Livros: "Fox Glacier"

1

Grapes, R. H. X.R.F. analyses of quartzo-feldspathic schists and metacherts, Franz Josef-Fox Glacier area, Southern Alps of New Zealand. [Wellington]: Victoria University of Wellington, 1985.

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2

Montana. Dept. of Labor and Industry. Office of Research and Analysis. Labor market information for Glacier County. Helena, MT: Office of Research & Analysis, Job Service Division, Montana Dept. of Labor & Industry, 1996.

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3

Fountain, Andrew G. A strategy for monitoring glaciers. [Washington]: U.S. G.P.O., 1997.

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4

Waitt, Richard B. Volcanic-hazard zonation for Glacier Peak Volcano, Washington. [Menlo Park, Calif.]: Dept. of the Interior, Geological Survey, 1995.

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5

Waitt, Richard B. Volcanic-hazard zonation for Glacier Peak Volcano, Washington. [Menlo Park, Calif.]: Dept. of the Interior, Geological Survey, 1995.

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6

Waitt, Richard B. Volcanic-hazard zonation for Glacier Peak Volcano, Washington. [Menlo Park, Calif.]: Dept. of the Interior, Geological Survey, 1995.

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7

Waitt, Richard B. Volcanic-hazard zonation for Glacier Peak Volcano, Washington. [Menlo Park, Calif.]: Dept. of the Interior, Geological Survey, 1995.

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8

Waitt, Richard B. Volcanic-hazard zonation for Glacier Peak Volcano, Washington. [Menlo Park, Calif.]: Dept. of the Interior, Geological Survey, 1995.

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9

Waitt, Richard B. Volcanic-hazard zonation for Glacier Peak Volcano, Washington. [Menlo Park, Calif.]: Dept. of the Interior, Geological Survey, 1995.

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10

Waitt, Richard B. Volcanic-hazard zonation for Glacier Peak Volcano, Washington. [Menlo Park, Calif.]: Dept. of the Interior, Geological Survey, 1995.

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11

Pellikka, Petri K. E. Remote sensing of glaciers: Techniques for topographic, spatial, and thematic mapping of glaciers. Boco Raton, FL: CRC Press, 2010.

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12

Pellikka, Petri K. E. Remote sensing of glaciers: Techniques for topographic, spatial, and thematic mapping of glaciers. Boco Raton, FL: CRC Press, 2010.

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13

Bergeron, Alain M. Crème glacée, limonade sucrée. Montréal]: Hurtubise HMH, 2007.

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14

Fitzpatrick, Joan J. EPOCH 2002 user's guide for ultrasonic velocity measurements in glacier ice. [Denver, CO]: U.S. Dept. of the Interior, U.S. Geological Survey, 1992.

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15

M, Brugman, Canada. Department of the Environment., Norwegian Water Resources and Energy Administration. e National Hydrological Research Institute (Canada), eds. Glacier mass-balance measurements: A manual for field and office work. Ottawa: Ministry of Supply and Services Canada, 1991.

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16

Barsch, Dietrich. Rockglaciers: Indicators for the present and former geoecology in high mountain environments. Berlin: Springer, 1996.

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17

M, Krimmel Robert. Photogrammetric data set, 1957-2000, and bathymetric measurements for Columbia Glacier, Alaska. Tacoma, Wash: U.S. Geological Survey, 2001.

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18

Krimmel, Robert M. Photogrammetric data set, 1957-2000, and bathymetric measurements for Columbia Glacier, Alaska. Tacoma, Wash: U.S. Geological Survey, 2001.

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19

Passmore, Blake. Climb Glacier National Park: Illustrated from routes for beginning and intermediate climbers. Kalispell, Mont: Montana Outdoor Guidebooks, 2011.

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20

Finklin, Arnold I. A climatic handbook for Glacier National Park: With data for Waterton Lakes National Park. Ogden, UT: U.S. Dept. of Agriculture, Forest Service, Intermountain Research Station, 1986.

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21

Good, Sarah. Lower Duwamish Waterway source control action plan for Glacier Bay source control area. [Olympia, Wash.]: Washington State Dept. of Ecology, Toxics Cleanup Program, 2007.

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22

Glacier Park wildlife: A watcher's guide : includes listings for Waterton Lakes National Park. Minocqua, WI: NorthWord Press, 1993.

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23

Good, Sarah. Lower Duwamish Waterway source control action plan for Glacier Bay source control area. [Olympia, Wash.]: Washington State Dept. of Ecology, 2007.

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24

International Hydrological Programme. IHP VI. A manual for monitoring the mass balance of mountain glaciers. Paris: UNESCO, 2003.

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25

Geographic information systems for geoscientists: Modelling with GIS. Oxford: Pergamon, 1994.

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26

Lowe, Andrew Timothy. Estimation of visible and near-infrared reflectivity for Peyto Glacier Basin usinf satellite data. Ottawa: National Library of Canada, 1993.

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27

A, Staples Stephanie, e Adey Walter H, eds. Geomorphologic trends in a glaciated coastal bay: A model for the Maine Coast. City of Washington: Smithsonian Institution Press, 1985.

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28

Hendricks, P. Preliminary results of an inventory of Algal Cave, Glacier National Park, Montana, for aquatic cave invertebrates. Helena, Mont: Montana Natural Heritage Program, 2000.

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29

McIntosh, Charles Barron. Intuitive pattern & formative process [in the] hypothesis for Sandhillian glaciation. Lincoln, Neb: Augstums Printing Service, 2004.

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30

Rossbacher, Lisa A. Periglacial and glacial analogs for Martian landforms: Final technical report. [Washington, DC: National Aeronautics and Space Administration, 1992.

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31

Cortequisse, Bruno. La galerie des glaces: De Louis XIV à nos jours. [Paris]: Perrin, 1998.

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32

Favey, Etienne. Investigation and improvement of Airborne Laser Scanning technique for monitoring surface elevation changes of glaciers. Zurich: Institut für Geodäsie und Photogrammetrie, Eidgenossische Technische Hochschule Zürich, 2001.

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33

Favey, Etienne. Investigation and improvement of Airborne Laser Scanning technique for monitoring surface elevation changes of glaciers. Zurich: Institut für Geodäsie und Photogrammetrie, Eidgenossische Technische Hochschule Zürich, 2001.

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34

Jennings, Sharon. Franklin joue au hockey sur glace. [Paris]: Deux coqs d'or, 2004.

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35

United States. Federal Highway Administration. Region 8. Environmental assessment for F 1-2(59)182, Goatlick Slide (Glacier Naional Park) (P.M.S. C#1958) in Flathead County. Helena, Mont: The Bureau [and] Region 8, Montana Division, Federal Highway Administration, 1993.

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36

Ford, Arthur B. Magnetic susceptibility and density determinations for plutonic and metamorphic rocks of the Glacier Peak Wilderness and vicinity, northern Cascades, Washington. [Denver, Colo.?]: Dept. of the Interior, U.S. Geological Survey, 1988.

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37

Meures, Thomas. Development of a Sub-glacial Radio Telescope for the Detection of GZK Neutrinos. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-18756-3.

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38

Tushingham, A. Mark. A global model of late Pleistocene deglaciation: Implications for earth structure and sea level change. Ottawa: National Library of Canada, 1990.

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39

Taillant, Jorge Daniel. Glaciers. Oxford University Press, 2015. http://dx.doi.org/10.1093/oso/9780199367252.001.0001.

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Though not traditionally thought of as strategic natural resources, glaciers are a crucial part of our global ecosystem playing a fundamental role in the sustaining of life around the world. Comprising three quarters of the world's freshwater, they freeze in the winter and melt in the summer, supplying a steady flow of water for agriculture, livestock, industry and human consumption. The white of glacier surfaces reflect sunrays which otherwise warm our planet. Without them, many of the planet's rivers would run dry shortly after the winter snow-melt. A single mid-sized glacier in high mountain environments of places like California, Argentina, India, Kyrgyzstan, or Chile can provide an entire community with a sustained flow of drinking water for generations. On the other hand, when global temperatures rise, not only does glacier ice wither away into the oceans and cease to act as water reservoirs, but these massive ice bodies can become highly unstable and collapse into downstream environments, resulting in severe natural events like glacier tsunamis and other deadly environmental catastrophes. But despite their critical role in environmental sustainability, glaciers often exist well outside our environmental consciousness, and they are mostly unprotected from atmospheric impacts of global warming or from soot deriving from transportation emissions, or from certain types of industrial activity such as mining, which has been shown to have devastating consequences for glacier survival. Glaciers: The Politics of Ice is a scientific, cultural, and political examination of the cryosphere -- the earth's ice -- and the environmental policies that are slowly emerging to protect it. Jorge Daniel Taillant discusses the debates and negotiations behind the passage of the world's first glacier-protection law in the mid-2000s, and reveals the tension that quickly arose between industry, politicians, and environmentalists when an international mining company proposed dynamiting three glaciers to get at gold deposits underneath. The book is a quest to educate general society about the basic science behind glaciers, outlines current and future risks to their preservation, and reveals the intriguing politics behind glacier melting debates over policies and laws to protect the resource. Taillant also makes suggestions on what can be done to preserve these crucial sources of fresh water, from both a scientific and policymaking standpoint. Glaciers is a new window into one of the earth's most crucial and yet most ignored natural resources, and a call to reawaken our interest in the world's changing climate.

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40

Hastenrath, Stefan. Changes in African Glaciers since the 19th Century. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.543.

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In equatorial East Africa, glaciers still exist on Mount Kenya, Kilimanjaro, and Ruwenzori. The decreasing ice extent has been documented by field reports since the end of the 19th century and a series of mappings. For Mount Kenya, the mappings are of 1947, 1963, 1987, 1993, and 2004, with more detailed mappings of Lewis Glacier in 1934, 1958, 1963, 1974, 1978, 1982, 1985, 1986, 1990, and 1993. For Kilimanjaro, the sequence is 1912, 1953, 1976, 1989, and 2000. For Ruwenzori (for which information is more scarce), the information is from 1906, 1955, and 1990. Photographs are valuable complementary evidence. At Lewis Glacier on Mount Kenya, measurements of mass budget and ice flow have been conducted over decades. The climatic forcing of ice recession in East Africa at the onset in the 1880s was radiationally controlled, affecting the most exposed locations. Later warming caused further ice shrinkage, except on the summit plateau of Kilimanjaro, above the freezing level. Whereas the ice recession in the Ecuadorian Andes and New Guinea began in the middle of the 19th century, plausibly caused by warming, the late onset in East Africa should be appreciated in the context of large-scale circulation changes evidenced by the historical ship observations in the equatorial Indian Ocean.

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41

All Aboard for Glacier: The Great Northern Railway and Glacier National Park. Farcountry Press, 2004.

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42

Glacier National Park: Statement for management. [Denver, Colo.?: Rocky Mountain Region, National Park Service, U.S. Dept. of Interior, 1988.

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43

Jacobsen, Dean, e Olivier Dangles. The waterscape at high altitudes. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198736868.003.0002.

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Chapter 2 presents the amazing variety of running waters, lakes, ponds, and wetlands found at high altitudes. These waterbodies are not equally distributed among the world’s high altitude places, but tend to be concentrated in certain areas, primarily determined by regional climate and topography. Thus, a large proportion of the world’s truly high altitude aquatic systems are found at lower latitudes, mostly in the tropics. The chapter presents general patterns in the geographical distribution of high altitude waters, and gives examples of some of the most extreme systems. High altitude aquatic systems and habitats cover a broad variety in dynamics and physical appearance. These differences may be related to, for example, water source (glacier-fed, rain-fed, or groundwater-fed streams), geological origin (e.g. glacial, volcanic, or tectonic lakes), or catchment slope and altitude (different types of peatland wetlands). This is exemplified and richly illustrated through numerous photos.

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44

Volcanic-hazard zonation for Glacier Peak Volcano, Washington. [Menlo Park, Calif.]: Dept. of the Interior, Geological Survey, 1995.

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45

Volcanic-hazard zonation for Glacier Peak Volcano, Washington. [Menlo Park, Calif.]: Dept. of the Interior, Geological Survey, 1995.

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46

G, Mastin Larry, Beget James E e Geological Survey (U.S.), eds. Volcanic-hazard zonation for Glacier Peak Volcano, Washington. [Menlo Park, Calif.]: Dept. of the Interior, Geological Survey, 1995.

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47

Arthur, Jean. Glacier National Park: Must-do hikes for everyone. 2014.

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48

Vuorinen, Ilppo. Post-Glacial Baltic Sea Ecosystems. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.675.

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Post-glacial aquatic ecosystems in Eurasia and North America, such as the Baltic Sea, evolved in the freshwater, brackish, and marine environments that fringed the melting glaciers. Warming of the climate initiated sea level and land rise and subsequent changes in aquatic ecosystems. Seminal ideas on ancient developing ecosystems were based on findings in Swedish large lakes of species that had arrived there from adjacent glacial freshwater or marine environments and established populations which have survived up to the present day. An ecosystem of the first freshwater stage, the Baltic Ice Lake initially consisted of ice-associated biota. Subsequent aquatic environments, the Yoldia Sea, the Ancylus Lake, the Litorina Sea, and the Mya Sea, are all named after mollusc trace fossils. These often convey information on the geologic period in question and indicate some physical and chemical characteristics of their environment. The ecosystems of various Baltic Sea stages are regulated primarily by temperature and freshwater runoff (which affects directly and indirectly both salinity and nutrient concentrations). Key ecological environmental factors, such as temperature, salinity, and nutrient levels, not only change seasonally but are also subject to long-term changes (due to astronomical factors) and shorter disturbances, for example, a warm period that essentially formed the Yoldia Sea, and more recently the “Little Ice Age” (which terminated the Viking settlement in Iceland).There is no direct way to study the post-Holocene Baltic Sea stages, but findings in geological samples of ecological keystone species (which may form a physical environment for other species to dwell in and/or largely determine the function of an ecosystem) can indicate ancient large-scale ecosystem features and changes. Such changes have included, for example, development of an initially turbid glacial meltwater to clearer water with increasing primary production (enhanced also by warmer temperatures), eventually leading to self-shading and other consequences of anthropogenic eutrophication (nutrient-rich conditions). Furthermore, the development in the last century from oligotrophic (nutrient-poor) to eutrophic conditions also included shifts between the grazing chain (which include large predators, e.g., piscivorous fish, mammals, and birds at the top of the food chain) and the microbial loop (filtering top predators such as jellyfish). Another large-scale change has been a succession from low (freshwater glacier lake) biodiversity to increased (brackish and marine) biodiversity. The present-day Baltic Sea ecosystem is a direct descendant of the more marine Litorina Sea, which marks the beginning of the transition from a primeval ecosystem to one regulated by humans. The recent Baltic Sea is characterized by high concentrations of pollutants and nutrients, a shift from perennial to annual macrophytes (and more rapid nutrient cycling), and an increasing rate of invasion by non-native species. Thus, an increasing pace of anthropogenic ecological change has been a prominent trend in the Baltic Sea ecosystem since the Ancylus Lake.Future development is in the first place dependent on regional factors, such as salinity, which is regulated by sea and land level changes and the climate, and runoff, which controls both salinity and the leaching of nutrients to the sea. However, uncertainties abound, for example the future development of the Gulf Stream and its associated westerly winds, which support the sub-boreal ecosystems, both terrestrial and aquatic, in the Baltic Sea area. Thus, extensive sophisticated, cross-disciplinary modeling is needed to foresee whether the Baltic Sea will develop toward a freshwater or marine ecosystem, set in a sub-boreal, boreal, or arctic climate.

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49

Rees, W. Gareth, e Petri Pellikka. Remote Sensing of Glaciers: Techniques for Topographic, Spatial and Thematic Mapping of Glaciers. Taylor & Francis Group, 2009.

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50

E, Pellikka Petri K., e Rees Gareth 1959-, eds. Remote sensing of glaciers: Techniques for topographic, spatial, and thematic mapping of glaciers. Boco Raton, FL: CRC Press, 2010.

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Livros sobre o tema "Fox Glacier"

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