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首页> 外文期刊>Global change biology >Response to 'The European nitrogen cycle: response to Schulze et al, Global Change Biology (2010) 16, pp. 1451-1469'
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Response to 'The European nitrogen cycle: response to Schulze et al, Global Change Biology (2010) 16, pp. 1451-1469'

机译:对“欧洲氮循环:对Schulze等人,Global Change Biology(2010)16,第1451-1469页”的响应

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摘要

Winniwarter and colleagues present alternative estimates for several of the nitrogen (N) fluxes provided by Schulze and colleagues. They reason that numeric discrepancies between largely dependent estimates and lack of detail in Schulze's estimates urges caution in interpreting these numbers. In this reply we provide methodological details enhancing the transparency of Schulze's estimates and argue that convergence between land-and atmosphere-based estimates should be reached before individual estimates can be rejected. Only for the nitrous oxide and NOx fluxes a balance between atmosphere and land-based estimates has been reached. Convergence between independent estimates has not been reached yet for NO-, NH3- and N-deposition estimates. As stated by Schulze and colleagues these N-fluxes remain potentially biased and therefore come with a large uncertainty, irrespective of the reported precision.
机译:Winniwarter及其同事提供了Schulze及其同事提供的几种氮通量的替代估计。他们认为,在很大程度上依赖的估计与舒尔茨的估计中缺乏细节之间的数字差异,在解释这些数字时应谨慎行事。在此答复中,我们提供了方法学上的细节,以增强Schulze估算的透明度,并主张应该在拒绝单个估算之前达到基于陆地和基于大气的估算之间的收敛。仅对于一氧化二氮和氮氧化物通量,大气和陆地估算之间就达到了平衡。对于NO,NH3和N沉积估算,尚未实现独立估算之间的收敛。如Schulze及其同事所述,这些N磁通仍可能存在偏差,因此,无论报道的精度如何,不确定性都很大。

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