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评价 11 个陆地碳氮循环模型与两项温带大气 CO2 增刊实验观测的一致性。

Evaluation of 11 terrestrial carbon-nitrogen cycle models against observations from two temperate Free-Air CO2 Enrichment studies.

机构信息

Biogeochemical Integration Department, Max Planck Institute for Biogeochemistry, Hans-Knöll-Str. 10, D-07745, Jena, Germany.

Department of Biological Science, Macquarie University, Sydney, NSW, 2109, Australia.

出版信息

New Phytol. 2014 May;202(3):803-822. doi: 10.1111/nph.12697. Epub 2014 Jan 28.

Abstract

We analysed the responses of 11 ecosystem models to elevated atmospheric [CO2 ] (eCO2 ) at two temperate forest ecosystems (Duke and Oak Ridge National Laboratory (ORNL) Free-Air CO2 Enrichment (FACE) experiments) to test alternative representations of carbon (C)-nitrogen (N) cycle processes. We decomposed the model responses into component processes affecting the response to eCO2 and confronted these with observations from the FACE experiments. Most of the models reproduced the observed initial enhancement of net primary production (NPP) at both sites, but none was able to simulate both the sustained 10-yr enhancement at Duke and the declining response at ORNL: models generally showed signs of progressive N limitation as a result of lower than observed plant N uptake. Nonetheless, many models showed qualitative agreement with observed component processes. The results suggest that improved representation of above-ground-below-ground interactions and better constraints on plant stoichiometry are important for a predictive understanding of eCO2 effects. Improved accuracy of soil organic matter inventories is pivotal to reduce uncertainty in the observed C-N budgets. The two FACE experiments are insufficient to fully constrain terrestrial responses to eCO2 , given the complexity of factors leading to the observed diverging trends, and the consequential inability of the models to explain these trends. Nevertheless, the ecosystem models were able to capture important features of the experiments, lending some support to their projections.

摘要

我们分析了 11 个生态系统模型对两个温带森林生态系统(杜克和橡树岭国家实验室(ORNL)自由空气 CO2 富集(FACE)实验)中大气[CO2](eCO2)升高的响应,以测试碳(C)-氮(N)循环过程的替代表示方法。我们将模型响应分解为影响对 eCO2 响应的组成过程,并将这些过程与 FACE 实验的观测结果进行了对比。大多数模型都再现了两个地点的净初级生产力(NPP)的观察到的初始增强,但没有一个能够模拟在杜克大学持续 10 年的增强和在 ORNL 的下降响应:模型通常表现出低于观察到的植物氮吸收的迹象,这表明氮限制逐渐加剧。尽管如此,许多模型与观察到的组成过程具有定性一致性。结果表明,改进地上-地下相互作用的表示方法并更好地约束植物化学计量学对于预测 eCO2 效应至关重要。改进土壤有机物质清单的准确性对于减少观察到的 C-N 预算中的不确定性至关重要。鉴于导致观察到的趋异趋势的因素的复杂性,以及模型无法解释这些趋势的后果,这两个 FACE 实验不足以完全约束陆地对 eCO2 的响应。尽管如此,生态系统模型能够捕捉到实验的重要特征,为其预测提供了一些支持。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/18b1/4288990/8e622c6db217/nph0202-0803-f1.jpg

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