universitet, Institutt for bygg, anlegg og transport, 2013. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-23559.

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Friction is one of the key phenomena during the interaction of ice with offshore structures and ships, ice rafting and ridging processes, and the brittle compressive failure of ice. Therefore, knowledge of the ice friction laws and a better understanding of this phenomenon are needed for the design of safe and reliable offshore structures and successful operations in ice-infested waters. This thesis presents experimental studies on ice friction in the field and in the laboratory and can be divided into three parts: field study of ice friction and the effects of different parameters on the kinetic and static friction coefficients; investigation of geometrical stick-slip interaction between ice and stainless steel in small-scale laboratory tests; field investigation of the vertical ice forces exerted on isolated vertical piles frozen in a level sea due to changes in the water level. The first version of the experimental setup for the field tests to study ice friction was relatively simple and was used only in 2010. Significant modifications and improvements were made to the setup in 2011 that allowed us to better control the test conditions (i.e., velocity, normal load). The available range of sliding velocities (between 6 mm s-1 and 43 mm s-1) did not cover the whole range of our interest. Therefore, a new pulling mechanism was introduced in the tests in 2012 that allowed us to extend the sliding range up to 110 mm s-1. The field experiments were conducted with first year sea ice in the Barents Sea and in fjords at Spitsbergen during three springs (2010-2012). In September of 2012, the ice friction tests were performed with multiyear sea ice northeast of Greenland. Most of the tests were performed to investigate the friction between sea ice and sea ice, while the rest were to study the friction between sea ice and corroded steel. The aim of the study was to survey the most important factors that affect ice friction in field conditions and to determine whether the existing friction models correctly predict the dependences observed in the field tests. The effects of the sliding velocity (6 mm s-1to 105 mm s-1), air temperatures (-2°C to -20°C), normal load (300 N to 2000 N), presence of sea water in the interface, and ice grain orientation with respect to the sliding direction on the friction coefficient were investigated. The effect of the hold time on the static friction coefficient was also studied. The test campaigns showed that ice surface roughness is likely to be the most important parameter in determining the friction coefficient. Repeated sliding over the same track led to surface polishing and decreased the kinetic friction coefficient from 0.48 to 0.05. When sliding occurs between unsmoothed surfaces, the friction coefficient was found to be independent of the sliding velocity. As the contacting surfaces become smoother, the kinetic friction coefficient begins to depend on the velocity, as predicted by existing ice friction models. Some attempts were made to characterise ice surface irregularities and real contact area using two techniques: 1) the production of an ice surface cast and its further analysis using an optical microscope and 2) measurements of the pressure distribution and real contact area using tactile sensors. The static friction coefficient increases logarithmically with the hold time and changes from approximately 0.6 at 5 s to 1.26 at 960 s. The small-scale laboratory studies on the stick-slip interaction between ice and stainless steel were performed at the University Centre in Svalbard (UNIS). A specially designed device allowed us to study the effect of well controlled steel surface roughness on the interaction between ice and steel under various test conditions. The effects of the relative sliding rate (1.67 × 10-6 m s-1 to 0.83 × 10-3 m s-1), temperature (-5°C to -25°C) and applied constant pushing force were also investigated. Stick-slip interaction was always observed in the tests on samples with an arithmetic average roughness (Ra) between 2 μm and 15 μm. Both steady state sliding and stick-slip were observed in the tests on samples with the lowest (Ra = 2 μm) and the highest (Ra = 25.2 μm) roughness. The slip distance was found to be equal to the mean pitch profile (mean profile wavelength) for all velocities studied. The elasticity of the ice was found to be an important factor in the stick-slip interaction. The field studies of the vertical ice forces exerted on isolated vertical piles frozen in the ice were performed in Svea, Spitsbergen, in March of 2010. Four different piles made of steel and aluminium were used in the experiments. The piles were pushed through the ice using a hydraulic jack. The first peak load measured in the tests is associated with the onset of the ice-pile relative movement. Because we always observed failure at or very near the ice-pile interface, the first peak load can be treated as the strength of adhesion or the cohesive failure of ice in the vicinity of the interface. Elastic plate theory was used to estimate theoretically the vertical forces exerted on a pile.

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Howe, Rachel. "Ice XI : the ordered form of ICE Ih". Thesis, University of Birmingham, 1988. http://etheses.bham.ac.uk//id/eprint/5255/.

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The history of the development of the understanding of the statistical arrangement of hydrogen bonds in ice Ih and the discovery of the transition at 72 K to the ordered phase, ice XI, catalysed by alkali hydroxide doping, is reviewed. Possible ordered arrangements of hydrogen bonds are discussed and enumerated. A theory is presented relating the entropy and permittivity of partially ordered ice to the degree of order. The apparatus developed for dielectric experiments on KOH-doped ice is described. The results of such measurements for polycrystalline specimens and one single crystal are presented. Measurements above the transition reveal that the main charge carriers are OH\(^-\) ions, with a temperature-independent mobility of approximately 10\(^-\)\(^1\)\(^0\) m\(^2\) v\(^-\)\(^1\) s\(^-\)\(^1\). The transformation to the ordered phase starts when the sample is cooled below about 65 K, and once started can be speeded up by heating the sample to 67-70 K: the static permittivity and the a.c. conductivity slowly decrease. Neutron powder diffraction experiments were performed on HRDP at ISIS. After one unsuccessful experiment, dielectric measurements on powder samples showed the importance of excluding CO\(_2\) during preparation. In a second experiment the structure of ice XI was confirmed and the lattice parameters determined for the first time.

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Andersson, Lars-Olof. "Ice accretion and ice adhesion to polymer material". Licentiate thesis, Luleå tekniska universitet, 1993. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-26519.

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Gripenvik, Christian. "Is/Ice". Thesis, Linnéuniversitetet, Institutionen för film och litteratur (IFL), 2020. http://urn.kb.se/resolve?urn=urn:nbn:se:lnu:diva-95589.

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Romanen ”Is” utspelar sig i en fiktiv framtid och skildrar ett Sverige i svallvågorna avklimatförändringarna. Landet styrs av auktoritära högerpartier som har infört strikt kontrollpå befolkningstillväxten genom att unga män steriliseras efter att ha donerat spermaoch senare i livet får ansöka om att skaffa barn.Inom ramen för det här arbetet skildras samhället ur två perspektiv:1. Chinua kommer som flykting till Sverige och försöker starta ett nytt liv, men möterhårt motstånd från både samhällsapparaten och befolkningen. I desperation tvingashan sälja sin kropp, eller snarare sina spermier, till barnlösa kvinnor.2. I det inhägnade samhället Gränna bor Arwen och Viggo. De har fyra barn och ärbåda högt uppsatta i samhällsadministrationen och näringslivet. Arwen är den mest karriärmässigtdrivna, medan Viggo känner sig mer utanför. Skillnaderna mellan dem växeri takt med att samhället radikaliseras och de driver sakta isär, samtidigt som de vinnläggersig om att upprätthålla en polerad fasad.Syftet är att skildra ett framtida Sverige ur flera perspektiv så att möjliga svagheteroch styrkor visas upp. Chinuas perspektiv utgår från positionen ”ute, vill in”, en personsom utan eget förskyllande befinner sig utanför gemenskapen och kämpar för att bli endel av den. Chinua har tidigare försökt hitta en plats i andra europeiska länder, menmisslyckats och därför tagit sig vidare till Sverige. Arwen och Viggo-perspektivet äristället ”inne, vill vara kvar”, vilket ger möjlighet att gestalta den styrande delen av samhället,där de som passar in och tror på systemet lever.Planen är att i framtiden utöka romanen med ytterligare två perspektiv: ett om detbarndrömmande paret Jani och Dani, som får avslag på sin ansökan om att skaffa barn(också ett ”inne, vill vara kvar”-perspektiv, men underifrån); ett om de som valt att lämnadet nya Sverige och försöka bygga en alternativ gemenskap längre norrut (”ute, villvara ute”). Inom de respektive perspektiven är det också meningen att det ska finnas nyanseroch glidningar, och centrala personer kommer att skifta tillhörighet.Till planen hör också att vidareutveckla världsbygget med centrala frågor som temperaturhöjningoch havsnivåhöjning och deras bredare konsekvenser, samt att utforskaframtida teknisk utveckling och dess effekter på samhället och hur människor umgås.

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Horgan, Huw J. Anandakrishnan Sridhar. "Geophysical observations of polar ice sheets and ice shelves". [University Park, Pa.] : Pennsylvania State University, 2009. http://etda.libraries.psu.edu/theses/approved/WorldWideIndex/ETD-4587/index.html.

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Berg, Niklas. "Ice navigation with ice compressionin the Gulf of Finland". Thesis, Uppsala University, Division of Systems and Control, 2010. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-131133.

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Safe winter navigation is a hot topic. Not only is the traffic density increasing but theenvironmental considerations are also getting bigger. An oil leakage from a big oiltanker can be of catastrophic proportions in the wrong area and more trafficincreases the risk of an accident. A project that aims for safer winter navigation isSafeWIN. The aim of this project is to develop a forecasting system for compressiveice and thus make winter navigation safer.This thesis is part of above mentioned project and aims to investigate what influenceice compression and ice class has on winter navigation. Vessels are exclusivelyAFRAMAX size tankers sailing on Primorsk in the Gulf of Finland during 2006. Transitdata comes from AIS tracks recorded by the Swedish Maritime Administration. Adatabase with tanker transits has been created and this information is the source forthe studies in this thesis. Included in the database are wind data, ice particulars andtransit information such as speed, and time at different activities during the transit.Average values for a transit has been investigated for comparison and to get a pictureof an average transit.Velocity, waiting time and time with assisting icebreaker are parameters that arebelieved to show how a tanker performs in winter navigation. These parameters arecompared with ice compression and ice class separately to see if there is acorrelation. Ice compression has also been investigated for correlation towards windforce to see if stronger wind generates stronger compression.Using the velocity in different ice compressions an estimate of ice resistance that stemfrom ice compression has been extracted by means of Lindqvist’s formula.

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Lopes, Inês Marques. "Ice cream and nutrition: modeling optimal ice cream formulations". Master's thesis, ISA, 2014. http://hdl.handle.net/10400.5/6779.

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Mestrado em Engenharia Alimentar - Instituto Superior de Agronomia
It is becoming more urgent for producers to design new products that follow the consumer’s trends and expectations, such as, “low fat”, “no sugars” or “low calorie” products, while maintaining the ice cream features. The aim of this thesis was to develop a computer aided-tool, based on a mathematical model that helps to design ice cream recipes. By combining different expertise information, a linear programming model has been developed with the objective of minimizing the recipes calorie content. It compiles information about ingredients that are commonly used in ice cream manufacture and their contribution to nutrient and processing constraints. After setting all requirement constraints for each specific ice cream, the Excel Solver optimization tool, gives a solution for the model establishing the ingredients and their quantities to be included in the recipe. The developed model can be easily updated to account for changes in market demands or production conditions. It was created a version of the model for each one of the following ice cream types: water ice, ice cream, milk ice, dairy ice, sorbet and artisanal recipe. In order to test the effectiveness of the model, seven innovative recipes, using Portuguese ingredients with healthy benefits, have been created and tested at DuPont, Denmark.

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Jordan, James. "Modelling ice-ocean interactions in and around ice shelves". Thesis, Imperial College London, 2014. http://hdl.handle.net/10044/1/28616.

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Physical processes in Antarctica and the Southern Ocean are of great importance to the global climate system. This thesis considers two such processes, namely ice- ocean interaction in ice shelf basal crevasses and the conditional instability of frazil ice growth. It has been suggested that freezing within basal crevasses can act as a stabilising in uence on ice shelves, preventing their break up. Using Fluidity, a nite element ocean model, it is found that ocean circulation within a crevasse is highly dependent upon the amount of freezing in the crevasse. It is also found that frazil ice formation is responsible for the vast majority of freezing within a crevasse, and that there is a non linear relationship between the amount of supercooling in a crevasse and its freeze rate. The conditional instability of frazil ice growth is a little investigated mechanism of ice growth. Any frazil forming in the water column reduces the bulk density of a parcel of frazil-seawater mixture, causing it to rise. Due to the pressure-decrease in the freezing point, this causes more frazil to form, causing the parcel to accelerate, and so on. Numerical modelling nds that the instability does not operate in the presence of strong strati cation, high thermal driving (warm water), a small initial perturbation, high 'background' mixing or the prevalence of large frazil ice crystals. Given a large enough initial perturbation this instability could allow signi cant rates of ice growth even in water that is above the freezing point. The research presented in this thesis forms the material for two peer-reviewed publi- cations; 'Modelling ice ocean interactions in ice shelf basal crevasses' (Jordan et al., 2014) and 'On the conditional frazil ice instability in seawater' (Jordan et al., 2015).

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Rosier, Sebastian H. R. "The interaction between tides, ice shelves and ice streams". Thesis, Bangor University, 2015. https://research.bangor.ac.uk/portal/en/theses/the-interaction-between-tides-ice-shelves-and-ice-streams(0590227d-ae56-4a4d-8e5b-302bbe768774).html.

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Observation of ice-stream and ice-shelf flow has revealed interaction with the ocean tide, in some cases far upstream of the grounding line. Ice-stream velocities can be greatly affected by local ocean tides at a variety of timescales but of particular interest is a fortnightly modulation in flow that has been observed on the Rutford Ice Stream. This frequency is absent in the forcing, far stronger than the dominant tidal constituent signals and has been observed far inland. Understanding what mechanism can produce this signal can provide a window into mechanisms at the base of the ice stream that affect its flow. A consequence of this nonlinearity is that the mean flow of the Rutford Ice Stream is increased in comparison to a situation where no tidal forcing is present, implying that changes in tides could alter the long term flow of ice from Antarctica. Since local tides are sensitive to bathymetry which can change drastically due to changes in ice-shelf geometry and grounding line position, a feedback exists between tides and the ice sheet whereby changes in the flow of ice could alter tides which in turn would change the ice velocity. This thesis presents results from both ice-stream/shelf and tidal models to investigate these two mechanisms. Firstly a nonlinear 3D viscoelastic full-Stokes finite element model explores possible sources of nonlinearity that can produce fortnightly modulation in ice-stream flow far upstream of the grounding line. This model looks at stress transmission, grounding zone flexure, hydrology and grounding line migration and the conclusion is that tidally-induced changes in the subglacial water pressure play the largest role in producing this effect. Then, the OTIS tidal model is used to demonstrate that reduction in the thickness and/or extent of ice-shelves, in particular the Filchner-Ronne ice shelf, could greatly impact both tidal amplitudes and dissipation rates in the region. The research in this thesis clearly shows the importance of tidal interactions with the Antarctic ice sheet and that these are not limited to short temporal timescales.

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Shafrova, Svetlana. "First-year sea ice features. Investigation of ice field strength heterogeneity and modelling of ice rubble behaviour". Doctoral thesis, Norwegian University of Science and Technology, Department of Civil and Transport Engineering, 2007. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-1919.

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For the nearest years the design load level for offshore structures in Arctic regions is likely to be controlled by first-year sea ice ridges and rubble fields if the icebergs are not present in the area. Drifting ridges may hit fixed or moored surface structure such as platforms or ships, or they may gouge the seabed endangering pipelines and wellheads. Both the temporal and spatial properties of the consolidated layer and the unconsolidated part (the ice rubble) of the ice ridge are important input into ridgeload models. A better understanding of the ice rubble behaviour will enable us to determine the ice-ridge load more accurately. This thesis deals with two separate but connected subjects, namely: the ice strength field heterogeneity of both first-year sea ice ridge and level ice and the mechanical behaviour of the ice rubble.

Field mechanical testing of first-year sea ice by uniaxial compression has been done in order to improve the knowledge of the ice fields strength heterogeneity. The inplane ice strength non-homogeneity of different ice fields on the landfast level ice in the Spitsbergen fjords were investigated. A typical ice strength variability was found to be about 20-40% for the vertical ice samples and 10-20% for the horizontal ones. The weak zones were found within the entire ice fields. It was established that the strength of the ice samples taken from a certain depth from the ice cover surface at the different locations of the same ice field varied by a factor of 3 to 4. Furthermore, two first-year sea ice ridges have been examined with respect to the 2D spatial strength distribution: one in the North-western Barents Sea and one in the Arctic Ocean nearby Spitsbergen. The ice ridges are characterized by high strength heterogeneity of 40-55%, where the ice strength varied more than 3 times along both vertical and horizontal directions.

Special Finite Difference program “Inhomogeneity” was used to study the influence of the ice strength heterogeneity on the ice loads. It was shown that the ice heterogeneity might be one of the reasons for the scale effect.

In order to investigate the nature of freeze bonds between the ice blocks, series of field and laboratory small scale tests were conducted with submerged ice blocks. The small scale field tests were carried out in Adventfjorden on Spitsbergen. An opening was made in the landfast level ice. The level ice was sawed into cubic blocks which then were submerged down into the water. Some of the ice blocks were cut in two parts and then frozen together in order to simulate the freeze bonds between the ice blocks. The other blocks were submerged without forming the adfreeze bond. In addition to that, laboratory tests with both artificial ice (fresh and sea water) and natural sea ice were conducted in the cold laboratories at the University Centre in Svalbard (UNIS). The temporal development of the freeze bonding strength and the local strength of the ice blocks in the ice rubble, their changes with block size, confinement and ice properties were studied. The average freeze bonding strength from the field tests was found as 32 ± 18 kPa after 48 hours of submerging. The corresponding freeze bonding strength from the laboratory tests was 67 ± 52 kPa for the natural sea ice and 274 ± 142 kPa for the artificial freshwater ice within 60 hours of testing. Moreover, the ratio of freeze bonding strength to the strength of the submerged ice was found in the range of 0.008 to 0.082 with an average around 0.03 after 48 hours of submerging in the field. The corresponding strength ratio varied from 0.14 to 0.38 for the artificial fresh water ice and from 0.015 to 0.40 for the sea ice within 60 hours of testing in the laboratory.

A pseudo-discrete continuum model has been developed to study the behaviour of the ice rubble and in particularly its initial failure mechanism that is associated with the breakage of the freeze bonding contacts (rubble skeleton). The model is a combination of discrete particle assembly generation and Finite Element analysis of this assembly. The model provides a possibility to simulate the contacts between the ice blocks. A parametric analysis simulating 2D direct shear tests shows that the pseudo-discrete continuum model is very sensitive to both strength and morphology of the freeze bonds between the ice blocks. An attempt to extend the model to study large deformations within the ice rubble (that is associated with rotation, rearrangement of the ice blocks and their breakage) was considered.

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Książki na temat "Ice"

(Firm), Hamlyn, red. Ice creams. London: Hamlyn, 2001.

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1915-, Williams Chuck, red. Ice cream. New York: Simon & Schuster Source, 2003.

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School, New York Cooking, red. Ice cream. New York, N.Y., U.S.A: Penguin, 1987.

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Marshall, Robert T. Ice cream. Wyd. 5. New York: Chapman & Hall, 1996.

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Marshall, Robert T. Ice cream. Wyd. 6. New York: Kluwer Academic/Plenum Publishers, 2003.

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Neimark, Jill. Ice cream. New York, NY: Hastings House, 1986.

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Hoffman, Mable. Ice cream, sherbets & sorbets. Tucson, AZ: Fisher Books, 1991.

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Bego, Mark. Ice Ice Ice: The extraordinary Vanilla Ice story. New York: Bantam, 1991.

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Bego, Mark. Ice, Ice, Ice: The extraordinary Vanilla Ice story. New York, N.Y: Dell Pub., 1991.

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Pappas, Lou Seibert. Ice creams & sorbets: Cool recipes. San Francisco: Chronicle Books, 2005.

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Części książek na temat "Ice"

Cleaves, Henderson James. "Ice". W Encyclopedia of Astrobiology, 1180–81. Berlin, Heidelberg: Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-662-44185-5_4018.

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Furukawa, Yoshinori. "Ice". W Encyclopedia of Earth Sciences Series, 557–60. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2642-2_253.

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Cleaves, Henderson Jim. "Ice". W Encyclopedia of Astrobiology, 804. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-11274-4_4018.

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Dodds, Klaus. "Ice". W The Routledge Handbook of Ocean Space, 401–12. London: Routledge, 2022. http://dx.doi.org/10.4324/9781315111643-37.

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Young, Timothy, Michael Ashcroft, Julian Cooke, Andrew Taylor, John D. Kimball, David W. Martowski, LeRoy Lambert i Michael F. Sturley. "Ice". W Voyage Charters, 999–1004. Wyd. 5. London: Informa Law from Routledge, 2022. http://dx.doi.org/10.4324/9781003046912-48.

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Cleaves, Henderson James. "Ice". W Encyclopedia of Astrobiology, 1–2. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-27833-4_4018-3.

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Bailey-Charteris, Bronwyn. "Ice". W The Hydrocene, 150–71. London: Routledge, 2024. http://dx.doi.org/10.4324/9781003397304-8.

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Cleaves, Henderson James. "Ice". W Encyclopedia of Astrobiology, 1–2. Berlin, Heidelberg: Springer Berlin Heidelberg, 2022. http://dx.doi.org/10.1007/978-3-642-27833-4_4018-4.

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Cleaves, Henderson James. "Ice". W Encyclopedia of Astrobiology, 1415–16. Berlin, Heidelberg: Springer Berlin Heidelberg, 2023. http://dx.doi.org/10.1007/978-3-662-65093-6_4018.

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Thomas, Robert. "Ice Sheets and Ice Volume". W Encyclopedia of Remote Sensing, 269–81. New York, NY: Springer New York, 2014. http://dx.doi.org/10.1007/978-0-387-36699-9_63.

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Streszczenia konferencji na temat "Ice"

Chen, Ke, Jiasheng Wu, Kun Liang i Qingxia Li. "Retrieval of Ice Cloud Parameters from Simulations of the Ice Cloud Imager (ICI) Based on Convolutional Neural Networks". W IGARSS 2024 - 2024 IEEE International Geoscience and Remote Sensing Symposium, 5695–98. IEEE, 2024. http://dx.doi.org/10.1109/igarss53475.2024.10641375.

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Strackx, Raoul, Bart Jacobs i Frank Piessens. "ICE". W the 30th Annual Computer Security Applications Conference. New York, New York, USA: ACM Press, 2014. http://dx.doi.org/10.1145/2664243.2664259.

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Wang, Chuan-Ju, Ting-Hsiang Wang, Hsiu-Wei Yang, Bo-Sin Chang i Ming-Feng Tsai. "ICE". W SIGIR '17: The 40th International ACM SIGIR conference on research and development in Information Retrieval. New York, NY, USA: ACM, 2017. http://dx.doi.org/10.1145/3077136.3080807.

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Niemczyk, Stefan, Stephan Opfer, Nugroho Fredivianus i Kurt Geihs. "ICE". W SAC 2017: Symposium on Applied Computing. New York, NY, USA: ACM, 2017. http://dx.doi.org/10.1145/3019612.3019653.

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Castro-Ochante, Jose, Guillermo Camara-Chavez i Erick Gomez-Nieto. "ICE". W SAC '21: The 36th ACM/SIGAPP Symposium on Applied Computing. New York, NY, USA: ACM, 2021. http://dx.doi.org/10.1145/3412841.3441921.

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Parkes, David C., Ruggiero Cavallo, Nick Elprin, Adam Juda, Sébastien Lahaie, Benjamin Lubin, Loizos Michael, Jeffrey Shneidman i Hassan Sultan. "ICE". W the 6th ACM conference. New York, New York, USA: ACM Press, 2005. http://dx.doi.org/10.1145/1064009.1064036.

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Belgin, Mehmet, Trever C. Nightingale, David A. Mercer, Fang Cherry Liu, Peter Wan, Andre C. McNeill, Ruben Lara, Paul Manno i Neil Bright. "ICE". W PEARC '18: Practice and Experience in Advanced Research Computing. New York, NY, USA: ACM, 2018. http://dx.doi.org/10.1145/3219104.3219112.

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Pucsek, Dean, Jonah Wall, Celina Gibbs, Jennifer Baldwin, Martin Salois i Yvonne Coady. "ICE". W Proceeding of the 1st workshop. New York, New York, USA: ACM Press, 2011. http://dx.doi.org/10.1145/1984708.1984731.

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Boyer, Truman Parks, i Mohsen Chitsaz. "ICE#8482; and ICE/T#8482;". W Working group reports from ITiCSE. New York, New York, USA: ACM Press, 2004. http://dx.doi.org/10.1145/1044550.1041657.

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Wallace, Randy, i Galdemir Botura. "Development of ICE/NO-ICE Sensor System for in-Flight Ice Detection". W FAA In-flight Icing / Ground De-icing International Conference & Exhibition. 400 Commonwealth Drive, Warrendale, PA, United States: SAE International, 2003. http://dx.doi.org/10.4271/2003-01-2113.

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Raporty organizacyjne na temat "Ice"

Dallimore, S. R. Ice Bonding and Excess Ice. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132231.

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Coon, Max D. Sea Ice Model for Marginal Ice Zone. Fort Belvoir, VA: Defense Technical Information Center, wrzesień 2003. http://dx.doi.org/10.21236/ada615524.

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Coon, Max D. Sea Ice Model for Marginal Ice Zone. Fort Belvoir, VA: Defense Technical Information Center, wrzesień 2001. http://dx.doi.org/10.21236/ada626073.

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Karig, Fred. Ice Camp. Fort Belvoir, VA: Defense Technical Information Center, wrzesień 1999. http://dx.doi.org/10.21236/ada629717.

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Wadhams, Peter. Wave-Ice Interaction and the Marginal Ice Zone. Fort Belvoir, VA: Defense Technical Information Center, wrzesień 2013. http://dx.doi.org/10.21236/ada601220.

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Wadhams, Peter, i Martin Doble. Wave-Ice Interaction and the Marginal Ice Zone. Fort Belvoir, VA: Defense Technical Information Center, wrzesień 2014. http://dx.doi.org/10.21236/ada617951.

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Ackley, S. F., T. Maksym i S. Stammerjohn. Wave-Ice and Air-Ice-Ocean Interaction During the Chukchi Sea Ice Edge Advance. Fort Belvoir, VA: Defense Technical Information Center, wrzesień 2013. http://dx.doi.org/10.21236/ada601218.

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Perovich, Don, i Bonnie Light. Sunlight, Sea Ice, and the Ice Albedo Feedback in a Changing Arctic Sea Ice Cover. Fort Belvoir, VA: Defense Technical Information Center, wrzesień 2013. http://dx.doi.org/10.21236/ada601068.

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Rogers, W. E., P. G. Posey, Clarence Collins i Yalin Fan. Wave-Ice interaction in the Marginal Ice Zone: Toward a Wave-Ocean-Ice Coupled Modeling System. Fort Belvoir, VA: Defense Technical Information Center, wrzesień 2015. http://dx.doi.org/10.21236/ad1013723.

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Rogers, W. E., i Pamela G. Posey. Wave-Ice Interaction in the Marginal Ice Zone: Toward a Wave-Ocean-Ice Coupled Modeling System. Fort Belvoir, VA: Defense Technical Information Center, wrzesień 2013. http://dx.doi.org/10.21236/ada601214.

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