Representation of phosphorus cycle in Joint UK Land Environment Simulator (vn5.5_JULES-CNP)
Representation of phosphorus cycle in Joint UK Land Environment Simulator (vn5.5_JULES-CNP)
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DOI:
10.5194/gmd-2021-403
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发表时间:
2021-12
影响因子:
5.1
通讯作者:
M. Nakhavali;L. Mercado;I. Hartley;S. Sitch;Fernanda V. Cunha;Raffaello di Ponzio;L. F. Lugli;C. Quesada;K. Andersen;S. Chadburn;A. Wiltshire;D. Clark;G. Ribeiro;Lara Siebert;A. M. Moraes;Jéssica Schmeisk Rosa;R. Assis;J. Camargo
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作者:
M. Nakhavali;L. Mercado;I. Hartley;S. Sitch;Fernanda V. Cunha;Raffaello di Ponzio;L. F. Lugli;C. Quesada;K. Andersen;S. Chadburn;A. Wiltshire;D. Clark;G. Ribeiro;Lara Siebert;A. M. Moraes;Jéssica Schmeisk Rosa;R. Assis;J. Camargo
Abstract. Most Land Surface Models (LSMs), the land components of Earth system models (ESMs), include representation of N limitation on ecosystem productivity. However only few of these models have incorporated phosphorus (P) cycling. In tropical ecosystems, this is likely to be particularly important as N tends to be abundant but the availability of rock-derived elements, such as P, can be very low. Thus, without a representation of P cycling, tropical forest response in areas such as Amazonia to rising atmospheric CO2 conditions remains highly uncertain. In this study, we introduced P dynamics and its interactions with the N and carbon (C) cycles into the Joint UK Land Environment Simulator (JULES). The new model (JULES-CNP) includes the representation of P stocks in vegetation and soil pools, as well as key processes controlling fluxes between these pools. We evaluate JULES-CNP at the Amazon nutrient fertilization experiment (AFEX), a low fertility site, representative of about 60 % of Amazon soils. We apply the model under ambient CO2 and elevated CO2. The model is able to reproduce the observed plant and soil P pools and fluxes under ambient CO2. We estimate P to limit net primary productivity (NPP) by 24 % under current CO2 and by 46 % under elevated CO2. Under elevated CO2, biomass in simulations accounting for CNP increase by 10 % relative to at contemporary CO2, although it is 5 % lower compared with CN and C-only simulations. Our results highlight the potential for high P limitation and therefore lower CO2 fertilization capacity in the Amazon forest with low fertility soils.