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Titlebook: Landscape Function and Disturbance in Arctic Tundra; James F. Reynolds,John D. Tenhunen Book 1996 Springer-Verlag Berlin Heidelberg 1996 L

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書目名稱Landscape Function and Disturbance in Arctic Tundra
編輯James F. Reynolds,John D. Tenhunen
視頻videohttp://file.papertrans.cn/581/580697/580697.mp4
叢書名稱Ecological Studies
圖書封面Titlebook: Landscape Function and Disturbance in Arctic Tundra;  James F. Reynolds,John D. Tenhunen Book 1996 Springer-Verlag Berlin Heidelberg 1996 L
描述Following the discovery of large petroleum reserves in northern Alaska, the US Department of Energy implemented an integrated field and modeling study to help define potential impacts of energy-related disturbances on tundra ecosystems. This volume presents major findings from this study. A broad range of basic and applied research topics are examined, ranging from ecosystem physiology and biogeochemistry to landscape models that quantify the impact of road-building on tundra hydrology and ecosystem structure. .It is an important resource for researchers and students interested in arctic ecology, as well as for environmental managers concerned with practical issues of disturbances.
出版日期Book 1996
關(guān)鍵詞Landschaft; Landschafts?kologie; St?rung, Landschaft; Tundra watershed; Tundra-Einzugsgebiet; chemistry; d
版次1
doihttps://doi.org/10.1007/978-3-662-01145-4
isbn_softcover978-3-662-01147-8
isbn_ebook978-3-662-01145-4Series ISSN 0070-8356 Series E-ISSN 2196-971X
issn_series 0070-8356
copyrightSpringer-Verlag Berlin Heidelberg 1996
The information of publication is updating

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Energy Balance and Hydrological Processes in an Arctic Watersheddgets and elucidate seasonal and annual patterns; subsequently, we present physical process models that further quantify the dynamics and interactions between thermal and hydrological regimes and provide additional insight with regard to water and energy budgets in tundra ecosystems.
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Shortwave Reflectance Properties of Arctic Tundra Landscapesch as biomass or vegetation composition (Chap. 18, this Vol.). Spectral radiances also constitute the basic data used in classical remote sensing studies (e.g., land cover classification) (Stow et al. 1989; Walsh and Davis 1994).
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Isotopic Tracers for Investigating Hydrological Processes et al. 1988; Swistock et al. 1989; Wels et al. 1991). However, there are few examples of simultaneous work tracing the fate of particle-reactive isotopes in snow, and even fewer isotopic applications in watersheds underlain by permafrost.
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Modeling Dry Deposition of Dust Along the Dalton Highwayularly during periods of dry weather. This dust is deposited on the adjacent vegetation where it has detrimental effects on some arctic species (Everett 1980; Santelmann and Gorham 1988; Walker and Everett 1987; Auerbach 1992; see Chaps. 3, 9, 11, and 18, this Vol.).
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