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Improving simulation of the terrestrial carbon cycle of China

The maximum rate of carboxylation (Vcmax) is a key photosynthetic parameter for gross primary production (GPP) estimation in terrestrial biosphere models. A set of observation-based Vcmax values, which take the nitrogen limitation on photosynthetic rates into consideration, are used in version 4.5 of the Community Land Model (CLM4.5). However, CLM4.5 with carbon-nitrogen (CN) biogeochemistry (CLM4.5-CN) still uses an independent decay coefficient for nitrogen after the photosynthesis calculation. This means that the nitrogen limitation on the carbon cycle is accounted for twice when CN biogeochemistry is active. Therefore, to avoid this double nitrogen down-regulation in CLM4.5-CN, the original Vcmax scheme is revised with a new one that only accounts for the transition between Vcmax and its potential value (without nitrogen limitation). Compared to flux tower-based observations, the new Vcmax scheme reduces the root-mean-square error (RMSE) in GPP for mainland China by 13.7 g C m−2 yr−1, with a larger decrease over humid areas (39.2 g C m−2 yr−1). Moreover, net primary production and leaf area index are also improved, with reductions in RMSE by 0.8% and 11.5%, respectively.

Eleven-year (2000–10) mean gross primary production (GPP) from the (a) control run (CTL_GPP), (b) new Vcmax scheme (NEW_GPP), (c) observations (MTE_GPP), (d) CTL_GPP minus MTE_GPP, (e) NEW_GPP minus MTE_GPP, and (f) NEW_GPP minus CTL_GPP. Panels (g–l) are the same as GPP but for net primary production (NPP) from (g) CTL_NPP, (h) NEW_NPP, (i) MODIS_NPP, (j) CTL_NPP minus MODIS_NPP, (k) NEW_NPP minus MODIS_NPP, and (l) NEW_NPP minus CTL_NPP. The grid shadow regions are significant at the 95% confidence level by student’s t test, and the isolines refer to the mean annual precipitation (mm yr−1).

Citation: Wang, Y.-Y., Z.-H. Xie, B.-H. Jia, et al., 2015: Improving simulation of the terrestrial carbon cycle of China in version 4.5 of the Community Land Model using a revised Vcmax scheme, Atmos. Oceanic Sci. Lett., 8, doi:10.3878/AOSL20140090.

Download: http://159.226.119.58/aosl/EN/abstract/abstract543.shtml

 

 
 
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