Global climate change and its impacts on the terrestrial Arctic carbon cycle with special regards to ecosystem components and the greenhouse‐gas balance
Abstract The climatic changes on earth may have serious implications for the carbon (C) cycle in the terrestrial Arctic throughout the 21st century. Arctic vegetation takes up carbon dioxide (CO 2 ) from the atmosphere producing biomass. In a cold and often moist soil environment, dead organic matte...
| Published in: | Journal of Plant Nutrition and Soil Science |
|---|---|
| Main Authors: | , , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Wiley
2010
|
| Subjects: | |
| Online Access: | http://dx.doi.org/10.1002/jpln.200900331 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjpln.200900331 https://onlinelibrary.wiley.com/doi/pdf/10.1002/jpln.200900331 |
| Summary: | Abstract The climatic changes on earth may have serious implications for the carbon (C) cycle in the terrestrial Arctic throughout the 21st century. Arctic vegetation takes up carbon dioxide (CO 2 ) from the atmosphere producing biomass. In a cold and often moist soil environment, dead organic matter is preferentially preserved as soil organic matter (SOM) due to the inhibition of decomposition processes. However, viable soil microbes exhale huge amounts of CO 2 and methane (CH 4 ) annually. Hence, Arctic ecosystems exhibit annual fluxes of both carbon‐based (CO 2 and CH 4 ) greenhouse gases (GHGs) that are in an order of magnitude of millions of tons. Rising Arctic temperatures lead to the degradation of much of today's permafrost in the long run. As a result, large quantities of frozen SOM may become available for decomposers, and GHGs that are entrapped in permafrost may be released. At the same time, warming tends to stimulate the growth, development, and reproduction of many Arctic plants, at least transiently. The present northward migration of boreal shrubs and trees into southern tundra areas may be amplified by that, increasing the ecosystems' gross primary production and, thus, their C sequestration. On the other hand, rising temperatures boost SOM decomposition and microbial respiration rates. In general, soil temperature and soil moisture are key environmental variables to control the intensity of aerobic and anaerobic respiration by microbes, and autotrophic respiration by plants. On the basis of published data on Arctic CO 2 and CH 4 fluxes, the calculations on the terrestrial C‐based Arctic GHG balance made in this review reveal a current annual GHG exchange that ranges between a weak storage of ≤ 225 Tg CO 2 equivalent (eq.) y –1 and a huge release of ≤ 1990 Tg CO 2 eq. y –1 . Hence, the Arctic GHG balance does apparently already contribute positively to the climatic changes at present. Regarding the future, the relative development of the uptake and release of CO 2 and CH 4 by northern ... |
|---|