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Journal articles on the topic 'Ice'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 July 2025

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1

Kokkinakis E, N., A. Fragkiadakis G, H. Ioakeimidi S, B. Giankoulof I, and N. Kokkinaki A. "Microbiological quality of ice cream after HACCP implementation: a factory case study." Czech Journal of Food Sciences 26, No. 5 (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 s

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2

Commissariat, Tushna. "Ice ice baby." Physics World 34, no. 8 (2021): 23. http://dx.doi.org/10.1088/2058-7058/34/08/26.

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3

Geli, Norma. "Ice, Ice Baby." ASHA Leader 21, no. 6 (2016): 8. http://dx.doi.org/10.1044/leader.gl.21062016.8.

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4

Armstrong, Gavin. "Ice ice maybe." Nature Chemistry 2, no. 4 (2010): 256. http://dx.doi.org/10.1038/nchem.608.

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5

Toliver, Richard. "Ice Is Ice?" Journal of the IEST 31, no. 3 (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 effect

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6

Fei, Xie, Lu Peng, Cheng Bin, Yang Qian, and Li Zhijun. "Magical spherical ice (ice balls, ice eggs)." Journal of Lake Sciences 34, no. 2 (2022): 695–98. http://dx.doi.org/10.18307/2022.0228.

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7

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

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8

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

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9

Guizzo, E. "Into deep ice [ice monitoring]." IEEE Spectrum 42, no. 12 (2005): 28–35. http://dx.doi.org/10.1109/mspec.2005.1549779.

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10

Moore, John. "Ice blisters and ice dolines." Journal of Glaciology 39, no. 133 (1993): 714–16. http://dx.doi.org/10.1017/s002214300001666x.

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11

Moore, John. "Ice blisters and ice dolines." Journal of Glaciology 39, no. 133 (1993): 714–16. http://dx.doi.org/10.3189/s002214300001666x.

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12

Kato, Manabu, Yu-Ichi Iijima, Masahiko Arakawa, et al. "Ice-on-Ice Impact Experiments." Icarus 113, no. 2 (1995): 423–41. http://dx.doi.org/10.1006/icar.1995.1032.

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13

Yano, J. I., and V. T. J. Phillips. "Ice–Ice Collisions: An Ice Multiplication Process in Atmospheric Clouds." Journal of the Atmospheric Sciences 68, no. 2 (2011): 322–33. http://dx.doi.org/10.1175/2010jas3607.1.

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Abstract Ice in atmospheric clouds undergoes complex physical processes, interacting especially with radiation, which leads to serious impacts on global climate. After their primary production, atmospheric ice crystals multiply extensively by secondary processes. Here, it is shown that a mostly overlooked process of mechanical breakup of ice particles by ice–ice collisions contributes to such observed multiplication. A regime for explosive multiplication is identified in its phase space of ice multiplication efficiency and number concentration of ice particles. Many natural mixed-phase clouds,

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14

Byrne, Grant. "ICE." Cancer Nursing Practice 14, no. 8 (2015): 10. http://dx.doi.org/10.7748/cnp.14.8.10.s12.

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15

LAST, BOB. "Ice." Critical Quarterly 36, no. 2 (1994): 102–5. http://dx.doi.org/10.1111/j.1467-8705.1994.tb01042.x.

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16

Exell, John. "Ice." British Journal of Psychiatry 202, no. 2 (2013): 149. http://dx.doi.org/10.1192/bjp.bp.111.102129.

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17

Borzutzky, Daniel. "Ice." NACLA Report on the Americas 56, no. 2 (2024): 226–27. http://dx.doi.org/10.1080/10714839.2024.2356321.

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18

González-Calle, David, Manuel Barreiro-Perez, Ignacio Cruz-González, and Pedro L. Sánchez. "ICE." JACC: Cardiovascular Interventions 12, no. 19 (2019): 1983–84. http://dx.doi.org/10.1016/j.jcin.2019.07.022.

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19

Sorokin, Vladimir, and Andrew Bromfield. "Ice." Index on Censorship 34, no. 4 (2005): 83–91. http://dx.doi.org/10.1080/03064220500429841.

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20

Williams, C. K. "Ice." Missouri Review 9, no. 1 (1985): 163. http://dx.doi.org/10.1353/mis.1985.0131.

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21

HIGASHI, Akira. "Ice in Tokyo and Antarctic ice." Journal of the Japanese Society of Snow and Ice 58, no. 2 (1996): 169–78. http://dx.doi.org/10.5331/seppyo.58.169.

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22

YASUTOME, Akira, Masahiko ARAKAWA, and Norikazu MAENO. "Measurements of ice-ice friction coefficients." Journal of the Japanese Society of Snow and Ice 61, no. 6 (1999): 437–43. http://dx.doi.org/10.5331/seppyo.61.437.

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23

Bai, J., J. Wang, and X. C. Zeng. "Multiwalled ice helixes and ice nanotubes." Proceedings of the National Academy of Sciences 103, no. 52 (2006): 19664–67. http://dx.doi.org/10.1073/pnas.0608401104.

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24

Bridges, Robert, Kaj Riska, Mark Hopkins, and Ying Wei. "Ice interaction processes during ice encroachment." Marine Structures 67 (September 2019): 102629. http://dx.doi.org/10.1016/j.marstruc.2019.05.007.

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25

Hendrikse, Hayo, and Andrei Metrikine. "Ice-induced vibrations and ice buckling." Cold Regions Science and Technology 131 (November 2016): 129–41. http://dx.doi.org/10.1016/j.coldregions.2016.09.009.

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26

Boyer, Truman Parks, and Mohsen Chitsaz. "ICE™ and ICE/T™." ACM SIGCSE Bulletin 36, no. 4 (2004): 55–57. http://dx.doi.org/10.1145/1041624.1041657.

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27

MAKITA, Shunsuke, Kunio ENOKI, Norihiro USAMI, Humihiro HARA, and Hirosi SAEKI. "MODE OF ICE LOAD ACTING ON ICE BOOM FOR ICE CONTROL." PROCEEDINGS OF CIVIL ENGINEERING IN THE OCEAN 15 (1999): 623–27. http://dx.doi.org/10.2208/prooe.15.623.

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28

KIOKA, Shinji, and Takahiro TAKEUCHI. "ICE LOAD ON ICE BOOM CONSIDERING ROUGHNESS OF SEA ICE BOTTOM." Journal of Japan Society of Civil Engineers, Ser. B3 (Ocean Engineering) 67, no. 2 (2011): I_1021—I_1026. http://dx.doi.org/10.2208/jscejoe.67.i_1021.

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29

Lou, Wenjuan, Siran Chen, Zuopeng Wen, Liqi Wang, and Dengguo Wu. "Effects of Ice Surface and Ice Shape on Aerodynamic Characteristics of Crescent-Shaped Iced Conductors." Journal of Aerospace Engineering 34, no. 3 (2021): 04021008. http://dx.doi.org/10.1061/(asce)as.1943-5525.0001246.

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30

Mathews, William H. "Ice Sheets and Ice Streams: Thoughts on the Cordilleran Ice Sheet Symposium." Géographie physique et Quaternaire 45, no. 3 (2007): 263–67. http://dx.doi.org/10.7202/032873ar.

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ABSTRACT This paper comments on preconceptions about what is meant by the terms "Cordilleran Ice Sheet" and "ice stream". Contemporary Antarctic ice streams are described. The Laurentian Channel and throughs crossing the continental ice shelf between Vancouver and Queens Charlotte Islands are suggested as candidates for the tracks of past ice streams.

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31

YOSHIKAWA, Yasuhiro, Yasuharu WATANABE, Hiroshi HAYAKAWA, and Yasuyuki HIRAI. "A STUDY OF ICE BREAK AND ICE FLOW DURING RIVER ICE BREAKUP." Journal of Japan Society of Civil Engineers, Ser. B1 (Hydraulic Engineering) 67, no. 4 (2011): I_1075—I_1080. http://dx.doi.org/10.2208/jscejhe.67.i_1075.

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32

Phillips, Vaughan T. J., Jun-Ichi Yano, Marco Formenton, et al. "Ice Multiplication by Breakup in Ice–Ice Collisions. Part II: Numerical Simulations." Journal of the Atmospheric Sciences 74, no. 9 (2017): 2789–811. http://dx.doi.org/10.1175/jas-d-16-0223.1.

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Abstract In Part I of this two-part paper, a formulation was developed to treat fragmentation in ice–ice collisions. In the present Part II, the formulation is implemented in two microphysically advanced cloud models simulating a convective line observed over the U.S. high plains. One model is 2D with a spectral bin microphysics scheme. The other has a hybrid bin–two-moment bulk microphysics scheme in 3D. The case consists of cumulonimbus cells with cold cloud bases (near 0°C) in a dry troposphere. Only with breakup included in the simulation are aircraft observations of particles with maximum

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33

Phillips, Vaughan T. J., Jun-Ichi Yano, and Alexander Khain. "Ice Multiplication by Breakup in Ice–Ice Collisions. Part I: Theoretical Formulation." Journal of the Atmospheric Sciences 74, no. 6 (2017): 1705–19. http://dx.doi.org/10.1175/jas-d-16-0224.1.

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Abstract For decades, enhancement of ice concentrations above those of active ice nucleus aerosols was observed in deep clouds with tops too warm for homogeneous freezing, indicating fragmentation of ice (multiplication). Several possible mechanisms of fragmentation have been suggested from laboratory studies, and one of these involves fragmentation in ice–ice collisions. In this two-part paper, the role of breakup in ice–ice collisions in a convective storm consisting of many cloud types is assessed with a modeling approach. The colliding ice particles can belong to any microphysical species,

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34

Mages, Stephan, Ole Hensel, Antonia Maria Zierz, Torsten Kraya, and Stephan Zierz. "Experimental provocation of ‘ice-cream headache’ by ice cubes and ice water." Cephalalgia 37, no. 5 (2016): 464–69. http://dx.doi.org/10.1177/0333102416650704.

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Background There are various studies on experimentally provoked ‘ice-cream headache’ or ‘headache attributed to ingestion or inhalation of a cold stimulus’ (HICS) using different provocation protocols. The aim of this study was to compare two provocation protocols. Methods Ice cubes pressed to the palate and fast ingestion of ice water were used to provoke HICS and clinical features were compared. Results The ice-water stimulus provoked HICS significantly more often than the ice-cube stimulus (9/77 vs. 39/77). Ice-water-provoked HICS had a significantly shorter latency (median 15 s, range 4–97

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35

MacAyeal, Douglas R., and Victor Barcilon. "Ice-shelf Response to Ice-stream Discharge Fluctuations: I. Unconfined Ice Tongues." Journal of Glaciology 34, no. 116 (1988): 121–27. http://dx.doi.org/10.1017/s002214300000914x.

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AbstractIce-stream discharge fluctuations constitute an independent means of forcing unsteady ice-shelf behavior, and their effect must be distinguished from those of oceanic and atmospheric climate to understand ice-shelf change. In addition, ice-stream-generated thickness anomalies may constitute a primary trigger of ice-rise formation in the absence of major sea-level fluctuations. Such triggering may maintain the current ice-rise population that, in turn, contributes to long-term ice-sheet stability. Here, we show that ice-stream-generated fluctuations of an ideal, two-dimensional ice shel

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36

Pinsky, M. B., and A. P. Khain. "Some effects of cloud turbulence on water–ice and ice–ice collisions." Atmospheric Research 47-48 (June 1998): 69–86. http://dx.doi.org/10.1016/s0169-8095(98)00041-6.

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37

Sayag, Roiy, Eli Tziperman, and Michael Ghil. "Rapid switch-like sea ice growth and land ice-sea ice hysteresis." Paleoceanography 19, no. 1 (2004): n/a. http://dx.doi.org/10.1029/2003pa000946.

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38

MacAyeal, Douglas R., and Victor Barcilon. "Ice-shelf Response to Ice-stream Discharge Fluctuations: I. Unconfined Ice Tongues." Journal of Glaciology 34, no. 116 (1988): 121–27. http://dx.doi.org/10.3189/s002214300000914x.

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AbstractIce-stream discharge fluctuations constitute an independent means of forcing unsteady ice-shelf behavior, and their effect must be distinguished from those of oceanic and atmospheric climate to understand ice-shelf change. In addition, ice-stream-generated thickness anomalies may constitute a primary trigger of ice-rise formation in the absence of major sea-level fluctuations. Such triggering may maintain the current ice-rise population that, in turn, contributes to long-term ice-sheet stability. Here, we show that ice-stream-generated fluctuations of an ideal, two-dimensional ice shel

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39

McDougall, Trevor J., Paul M. Barker, Rainer Feistel, and Ben K. Galton-Fenzi. "Melting of Ice and Sea Ice into Seawater and Frazil Ice Formation." Journal of Physical Oceanography 44, no. 7 (2014): 1751–75. http://dx.doi.org/10.1175/jpo-d-13-0253.1.

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Abstract The thermodynamic consequences of the melting of ice and sea ice into seawater are considered. The International Thermodynamic Equation Of Seawater—2010 (TEOS-10) is used to derive the changes in the Conservative Temperature and Absolute Salinity of seawater that occurs as a consequence of the melting of ice and sea ice into seawater. Also, a study of the thermodynamic relationships involved in the formation of frazil ice enables the calculation of the magnitudes of the Conservative Temperature and Absolute Salinity changes with pressure when frazil ice is present in a seawater parcel

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40

Nortala-Hoikkanen, Anita, Kaj Riska, Olli Salmela, and G�ran Wilkman. "Methods to map ice conditions, measure ice properties and quantify ice features." Hydrotechnical Construction 28, no. 3 (1994): 180–88. http://dx.doi.org/10.1007/bf01545936.

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41

Eccles, R., L. Du-Plessis, Y. Dommels, and J. E. Wilkinson. "Cold pleasure. Why we like ice drinks, ice-lollies and ice cream." Appetite 71 (December 2013): 357–60. http://dx.doi.org/10.1016/j.appet.2013.09.011.

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42

SHIMADA, Rigen, Nozomu TAKEUCHI, and Teruo AOKI. "Remote Sensing of bare ice and dark ice on Greenland ice sheet." Journal of the Japanese Society of Snow and Ice 78, no. 6 (2016): 391–400. http://dx.doi.org/10.5331/seppyo.78.6_391.

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43

Nurjanah, Siti, Qonitatin Wafiyah, Winiati P. Rahayu, and C. C. Nurwitri. "Titik Kritis Keamanan Pangan pada Tahap Pengolahan dan Penyajian Beberapa Jenis Minuman Es." Jurnal Mutu Pangan : Indonesian Journal of Food Quality 8, no. 2 (2022): 80–87. http://dx.doi.org/10.29244/jmpi.2021.8.2.80.

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In small vendors, iced beverages potentially contain microbiological and chemical hazards. The objective of this study was to identify critical points of hazard during processing and serving steps various types of most popular iced beverages. Based on processing step, there were identified nine types of iced beverages i.e. coconut, grass jelly, sliced fruit, orange, mixed, cendol, juice, blended and flavouring ice. The study was conducted by observation 90 vendors addressed to processing step, utilities, and environ-mental condition at low, middle and high economic scale of vendors. The critic

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44

Schwenk, Thomas. "Ice Massage Cools Faster Than Ice Bag." Physician and Sportsmedicine 26, no. 8 (1998): 7–8. http://dx.doi.org/10.3810/psm.1998.08.1581.

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45

Röthlisberger, Regine, and Nerilie Abram. "Sea-ice proxies in Antarctic ice cores." PAGES news 17, no. 1 (2009): 24–26. http://dx.doi.org/10.22498/pages.17.1.24.

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46

TAKEUCHI, Takahiro, Mikio SASAKI, Satoshi AKAGAWA, et al. "ICE LOAD OF MULTI ICE FAILURE ZONES." PROCEEDINGS OF CIVIL ENGINEERING IN THE OCEAN 15 (1999): 605–10. http://dx.doi.org/10.2208/prooe.15.605.

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47

Haugen, Joakim, and Lars Imsland. "Autonomous Aerial Ice Observation for Ice Defense." Modeling, Identification and Control: A Norwegian Research Bulletin 35, no. 4 (2014): 279–91. http://dx.doi.org/10.4173/mic.2014.4.5.

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48

Aleksandrov, A., V. Platonov, and V. Shaposhnikov. "Ice going ships: speed vs ice load." Transactions of the Krylov State Research Centre 2, no. 388 (2019): 69–76. http://dx.doi.org/10.24937/2542-2324-2019-2-388-69-76.

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49

Bindschadler, Robert, Ted A. Scambos, Helmut Rott, Pedro Skvarca, and Patricia Vornberger. "Ice dolines on Larsen Ice Shelf, Antarctica." Annals of Glaciology 34 (2002): 283–90. http://dx.doi.org/10.3189/172756402781817996.

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AbstractIce dolines on the Larsen Ice Shelf, Antarctica, are observed to be elongated depressions a few hundred meters across and up to 19 m deep. One-meter resolution imagery is used to quantify these dimensions. Elevation profiles across five dolines are derived by photoclinometry. Landsat and radar imagery is also used to show that dolines can form in a single melt season and persist for years. Dolines occur in clusters and in direct proximity to surface meltwater lakes. Field observations suggest dolines form by collapse into a subsurface cavity. A direct hydraulic connection with the unde

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50

Aldus, R. J., T. Fennell, P. P. Deen, et al. "Ice rule correlations in stuffed spin ice." New Journal of Physics 15, no. 1 (2013): 013022. http://dx.doi.org/10.1088/1367-2630/15/1/013022.

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