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Water-carbon dynamics in Eastern Siberia
~
Ohta, Takeshi.
Water-carbon dynamics in Eastern Siberia
紀錄類型:
書目-語言資料,印刷品 : Monograph/item
正題名/作者:
Water-carbon dynamics in Eastern Siberia/ edited by Takeshi Ohta ... [et al.].
其他作者:
Ohta, Takeshi.
出版者:
Singapore :Springer Singapore : : 2019.,
面頁冊數:
x, 309 p. :ill., digital ; : 24 cm.;
Contained By:
Springer eBooks
標題:
Ecohydrology - Russia (Federation) -
電子資源:
https://doi.org/10.1007/978-981-13-6317-7
ISBN:
9789811363177
Water-carbon dynamics in Eastern Siberia
Water-carbon dynamics in Eastern Siberia
[electronic resource] /edited by Takeshi Ohta ... [et al.]. - Singapore :Springer Singapore :2019. - x, 309 p. :ill., digital ;24 cm. - Ecological studies, analysis and synthesis,v.2360070-8356 ;. - Ecological studies, analysis and synthesis ;v.173..
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.
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.
ISBN: 9789811363177
Standard No.: 10.1007/978-981-13-6317-7doiSubjects--Topical Terms:
1227871
Ecohydrology
--Russia (Federation)
LC Class. No.: QH541.15.E19 / W37 2019
Dewey Class. No.: 577
Water-carbon dynamics in Eastern Siberia
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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.
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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.
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