Carbon cycle in the Russian Arctic seas [Libro electrónico] / autores: Alexander A. Vetrov, Evgenii A. Romankevich
Por: Vetrov, Alexander A [autor/a].
Romankevich, Evgenii A [autor/a].
Tipo de material: Libro en línea Editor: New York, New York, United States: Springer-Verlag Berlin Heidelberg, c2004Descripción: x, 331 páginas : ilustraciones mapas ; 25 centímetros.ISBN: 3540214771; 9783642059919 (Print); 9783662062081 (Online).Tema(s): Aguas marinas | Carbon dioxide content | Ciclo del carbono (Biogeoquímica) | Oceanografía química | Arctic OceanNota de acceso: Disponible para usuarios de ECOSUR con su clave de acceso Nota de bibliografía: Incluye bibliografía e índice: páginas 287-326 Número de sistema: 56525Contenidos:Mostrar Resumen:Tipo de ítem | Biblioteca actual | Colección | Signatura | Estado | Fecha de vencimiento | Código de barras |
---|---|---|---|---|---|---|
Libros | Biblioteca Electrónica Recursos en línea (RE) | Acervo General | Recurso digital | ECO400565256864 |
Incluye bibliografía e índice: páginas 287-326
1. Introduction.. 2. Features of the arctic seas of Russia and their ecosystems.. 3. Biological production of the arctic seas of Russia.. 4. Particulate matter and vertical carbon fluxes in the water-bottom system.. 5. Horizontal carbon fluxes in the land-sea system.. 6. Carbon in the bottom sediments.. 7. Elements of carbon balance and cycling in the arctic seas of Russia.. Index
Disponible para usuarios de ECOSUR con su clave de acceso
At present, studies of the Arctic Basin are of particular importance to the world scientific community due to the strong influence of this region on the global climate, its enormous mineral and hydrocarbon resources, the poor knowledge about the polar biosphere, and the growing anthropogenic pollution of the Arctic (Gramberg et al. 2000; KIuev 2000). Therefore, the forthcoming century is sometimes justly named "the century of the Arctic. " Global climatic changes attract the close attention of scientists from all over the world. The prevalent concept that climate warming is a minor positive anomaly in the planetary temperature is documented by the analyses of hundreds of thousands of deep-sea samples. Forecasts predict a tendency to even stronger warming over the next decades (Watson et al. 1998). The climate warming is accompanied by a reduction in the area and thickness of the ice cover, a negative balance of the Arctic glaciers, a northward migration of the arboreal front, an increase in the permafrost temperature in the Russian Arctic, and a tendency to the growth of biological productivity (Serreze et al. 2000; Morison et al. 2001). Carbon cycling strongly affects the earth's climate;, its study in the Arctic Seas of Russia is an essential link in the solution of the global climate change problem. eng
Disponible en línea
Adobe Acrobat profesional 6.0 o superior
Subscripción a ELSEVIER 26 de diciembre del 2013