B13G-0728
Effects of nitrogen deposition on carbon and nitrogen dynamics: a model-data comparison at an alpine meadow on the Qinghai Tibetan Plateau

Monday, 14 December 2015
Poster Hall (Moscone South)
Li Zhang1, Pan Li2, Huajun Fang1, Xiaoli Ren1, Honglin He3, Yingnian Li4 and Guirui Yu1, (1)IGSNRR Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing, China, (2)Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, China, (3)Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China, (4)Northwest Institute of Plateau Biology, Chinese Academy of Sciences, Xining, China
Abstract:
Significant increases in atmospheric nitrogen (N) deposition due to human activities are likely to alter the carbon (C) and nitrogen cycles of terrestrial ecosystems. N deposition has the potential to affect photosynthesis, plant and soil respiration, and thus vegetation and soil C storages. Accurate estimation of the change in plant uptake of carbon dioxide due to N deposition is essential to dealing with the climate change. Among the 11 earth system models which provide climate projection for the Fifth Assessment Report of the Intergovernmental Panel for Climate Change, only the community land model (CLM-CN) used in two of them includes a dynamic terrestrial nitrogen cycle. However, the responses of carbon and nitrogen dynamics to nitrogen deposition in CLM-CN have not been well evaluated. In this study, we examine the performance of CLM-CN (version 4.0) in simulating how leaf N content, leaf area index (LAI), aboveground biomass, soil respiration, and soil organic C and N respond to low-level N addition (40 kg N m-2 yr-1) using observations at an alpine meadow on the Qinghai Tibetan Plateau. CLM-CN well reproduced the positive responses of LAI and soil respiration (+13% and +8%) to the N addition, compared to observed increases (+14% and +12%). However, the CLM-CN leaf N content response to N addition (+13%) was larger than observed (+5%), and modeled response of aboveground biomass C (+5%) was smaller than observed (+12%). Moreover, modeled slight positive response (+0.2%) of soil organic C to N addition was inconsistent with observed decrease of 8.8%. Additional manipulation experimental data are required for evaluating and improving models in simulating responses of plant N uptake, C and N allocation, litter and soil organic matter decomposition to N deposition.