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Journal articles on the topic 'Glaciology'

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1

Peterson, Beth. "Glaciology." River Teeth: A Journal of Nonfiction Narrative 15, no. 1 (2013): 73–85. http://dx.doi.org/10.1353/rvt.2013.0021.

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2

Mair, Douglas. "Glaciology." Progress in Physical Geography: Earth and Environment 36, no. 6 (2012): 813–32. http://dx.doi.org/10.1177/0309133312460265.

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3

Hambrey, Michael J. "Glaciology." Earth-Science Reviews 30, no. 3-4 (1991): 326–27. http://dx.doi.org/10.1016/0012-8252(91)90006-2.

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4

Fukazawa, Hiroshi. "Space Glaciology." hamon 18, no. 2 (2008): 97–102. http://dx.doi.org/10.5611/hamon.18.97.

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5

Rea, Brice R., Alastair M. D. Gemmell, and Matteo Spagnolo. "Glaciology in Aberdeen." Scottish Geographical Journal 135, no. 3-4 (2019): 236–56. http://dx.doi.org/10.1080/14702541.2019.1695891.

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6

Alam, Brishty, Valerie Deifel, Chloë Lalonde, and Lindsey Nicholson. "APPRENTICESHIP TO GLACIOLOGY." Landing, no. 1 (February 21, 2025): 77–101. https://doi.org/10.37522/pfa8nt20.

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The first resonance of Issue 1 closes with a photo essay by the collective of artists and scientists Brishty Alam, Valerie Deifel, Chloë Lalonde, and Lindsey Nicholson. They report on their attempt to dwell in the Suldenferner glacier in Austria through various interventions; some poetic, some scientific, some in between glossaries. Instead of representing this living glacier, they critically examine their own impact on the land.
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7

Anonymous. "Polar glaciology proposals sought." Eos, Transactions American Geophysical Union 69, no. 21 (1988): 612. http://dx.doi.org/10.1029/eo069i021p00612-02.

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8

Warman, Timothy. "Elsevier's dictionary of glaciology." Palaeogeography, Palaeoclimatology, Palaeoecology 100, no. 3 (1993): 333. http://dx.doi.org/10.1016/0031-0182(93)90062-n.

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9

Sharp, Martin. "Glaciology news in brief." Environmental Earth Sciences 71, no. 6 (2014): 2973–78. http://dx.doi.org/10.1007/s12665-014-3045-8.

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10

Cameron, Richard L. "The foundations of Antarctic glaciology." Archives of Natural History 32, no. 2 (2005): 231–44. http://dx.doi.org/10.3366/anh.2005.32.2.231.

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Heroic treks inland by Scott, Shackleton, and Amundsen in the early 1900s demonstrated the immensity of the Antarctic ice cover. But it has taken a century to estimate its volume and elucidate its intricate dynamics. Three significant milestones in the development of Antarctic glaciology have been: the memoir Glaciology by Charles Wright and Raymond Priestly arising from the Terra Nova expedition (1910–1913); the Norwegian-British-Swedish Expedition (1949–1952); the International Geophysical Year (1957–1958). Robert Scott thought glaciology so important he appointed a physicist as glaciologist
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11

WATANABE, Okitsugu. "Recent activities in Arctic glaciology." Journal of the Japanese Society of Snow and Ice 59, no. 2 (1997): 111–14. http://dx.doi.org/10.5331/seppyo.59.111.

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12

HONDO, TAKEO. "X-ray diffraction in glaciology." Journal of the Japanese Society of Snow and Ice 51, no. 3 (1989): 184–94. http://dx.doi.org/10.5331/seppyo.51.184.

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13

Ackert Jr., R. P. "GLACIOLOGY: An Ice Sheet Remembers." Science 299, no. 5603 (2003): 57–58. http://dx.doi.org/10.1126/science.1079568.

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14

Savage, Neil. "Glaciology: Climatology on thin ice." Nature 520, no. 7547 (2015): 395–97. http://dx.doi.org/10.1038/nj7547-395a.

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15

REES, W. G., and V. A. SQUIRE. "Technological limitations to satellite glaciology." International Journal of Remote Sensing 10, no. 1 (1989): 7–22. http://dx.doi.org/10.1080/01431168908903844.

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16

Hulbe, C. L. "GLACIOLOGY: How Ice Sheets Flow." Science 294, no. 5550 (2001): 2300–2301. http://dx.doi.org/10.1126/science.1066730.

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17

Moore, John C. "Glaciology and Global Climate Change." Engineering 4, no. 1 (2018): 6–8. http://dx.doi.org/10.1016/j.eng.2018.01.001.

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18

Weertman, J. "Impact of the International Glaciological Society on the development of glaciology and its future role." Journal of Glaciology 33, S1 (1987): 86–90. http://dx.doi.org/10.3189/s0022143000215864.

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AbstractAfter the end of World War II glaciology entered a new golden age, which has yet to end. The quality of this golden age is comparable to the classic period of the nineteenth century. The International Glaciological Society has been the major catalyst, through its very active and co-operative international membership and its Journal of Glaciology in setting the modern major advances in the science of glacier and ice phenomena in motion and sustaining them.
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19

Hulbe, Christina L., Weili Wang, and Simon Ommanney. "Women in glaciology, a historical perspective." Journal of Glaciology 56, no. 200 (2010): 944–64. http://dx.doi.org/10.3189/002214311796406202.

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AbstractWomen’s history in glaciology extends as far back in time as the discipline itself, although their contributions to the scientific discourse have for all of that history been constrained by the sociopolitical contexts of the times. The firstJournal of Glaciologypaper authored by a woman appeared in 1948, within a year of the founding of theJournal, but it was not until the 1980s that women produced more than a few percent ofJournalandAnnals of Glaciologypapers. Here international perspectives on women’s participation in the sciences are presented in order to establish an economic and s
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20

Walford, M. "Radio-Glaciology: Exploration of temperate glaciers." Physics Bulletin 36, no. 3 (1985): 108–9. http://dx.doi.org/10.1088/0031-9112/36/3/015.

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21

Zwally, H. Jay. "Technology in the advancement of glaciology." Journal of Glaciology 33, S1 (1987): 66–77. http://dx.doi.org/10.3189/s0022143000215840.

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AbstractMany of the major advances in glaciology during the past 50 years have followed the development and application of new technology for viewing and measuring various characteristics of ice. Microscopes to study ice crystals, radars to probe the internal structure of large ice masses, mass spectrometers to analyze the atomic composition of ice cores, and satellite sensors to measure the global distribution of ice are some of the tools readily adapted by glaciologists. Today, new tools include microcomputers for automatic data logging, large-memory computers for data processing and numeric
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22

Boulton, G. S. "Geophysics: A paradigm shift in glaciology?" Nature 322, no. 6074 (1986): 18. http://dx.doi.org/10.1038/322018a0.

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23

Hammer, Claus. "Glaciology: Frozen news on hot events." Nature 322, no. 6082 (1986): 778. http://dx.doi.org/10.1038/322778a0.

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24

Raymond, C. F. "GLACIOLOGY: Ice Sheets on the Move." Science 298, no. 5601 (2002): 2147–48. http://dx.doi.org/10.1126/science.1079169.

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25

Díaz, J. I., and E. Schiavi. "A note on hysteresis in glaciology." Applied Mathematics Letters 13, no. 3 (2000): 125–29. http://dx.doi.org/10.1016/s0893-9659(99)00197-4.

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26

Bindschadler, Robert. "Symposium on remote sensing in glaciology." Photogrammetria 41, no. 4 (1987): 263–64. http://dx.doi.org/10.1016/0031-8663(87)90023-8.

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27

Pritchard, H. D., and R. G. Bingham. "Exploration glaciology: radar and Antarctic ice." Physics Education 42, no. 5 (2007): 442–56. http://dx.doi.org/10.1088/0031-9120/42/5/001.

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28

Gresswell, R. Kay. "The glaciology of the coniston basin." Geological Journal 3, no. 1 (2007): 83–96. http://dx.doi.org/10.1002/gj.3350030107.

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29

Kotlyakov, V. M., and L. P. Chernova. "Annotated bibliography of the Russian literature on glaciology for 2014." Ice and Snow 56, no. 2 (2016): 267–88. http://dx.doi.org/10.15356/2076-6734-2016-2-267-286.

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The proposed annual bibliography continues annotated lists of the Russian-language literature on glaciology that were regularly published in the past. It includes 271 references grouped into the following ten sections: 1) general issues of glaciology; 2) physics and chemistry of ice; 3) atmospheric ice; 4) snow cover; 5) avalanches and glacial mudflows; 6) sea ice; 7) river and lake ice; 8) icings and ground ice; 9) the glaciers and ice caps; 10) palaeoglaciology. In addition to the works of the current year, some works of earlier years are added, that, for various reasons, were not included i
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30

Alley, Richard B. "Reliability of ice-core science: historical insights." Journal of Glaciology 56, no. 200 (2010): 1095–103. http://dx.doi.org/10.3189/002214311796406130.

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AbstractIce cores are remarkably faithful recorders of past climate, providing multiply duplicated reconstructions with small and quantifiable uncertainties. Ice core reconstructions in general do not rely on assumed quantitative time-invariance of empirical calibrations between climate and sedimentary characteristics, but instead rely on assuming little more than the constancy of physical law over time. The history of some of the discoveries that allow these ice-core climatic reconstructions is instructive for students, citizens and policymakers. Much important ice-core science was published
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31

Carey, Mark, M. Jackson, Alessandro Antonello, and Jaclyn Rushing. "Glaciers, gender, and science." Progress in Human Geography 40, no. 6 (2016): 770–93. http://dx.doi.org/10.1177/0309132515623368.

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Glaciers are key icons of climate change and global environmental change. However, the relationships among gender, science, and glaciers – particularly related to epistemological questions about the production of glaciological knowledge – remain understudied. This paper thus proposes a feminist glaciology framework with four key components: 1) knowledge producers; (2) gendered science and knowledge; (3) systems of scientific domination; and (4) alternative representations of glaciers. Merging feminist postcolonial science studies and feminist political ecology, the feminist glaciology framewor
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32

Schroeder, Dustin M., Robert G. Bingham, Donald D. Blankenship, et al. "Five decades of radioglaciology." Annals of Glaciology 61, no. 81 (2020): 1–13. http://dx.doi.org/10.1017/aog.2020.11.

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AbstractRadar sounding is a powerful geophysical approach for characterizing the subsurface conditions of terrestrial and planetary ice masses at local to global scales. As a result, a wide array of orbital, airborne, ground-based, and in situ instruments, platforms and data analysis approaches for radioglaciology have been developed, applied or proposed. Terrestrially, airborne radar sounding has been used in glaciology to observe ice thickness, basal topography and englacial layers for five decades. More recently, radar sounding data have also been exploited to estimate the extent and config
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33

Zhao, Chuanxi, Shengyu Kang, Yihan Fan, et al. "Unmanned Aerial Vehicle Technology for Glaciology Research in the Third Pole." Drones 9, no. 4 (2025): 254. https://doi.org/10.3390/drones9040254.

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The Third Pole region contains vast glaciers, and changes in these glaciers profoundly affect the lives and development of billions of people. Therefore, accurate glacier monitoring in this region is of great scientific and practical significance. Unmanned Aerial Vehicles (UAVs) provide high-resolution observation capabilities and flexible deployment options, effectively overcoming certain limitations associated with traditional in situ and satellite remote sensing observations. Thus, UAV technology is increasingly gaining traction and application in the glaciology community. This review syste
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34

Glen, John W. "The Journal of Glaciology: its origin and early history." Journal of Glaciology 56, no. 200 (2010): 941–43. http://dx.doi.org/10.3189/002214311796406211.

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35

Bhardwaj, Anshuman, and Lydia Sam. "Editorial: Applications of Remote Sensing in Glaciology." Remote Sensing 14, no. 17 (2022): 4146. http://dx.doi.org/10.3390/rs14174146.

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Contemporary and significant spatiotemporal changes in glaciers are a result of rapidly evolving regional and global climate, and continuous monitoring is imperative for understanding the complexities of glacio–climatic interactions [...]
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36

Fox, A. J., and A. M. Nuttall. "Photogrammetry as A Research Tool for Glaciology." Photogrammetric Record 15, no. 89 (1997): 725–37. http://dx.doi.org/10.1111/0031-868x.00081.

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37

Colinge, Jacques, and Jacques Rappaz. "A strongly nonlinear problem arising in glaciology." ESAIM: Mathematical Modelling and Numerical Analysis 33, no. 2 (1999): 395–406. http://dx.doi.org/10.1051/m2an:1999122.

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38

Chow, Sum S., Graham F. Carey, and Michael L. Anderson. "Finite element approximations of a glaciology problem." ESAIM: Mathematical Modelling and Numerical Analysis 38, no. 5 (2004): 741–56. http://dx.doi.org/10.1051/m2an:2004033.

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39

Jennings, Stephen J. A., Michael J. Hambrey, Neil F. Glasser, Timothy D. James, and Bryn Hubbard. "Structural glaciology of Austre Brøggerbreen, northwest Svalbard." Journal of Maps 12, no. 5 (2015): 790–96. http://dx.doi.org/10.1080/17445647.2015.1076744.

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40

Jones, Christine, Jonathan Ryan, Tom Holt, and Alun Hubbard. "Structural glaciology of Isunguata Sermia, West Greenland." Journal of Maps 14, no. 2 (2018): 517–27. http://dx.doi.org/10.1080/17445647.2018.1507952.

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41

Yao, Tandong, and L. G. Thompson. "New achievements in glaciology in Tibet, China." Chinese Science Bulletin 43, no. 14 (1998): 1231–32. http://dx.doi.org/10.1007/bf02883232.

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42

Benediktsson, Ívar Örn, Helgi Björnsson, Guðrún Larsen, and Olgeir Sigmarsson. "Glaciology and volcanology on the centenary of Sigurður Þórarinsson's birth: a special issue." Jökull 62, no. 1 (2012): 1–2. http://dx.doi.org/10.33799/jokull2012.62.001o.

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The year 2012 marks the centenary of the birth of the late Sigurður Þórarinsson, the first professor of geology at the University of Iceland. His legacy is widely recognized in the international geoscientific community and the highest award of the International Association of Volcanology and Chemistry of the Earth’s Interior (IAVCEI), the Thorarinsson Medal, is awarded to scientists for outstanding contributions to volcanology. Sigurður’s influence on Icelandic geoscientists was immense both through his university teaching and scientific collaborations. Although his research spanned a broad ra
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43

Granzow, Glen D. "A tutorial on adjoint methods and their use for data assimilation in glaciology." Journal of Glaciology 60, no. 221 (2014): 440–46. http://dx.doi.org/10.3189/2014jog13j205.

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AbstractThis paper provides an introduction to adjoint methods, which are used to find the gradient of an objective function, as required by optimization algorithms. Examples are included, culminating in a data-assimilation problem from glaciology.
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44

Dowdeswell, Julian A., and Jonathan L. Bamber. "On the glaciology of Edgeøya and Barentsøya, Svalbard." Polar Research 14, no. 2 (1995): 105–22. http://dx.doi.org/10.3402/polar.v14i2.6658.

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45

Editorial, Article. "New scientific discovery in the field of glaciology." Ice and Snow 130, no. 2 (2015): 141. http://dx.doi.org/10.15356/2076-6734-2015-2-141.

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46

FUJITA, SHUJI. "An Introduction on the Polar Meteorology and Glaciology." Journal of the Institute of Electrical Engineers of Japan 124, no. 2 (2004): 92–93. http://dx.doi.org/10.1541/ieejjournal.124.92.

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47

Pidlisetska, I., H. Silveistrov, and O. Tomchenko. "Data processing technology of remote sensing in glaciology." Bulletin of Taras Shevchenko National University of Kyiv. Geography, no. 65 (2016): 52–57. http://dx.doi.org/10.17721/1728-2721.2016.65.11.

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This article shows the analysis of remote sensing methods for needs of glaciology and trends of modern research. Remote sensing not only accelerates the process of investigation of natural resources, but also provides fundamentally new information about the nature of the Earth, its components, phenomena and processes, which cannot be obtained by conventional methods. For most of glacial regions of the world scientists continue collecting information about the current condition of glaciers and changes that occur to them. However, often it is difficult to organize direct observation of some glac
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48

Krajick, K. "GLACIOLOGY: Tracking Icebergs for Clues to Climate Change." Science 292, no. 5525 (2001): 2244–45. http://dx.doi.org/10.1126/science.292.5525.2244.

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49

Kaiser, J. "GLACIOLOGY: Warmer Ocean Could Threaten Antarctic Ice Shelves." Science 302, no. 5646 (2003): 759a—759. http://dx.doi.org/10.1126/science.302.5646.759a.

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50

DREWRY, D. J., J. TURNER, and W. G. REES. "The contribution of Seasat to ice sheet glaciology." International Journal of Remote Sensing 12, no. 8 (1991): 1753–74. http://dx.doi.org/10.1080/01431169108955206.

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