Potential feedback of thawing permafrost to the global climate system through methane emission
Datos Bibliográficos
| ID | 15548552 |
|---|---|
| Autores | O A Anisimov (0000-0002-9515-4576, State Hydrological Institute, autor de correspondencia) |
| Año | 2007 |
| Volumen | 2 |
| Número | 4 |
| Páginas | 045016-045016 |
| Fecha de publicación | 2007-10-01 |
| Peer Reviewed | Sí |
| Open Access | Sí |
| Tipo | ARTICLE |
| Revista | Environmental Research Letters (JOURNAL) |
| Identificadores de la revista | ISSN: 1748-9326 • E-ISSN: 1748-9326 |
| Editorial | IOP Publishing (PUBLISHER • GB) |
| DOI | 10.1088/1748-9326/2/4/045016 |
| OpenAlex | W2119730771 |
| Idioma | EN |
| Citas recibidas | 16 |
| Referencias citadas | 21 |
Large amounts of soil carbon deposited in permafrost may be released due to deeper seasonal thawing under the climatic conditions projected for the future. An increase in the volume of the available organic material together with the higher ground temperatures may lead to enhanced emission of greenhouse gasses. Particular concerns are associated with methane, which has a much stronger greenhouse effect than an equal amount of CO2. Production of methane is favored in the wetlands, which occupy up to 0.7 million km2 in Russian permafrost regions and have accumulated about 50 Gt of carbon (Gt C). We used the permafrost model and several climatic scenarios to construct projections of the soil temperature and the depth of seasonal thawing. To evaluate the effect of such changes on the volume of the seasonally thawing organic material, we overlaid the permafrost projections on the digitized geographically referenced contours of 59 846 wetlands in the Russian Arctic. Results for the mid-21st century climate indicated up to 50% increase in the volume of organic substrate in the northernmost locations along the Arctic coast and in East Siberia, where wetlands are sparse, and a relatively small increase by 10%–15% in West Siberia, where wetlands occupy 50%–80% of the land. We developed a soil carbon model and used it to estimate the changes in the methane fluxes due to higher soil temperature and increased substrate availability. According to our results, by mid-21st century the annual net flux of methane from Russian permafrost regions may increase by 6–8 Mt, depending on climatic scenario. If other sinks and sources of methane remain unchanged, this may increase the overall content of methane in the atmosphere by approximately 100 Mt, or 0.04 ppm, and lead to 0.012 °C global temperature rise
Arctic · Atmospheric sciences · Carbon fibers · Climate change · Geography · Global warming · Greenhouse gas · Hydrology (agriculture · Methane · Permafrost · Physical geography · Soil carbon · Soil water · Substrate (aquarium · Thermokarst · Wetland · Climate change and permafrost · Cryospheric studies and observations · Environmental Science · Methane Hydrates and Related Phenomena · Ecology · Geology · Oceanography · Soil Science
The Melting Himalayas
Permafrost degradation and soil erosion as drivers of greenhouse gas emissions from tundra ponds
New satellite climate data records indicate strong coupling between recent frozen season changes and snow cover over high northern latitudes
Large methane emission upon spring thaw from natural wetlands in the northern permafrost region
Rising methane emissions in response to climate change in Northern Eurasia during the 21st century
Assessing landscape potential for human sustainability and ‘attractiveness’ across Asian Russia in a warmer 21st century
Application of a Bayesian belief network for assessing the vulnerability of permafrost to thaw and implications for greenhouse gas production and climate feedback
Testate amoebae and δ13C of Sphagnum as surface-moisture proxies in Alaskan peatlands
Thawing permafrost and methane emission in Siberia
Permafrost degradation and methane
The impact of the permafrost carbon feedback on global climate
Evaluation of methane emissions from West Siberian wetlands based on inverse modeling
Water and energy footprint of irrigated agriculture in the Mediterranean region
Impact of changes in GRACE derived terrestrial water storage on vegetation growth in Eurasia
Arctic amplification causes earlier onset of seasonal tree growth in northeastern Siberia
Contribution of permafrost soils to the global carbon budget
| Obras citantes distintas | 16 |
|---|---|
| Citas por año | 0,94 |
| Intervalo de citas | 2009 - 2024 (16) |
| Velocidad de citación | recent |
| Altamente citado | No |
| Tipos de cita | Neutras: 16 |