Methane emissions from wet polygonal tundra II: Modelling methane fluxes on the regional scale a case study for the Lena River Delta region

Arctic regions are especially influenced by a warming climate and thus are of high scientific interest. Methane, a highly radiative active trace gas and hence affecting global warming, is produced in permafrost soils and released into the atmosphere. The Lena River Delta, located at the Laptev Sea i...

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Main Authors: Kirschke, S., Guenther, K., Wisskirchen, K., Sachs, Torsten
Format: Conference Object
Language:unknown
Published: 2007
Subjects:
Online Access:https://epic.awi.de/id/eprint/16911/
https://hdl.handle.net/10013/epic.26749
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spelling ftawi:oai:epic.awi.de:16911 2024-09-15T17:34:55+00:00 Methane emissions from wet polygonal tundra II: Modelling methane fluxes on the regional scale a case study for the Lena River Delta region Kirschke, S. Guenther, K. Wisskirchen, K. Sachs, Torsten 2007 https://epic.awi.de/id/eprint/16911/ https://hdl.handle.net/10013/epic.26749 unknown Kirschke, S. , Guenther, K. , Wisskirchen, K. and Sachs, T. (2007) Methane emissions from wet polygonal tundra II: Modelling methane fluxes on the regional scale a case study for the Lena River Delta region , International Conference "Cryogenic Resources of Polar Regions", Salekhard, Russia, June 17-21 . hdl:10013/epic.26749 EPIC3International Conference "Cryogenic Resources of Polar Regions", Salekhard, Russia, June 17-21, 2007 p. Conference notRev 2007 ftawi 2024-06-24T03:59:51Z Arctic regions are especially influenced by a warming climate and thus are of high scientific interest. Methane, a highly radiative active trace gas and hence affecting global warming, is produced in permafrost soils and released into the atmosphere. The Lena River Delta, located at the Laptev Sea in northeast Siberia, is characterized by arctic tundra ecosystems and is underlain by continuous permafrost. Modelling methane flux is an important step in determining its source strength in high arctic environments.We present a methodical structure wherein two models are coupled and used to assess methane emissions from permafrost soils in the Lena River Delta on the regional scale. The process-based vegetation model BETHY/DLR (Biosphere Energy Transfer Hydrology Model; Knorr 1997, Wisskirchen 2005) is applied to calculate the net primary productivity (NPP) of high arctic tundra vegetation. NPP is parameterised as a measure for substrate availability and thus an important input parameter for the second model: the process-based methane model (Walter 1998) is subsequently used to explicitly model methane emissions for a given soil column, taking into account thawing permafrost.Model forcing consists of meteorological data, e.g. radiation, air and soil temperature and precipitation, obtained from the European Centre for Medium-Range Weather Forecasts (ECMWF). They are validated by field measurements. Auxiliary input data for both models are derived from satellite-borne remote sensing data. A land use/land classification (LULC) scheme based on multispectral LANDSAT-7 ETM+ data (Schneider 2005) is used to derive information on wetland distribution as well as on vegetation and active layer thickness (ALT). The three parameters are key factors in modelling methane emissions from permafrost affected tundra ecosystems.Various measurements of methane flux on the landscape scale and small scale have been carried out during the entire growing season 2006 in the southern part of the Lena River delta (72°N, 126°E) by Alfred ... Conference Object Active layer thickness Global warming laptev Laptev Sea lena river permafrost Tundra Siberia Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description Arctic regions are especially influenced by a warming climate and thus are of high scientific interest. Methane, a highly radiative active trace gas and hence affecting global warming, is produced in permafrost soils and released into the atmosphere. The Lena River Delta, located at the Laptev Sea in northeast Siberia, is characterized by arctic tundra ecosystems and is underlain by continuous permafrost. Modelling methane flux is an important step in determining its source strength in high arctic environments.We present a methodical structure wherein two models are coupled and used to assess methane emissions from permafrost soils in the Lena River Delta on the regional scale. The process-based vegetation model BETHY/DLR (Biosphere Energy Transfer Hydrology Model; Knorr 1997, Wisskirchen 2005) is applied to calculate the net primary productivity (NPP) of high arctic tundra vegetation. NPP is parameterised as a measure for substrate availability and thus an important input parameter for the second model: the process-based methane model (Walter 1998) is subsequently used to explicitly model methane emissions for a given soil column, taking into account thawing permafrost.Model forcing consists of meteorological data, e.g. radiation, air and soil temperature and precipitation, obtained from the European Centre for Medium-Range Weather Forecasts (ECMWF). They are validated by field measurements. Auxiliary input data for both models are derived from satellite-borne remote sensing data. A land use/land classification (LULC) scheme based on multispectral LANDSAT-7 ETM+ data (Schneider 2005) is used to derive information on wetland distribution as well as on vegetation and active layer thickness (ALT). The three parameters are key factors in modelling methane emissions from permafrost affected tundra ecosystems.Various measurements of methane flux on the landscape scale and small scale have been carried out during the entire growing season 2006 in the southern part of the Lena River delta (72°N, 126°E) by Alfred ...
format Conference Object
author Kirschke, S.
Guenther, K.
Wisskirchen, K.
Sachs, Torsten
spellingShingle Kirschke, S.
Guenther, K.
Wisskirchen, K.
Sachs, Torsten
Methane emissions from wet polygonal tundra II: Modelling methane fluxes on the regional scale a case study for the Lena River Delta region
author_facet Kirschke, S.
Guenther, K.
Wisskirchen, K.
Sachs, Torsten
author_sort Kirschke, S.
title Methane emissions from wet polygonal tundra II: Modelling methane fluxes on the regional scale a case study for the Lena River Delta region
title_short Methane emissions from wet polygonal tundra II: Modelling methane fluxes on the regional scale a case study for the Lena River Delta region
title_full Methane emissions from wet polygonal tundra II: Modelling methane fluxes on the regional scale a case study for the Lena River Delta region
title_fullStr Methane emissions from wet polygonal tundra II: Modelling methane fluxes on the regional scale a case study for the Lena River Delta region
title_full_unstemmed Methane emissions from wet polygonal tundra II: Modelling methane fluxes on the regional scale a case study for the Lena River Delta region
title_sort methane emissions from wet polygonal tundra ii: modelling methane fluxes on the regional scale a case study for the lena river delta region
publishDate 2007
url https://epic.awi.de/id/eprint/16911/
https://hdl.handle.net/10013/epic.26749
genre Active layer thickness
Global warming
laptev
Laptev Sea
lena river
permafrost
Tundra
Siberia
genre_facet Active layer thickness
Global warming
laptev
Laptev Sea
lena river
permafrost
Tundra
Siberia
op_source EPIC3International Conference "Cryogenic Resources of Polar Regions", Salekhard, Russia, June 17-21, 2007 p.
op_relation Kirschke, S. , Guenther, K. , Wisskirchen, K. and Sachs, T. (2007) Methane emissions from wet polygonal tundra II: Modelling methane fluxes on the regional scale a case study for the Lena River Delta region , International Conference "Cryogenic Resources of Polar Regions", Salekhard, Russia, June 17-21 . hdl:10013/epic.26749
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