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Permafrost --- Eternally frozen ground --- Ever frozen ground --- Perennially frozen ground --- Pergelisol --- Permanently frozen ground --- Perpetually frozen ground --- Tjale --- Frozen ground
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Permafrost is a thermal condition -- its formation, persistence and disappearance are highly dependent on climate. General circulation models predict that, for a doubling of atmospheric concentrations of carbon dioxide, mean annual air temperatures may rise up to several degrees over much of the Arctic. In the discontinuous permafrost region, where ground temperatures are within 1-2 degrees of thawing, permafrost will likely ultimately disappear as a result of ground thermal changes associated with global climate warming. Where ground ice contents are high, permafrost degradation will have associated physical impacts. Permafrost thaw stands to have wide-ranging impacts, such as the draining and drying of the tundra, erosion of riverbanks and coastline, and destabilization of infrastructure (roads, airports, buildings, etc.), and including potential implications for ecosystems and the carbon cycle in the high latitudes."Opportunities to Use Remote Sensing in Understanding Permafrost and Related Ecological Characteristics" is the summary of a workshop convened by the National Research Council to explore opportunities for using remote sensing to advance our understanding of permafrost status and trends and the impacts of permafrost change, especially on ecosystems and the carbon cycle in the high latitudes. The workshop brought together experts from the remote sensing community with permafrost and ecosystem scientists. The workshop discussions articulated gaps in current understanding and potential opportunities to harness remote sensing techniques to better understand permafrost, permafrost change, and implications for ecosystems in permafrost areas. This report addresses questions such as how remote sensing might be used in innovative ways, how it might enhance our ability to document long-term trends, and whether it is possible to integrate remote sensing products with the ground-based observations and assimilate them into advanced Arctic system models. Additionally, the report considers the expectations of the quality and spatial and temporal resolution possible through such approaches, and the prototype sensors that are available that could be used for detailed ground calibration of permafrost/high latitude carbon cycle studies.
Permafrost --- Permafrost ecosystems. --- Biotic communities --- Eternally frozen ground --- Ever frozen ground --- Perennially frozen ground --- Pergelisol --- Permanently frozen ground --- Perpetually frozen ground --- Tjale --- Frozen ground --- Remote sensing.
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Permafrost. --- Glaciers. --- Cryosphere --- Ice --- Glaciology --- Meltwater --- Eternally frozen ground --- Ever frozen ground --- Perennially frozen ground --- Pergelisol --- Permanently frozen ground --- Perpetually frozen ground --- Tjale --- Frozen ground
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Russia (Federation) --- Siberia, Western (Russia) --- Russie --- Sibérie occidentale (Russie) --- History --- Histoire --- Sibérie occidentale (Russie) --- Permafrost --- Eternally frozen ground --- Ever frozen ground --- Perennially frozen ground --- Pergelisol --- Permanently frozen ground --- Perpetually frozen ground --- Tjale --- Frozen ground --- Siberie (russie) --- Descriptions et voyages
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Frozen ground --- -Frozen soil --- Cryosphere --- Soils --- Cryopedology --- Civil engineering --- Permafrost --- Eternally frozen ground --- Ever frozen ground --- Perennially frozen ground --- Pergelisol --- Permanently frozen ground --- Perpetually frozen ground --- Tjale --- Engineering --- Public works
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Drawing from a decade-long collaboration between Japan and Russia, this important volume presents the first major synthesis of current knowledge on the ecophysiology of the coniferous forests growing on permafrost at high latitudes. It presents ecological data for a region long inaccessible to most scientists, and raises important questions about the global carbon balance as these systems are affected by the changing climate. Making up around 20% of the entire boreal forests of the northern hemisphere, these ‘permafrost forest ecosystems’ are subject to particular constraints in terms of temperature, nutrient availability, and root space, creating exceptional ecosystem characteristics not known elsewhere. This authoritative text explores their diversity, structure, dynamics and physiology. It provides a comparison of these forests in relation to boreal forests elsewhere, and concludes with an assessment of the potential responses of this unique biome to climate change. The book will be invaluable to advanced students and researchers interested in boreal vegetation, forest ecology, silviculture and forest soils, as well as to researchers into climate change and the global carbon balance.
Larches --- Forest ecology --- Biotic communities --- Permafrost --- Forests and forestry --- Larch --- Larix --- Eternally frozen ground --- Ever frozen ground --- Perennially frozen ground --- Pergelisol --- Permanently frozen ground --- Perpetually frozen ground --- Tjale --- Biocenoses --- Biocoenoses --- Biogeoecology --- Biological communities --- Biomes --- Biotic community ecology --- Communities, Biotic --- Community ecology, Biotic --- Ecological communities --- Ecosystems --- Natural communities --- Ecology --- Life sciences. --- Ecology. --- Ecosystems. --- Plant ecology. --- Forestry. --- Soil science. --- Soil conservation. --- Life Sciences. --- Plant Ecology. --- Terrestial Ecology. --- Soil Science & Conservation. --- Frozen ground --- Population biology --- Pinaceae --- Forest ecosystems
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This book provides a cross-disciplinary overview of permafrost and the carbon cycle by providing an introduction into the geographical distribution of permafrost, with a focus on the distribution of permafrost and its soil carbon reservoirs. The chapters explain the basic physical properties and processes of permafrost soils: ice, mineral and organic components, and how these interact with climate, vegetation and geomorphological processes. In particular, the book covers the role of the large quantities of ice in many permafrost soils which are crucial to understanding carbon cycle processes. An explanation is given on how permafrost becomes loaded with ice and carbon. Gas hydrates are also introduced. Structures and processes formed by the intense freeze-thaw action in the active layer are considered (e.g. ice wedging, cryoturbation), and the processes that occur as the permafrost thaws, (pond and lake formation, erosion). The book introduces soil carbon accumulation and decomposition mechanisms and how these are modified in a permafrost environment. A separate chapter deals with deep permafrost carbon, gas reservoirs and recently discovered methane emission phenomena from regions such as Northwest Siberia and the Siberian yedoma permafrost.
Physical geography. --- Climate change. --- Atmospheric sciences. --- Landscape ecology. --- Earth System Sciences. --- Climate Change/Climate Change Impacts. --- Atmospheric Sciences. --- Landscape Ecology. --- Ecology --- Atmospheric sciences --- Earth sciences --- Atmosphere --- Changes, Climatic --- Changes in climate --- Climate change --- Climate change science --- Climate changes --- Climate variations --- Climatic change --- Climatic changes --- Climatic fluctuations --- Climatic variations --- Global climate changes --- Global climatic changes --- Climatology --- Climate change mitigation --- Teleconnections (Climatology) --- Geography --- Environmental aspects --- Permafrost. --- Eternally frozen ground --- Ever frozen ground --- Perennially frozen ground --- Pergelisol --- Permanently frozen ground --- Perpetually frozen ground --- Tjale --- Frozen ground --- Global environmental change
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Permafrost Hydrology systematically elucidates the roles of seasonally and perennially frozen ground on the distribution, storage and flow of water. Cold regions of the World are subject to mounting development which significantly affects the physical environment. Climate change, natural or human-induced, reinforces the impacts. Knowledge of surface and ground water processes operating in permafrost terrain is fundamental to planning, management and conservation. This book is an indispensable reference for libraries and researchers, an information source for practitioners, and a valuable text for training the next generations of cold region scientists and engineers.
Hydrology. --- Permafrost. --- Hydrology --- Permafrost --- Geography --- Earth & Environmental Sciences --- Physical Geography --- Eternally frozen ground --- Ever frozen ground --- Perennially frozen ground --- Pergelisol --- Permanently frozen ground --- Perpetually frozen ground --- Tjale --- Earth sciences. --- Hydrogeology. --- Physical geography. --- Climate change. --- Soil science. --- Soil conservation. --- Earth Sciences. --- Climate Change. --- Physical Geography. --- Soil Science & Conservation. --- Frozen ground --- Aquatic sciences --- Earth sciences --- Hydrography --- Water --- Hydraulic engineering. --- Climatic changes. --- Conservation of soil --- Erosion control, Soil --- Soil erosion --- Soil erosion control --- Soils --- Agricultural conservation --- Soil management --- Changes, Climatic --- Changes in climate --- Climate change --- Climate change science --- Climate changes --- Climate variations --- Climatic change --- Climatic changes --- Climatic fluctuations --- Climatic variations --- Global climate changes --- Global climatic changes --- Climatology --- Climate change mitigation --- Teleconnections (Climatology) --- Engineering, Hydraulic --- Engineering --- Fluid mechanics --- Hydraulics --- Shore protection --- Control --- Prevention --- Conservation --- Environmental aspects --- Pedology (Soil science) --- Agriculture --- Geohydrology --- Geology --- Groundwater --- Global environmental change
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Most of the Earth’s biosphere is characterized by low temperatures. Vast areas (>20%) of the soil ecosystem are permanently frozen or are unfrozen for only a few weeks in summer. Permafrost regions occur at high latitudes and also at high ele- tions; a significant part of the global permafrost area is represented by mountains. Permafrost soils are of global interest, since a significant increase in temperature is predicted for polar regions. Global warming will have a great impact on these soils, especially in northern regions, since they contain large amounts of organic carbon and act as carbon sinks, and a temperature increase will result in a release of carbon into the atmosphere. Additionally, the intensified release of the clima- relevant tracer gas methane represents a potential environmental harzard. Significant numbers of viable microorganisms, including bacteria, archaea, p- totrophic cyanobacteria and green algae, fungi and protozoa, are present in per- frost, and the characteristics of these microorganisms reflect the unique and extreme conditions of the permafrost environment. Remarkably, these microorg- isms have been reported to be metabolically active at subzero temperatures, even down to ?20°C.
Biodiversity. --- Climatic changes. --- Exobiology. --- Microbial ecology. --- Microbial genetics. --- Permafrost. --- Soil biology. --- Soil conservation. --- Soil microbiology. --- Earth & Environmental Sciences --- Biology --- Health & Biological Sciences --- Ecology --- Microbiology & Immunology --- Eternally frozen ground --- Ever frozen ground --- Perennially frozen ground --- Pergelisol --- Permanently frozen ground --- Perpetually frozen ground --- Tjale --- Earth sciences. --- Sedimentology. --- Microbial genomics. --- Astrobiology. --- Climate change. --- Earth Sciences. --- Climate Change. --- Microbial Ecology. --- Microbial Genetics and Genomics. --- Frozen ground --- Natural history --- Astrobiology --- Habitable planets --- Life --- Genomics --- Microbial genetics --- Microorganisms --- Genetics --- Microbiology --- Environmental microbiology --- Changes, Climatic --- Changes in climate --- Climate change --- Climate change science --- Climate changes --- Climate variations --- Climatic change --- Climatic changes --- Climatic fluctuations --- Climatic variations --- Global climate changes --- Global climatic changes --- Climatology --- Climate change mitigation --- Teleconnections (Climatology) --- Biological diversification --- Biological diversity --- Biotic diversity --- Diversification, Biological --- Diversity, Biological --- Biocomplexity --- Ecological heterogeneity --- Numbers of species --- Petrology --- Origin --- Environmental aspects --- Global environmental change
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