Water-Carbon Dynamics in Eastern Siberia: Ecological Studies, cartea 236
Editat de Takeshi Ohta, Tetsuya Hiyama, Yoshihiro Iijima, Ayumi Kotani, Trofim C. Maximoven Limba Engleză Hardback – 12 iul 2019
Eastern Siberia is located in the easternmost part of the Eurasian continent, and the land surface with underlying permafrost has developed over a period of seventy thousand years. The permafrost ecosystem has specific hydrological and meteorological characteristics in terms of the water and carbon dynamics, and the current global warming and resulting changes in the permafrost environment are serious issues in the high-latitude regions.
The book is a valuable resource for students, researchers and professionals interested in forest meteorology and hydrology, forest ecology, and boreal vegetation, as well as the impact of climate change and water-carbon cycles in permafrost and non-permafrost regions.
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Specificații
ISBN-13: 9789811363160
ISBN-10: 9811363161
Pagini: 280
Ilustrații: X, 309 p. 97 illus., 62 illus. in color.
Dimensiuni: 155 x 235 x 22 mm
Greutate: 0.59 kg
Ediția:1st ed. 2019
Editura: Springer Nature Singapore
Colecția Springer
Seria Ecological Studies
Locul publicării:Singapore, Singapore
ISBN-10: 9811363161
Pagini: 280
Ilustrații: X, 309 p. 97 illus., 62 illus. in color.
Dimensiuni: 155 x 235 x 22 mm
Greutate: 0.59 kg
Ediția:1st ed. 2019
Editura: Springer Nature Singapore
Colecția Springer
Seria Ecological Studies
Locul publicării:Singapore, Singapore
Cuprins
Introduction.- Atmospheric water cycle.- Water cycles in forests.- Carbon cycles in forests.- Methane and biogenic volatile organic compound emissions in eastern Siberia.- Stable isotopes of water in Permafrost ecosystem.- Water-carbon cycle in dendrochronology.- Permafrost-forest dynamic.- River Discharge.- Remote sensing of vegetation.- Remote sensing of terrestrial water.- Water-carbon cycle modeling.- Concluding Remarks.
Textul de pe ultima copertă
This book discusses the water and carbon cycle system in the permafrost region of eastern Siberia, providing vital insights into how climate change has affected the permafrost environment in recent decades. It analyzes the relationships between precipitation and evapotranspiration, gross primary production and runoff in the permafrost regions, which differ from those intropical and temperate forests.
Eastern Siberia is located in the easternmost part of the Eurasian continent, and the land surfacewith underlying permafrost has developed over a period of seventy thousand years. The permafrost ecosystem has specific hydrological and meteorological characteristics in terms of the water and carbon dynamics, and the current global warming and resulting changes in the permafrost environment are serious issues in the high-latitude regions.
The book is a valuable resource for students, researchers and professionals interested in forest meteorology and hydrology, forest ecology, and boreal vegetation, as well as the impact of climate change and water-carbon cycles in permafrost and non-permafrost regions.
Eastern Siberia is located in the easternmost part of the Eurasian continent, and the land surfacewith underlying permafrost has developed over a period of seventy thousand years. The permafrost ecosystem has specific hydrological and meteorological characteristics in terms of the water and carbon dynamics, and the current global warming and resulting changes in the permafrost environment are serious issues in the high-latitude regions.
The book is a valuable resource for students, researchers and professionals interested in forest meteorology and hydrology, forest ecology, and boreal vegetation, as well as the impact of climate change and water-carbon cycles in permafrost and non-permafrost regions.
Caracteristici
Describes the processes of ecohydrology, permafrost hydrology, meteorology, and climatology in the context of water, energy, and carbon exchanges in the Arctic circumpolar region of eastern Siberia Discusses the unique water and carbon cycle system in the permafrost region in eastern Siberia, which is not seen in non-permafrost regions (tropical and mid-latitude regions) Highlights water-carbon dynamics influenced by the changing permafrost environment in recent decades