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Latitudinal differentiated water table control of carbon dioxide, methane and nitrous oxide fluxes from hydromorphic soils: feedbacks to climate change
Author(s) -
JUNGKUNST HERMANN F.,
FIEDLER SABINE
Publication year - 2007
Publication title -
global change biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 4.146
H-Index - 255
eISSN - 1365-2486
pISSN - 1354-1013
DOI - 10.1111/j.1365-2486.2007.01459.x
Subject(s) - environmental science , nitrous oxide , carbon dioxide , soil water , radiative forcing , greenhouse gas , methane , atmospheric sciences , water table , subarctic climate , temperate climate , climate change , chemistry , soil science , ecology , geology , geotechnical engineering , organic chemistry , groundwater , biology
The possibility of carbon (C) being locked away from the atmosphere for millennia is given in hydromorphic soils. However, the water‐table‐dependent feedback from soil organic matter (SOM) decomposition to the climate system is less clear. At least three greenhouse gases are produced: carbon dioxide (CO 2 ), methane (CH 4 ) and nitrous oxide (N 2 O). These gases show emission peaks at different water table positions and have different global warming potentials (GWP), for example a factor of 23 for CH 4 and 296 for N 2 O as compared with the equivalent mass of CO 2 on a 100‐year time horizon. This review of available annual data on all three gases revealed that the radiative forcing effect of SOM decomposition is principally dictated by CO 2 despite its low GWP. Anaerobic SOM decomposition generally has a lower potential feedback to the climatic system than aerobic SOM decomposition. Concrete values are constrained by a lack of data from tropical and subarctic regions. Furthermore, data on N 2 O and on plant effects are generally rare. However, there is a clear latitudinal differentiation for the GWP of soils under anaerobic conditions compared with aerobic conditions when looking at CO 2 and CH 4 : in the tropical and temperate regions, the anaerobic GWP showed a range of 25–60% of the aerobic value, but values varied between 80% and 110% in the boreal zone. Hence, particularly in the vulnerable boreal zone, the feedback from ecosystems to climate change will highly depend on plant responses to changing water tables at elevated temperatures.