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Journal articles on the topic 'Ice growing'

Author: Grafiati

Published: 30 May 2022

Last updated: 31 July 2025

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1

Searby, Adam, Phil Maude, and Ian McGrath. "Growing Old With Ice." Journal of Addictions Nursing 26, no. 2 (2015): 93–98. http://dx.doi.org/10.1097/jan.0000000000000076.

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2

Bensassi, Sami, Julienne C. Stroeve, Inmaculada Martínez-Zarzoso, and Andrew P. Barrett. "Melting ice, growing trade?" Elementa: Science of the Anthropocene 4 (May 20, 2016): 000107. http://dx.doi.org/10.12952/journal.elementa.000107.

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3

Jacobs, S. S. "Is the Antarctic ice sheet growing?" Nature 360, no. 6399 (1992): 29–33. http://dx.doi.org/10.1038/360029a0.

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4

Wells, A. J., J. S. Wettlaufer, and S. A. Orszag. "Brine fluxes from growing sea ice." Geophysical Research Letters 38, no. 4 (2011): n/a. http://dx.doi.org/10.1029/2010gl046288.

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5

Hart, Carl R., Cody M. Best, Emily Asenath-Smith, Kiera L. Thompson Towell, Michelle E. Swearingen, and Michael B. Muhlestein. "Experimental modal testing of growing thin ice." Journal of the Acoustical Society of America 155, no. 3_Supplement (2024): A332. http://dx.doi.org/10.1121/10.0027709.

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Current practices for assessing the thickness of growing ice include drilling and coring. This is inherently risky and motivates the use of a stand-off method. Laser Doppler vibrometry is a potential technique, however, the interpretation of vibrometer signals must be informed by a physical understanding of ice subjected to mechanical vibrations. The vibrational response of growing, thin ice is largely unknown. For thick ice, adequate predictions for the vibrational response assumes ice behaves as an elastic plate. It is hypothesized that thin ice responds in a fashion somewhere between an ela

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6

Verdaguer, Albert, Juan José Segura, Laura López-Mir, Guillaume Sauthier, and Jordi Fraxedas. "Communication: Growing room temperature ice with graphene." Journal of Chemical Physics 138, no. 12 (2013): 121101. http://dx.doi.org/10.1063/1.4798941.

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7

Arakawa, Masahiko, Norikazu Maeno, and Michiya Higa. "Direct observations of growing cracks in ice." Journal of Geophysical Research 100, E4 (1995): 7539. http://dx.doi.org/10.1029/95je00278.

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8

Lilach, Yigal, Martin J. Iedema, and James P. Cowin. "Proton segregation on a growing ice interface." Surface Science 602, no. 17 (2008): 2886–93. http://dx.doi.org/10.1016/j.susc.2008.07.008.

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9

Audh, Riesna Reuben, Sarah Fawcett, Siobhan Johnson, Tokoloho Rampai, and Marcello Vichi. "Rafting of Growing Antarctic Sea Ice Enhances In-Ice Biogeochemical Activity in Winter." Journal of Geophysical Research: Oceans 128, no. 12 (2023): e2023JC019925. https://doi.org/10.1029/2023JC019925.

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The study of Antarctic first-year sea-ice biogeochemistry has been limited by samples mostly being collected in pack ice during summer, with few winter data available. Measurements from the Antarctic marginal ice zone (AMIZ) have proven even more difficult to obtain. The AMIZ is a broad, circumpolar feature of the Southern Ocean found at different latitudes during the year where light and nutrients are high enough to sustain primary production and influence ecosystem functioning. We present the first biogeochemical data set from growing ice collected in the Atlantic AMIZ during winter 2019, in

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10

Dolev, Maya Bar, J. J. Liu, Yangzong Qin, et al. "143 Ice shaping in solutions of ice-binding proteins – Melting vs growing morphologies." Cryobiology 67, no. 3 (2013): 438–39. http://dx.doi.org/10.1016/j.cryobiol.2013.09.149.

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11

Douglas, Bruce C., Robert E. Cheney, Laury Miller, Russell W. Agreen, William E. Carter, and Douglas S. Robertson. "Greenland Ice Sheet: Is It Growing or Shrinking?" Science 248, no. 4953 (1990): 288. http://dx.doi.org/10.1126/science.248.4953.288.a.

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12

Kärcher, B., and M. M. Basko. "Trapping of trace gases in growing ice crystals." Journal of Geophysical Research: Atmospheres 109, no. D22 (2004): n/a. http://dx.doi.org/10.1029/2004jd005254.

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13

Shen, XiaoFeng. "Emission of unidentified energy from growing ice crystals." Applied Physics Letters 90, no. 7 (2007): 071902. http://dx.doi.org/10.1063/1.2472536.

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14

Finnegan, William G., Steven K. Chai, and Andrew Detwiler. "Enhanced and Oriented Riming of Growing Ice Crystals." Journal of the Atmospheric Sciences 61, no. 15 (2004): 1976–81. http://dx.doi.org/10.1175/1520-0469(2004)061<1976:eaorog>2.0.co;2.

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15

Douglas, B. C., R. E. Cheney, L. Miller, R. W. Agreen, W. E. Carter, and D. S. Robertson. "Greenland Ice Sheet: Is It Growing or Shrinking?" Science 248, no. 4953 (1990): 288. http://dx.doi.org/10.1126/science.248.4953.288.

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16

Lipp, G., S. Galow, Ch Körber, and G. Rau. "Encapsulation of Human Erythrocytes by Growing Ice Crystals." Cryobiology 31, no. 3 (1994): 305–12. http://dx.doi.org/10.1006/cryo.1994.1036.

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17

Chu, P. C. "Air-Ice-Ocean Feedback Mechanisms and Ice Oscillation on Millennial Time Scales." Annals of Glaciology 14 (1990): 28–31. http://dx.doi.org/10.3189/s026030550000820x.

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Air-ice-ocean feedback mechanisms, which are not conventionally incorporated within either climate or glacial models, are investigated to illustrate their potential role in generating ice advance/retreat on the time scale of 103–104 years; i.e. for examining the internal causes for the ice oscillation.Three main feedback loops are found from a coupled air-ice-ocean model developed in this paper: (a) ice advance → lower air temperature → ice freezing → ice advance; and (b) ice advance → higher ocean temperature → ice melting → ice retreat; (c) ice advance/retreat → modification of evaporation r

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18

Chu, P. C. "Air-Ice-Ocean Feedback Mechanisms and Ice Oscillation on Millennial Time Scales." Annals of Glaciology 14 (1990): 28–31. http://dx.doi.org/10.1017/s026030550000820x.

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Air-ice-ocean feedback mechanisms, which are not conventionally incorporated within either climate or glacial models, are investigated to illustrate their potential role in generating ice advance/retreat on the time scale of 103–104 years; i.e. for examining the internal causes for the ice oscillation. Three main feedback loops are found from a coupled air-ice-ocean model developed in this paper: (a) ice advance → lower air temperature → ice freezing → ice advance; and (b) ice advance → higher ocean temperature → ice melting → ice retreat; (c) ice advance/retreat → modification of evaporation

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19

Kippenberger, Matthias, Gerhard Schuster, Jos Lelieveld, and John N. Crowley. "Trapping of HCl and oxidised organic trace gases in growing ice at temperatures relevant to cirrus clouds." Atmospheric Chemistry and Physics 19, no. 18 (2019): 11939–51. http://dx.doi.org/10.5194/acp-19-11939-2019.

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Abstract. The uptake of hydrochloric acid (HCl), ethanol (C2H5OH), 1-butanol (1-C4H9OH), formic acid HC(O)OH and trifluoroacetic (CF3C(O)OH) acid to growing ice surfaces was investigated at temperatures between 194 and 228 K. HCl displayed extensive, continuous uptake during ice growth, which was strongly dependent on the ice growth velocity, the temperature of the ice surface and the gas phase concentration of HCl. Trifluoroacetic acid was also observed to be trapped in growing ice, albeit approximately an order of magnitude less efficiently than HCl, whereas the adsorption and desorption kin

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20

Elif Genceli Güner, F., Johan Wåhlin, Mogens Hinge, and Signe Kjelstrup. "The temperature jump at a growing ice–water interface." Chemical Physics Letters 622 (February 2015): 15–19. http://dx.doi.org/10.1016/j.cplett.2015.01.013.

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21

Molemaker, M. Jeroen, and Henk A. Dijkstra. "Double diffusive and direct instabilities below growing sea ice." International Journal of Heat and Mass Transfer 37, no. 16 (1994): 2547–59. http://dx.doi.org/10.1016/0017-9310(94)90292-5.

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22

Suzuki, Yoshihisa, Gen Sazaki, Kaori Hashimoto, Takahisa Fujiwara, and Yoshinori Furukawa. "Colloidal crystallization utilizing interfaces of unidirectionally growing ice crystals." Journal of Crystal Growth 383 (November 2013): 67–71. http://dx.doi.org/10.1016/j.jcrysgro.2013.08.026.

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23

Bednarz, G., and M. J. Krasinski. "Visualization of the boundary layer on the growing ice." Crystal Research and Technology 22, no. 9 (1987): K145—K147. http://dx.doi.org/10.1002/crat.2170220928.

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24

Kawamura, Toshiyuki. "A Method for Growing Large Single Crystals of Sea Ice." Journal of Glaciology 32, no. 111 (1986): 302–3. http://dx.doi.org/10.1017/s002214300001563x.

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Abstract A simple technique is presented for growing large single crystals of sea ice. Using this technique, crystals with dimensions of 20 cm × 20 cm × 10 cm or more can be readily obtained within an orientational accuracy of 3°. Such crystals can then be used to investigate the physical properties of sea ice.

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25

Kawamura, Toshiyuki. "A Method for Growing Large Single Crystals of Sea Ice." Journal of Glaciology 32, no. 111 (1986): 302–3. http://dx.doi.org/10.3189/s002214300001563x.

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AbstractA simple technique is presented for growing large single crystals of sea ice. Using this technique, crystals with dimensions of 20 cm × 20 cm × 10 cm or more can be readily obtained within an orientational accuracy of 3°. Such crystals can then be used to investigate the physical properties of sea ice.

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26

Knight, Charles A. "A simple technique for growing large, optically “perfect” ice crystals." Journal of Glaciology 42, no. 142 (1996): 585–87. http://dx.doi.org/10.1017/s0022143000003567.

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AbstractLarge, single ice crystals containing nо air bubbles and free of both small-angle grain boundaries and visible stress birefringence can be grown using a very simple growth chamber within a temperature-controlled, outer enclosure. The method relies upon the spontaneous formation of an ice crystal with itsсaxis accurately normal to a free, slightly supercooled, water surface.

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27

Knight, Charles A. "A simple technique for growing large, optically “perfect” ice crystals." Journal of Glaciology 42, no. 142 (1996): 585–87. http://dx.doi.org/10.3189/s0022143000003567.

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AbstractLarge, single ice crystals containing nо air bubbles and free of both small-angle grain boundaries and visible stress birefringence can be grown using a very simple growth chamber within a temperature-controlled, outer enclosure. The method relies upon the spontaneous formation of an ice crystal with its с axis accurately normal to a free, slightly supercooled, water surface.

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28

Knight, Charles A. "An exploratory study of ice-cube spikes." Journal of Glaciology 51, no. 173 (2005): 191–200. http://dx.doi.org/10.3189/172756505781829368.

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AbstractIt is well known that ice-cube spikes form by the extrusion of water at the surface of a freezing ice cube, driven by the expansion accompanying freezing. The growing spikes are water-filled ice tubes, growing at their tips as the water is expelled. This paper represents an exploration of their formation and the principles behind whether a freezing ice cube grows a spike or not. For this purpose, ice cubes are frozen in one set of conditions to observe what happens when spikes do or do not form. Spike formation requires a nearly steady-state freezing-and-extrusion process at the growin

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29

Baccile, Niki, Thomas Zinn, Guillaume P. Laurent, Ghazi Ben Messaoud, Viviana Cristiglio, and Francisco M. Fernandes. "Unveiling the Interstitial Pressure between Growing Ice Crystals during Ice-Templating Using a Lipid Lamellar Probe." Journal of Physical Chemistry Letters 11, no. 6 (2020): 1989–97. http://dx.doi.org/10.1021/acs.jpclett.9b03347.

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30

Lund-Hansen, Lars Chresten, Ian Hawes, Morten Holtegaard Nielsen, and Brian K. Sorrell. "Is colonization of sea ice by diatoms facilitated by increased surface roughness in growing ice crystals?" Polar Biology 40, no. 3 (2016): 593–602. http://dx.doi.org/10.1007/s00300-016-1981-3.

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31

Ladan, John, and Stephen W. Morris. "Experiments on the dynamic wetting of growing icicles." New Journal of Physics 23, no. 12 (2021): 123017. http://dx.doi.org/10.1088/1367-2630/ac3cf4.

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Abstract The distinctive shape of an icicle is the outcome of a highly non-equilibrium process involving heat and mass transport in the presence of fluid flowing over an evolving topography. It has previously been shown that the ripple patterns with a near universal wavelength that are observed on many icicles are correlated with small levels of impurities in the feed water. Models of icicle shape evolution, and of the origin of the ripple pattern, require a detailed understanding of how liquid water flows over a growing icicle. The impurity effect is not accounted for by any existing model of

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32

Keizer, Joel, Peter Mazur, and Terumitsu Morita. "Theory for the anomalous light scattering in growing ice crystals." Physical Review A 32, no. 5 (1985): 2944–62. http://dx.doi.org/10.1103/physreva.32.2944.

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33

Avila, Eldo E., Guillermo G. Aguirre Varela, and Giorgio M. Caranti. "Temperature Dependence of Static Charging in Ice Growing by Riming." Journal of the Atmospheric Sciences 52, no. 24 (1995): 4515–22. http://dx.doi.org/10.1175/1520-0469(1995)052<4515:tdosci>2.0.co;2.

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34

Petrich, Chris, Jonas Karlsson, and Hajo Eicken. "Porosity of growing sea ice and potential for oil entrainment." Cold Regions Science and Technology 87 (March 2013): 27–32. http://dx.doi.org/10.1016/j.coldregions.2012.12.002.

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35

Ng, Felix, Bernard Hallet, Ronald S. Sletten, and John O. Stone. "Fast-growing till over ancient ice in Beacon Valley, Antarctica." Geology 33, no. 2 (2005): 121. http://dx.doi.org/10.1130/g21064.1.

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36

Zwally, H. J., A. C. Brenner, J. A. Major, R. A. Bindschadler, and J. G. Marsh. "In Reply: Greenland Ice Sheet: Is It Growing or Shrinking?" Science 248, no. 4953 (1990): 288–89. http://dx.doi.org/10.1126/science.248.4953.288-a.

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37

FRIES, E., W. HAUNOLD, W. JAESCHKE, I. HOOG, S. MITRA, and S. BORRMANN. "Uptake of gaseous aromatic hydrocarbons by non-growing ice crystals." Atmospheric Environment 40, no. 28 (2006): 5476–85. http://dx.doi.org/10.1016/j.atmosenv.2006.03.055.

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38

Thornton, Daniel C. O., Sarah D. Brooks, Elise K. Wilbourn, et al. "Production of ice-nucleating particles (INPs) by fast-growing phytoplankton." Atmospheric Chemistry and Physics 23, no. 19 (2023): 12707–29. http://dx.doi.org/10.5194/acp-23-12707-2023.

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Abstract. Sea spray aerosol contains ice-nucleating particles (INPs), which affect the formation and properties of clouds. Here, we show that aerosols emitted from fast-growing marine phytoplankton produce effective immersion INPs, which nucleate at temperatures significantly warmer than the atmospheric homogeneous freezing (−38.0 ∘C) of pure water. Aerosol sampled over phytoplankton cultures grown in a Marine Aerosol Reference Tank (MART) induced nucleation and freezing at temperatures as high as −15.0 ∘C during exponential phytoplankton growth. This was observed in monospecific cultures repr

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39

Sim, Franklin H., William T. Simonet, L. Joseph Melton, and Tracy A. Lehn. "Ice Hockey Injuries." American Journal of Sports Medicine 16, no. 1_suppl (1988): S—86—S—96. http://dx.doi.org/10.1177/03635465880160s119.

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Ice hockey is a team sport that has recently grown in popularity not only in the United States but also in Canada and Europe. With this increase in popularity has come a growing concern about the number and severity of injuries. The world literature on the biomechanics and physiology of ice hockey was reviewed in an attempt to evaluate the forces and mechanisms involved in the game. The influence of rule and equipment changes on injury patterns was particularly studied. Several studies on the epidemiology of injuries, providing data on the types of injuries and the mechanisms of those injuries

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40

Mitchell, Robyn, Laura Mataseje, David Boyd, et al. "A Growing Concern: The Emergence and Dissemination of Carbapenemase-producing Enterobacterales (CPE) in Canada." Infection Control & Hospital Epidemiology 41, S1 (2020): s454. http://dx.doi.org/10.1017/ice.2020.1126.

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Background: Carbapenemase-producing Enterobacterales (CPE) have rapidly become a global health concern and are associated with substantial morbidity and mortality due to limited treatment options. Travel to endemic areas, especially healthcare exposure in these areas, is an important risk factor for acquisition. We describe the evolving epidemiology, molecular features, and outcomes of CPE in Canada through surveillance by the Canadian Nosocomial Infection Surveillance Program (CNISP). Methods: CNISP has conducted surveillance for CPE among inpatients and outpatients of all ages since 2010. Pa

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41

Ghantous, Eihab, and Jamil A. Aboulhosn. "The Growing Role of Intracardiac Echo in Congenital Heart Disease Interventions." Journal of Clinical Medicine 14, no. 7 (2025): 2414. https://doi.org/10.3390/jcm14072414.

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Advancements in congenital heart disease (CHD) care have significantly improved survival, leading to a growing population of adults with congenital heart disease (ACHDs). Many of these patients require ongoing interventions for residual defects, conduit or valve dysfunction, and arrhythmia management, often performed using transcatheter techniques. Imaging plays a critical role in ensuring procedural success and safety. Intracardiac echocardiography (ICE) has emerged as an essential imaging modality in ACHD interventions. With continuous technological advancements, ICE offers several advantage

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42

Günther, Sven, and Gerhard S. Dieckmann. "Vertical zonation and community transition of sea-ice diatoms in fast ice and platelet layer, Weddell Sea, Antarctica." Annals of Glaciology 33 (2001): 287–96. http://dx.doi.org/10.3189/172756401781818590.

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AbstractChanges in the taxonomic composition of diatoms in fast ice as well as in the underlying platelet layer were followed from June to December 1995 in Atka Bay Antarctica. Four communities were clearly distinguished: (1) an interior community dominated by flagellates in spring; (2) a bottom community dominated by a small form of Fragilariopsis cylindrus; (3) a platelet-ice layer dominated by Amphiprora Kufferathii and Thalassionema sp. growing attached to the ice platelets; and (4) an interstitial community dominated by Chaetoceros neglectus growing in the water between the platelets. Spe

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43

Watanabe, Kunio, and Masaru Mizoguchi. "Ice configuration near a growing ice lens in a freezing porous medium consisting of micro glass particles." Journal of Crystal Growth 213, no. 1-2 (2000): 135–40. http://dx.doi.org/10.1016/s0022-0248(00)00353-5.

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44

Bassett, Christopher, Andone C. Lavery, and Ted Maksym. "Laboratory measurements of high-frequency, broadband acoustic scattering of growing sea ice and oil beneath sea ice." Journal of the Acoustical Society of America 135, no. 4 (2014): 2302. http://dx.doi.org/10.1121/1.4877579.

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45

Young, S., D. Hall, S. Sharma, and J. Anderson. "Abstract No. 505 Growing ice: evaluation of change in ice ball size during the second freeze cycle." Journal of Vascular and Interventional Radiology 30, no. 3 (2019): S219. http://dx.doi.org/10.1016/j.jvir.2018.12.586.

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46

Kumaraswamy, Guruswamy, Bipul Biswas, and Chandan Kumar Choudhury. "Colloidal assembly by ice templating." Faraday Discussions 186 (2016): 61–76. http://dx.doi.org/10.1039/c5fd00125k.

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We investigate ice templating of aqueous dispersions of polymer coated colloids and crosslinkers, at particle concentrations far below that required to form percolated monoliths. Freezing the aqueous dispersions forces the particles into close proximity to form clusters, that are held together as the polymer chains coating the particles are crosslinked. We observe that, with an increase in the particle concentration from about 10<sup>6</sup> to 10<sup>8</sup> particles per ml, there is a transition from isolated single particles to increasingly larger clusters. In this concentration range, mos

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47

Wang, Shiqi, Yumeng Wu, Paiwei Zhang, Meiyuan Yang, Zhenying Zhang, and Hongli Wang. "Analysis of Unsteady Heat Transfer during Ice-Making Process for Ice Rink Buildings." Buildings 13, no. 2 (2023): 291. http://dx.doi.org/10.3390/buildings13020291.

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The ice-making process is an important factor that affects the ice quality and the energy consumption of ice rinks. An unsteady heat transfer model is established and validated for the ice-making process. The transient temperature variation and ice thickness growing characteristics during the ice-making process are analyzed. The freezing time of a water layer and the final temperature of the stabilized ice layer are quantified. The effects of ice rink structural parameters on the ice-making process are studied. The results show that the water temperature variations during the process go throug

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48

Smith, Earl. "Understanding Ice Cream." After Dinner Conversation 4, no. 3 (2023): 28–43. http://dx.doi.org/10.5840/adc20234324.

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What is the root cause of political polarization? In this philosophical short story, Professor Gault is having a rough day. His graduate-level class on the growing polarization in politics is just as heated and polarized as the subject they're discussing. He thinks his students are the bugs trapped in the web of rhetoric, instead of being the spider. In a daze after class, a strange woman strikes up a conversation with him and presents an alternate theory. Perhaps, she argues, the underlying foundation of our time is narcissism. Maybe politics is just fertile ground for those who want to feel

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49

Löfverström, Marcus, Johan Liakka, and Johan Kleman. "The North American Cordillera—An Impediment to Growing the Continent-Wide Laurentide Ice Sheet." Journal of Climate 28, no. 23 (2015): 9433–50. http://dx.doi.org/10.1175/jcli-d-15-0044.1.

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Abstract This study examines the evolution of a continental-scale ice sheet on a triangular representation of North America, with and without the influence of the Cordilleran region. Simulations are conducted using a comprehensive atmospheric general circulation model asynchronously coupled to a three-dimensional thermomechanical ice-sheet model. The atmospheric state is updated for every 2 × 106 km3 increase in ice volume, and the coupled model is integrated to steady state. In the first experiment a flat continent with no background topography is used. The ice sheet evolves fairly zonally sy

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50

Zwally, H. Jay, Anita C. Brenner, Judy A. Major, Robert A. Bindschadler, and James G. Marsh. "Response : Greenland Ice Sheet: Is It Growing or Shrinking?" Science 248, no. 4953 (1990): 288–89. http://dx.doi.org/10.1126/science.248.4953.288.b.

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