International audienceNitrogen limitation of ecosystem productivity is ubiquitous, and it is thought that it has and will have a significant impact on net ecosystem productivity, and thus carbon sequestration, in the context of ongoing future increase of atmospheric CO2 concentration and climate change. However, many vegetation models do not represent nitrogen limitation, and might thus overestimate future terrestrial C sequestration. This work presents a simple parameterization of nitrogen limitation that can be easily implemented in vegetation models which do not yet include a complete nitrogen cycle. This parameterization is based on the ratio between heterotrophic respiration (considered a "proxy" of net mineralization rate) and net pri...
Projections of future changes in land carbon (C) storage using biogeochemical models depend on accur...
The magnitude and variability of the terrestrial CO2 sink remain uncertain, partly due to limited gl...
Abstract. Terrestrial carbon (C) sequestration is limited by nitrogen (N), an empirically establishe...
International audienceNitrogen limitation of ecosystem productivity is ubiquitous, and it is thought...
Terrestrial carbon (C) cycle models applied for climate projections simulate a strong increase in ne...
Increase of forest areas has the potential to increase the terrestrial carbon (C) sink. However, the...
Recently a considerable amount of effort has been put into quantifying how interactions of the carbo...
The availability of nitrogen is one of the primary nutritional controls on plant growth. Terrestrial...
The LPJ-GUESS dynamic vegetation model uniquely combines an individual- and patch-based representati...
The well-established dynamical global vegetation, hydrology, and crop growth model LPJmL is extended...
The well-established dynamical global vegetation, hydrology, and crop growth model LPJmL is extended...
Projections of future changes in land carbon (C) storage using biogeochemical models depend on accur...
The magnitude and variability of the terrestrial CO2 sink remain uncertain, partly due to limited gl...
Abstract. Terrestrial carbon (C) sequestration is limited by nitrogen (N), an empirically establishe...
International audienceNitrogen limitation of ecosystem productivity is ubiquitous, and it is thought...
Terrestrial carbon (C) cycle models applied for climate projections simulate a strong increase in ne...
Increase of forest areas has the potential to increase the terrestrial carbon (C) sink. However, the...
Recently a considerable amount of effort has been put into quantifying how interactions of the carbo...
The availability of nitrogen is one of the primary nutritional controls on plant growth. Terrestrial...
The LPJ-GUESS dynamic vegetation model uniquely combines an individual- and patch-based representati...
The well-established dynamical global vegetation, hydrology, and crop growth model LPJmL is extended...
The well-established dynamical global vegetation, hydrology, and crop growth model LPJmL is extended...
Projections of future changes in land carbon (C) storage using biogeochemical models depend on accur...
The magnitude and variability of the terrestrial CO2 sink remain uncertain, partly due to limited gl...
Abstract. Terrestrial carbon (C) sequestration is limited by nitrogen (N), an empirically establishe...