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1

Gjermundsen, E. F., R. Mathieu, A. Kääb, T. Chinn, B. Fitzharris, and J. O. Hagen. "Assessment of multispectral glacier mapping methods and derivation of glacier area changes, 1978–2002, in the central Southern Alps, New Zealand, from ASTER satellite data, field survey and existing inventory data." Journal of Glaciology 57, no. 204 (2011): 667–83. http://dx.doi.org/10.3189/002214311797409749.

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AbstractWe have measured the glacier area changes in the central Southern Alps, New Zealand, between 1978 and 2002 and have compiled the 2002 glacier outlines using an image scene from the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER). Three automated classification methods were tested: (1) band ratio, (2) normalized-difference snow index and (3) supervised classification. The results were compared with the glacier outlines photo-interpreted from the ASTER data, and were further validated using GPS-aided field mapping of selected test glaciers. The ASTER 3/4 band ratio
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2

Appleby, John R., Martin S. Brook, Simon S. Vale, and Amanda M. Macdonald‐creevey. "Structural glaciology of a temperate maritime glacier: lower fox glacier, new zealand." Geografiska Annaler: Series A, Physical Geography 92, no. 4 (December 2010): 451–67. http://dx.doi.org/10.1111/j.1468-0459.2010.00407.x.

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3

Herman, Frédéric, Brian Anderson, and Sébastien Leprince. "Mountain glacier velocity variation during a retreat/advance cycle quantified using sub-pixel analysis of ASTER images." Journal of Glaciology 57, no. 202 (2011): 197–207. http://dx.doi.org/10.3189/002214311796405942.

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AbstractCoverage of ice velocities in the central part of the Southern Alps, New Zealand, is obtained from feature tracking using repeat optical imagery in 2002 and 2006. Precise orthorectification, co-registration and correlation is carried out using the freely available software COSI-Corr. This analysis, combined with short times between image acquisitions, has enabled velocities to be captured even in the accumulation areas, where velocities are lowest and surface features ephemeral. The results indicate large velocities for mountain glaciers (i.e. up to ∼5 m d−1) as well as dynamic changes
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4

Appleby, John R., Martin S. Brook, Travis W. Horton, Ian C. Fuller, Katherine A. Holt та Duncan J. Quincey. "Stable isotope (δD–δ18O) relationships of ice facies and glaciological structures within the mid-latitude maritime Fox Glacier, New Zealand". Annals of Glaciology 58, № 75pt2 (липень 2017): 155–65. http://dx.doi.org/10.1017/aog.2017.11.

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ABSTRACT Relationships between stable isotopes (δD–δ18O), ice facies and glacier structures have hitherto gone untested in the mid-latitude maritime glaciers of the Southern Hemisphere. Here, we present δD–δ18O values as part of a broader study of the structural glaciology of Fox Glacier, New Zealand. We analyzed 94 samples of δD–δ18O from a range of ice facies to investigate whether isotopes have potential for structural glaciological studies of a rapidly deforming glacier. The δD–δ18O measurements were aided by structural mapping and imagery from terminus time-lapse cameras. The current retr
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5

Purdie, H. L., M. S. Brook, and I. C. Fuller. "Seasonal Variation in Ablation and Surface Velocity on a Temperate Maritime Glacier: Fox Glacier, New Zealand." Arctic, Antarctic, and Alpine Research 40, no. 1 (February 2008): 140–47. http://dx.doi.org/10.1657/1523-0430(06-032)[purdie]2.0.co;2.

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6

Carrivick, Jonathan L., and E. Lucy Rushmer. "Inter- and Intra-Catchment Variations in Proglacial Geomorphology: An Example From Franz Josef Glacier and Fox Glacier, New Zealand." Arctic, Antarctic, and Alpine Research 41, no. 1 (February 2009): 18–36. http://dx.doi.org/10.1657/1523-0430-41.1.18.

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7

Carrivick, Jonathan L., and E. Lucy Rushmer. "Inter- and Intra-Catchment Variations in Proglacial Geomorphology: An Example From Franz Josef Glacier and Fox Glacier, New Zealand." Arctic, Antarctic, and Alpine Research 41, no. 1 (February 2009): 18–36. http://dx.doi.org/10.1657/1938-4246(07-099)[carrivick]2.0.co;2.

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8

Grapes, Rodney, and Teruo Watanabe. "Paragenesis of titanite in metagreywackes of the Franz Josef-Fox Glacier area, Southern Alps, New Zealand." European Journal of Mineralogy 4, no. 3 (June 11, 1992): 547–56. http://dx.doi.org/10.1127/ejm/4/3/0547.

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9

Brook, Martin S., and Sheryl Paine. "Ablation of ice‐cored moraine in a humid, maritime climate: fox glacier, new zealand." Geografiska Annaler: Series A, Physical Geography 94, no. 3 (September 2012): 339–49. http://dx.doi.org/10.1111/j.1468-0459.2011.00442.x.

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10

Nuth, C., and A. Kääb. "What's in an elevation difference? Accuracy and corrections of satellite elevation data sets for quantification of glacier changes." Cryosphere Discussions 4, no. 4 (October 13, 2010): 2013–77. http://dx.doi.org/10.5194/tcd-4-2013-2010.

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Abstract. There is an increasing number of DEMs available worldwide for deriving elevation differences over time, including vertical changes on glaciers. Most of these DEMs are heavily post-processed or merged, so that physical error modelling becomes impossible and statistical error modelling is required instead. We propose a three-step methodological framework for assessing and correcting DEMs to quantify glacier elevation changes: remove DEM shifts, check for elevation-dependent biases, and check for higher-order, sensor-specific biases. An analytic, simple and robust method to co-register
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11

Green, Susan, and Dr Michael Krop. "A Photographic Record of the Upper Headwater Tributaries, Basins and Riparia of the Snake River." UW National Parks Service Research Station Annual Reports 33 (January 1, 2011): 107–13. http://dx.doi.org/10.13001/uwnpsrc.2011.3797.

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Photographic surveys have been used since the early 1940’s to document coastlines, fuel supplies and river courses. The US Navy, post world war II, flew over the Arctic coast to document possible locations for oil extraction. These very same photos are now being utilized to compare changes in tundra vegetation at the same locations today. John Muirs’ photos of Glacier Bay are a startling testament to the melted glaciers no longer visible from the same vantage point in present times. Taking photographs to monitor change may not tell the entire story behind a change in landscape. However, ph
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Purdie, Heather L., Martin S. Brook, Ian C. Fuller, and John Appleby. "Seasonal variability in velocity and ablation of Te Moeka o Tuawe/Fox Glacier, south Westland, New Zealand." New Zealand Geographer 64, no. 1 (April 2008): 5–19. http://dx.doi.org/10.1111/j.1745-7939.2008.00123.x.

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13

McColl, Samuel T., and Ian C. Fuller. "Exploring the implications of advance and retreat of a New Zealand icon: Fox Glacier 2005-2015 and beyond." New Zealand Geographer 71, no. 2 (July 30, 2015): 110–12. http://dx.doi.org/10.1111/nzg.12085.

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14

GRAPES, R., and T. WATANABE. "Metamorphism and uplift of Alpine schist in the Franz Josef?Fox Glacier area of the Southern Alps, New Zealand." Journal of Metamorphic Geology 10, no. 2 (March 1992): 171–80. http://dx.doi.org/10.1111/j.1525-1314.1992.tb00077.x.

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15

Carrasco, Jorge F., Roberto Osorio, and Gino Casassa. "Secular trend of the equilibrium-line altitude on the western side of the southern Andes, derived from radiosonde and surface observations." Journal of Glaciology 54, no. 186 (2008): 538–50. http://dx.doi.org/10.3189/002214308785837002.

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AbstractThe altitude of the 0°C isotherm obtained from radiosonde data of the aerological Chilean stations Antofagasta, Quintero/Santo Domingo, Puerto Montt and Punta Arenas are analyzed, along with surface temperature and precipitation records from nearby stations. The strong effect of the 1976/77 climate shift due to a change in the Pacific Decadal Oscillation is evident in the temperature and precipitation data. The data are used as input for an empirical model which reconstructs annually the equilibrium-line altitude (ELA) for the last 49 years on the western side of the southern Andes. Th
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Stumm, Dorothea, Sharad Prasad Joshi, Tika Ram Gurung, and Gunjan Silwal. "Mass balances of Yala and Rikha Samba glaciers, Nepal, from 2000 to 2017." Earth System Science Data 13, no. 8 (August 6, 2021): 3791–818. http://dx.doi.org/10.5194/essd-13-3791-2021.

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Abstract. The glacier mass balance is an important variable to describe the climate system and is used for various applications like water resource management or runoff modelling. The direct or glaciological method and the geodetic method are the standard methods to quantify glacier mass changes, and both methods are an integral part of international glacier monitoring strategies. In 2011, we established two glacier mass-balance programmes on Yala and Rikha Samba glaciers in the Nepal Himalaya. Here we present the methods and data of the directly measured annual mass balances for the first six
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17

Brook, Martin S., and Sven Lukas. "A revised approach to discriminating sediment transport histories in glacigenic sediments in a temperate alpine environment: a case study from Fox Glacier, New Zealand." Earth Surface Processes and Landforms 37, no. 8 (May 20, 2012): 895–900. http://dx.doi.org/10.1002/esp.3250.

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18

Clark, Adam M., Daniel B. Fagre, Erich H. Peitzsch, Blase A. Reardon, and Joel T. Harper. "Glaciological measurements and mass balances from Sperry Glacier, Montana, USA, years 2005–2015." Earth System Science Data 9, no. 1 (January 23, 2017): 47–61. http://dx.doi.org/10.5194/essd-9-47-2017.

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Abstract. Glacier mass balance measurements help to provide an understanding of the behavior of glaciers and their response to local and regional climate. In 2005 the United States Geological Survey established a surface mass balance monitoring program on Sperry Glacier, Montana, USA. This project is the first quantitative study of mass changes of a glacier in the US northern Rocky Mountains and continues to the present. The following paper describes the methods used during the first 11 years of measurements and reports the associated results. From 2005 to 2015, Sperry Glacier had a cumulative
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19

Jiskoot, Hester, Dan Juhlin, Heather St Pierre, and Michele Citterio. "Tidewater glacier fluctuations in central East Greenland coastal and fjord regions (1980s–2005)." Annals of Glaciology 53, no. 60 (2012): 35–44. http://dx.doi.org/10.3189/2012aog60a030.

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AbstractSummer 2000/01 ASTER and Landsat 7 scenes and semi-automated digitization were used to compile a glacier inventory for local glaciers of the Geikie Plateau region, central East Greenland. Of the 332 glaciers (41 591 km2), 120 are tidewater-terminating and drain 90% of the glacierized area. Differencing the 2000/01 tidewater margins from the 1980s GEUS map database ice polygons (113 glaciers) and from 2004/05 ASTER tidewater margins (78 glaciers) shows a cumulative tidewater terminus width decrease from 196 km to 183 km between the 1980s and 2000s, with a corresponding areal loss of ~31
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20

Purdie, Heather, Brian Anderson, Trevor Chinn, Ian Owens, Andrew Mackintosh, and Wendy Lawson. "Franz Josef and Fox Glaciers, New Zealand: Historic length records." Global and Planetary Change 121 (October 2014): 41–52. http://dx.doi.org/10.1016/j.gloplacha.2014.06.008.

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21

Brook, Martin, Wilfried Hagg, and Stefan Winkler. "Contrasting medial moraine development at adjacent temperate, maritime glaciers: Fox and Franz Josef Glaciers, South Westland, New Zealand." Geomorphology 290 (August 2017): 58–68. http://dx.doi.org/10.1016/j.geomorph.2017.04.015.

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22

Berrittella, C., and J. van Huissteden. "Uncertainties in modelling CH<sub>4</sub> emissions from northern wetlands in glacial climates: the role of vegetation parameters." Climate of the Past 7, no. 4 (October 11, 2011): 1075–87. http://dx.doi.org/10.5194/cp-7-1075-2011.

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Abstract. Marine Isotope Stage 3 (MIS 3) interstadials are marked by a sharp increase in the atmospheric methane (CH4) concentration, as recorded in ice cores. Wetlands are assumed to be the major source of this CH4, although several other hypotheses have been advanced. Modelling of CH4 emissions is crucial to quantify CH4 sources for past climates. Vegetation effects are generally highly generalized in modelling past and present-day CH4 fluxes, but should not be neglected. Plants strongly affect the soil-atmosphere exchange of CH4 and the net primary production of the vegetation supplies orga
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23

Vallot, Dorothée, Sigit Adinugroho, Robin Strand, Penelope How, Rickard Pettersson, Douglas I. Benn, and Nicholas R. J. Hulton. "Automatic detection of calving events from time-lapse imagery at Tunabreen, Svalbard." Geoscientific Instrumentation, Methods and Data Systems 8, no. 1 (March 29, 2019): 113–27. http://dx.doi.org/10.5194/gi-8-113-2019.

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Abstract. Calving is an important process in glacier systems terminating in the ocean, and more observations are needed to improve our understanding of the undergoing processes and parameterize calving in larger-scale models. Time-lapse cameras are good tools for monitoring calving fronts of glaciers and they have been used widely where conditions are favourable. However, automatic image analysis to detect and calculate the size of calving events has not been developed so far. Here, we present a method that fills this gap using image analysis tools. First, the calving front is segmented. Secon
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24

Franzo, Giovanni, Maria Luisa Menandro, Claudia Maria Tucciarone, Giacomo Barbierato, Lorenzo Crovato, Alessandra Mondin, Martina Libanora, et al. "Canine Circovirus in Foxes from Northern Italy: Where Did It All Begin?" Pathogens 10, no. 8 (August 9, 2021): 1002. http://dx.doi.org/10.3390/pathogens10081002.

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Canine circovirus (CanineCV) is a recently identified virus affecting both domestic and wild carnivores, including foxes, sometimes in presence of severe clinical signs. Its circulation in wild animals can thus represent a potential threat for endangered species conservation and an infection source for dogs. Nevertheless, no data were available on its circulation in the Alps region of Northern Italy. In the present study, samples collected from 186 foxes in the period 2009–2020 from Valle d’Aosta and Veneto regions were tested using a real-time PCR assay, demonstrating a viral circulation of a
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25

Hanson, Carl R., Richard J. Norris, and Alan F. Cooper. "Regional fracture patterns east of the Alpine Fault between the Fox and Franz Josef Glaciers, Westland, New Zealand." New Zealand Journal of Geology and Geophysics 33, no. 4 (October 1990): 617–22. http://dx.doi.org/10.1080/00288306.1990.10421379.

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26

Leshchinskiy, S. V. "Results of latest paleontological, stratigraphic and geoarchaeological research of the Volchia Griva mammoth fauna site." Proceedings of the Zoological Institute RAS 322, no. 3 (September 26, 2018): 315–84. http://dx.doi.org/10.31610/trudyzin/2018.322.3.315.

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The Volchia Griva is the largest site in Asia where the mammoth fauna remains are buried in situ. It is located in the Baraba forest-steppe (Western Siberia). In the 20th century, remains of at least 70 mammoths, 5 horses, 3 bisons and 1 wolf, as well as 37 stone artifacts were found here. The latest excavations of 2015–2017 on ~30 m2 revealed over 1500 bones and teeth, 95% of which belong to mammoths (at least 14 individuals), and the rest are from horses (3), bison, wolf, red fox, arctic fox, and rodents; associated artifacts – 23 items. With an average thickness of the bonebearing lens ~ 0.
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27

Mankoff, Kenneth D., Anne Solgaard, William Colgan, Andreas P. Ahlstrøm, Shfaqat Abbas Khan, and Robert S. Fausto. "Greenland Ice Sheet solid ice discharge from 1986 through March 2020." Earth System Science Data 12, no. 2 (June 19, 2020): 1367–83. http://dx.doi.org/10.5194/essd-12-1367-2020.

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Abstract. We present a 1986 through March 2020 estimate of Greenland Ice Sheet ice discharge. Our data include all discharging ice that flows faster than 100 m yr−1 and are generated through an automatic and adaptable method, as opposed to conventional handpicked gates. We position gates near the present-year termini and estimate problematic bed topography (ice thickness) values where necessary. In addition to using annual time-varying ice thickness, our time series uses velocity maps that begin with sparse spatial and temporal coverage and end with near-complete spatial coverage and 12 d upda
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Fuentes‐Hurtado, Marcelo, Anouschka R. Hof, and Roland Jansson. "Paleodistribution modeling suggests glacial refugia in Scandinavia and out‐of‐Tibet range expansion of the Arctic fox." Ecology and Evolution 6, no. 1 (December 15, 2015): 170–80. http://dx.doi.org/10.1002/ece3.1859.

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29

Borden, W. Calvin, and Robert A. Krebs. "Phylogeography and postglacial dispersal of smallmouth bass (Micropterus dolomieu) into the Great Lakes." Canadian Journal of Fisheries and Aquatic Sciences 66, no. 12 (December 2009): 2142–56. http://dx.doi.org/10.1139/f09-155.

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Refugia and dispersal routes of smallmouth bass ( Micropterus dolomieu ) into the Great Lakes were identified using 427 mitochondrial sequences from across their native range. Overall, smallmouth bass accessed the Great Lakes via long-distance dispersal from multiple refugia, and the distribution of genetic variation reflected the consequences of vicariant, dispersal, and paleogeological events. Proximity of lakes to glacial outlets had a greater predictive power on the resulting distribution of mitochondrial diversity relative to interbasin migration. Populations in the Eastern and Interior H
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30

Saber, Abdullah A., Marco Cantonati, Morgan L. Vis, Andrea Anesi, and Graziano Guella. "Multifaceted characterization of a Lemanea fluviatilis population (Batrachospermales, Rhodophyta) from a glacial stream in the south-eastern Alps." Fottea 16, no. 2 (October 14, 2016): 234–43. http://dx.doi.org/10.5507/fot.2016.014.

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31

Telling, J., A. M. Anesio, J. Hawkings, M. Tranter, J. L. Wadham, A. J. Hodson, T. Irvine-Fynn, and M. L. Yallop. "Measuring rates of gross photosynthesis and net community production in cryoconite holes: a comparison of field methods." Annals of Glaciology 51, no. 56 (2010): 153–62. http://dx.doi.org/10.3189/172756411795932056.

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AbstractPhotosynthesis by microbes on the surfaces of glaciers and ice sheets has the potential to fix carbon, alter the albedo of ice surfaces via the production of organic matter and so enhance ice melt. It could also be important for supplying labile organic matter and nutrients to in situ and downstream ecosystems. This study compares in situ 24 hour incubation methods for measuring rates of gross photosynthesis, respiration and net community production (NCP) in cryoconite holes on three Svalbard valley glaciers. Rates of gross photosynthesis and respiration measured by the ΔCO2method were
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32

Liu, Shiwei, Cunde Xiao, Zhiheng Du, Augusto Marcelli, Giannantonio Cibin, Giovanni Baccolo, Yingcai Zhu, Alessandro Puri, Valter Maggi, and Wei Xu. "Iron Speciation in Insoluble Dust from High-Latitude Snow: An X-ray Absorption Spectroscopy Study." Condensed Matter 3, no. 4 (December 10, 2018): 47. http://dx.doi.org/10.3390/condmat3040047.

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Iron is thought to limit the biomass of phytoplankton populations in extensive regions of the ocean, which are referred to as high-nutrient low-chlorophyll (HNLC) regions. Iron speciation in soils is still poorly understood. We have investigated inorganic and organic standard substances, diluted mixtures of common Fe minerals in insoluble dust in snow from the Laohugou No.12 glacier, and sand (including soil and moraine) samples that were collected from western China. The speciation of iron (Fe) in insoluble dust and sand was determined by X-ray absorption near-edge structure (XANES) spectrosc
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33

Idalino, Filipe Daros, Cleiva Perondi, Kátia Kellem da Rosa, and Jefferson Cardia Simões. "Uso de Imgens Sentinel–2 para Análises de Retração de Geleiras: Comparativo Entre Ambientes nas Latitudes 44ºS e 62ºS." Revista Brasileira de Geografia Física 11, no. 3 (2018): 1101–11. http://dx.doi.org/10.26848/rbgf.v10.6.p1101-1111.

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Idalino, Filipe Daros, Cleiva Perondi, Kátia Kellem da Rosa, and Jefferson Cardia Simões. "Uso de Imgens Sentinel–2 para Análises de Retração de Geleiras: Comparativo Entre Ambientes nas Latitudes 44ºS e 62ºS." Revista Brasileira de Geografia Física 11, no. 3 (2018): 1101–11. http://dx.doi.org/10.26848/rbgf.v11.3.p1101-1111.

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35

Šnábel, Viliam, Tamás Sréter, Bruno Gottstein, Jakub Gawor, Thomas Romig, and Martina Miterpáková. "GENETIC DIVERSITY OF ECHINOCOCCUS MULTILOCULARIS CESTODES IN EUROPE AS DETERMINED BY MITOCHONDRIAL AND NUCLEAR SEQUENCES." THEORY AND PRACTICE OF PARASITIC DISEASE CONTROL, no. 20 (May 14, 2019): 754–58. http://dx.doi.org/10.31016/978-5-9902340-8-6.2019.20.754-758.

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Alveolar echinococcosis caused by metacestode stage of the tapeworm Echinococcus multilocularis is considered as one of the most pathogenic zoonoses in temperate and arctic regions. To more thoroughly ascertain genetic diversity in E. multilocularis tapeworms from Europe and to indicate transmission patterns of parasite, 25 isolates from a contiguous territory of eight European countries were subjected to sequencing of mitochondrial and nuclear DNA. A total of 2 715 nucleotide sequences in nad1, cox1, rrnS, atp6 and actII genes were screened in the current study. Whereas in 24 isolates profile
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36

Jiskoot, Hester, Theo Harvey, and Tyrell R. Nielsen. "MODIS-Derived Arctic Melt Season Fog and Low Stratus over East Greenland Glaciers and the Ice Sheet." Canadian Journal of Remote Sensing 45, no. 3-4 (July 4, 2019): 386–404. http://dx.doi.org/10.1080/07038992.2019.1635878.

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37

Blower, Brooke L. "The Life of Mary Anderson: An Intimate Response to the Turn-of-the-Century World of Transatlantic Migration." Prospects 29 (October 2005): 185–217. http://dx.doi.org/10.1017/s0361233300001733.

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On the green slopes of Slieve Martin in County Down where the Mourne Mountains reach Carlingford Lough rests a forty-ton glacial rock called Cloughmore. According to Irish folklore, the giant Fionn M'Comhal hurled the enormous boulder at Benandonner, his Caledonian foe from Scotland, and many believe that ancient Druids chose the site for their rituals. Rain obscures the view from the stone's side some two hundred days of the year, but on a clear day, a stunning vista from Cloughmore emerges: streams trickling down to the shores of the deep Irish Sea and, amidst woods running uphill, the small
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Brückner, Helmut, Gerhard Schellmann, and Klaas van der Borg. "Uplifted Beach Ridges in Northern Spitsbergen as Indicators for Glacio-Isostasy and Palaeo-Oceanography." Zeitschrift für Geomorphologie 46, no. 3 (September 20, 2002): 309–36. http://dx.doi.org/10.1127/zfg/46/2002/309.

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39

Demay, L., P. M. Vasyliev, L. V. Koulakovska, D. V. Stupak, P. S. Shydlovskyi, and V. I. Belyaeva. "PALAEOLITHIC HUMAN SOCIETIES DURING THE UPPER PLENIGLACIAL THROUGHT THEIR RELATIONS WITH OTHER ANIMALS IN UKRAINIAN ARCHAEOLOGICAL SITES." Archaeology and Early History of Ukraine 37, no. 4 (December 23, 2020): 82–93. http://dx.doi.org/10.37445/adiu.2020.04.06.

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The first part of the Upper Pleniglacial (around 26000—20000 BP) is characterized by a deterioration in weather conditions, which reached its peak during the Last Glacial Maximum. In the East European Plain, most of its lands were dominated by a periglacial steppe-tundra with the maximum extension of ice sheet in the North and permafrost. The different animal species had to adapt to these environments, also as human groups.The recent works realized in Ukraine permit to better understand the lifestyles of the Palaeolithic human groups, particularly their subsistence activities, the modalities o
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40

Marshall, H. Dawn, Barbara L. Langille, Crystal A. Hann, and Hugh G. Whitney. "Patterns of MHC-DRB1 polymorphism in a post-glacial island canid, the Newfoundland red fox (Vulpes vulpes deletrix), suggest balancing selection at species and population timescales." Immunogenetics 68, no. 5 (February 19, 2016): 381–89. http://dx.doi.org/10.1007/s00251-016-0907-0.

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41

Vosshall, Leslie B. "The Glacial Pace of Scientific Publishing: Why It Hurts Everyone and What We Can Do To Fix It." FASEB Journal 26, no. 9 (September 2012): 3589–93. http://dx.doi.org/10.1096/fj.12-0901ufm.

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42

Giorgetti, G., F. S. Aghib, K. J. T. Livi, A. C. Gaillot, and T. J. Wilson. "Newly formed phyllosilicates in rock matrices and fractures from CRP-3 core (Antarctica): an electron microscopy study." Clay Minerals 42, no. 1 (March 2007): 21–43. http://dx.doi.org/10.1180/claymin.2007.042.1.03.

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AbstractA scanning and transmission electron microscopy study has been performed on Oligocene glacio-marine sediments, Devonian sandstones, and Jurassic dolerites recovered during CRP-3 drilling in the Ross Sea (Antarctica). Newly formed clay minerals occur in the rock matrices and as fillings in veins and faults which crosscut the whole sequence. Authigenic clays in sediments consist of beidellite-montmorillonite, berthierine/chlorite intergrowths and illite. Al,K-rich smectites and kaolinite occur in the Devonian sandstones. Saponite, berthierine/chlorite intergrowths, and Fe-hydroxides deve
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43

Graham, D. F., and D. R. Grant. "A test of airborne, side-looking synthetic-aperture radar in central Newfoundland for geological reconnaissance." Canadian Journal of Earth Sciences 28, no. 2 (February 1, 1991): 257–65. http://dx.doi.org/10.1139/e91-025.

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Side-looking, C-band synthetic-aperture radar (SAR) penetrates cloud and fog, and operates day or night, to produce pseudo-three-dimensional terrain images with enhanced topography and surface roughness. The images, which have a 20 m resolution and cover large areas, have been used to map the regional trends, patterns of lineaments, and terrain types over a 6200 km2 area of complex lithology, structure, and drift cover. Four lineament classes are differentiated. Glacial trends are clear, and bedrock structures (faults, fractures, joints, foliation, and folded bedding) with relief expression at
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44

Schultz, David M., Jonathan G. Fairman, Stuart Anderson, and Sharon Gardner. "Build Your Own Earth: A Web-Based Tool for Exploring Climate Model Output in Teaching and Research." Bulletin of the American Meteorological Society 98, no. 8 (August 1, 2017): 1617–23. http://dx.doi.org/10.1175/bams-d-16-0121.1.

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Abstract Build Your Own Earth was designed as a web-based tool for the user to select various characteristics of a planet and see what the climate of that planet would be like. Because of the limitations of computer resources, presimulated Earths were run using the Fast Ocean Atmosphere Model at relatively coarse resolution. The tool provides 50 different Earth configurations in three categories: Recent, Ancient, and Alien Earths. Recent Earths fix the continental configuration at the present day and vary the axial tilt, eccentricity, and greenhouse gas concentrations. Ancient Earths include a
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45

McGrath, CDR Gabrielle G. "Preventing a Nationally-Significant Oil Spill on the Grand Banks of Newfoundland." International Oil Spill Conference Proceedings 2014, no. 1 (May 1, 2014): 1226–38. http://dx.doi.org/10.7901/2169-3358-2014.1.1226.

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ABSTRACT As the Arctic becomes more heavily populated and more open to commercial shipping operations, the threat of an oil spill increases. On the Grand Banks of Newfoundland, both fixed and mobile oil rigs drill for the region's highly lucrative natural oil resources. This region also happens to be one of the most dangerous shipping areas in the world. The cold Labrador Current travels south from the Arctic bringing with it icebergs calved from the glaciers along the Western Greenland coast. As these icebergs travel south, they intersect directly with the transatlantic shipping lanes followi
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Dublyansky, Y. V., and V. N. Shirokov. "Age of the Upper Paleolithic sites in Kapova and Ignatievskaya caves (Southern Ural): revision and interpretations of the radiocarbon dates." VESTNIK ARHEOLOGII, ANTROPOLOGII I ETNOGRAFII, no. 3 (50) (August 28, 2020): 5–16. http://dx.doi.org/10.20874/2071-0437-2020-50-3-1.

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There are two caves containing groups of wall paintings of the Upper Paleolithic age known in the Southern Ural: Kapova (Shulgan-Tash) and Ignatievskaya (Yamazy-Tash). In total, about 200 pictorial motifs have been recorded in the Kapova cave, among which there are life-like depictions of Pleistocene animals (mammoth and rhinoceros). Some 180 pictorial motifs have been found in the Ignatievskaya cave, which also show images of the Pleistocene fauna (mammoth and rhinoceros), although less realistic than those in the Kapova cave. The cultural layers have been discovered in the cave sediments at
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47

Splodytel, Anastasiia O., Liudmyla Yu Sorokina, and Oksana V. Lunova. "Landscape geochemical conditions and patterns of inter-element redistribution of heavy metals in landscapes of Kivertsi National Nature Park “Tsumanska Pushcha”." Journal of Geology, Geography and Geoecology 30, no. 1 (April 10, 2021): 165–78. http://dx.doi.org/10.15421/112115.

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&#x0D; &#x0D; &#x0D; nalysis of landscape geochemical conditions of the territory of Kivertsi National Nature Park “Tsumanska Pushcha” was carried out also the levels of pollution of landscapes within the park and adjacent territories were established. Features of the accumulation and distribution of pollutants in the landscapes of the territory under conditions of natural and Technogenic geochemical anomalies are considered. The landscapes of the studied migration classes (calcium, calcium carbonate, carbonate clayey, acidic calcium) are characterized by a relatively high coefficient of migra
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Singh, Ramesh, Sarvan Kumar, and Abhay Singh. "Elevated Black Carbon Concentrations and Atmospheric Pollution around Singrauli Coal-Fired Thermal Power Plants (India) Using Ground and Satellite Data." International Journal of Environmental Research and Public Health 15, no. 11 (November 5, 2018): 2472. http://dx.doi.org/10.3390/ijerph15112472.

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The tropospheric NO2 concentration from OMI AURA always shows high concentrations of NO2 at a few locations in India, one of the high concentrations of NO2 hotspots is associated with the locations of seven coal-fired Thermal Power plants (TPPs) in Singrauli. Emissions from TPPs are among the major sources of black carbon (BC) soot in the atmosphere. Knowledge of BC emissions from TPPs is important in characterizing regional carbonaceous particulate emissions, understanding the fog/haze/smog formation, evaluating regional climate forcing, modeling aerosol optical parameters and concentrations
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Farheen, Jabeen, and Simeen Mansoor. "Anti-stress phytohormones impact on proteome profile of green gram (Vigna radiata) under salt toxicity." World Journal of Biology and Biotechnology 5, no. 2 (April 30, 2020): 17. http://dx.doi.org/10.33865/wjb.005.02.0213.

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Green gram (Vigna radiata) is considered the chief legume in Pakistan. Thus, current study was conducted to examine the ameliorating effect of phytohormones pre-treatments under salt stress on proteome profile of green gram by sodium-dodecyl-sulphate-polyacrylamide gel electrophoresis (SDS-PAGE). The soluble green gram seedlings proteins were resolved on 4% stacking and 12% resolving gels. The SDS-PAGE resolved 24 polypeptide bands ranging from 200 to 17kDa. Among these, 12 out of 24 bands of proteins were essentials house-keeping or growth proteins of green grams. While, 120, 114.6, 51.8, 29.
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Purdie, Heather, Paul Bealing, Christopher Gomez, Brian Anderson, and Oliver J. Marsh. "Morphological changes to the terminus of a maritime glacier during advance and retreat phases: Fox Glacier/Te Moeka o Tuawe, New Zealand." Geografiska Annaler: Series A, Physical Geography, November 29, 2020, 1–19. http://dx.doi.org/10.1080/04353676.2020.1840179.

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