Relevant bibliographies by topics / Non polar Ice core

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Non polar Ice core'

Author: Grafiati
Published: 9 March 2023
Last updated: 31 July 2025

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Journal articles on the topic "Non polar Ice core"

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Song, Jing. "Ice Core Methane Analytical Techniques, Chronology and Concentration History Changes: A Review." Sustainability 15, no. 12 (2023): 9346. http://dx.doi.org/10.3390/su15129346.

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Ice cores are invaluable in paleoclimate research, offering unique insights into the evolution of the natural environment, human activities, and Earth’s climate system. Methane (CH4) is a crucial greenhouse gas, second only to CO2 in its contribution to global warming, and is one of the primary anthropogenic greenhouse gases. Understanding historical CH4 concentration changes is essential for predicting future trends and informing climate change mitigation strategies. By analyzing gas components trapped in ice core bubbles, we can directly examine the composition of ancient atmospheres. Howeve
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Legrand, Michel. "Ice–core records of atmospheric sulphur." Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences 352, no. 1350 (1997): 241–50. http://dx.doi.org/10.1098/rstb.1997.0019.

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Sulphate and methanesulphonate (MSA), the two major sulphur species trapped in polar ice, have been extensivelyh studied in Antarctic and Greenland ice cores spanning the last centuries, as well as the entire last climatic cycle. Data from the cores are used to investigate the past contribution of volcanic and biogenic emissions to the natural sulphur budget in high latitude regions of both Hemispheres. Sulphate concentrations in polar ice very often increased during one or two years after large volcanic eruptions. Sulphate records show that fossil fuel combustion has enhanced sulphate concent
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Shoji, Hitoshi, Atau Mitani, Kohji Horita, and Chester C. Langway. "Crystal growth rates in polar firn." Annals of Glaciology 18 (1993): 208–10. http://dx.doi.org/10.3189/s0260305500011526.

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Continuous crystal-size measurements made on the G6 Antarctic ice core (100m deep) show enhanced growth rates above a depth of 30 m (Zone 1) and in the interval between 70 and 80 m (Zone 2). Crystal growth in Zone 1 most probably takes place by a process of sublimation and condensation. The higher growth rate in Zone 2 is most probably related to the pore close-off transformation process in which a non-uniform strain field is created to form air bubbles by plastic deformation and “cannibalization” of individual ice crystals.
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Shoji, Hitoshi, Atau Mitani, Kohji Horita, and Chester C. Langway. "Crystal growth rates in polar firn." Annals of Glaciology 18 (1993): 208–10. http://dx.doi.org/10.1017/s0260305500011526.

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Continuous crystal-size measurements made on the G6 Antarctic ice core (100m deep) show enhanced growth rates above a depth of 30 m (Zone 1) and in the interval between 70 and 80 m (Zone 2). Crystal growth in Zone 1 most probably takes place by a process of sublimation and condensation. The higher growth rate in Zone 2 is most probably related to the pore close-off transformation process in which a non-uniform strain field is created to form air bubbles by plastic deformation and “cannibalization” of individual ice crystals.
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Tornow, Carmen, Ekkehard Kührt, Stefan Kupper, and Uwe Motschmann. "Interaction between gas and ice phase in the three periods of the solar nebula." Proceedings of the International Astronomical Union 5, S263 (2009): 50–54. http://dx.doi.org/10.1017/s1743921310001493.

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AbstractWe simulate the chemical processes in the three evolution periods of the solar nebula, which are (i) the quasi-stationary prestellar cloud core, (ii) the gravitationally collapsing protostellar core, and (iii) the evolving gas-dust disk. Our purpose is to identify chemical parameters which reflect special aspects of the interactions between the gas and ice phase in the different periods, e.g. isotopic or molecular ratios. In this study we derive the D/H and 15N/14N ratio of selected compounds as well as the CO2/H2O ratio to measure the fraction of non-polar to polar ice in the grain ma
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Kerch, Johanna, Anja Diez, Ilka Weikusat, and Olaf Eisen. "Deriving micro- to macro-scale seismic velocities from ice-core <i>c</i> axis orientations." Cryosphere 12, no. 5 (2018): 1715–34. http://dx.doi.org/10.5194/tc-12-1715-2018.

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Abstract. One of the great challenges in glaciology is the ability to estimate the bulk ice anisotropy in ice sheets and glaciers, which is needed to improve our understanding of ice-sheet dynamics. We investigate the effect of crystal anisotropy on seismic velocities in glacier ice and revisit the framework which is based on fabric eigenvalues to derive approximate seismic velocities by exploiting the assumed symmetry. In contrast to previous studies, we calculate the seismic velocities using the exact c axis angles describing the orientations of the crystal ensemble in an ice-core sample. We
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Weikusat, Ilka, Ernst-Jan N. Kuiper, Gill M. Pennock, Sepp Kipfstuhl, and Martyn R. Drury. "EBSD analysis of subgrain boundaries and dislocation slip systems in Antarctic and Greenland ice." Solid Earth 8, no. 5 (2017): 883–98. http://dx.doi.org/10.5194/se-8-883-2017.

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Abstract. Ice has a very high plastic anisotropy with easy dislocation glide on basal planes, while glide on non-basal planes is much harder. Basal glide involves dislocations with the Burgers vector b = 〈a〉, while glide on non-basal planes can involve dislocations with b = 〈a〉, b = [c], and b = 〈c + a〉. During the natural ductile flow of polar ice sheets, most of the deformation is expected to occur by basal slip accommodated by other processes, including non-basal slip and grain boundary processes. However, the importance of different accommodating processes is controversial. The recent appl
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NG, Felix, and T. H. Jacka. "A model of crystal-size evolution in polar ice masses." Journal of Glaciology 60, no. 221 (2014): 463–77. http://dx.doi.org/10.3189/2014jog13j173.

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AbstractIn the deep ice cores drilled at the GRIP, NGRIP and GISP2 sites in Greenland and at Byrd Station and the summit of Law Dome in Antarctica, the mean crystal size increases with depth in the shallow subsurface and reaches steady values at intermediate depth. This behaviour has been attributed to the competition between grain-boundary migration driven crystal growth and crystal polygonization, but the effects of changing crystal dislocation density and non-equiaxed crystal shape in this competition are uncertain. We study these effects with a simple model. It describes how the mean heigh
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Shen, Liang, Yongqin Liu, Tandong Yao, et al. "Dyadobacter tibetensis sp. nov., isolated from glacial ice core." International Journal of Systematic and Evolutionary Microbiology 63, Pt_10 (2013): 3636–39. http://dx.doi.org/10.1099/ijs.0.050328-0.

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A Gram-stain-negative, rod-shaped, aerobic, non-motile bacterium, designated Y620-1T, was isolated from a glacier on the Tibetan Plateau, China. The 16S rRNA gene sequence of the novel isolate shared 93.6–95.1 % similarity with type strains of species of the genus Dyadobacter . The major fatty acids of strain Y620-1T were summed feature 3 (C16 : 1ω7c and/or iso-C15 : 0 2-OH), iso-C15 : 0, C16 : 1ω5c and iso-C17 : 0 3-OH. The predominant isoprenoid quinone and polar lipid were MK-7 and phosphatidylethanolamine (PE), respectively. The DNA G+C content was 44.4±0.3 mol% (T m). Flexirubin-type pigm
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Elsässer, C., D. Wagenbach, I. Levin, et al. "Simulating ice core <sup>10</sup>Be on the glacial–interglacial timescale." Climate of the Past 11, no. 2 (2015): 115–33. http://dx.doi.org/10.5194/cp-11-115-2015.

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Abstract. 10Be ice core measurements are an important tool for paleoclimate research, e.g., allowing for the reconstruction of past solar activity or changes in the geomagnetic dipole field. However, especially on multi-millennial timescales, the share of production and climate-induced variations of respective 10Be ice core records is still up for debate. Here we present the first quantitative climatological model of the 10Be ice concentration up to the glacial–interglacial timescale. The model approach is composed of (i) a coarse resolution global atmospheric transport model and (ii) a local
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Dissertations / Theses on the topic "Non polar Ice core"

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MATTAVELLI, MATTEO. "Development of a Glaciological Spatial Data Infrastructure to assess glacier response to climatic fluctuation." Doctoral thesis, Università degli Studi di Milano-Bicocca, 2016. http://hdl.handle.net/10281/102679.

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L’obiettivo del progetto di ricerca è creare una metodologia per ricercare, archiviare e diffondere dati glaciologici partendo dallo sviluppo di una infrastruttura di dati spaziali (SDI) che possa essere utile allo studio dell’evoluzione glaciale in relazione ai cambiamenti climatici. Questa ricerca è parte del progetto di interesse nazionale NextData (www.nextdataproject.it). Nei primi due anni è stato sviluppato un geodatabase contenente dati riguardanti la caratterizzazione chimico-fisica di carote di ghiaccio. La prima versione del geodb presentava delle criticità che sono state superate c
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Su, Yixiang. "Analyses of Two Ice Class Rules : for The Design Process of a Container Ship." Thesis, KTH, Marina system, 2017. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-214992.

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During ice voyages, level ice and iceberg with huge inertia force can cause large deformation and even damage on the ship hull structure. Hence the hull structure for ice voyage requires higher strength than it for open water voyages. A container ship will be re-designed for ice voyages in the thesis. Generally, the ice strength is evaluated in ice class rules. IACS polar class and FSICR are adopted in this thesis. Ice class rules are based on experience and experiment data, but there has been no exact formula or parameters to described the ice properties so far. In other words, the results fr
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Huang, Po-yu, and 黃柏渝. "The photolysis difference between Polar and non-polar molecule in CH4-ice mixture." Thesis, 2010. http://ndltd.ncl.edu.tw/handle/64394727286788084750.

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碩士<br>國立中央大學<br>物理研究所<br>98<br>The astronomical observation in resent years shows that the main composition of those TNOs ice are H2O, CH4 and N2. We choose these species as the ice composition and compare their difference in reaction products after exposed to and altered by VUV photons. N2 : CH4 = 1 : 1, CH4 : H2O = 1 : 1 and N2 : CH4 : H2O = 1 : 1 : 1 mixtures were prepared in gas-phase before condensation on to a precooled (16K) substrate. We use the High Flux beamline at Synchrotron Radiation Research Cente as the VUV light source. New molecules produced during photolysis were identified
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Nedelcu, Aneta Florentina. "The microscopic dimension of paleoclimate in the EPICA-DML(Antarctica) deep ice core." Doctoral thesis, 2011. http://hdl.handle.net/11858/00-1735-0000-000E-0CF1-C.

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Verpaelst, Manuel. "Mouvements de masse par solifluxion et dynamique syngénétique du pergélisol du Haut-Arctique." Thèse, 2016. http://hdl.handle.net/1866/18727.

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Le Haut-Arctique est caractérisé par de nombreux phénomènes climatiques et géomorphologiques extrêmes. Les températures très froides, les faibles précipitations et la couverture végétale disparate permettent une pénétration en profondeur du froid dans le sol. Ceci, combiné à un grand nombre de cycles de gel et de dégel, donne naissance à différentes formes de surface qui affectent les dynamiques d’évolution du pergélisol et induisent une variabilité verticale et latérale de la distribution des teneurs en glace dans le sol. Ce mémoire porte sur l’influence d’un lobe de solifluxion de type roche
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Books on the topic "Non polar Ice core"

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International Symposium on the Dome Fuji Ice Core and Related Topics (2001 Tokyo, Japan). Global scale climate and environment study through polar deep ice cores: Proceedings of the International Symposium on the Dome Fuji Ice Core and Related Topics, 27-28 February 2001, Tokyo. National Institute of Polar Research, 2003.

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Sigurdsson, Haraldur. Sulfur mass loading of the atmosphere from volcanic eruptions: Calibration of the ice core record on basis of sulfate aerosol deposition in polar regions from the 1982 El Chichon eruption, NASA grant NAG51304. University of Rhode Island Graduate School of Oceanography, 1990.

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Paolo, Laj, and United States. National Aeronautics and Space Administration., eds. Sulfur mass loading of the atmosphere from volcanic eruptions: Calibration of the ice core record on basis of sulfate aerosol deposition in polar regions from the 1982 El Chichon eruption, NASA grant NAG51304. University of Rhode Island Graduate School of Oceanography, 1990.

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Government, U. S., and U. S. Army Corps of Engineers (USACE). Fifty Years of Soviet and Russian Drilling Activity in Polar and Non-Polar Ice: A Chronological History - Polar Research, Antarctica, Arctic, Glaciers, Thermal Drills, Deep Core Holes. Independently Published, 2017.

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The Ice: A Journey to Antarctica. Univ of Iowa Press, 1986.

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Stilwell, Jeffrey D., and John A. Long. Frozen in Time. CSIRO Publishing, 2011. http://dx.doi.org/10.1071/9780643104013.

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No other continent on Earth has undergone such radical environmental changes as Antarctica. In its transition from rich biodiversity to the barren, cold land of blizzards we see today, Antarctica provides a dramatic case study of how subtle changes in continental positioning can affect living communities, and how rapidly catastrophic changes can come about. Antarctica has gone from paradise to polar ice in just a few million years, a geological blink of an eye when we consider the real age of Earth.&#x0D; Frozen in Time presents a comprehensive overview of the fossil record of Antarctica frame
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Bloom, Lisa E. Climate Change and the New Polar Aesthetics. Duke University Press, 2022. http://dx.doi.org/10.1215/9781478018643.

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In Climate Change and the New Polar Aesthetics, Lisa E. Bloom considers the ways artists, filmmakers, and activists engaged with the Arctic and Antarctic to represent our current environmental crises and reconstruct public understandings of them. Bloom engages feminist, Black, Indigenous, and non-Western perspectives to address the exigencies of the experience of the Anthropocene and its attendant ecosystem failures, rising sea levels, and climate-led migrations. As opposed to mainstream media depictions of climate change that feature apocalyptic spectacles of distant melting ice and desperate
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Book chapters on the topic "Non polar Ice core"

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Wolff, Eric W. "Nitrate in Polar Ice." In Ice Core Studies of Global Biogeochemical Cycles. Springer Berlin Heidelberg, 1995. http://dx.doi.org/10.1007/978-3-642-51172-1_10.

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Beer, J., M. Andrée, H. Oeschger, et al. "10Be Variations in polar ice cores." In Greenland Ice Core: Geophysics, Geochemistry, and the Environment. American Geophysical Union, 1985. http://dx.doi.org/10.1029/gm033p0066.

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Legrand, Michel. "Sulphur-Derived Species in Polar Ice: A Review." In Ice Core Studies of Global Biogeochemical Cycles. Springer Berlin Heidelberg, 1995. http://dx.doi.org/10.1007/978-3-642-51172-1_5.

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Legrand, M. "Ice Core Analysis in Arctic and Antarctic Regions." In The Tropospheric Chemistry of Ozone in the Polar Regions. Springer Berlin Heidelberg, 1993. http://dx.doi.org/10.1007/978-3-642-78211-4_14.

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Neftel, Albrecht, Roger C. Bales, and Daniel J. Jacob. "H2O2 and HCHO in Polar Snow and Their Relation to Atmospheric Chemistry." In Ice Core Studies of Global Biogeochemical Cycles. Springer Berlin Heidelberg, 1995. http://dx.doi.org/10.1007/978-3-642-51172-1_14.

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Patterson, C. C., C. Boutron, and R. Flegal. "Present status and future of lead studies in polar snow." In Greenland Ice Core: Geophysics, Geochemistry, and the Environment. American Geophysical Union, 1985. http://dx.doi.org/10.1029/gm033p0101.

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Waddington, E. D. "Where are We Going? The Ice Core — Paleoclimate Inverse Problem." In Chemical Exchange Between the Atmosphere and Polar Snow. Springer Berlin Heidelberg, 1996. http://dx.doi.org/10.1007/978-3-642-61171-1_34.

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De Angelis, Martine, and Michel Legrand. "Preliminary Investigations of Post Depositional Effects on HCl, HNO3, and Organic Acids in Polar Firn Layers." In Ice Core Studies of Global Biogeochemical Cycles. Springer Berlin Heidelberg, 1995. http://dx.doi.org/10.1007/978-3-642-51172-1_19.

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Koide, Minoru, and Edward D. Goldberg. "The historical record of artificial radioactive fallout from the atmosphere in polar glaciers." In Greenland Ice Core: Geophysics, Geochemistry, and the Environment. American Geophysical Union, 1985. http://dx.doi.org/10.1029/gm033p0095.

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Talalay, Pavel G. "Geological and Scientific Offshore Drilling and Core Sampling in Ice-Covered Waters." In Geotechnical and Exploration Drilling in the Polar Regions. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-07269-7_11.

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Conference papers on the topic "Non polar Ice core"

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Kvamme, Bjarte O., Jino Peechanatt, and Ove T. Gudmestad. "Calculation of Time-to-Freeze for Liquids in Pipes." In ASME 2017 36th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2017. http://dx.doi.org/10.1115/omae2017-62000.

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In recent years, there has been unprecedented interest shown in the Arctic region by the industry, as it has become increasingly accessible for oil and gas exploration, shipping, and tourism. The decrease in ice extent in the Arctic has renewed the interest in the Northern Sea route, necessitating further research to evaluate the adequacy of the equipment and appliances used on vessels traversing in polar waters. In the oil and gas industry, exploration and production vessels and platforms are highly dependent on the piping facilities for rendering their intended function, and therefore, flow
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Yonebayashi, Hideharu, Takeshi Hiraiwa, Tatsuya Yamada, et al. "Diethyl Ketone Based Waterflood in Carbonate Reservoirs-Boosting Fluid-Fuid Interaction and Oil Recovery." In ADIPEC. SPE, 2024. http://dx.doi.org/10.2118/221983-ms.

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Abstract Water-based enhanced oil recovery (EOR) has become more important in oil fields which have applied water injection because of lowering additional investment with use of existing facilities, minimizing carbon footprint, and keeping profit of sales gas by excluding a use for gas-based EOR purpose. Thus, several EOR options such as low salinity water (LSW), polymer, and hybrid methods have been studied in Middle East carbonates. This paper focuses on a new water-based option using dialkyl ketones as more polar solvents which have larger dipole moment compared with common ones such as dim
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Yonebayashi, Hideharu, Takeshi Hiraiwa, Tatsuya Yamada, et al. "Structural Characterization of Functional Molecules Involved in Micro-Dispersion Formation for Low Salinity Waterflood in Carbonate Reservoirs." In International Petroleum Technology Conference. IPTC, 2025. https://doi.org/10.2523/iptc-24942-ms.

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Abstract The academia and industry have paid attention to low salinity water (LSW) enhanced oil recovery (EOR) in carbonate reservoirs with a variety of proposed mechanisms. Our research has focused on fluid-fluid interaction (FFI) during static contact between oil and LSW, forming a water micro-dispersion (MD) phase at the oil/LSW interface as a potential driver of the mechanism in LSW EOR. In the study, LSW-reactive oil forming more MD is defined as positive oil, while LSW-non-reactive oil is defined as negative oil. We elucidated the functional components in positive crude oil which showed
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Gosse, Joshua, Bruce Quinton, Claude Daley, Andrew Kendrick, and James Bond. "Using Non-Linear Finite Element Analysis to Analyze the Effects of Connection Designs on the Ice Strength of a Vessel." In ASME 2023 42nd International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2023. http://dx.doi.org/10.1115/omae2023-104860.

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Abstract As global temperatures rise, ice clears in the Arctic Ocean and the demand for Canadian Coast Guard presence in the Canadian Arctic increases. The Canadian government intends to acquire two new heavy icebreakers as part of the “Polar Icebreaker Project”. These icebreakers are to be built to IACS Polar Class 2 standards. Some classification societies require fully welded collars to support stiffener penetrations through deeper hull structure in the ice-strengthened region of the ship. This, however, is a labour-intensive, material-heavy, and thus costly way to manufacture these vessels
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Liu, An, Zhigang Shan, Ting Shi, and Weida Ni. "Numerical Simulation Research About the Influence of Nozzle Parameters on the Quality of Ice-Core in Hot-Water Ice-Drilling." In ASME 2022 41st International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2022. http://dx.doi.org/10.1115/omae2022-80173.

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Abstract Ice sheets in the Arctic contain well-ordered accumulations of ancient ice that fell as snow years to millions of years ago. Ice-core data have become central to our understanding of climate change in the past, and to assessments of possible future climate change. Hot-water ice-coring drills are often used to recover ice-core samples from a desirable depth in conjunction with a full-scaled hot-water drilling systems. However, the recovered cores had the varying quality. In hot-water ice-coring drilling, many small nozzles are used to spray water out and melt out a cylindrical ice. Par
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Luping, Liu, Li Xin, Wu Xiao, and Wu Bo. "Ice Model Tests for Semi-Submersible Platforms in Pack Ice Conditions." In ASME 2019 38th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2019. http://dx.doi.org/10.1115/omae2019-95786.

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Abstract As development of the Arctic grows in intensity, semi-submersible platforms are one of promising type of offshore structures used for arctic oil exploitation. Generally a good ice management is equipped by a moored floating platform to reduce ice loads to manageable levels, thus the most common scenario for a polar operating semi-submersible platform is pack ice conditions. The resistance test of a 4-columns structure is performed in a normal towing tank in China using synthetic non-refrigerated material with similar density to model sea ice. Three component load cells on top of each
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Lande Andrade, Sthefano, Ahmed Elruby, Dan Oldford, and Bruce Quinton. "Assessing Polar Class Ship Overload and Ice Impact on Low-ice Class Vessels using a “Quasi Real Time” Popov/Daley Approach." In SNAME Maritime Convention. SNAME, 2022. http://dx.doi.org/10.5957/smc-2022-108.

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The methodology presented in this work considers an impact’s available kinetic energy as balanced by the ice crushing energy as well as the structural deformation energy. The algorithm re-calculates the kinetic energy iteratively by subtracting the energy lost to structural deformation and ice crushing at specified time-intervals. The updated kinetic energy is then used to determine the current impact speed, which controls the indentation rate of ice on the structure. The result is a contactless ice load model which is intrinsically coupled to structural deformation. Accounting for structural
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Barz, Dominik P. J., Michael J. Vogel, and Paul H. Steen. "Generation of Electrokinetic Flow in a Doped Non-Polar Liquid." In ASME 2010 8th International Conference on Nanochannels, Microchannels, and Minichannels collocated with 3rd Joint US-European Fluids Engineering Summer Meeting. ASMEDC, 2010. http://dx.doi.org/10.1115/fedsm-icnmm2010-30258.

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The presence of considerable amounts of free charge dispersed in a liquid is the basis for electrokinetic phenomena which are related to the existence of an electrical double layer (EDL). In polar liquids, the dissociation of electrolytes into ionic species is well understood and numerous electrokinetic phenomena are known; a good overview is given by e.g. Delgado et al. [1]. In nonpolar liquids it is known that electrical charges can exist as well. The presence of these electrical charges is utilized, for example, in colloid science to stabilize particle suspensions [2]. For this purpose, sur
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Bryson, Edward, Bruce W. T. Quinton, and Claude Daley. "Probable Ice Impact Locations and Magnitudes on a Naval Hull Form in Forward Transit Through Marginal Ice Zones." In ASME 2023 42nd International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2023. http://dx.doi.org/10.1115/omae2023-104854.

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Abstract Operational capability assessment of ships in the Arctic have traditionally focused on icebreaking hull forms. The classification of these capabilities resulted in the development of the International Association of Classification Societies (IACS) Unified Requirements for Polar Ships, which requires the hull structure to withstand a predetermined glancing bow impact. The assumptions made when developing the Polar Class Rules, such as the collision with a thick and semi-infinite multiyear ice floe, slow speeds, and a glancing bow impact on an icebreaking bow shape, are not always valid
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Pilkington, Roger, Arno Keinonen, and Igor Sheikin. "Ice Observations and Forecasting During the Arctic Coring Project, August - September 2004." In SNAME 7th International Conference and Exhibition on Performance of Ships and Structures in Ice. SNAME, 2006. http://dx.doi.org/10.5957/icetech-2006-171.

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The Arctic Coring Expedition or ACEX was conducted as a special project under the Integrated Ocean Drilling Project. A review of the operational and ice management aspects of this project is provided in Keinonen et al (2006). This current paper reviews the ice observations and forecasting in more detail. Six scientists and naval architects were on board the IB Oden and Sovetskiy Soyuz to collect relevant ice data and forecast ice movement. The work involved the collection of ice data during transit and ice management, interpreting satellite imagery, ice forecasting, and providing the informati
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Reports on the topic "Non polar Ice core"

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Ueda, Herbert T., and Pavel G. Talalay. Fifty Years of Soviet and Russian Drilling Activity in Polar and Non-Polar Ice: A Chronological History. Defense Technical Information Center, 2007. http://dx.doi.org/10.21236/ada472548.

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Elbaum, Michael, and Peter J. Christie. Type IV Secretion System of Agrobacterium tumefaciens: Components and Structures. United States Department of Agriculture, 2013. http://dx.doi.org/10.32747/2013.7699848.bard.

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Objectives: The overall goal of the project was to build an ultrastructural model of the Agrobacterium tumefaciens type IV secretion system (T4SS) based on electron microscopy, genetics, and immunolocalization of its components. There were four original aims: Aim 1: Define the contributions of contact-dependent and -independent plant signals to formation of novel morphological changes at the A. tumefaciens polar membrane. Aim 2: Genetic basis for morphological changes at the A. tumefaciens polar membrane. Aim 3: Immuno-localization of VirB proteins Aim 4: Structural definition of the substrate
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Perrels, Adriaan, and Kaisa Juhanko. Socio-economic Benefits of the EPS Sterna constellation at high latitudes. Finnish Meteorological Institute, 2023. http://dx.doi.org/10.35614/isbn.9789523361836.

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This report presents a combined meteorological and economic study commissioned by EUMETSAT as part of the planning trajectory for the EPS-Sterna polar-orbiting satellite constellation. The focus of the study is on the foreseeable effects of EPS Sterna on meteorological forecasts and the resulting socioeconomic benefits, particularly regarding application at high latitudes, with emphasis on the Nordic countries. The study has an explorative character, hence the quantified estimates of benefits only indicate orders of magnitude for selected sectors. A more comprehensive assessment of expected be
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