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Effect of climate dataset selection on simulations of terrestrial GPP: Highest uncertainty for tropical regions

机译:气候数据集选择对地面GPP模拟的影响:热带地区的最高不确定性

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摘要

Biogeochemical models use meteorological forcing data derived with different approaches (e.g. based on interpolation or reanalysis of observation data or a hybrid hereof) to simulate ecosystem processes such as gross primary productivity (GPP). This study assesses the impact of different widely used climate datasets on simulated gross primary productivity and evaluates the suitability of them for reproducing the global and regional carbon cycle as mapped from independent GPP data. We simulate GPP with the biogeochemical model LPJ-GUESS using six historical climate datasets (CRU, CRUNCEP, ECMWF, NCEP, PRINCETON, and WFDEI). The simulated GPP is evaluated using an observation-based GPP product derived from eddy covariance measurements in combination with remotely sensed data. Our results show that all datasets tested produce relatively similar GPP simulations at a global scale, corresponding fairly well to the observation-based data with a difference between simulations and observations ranging from -50 to 60 g m-2 yr-1. However, all simulations also show a strong underestimation of GPP (ranging from -533 to -870 g m-2 yr-1) and low temporal agreement (r < 0.4) with observations over tropical areas. As the shortwave radiation for tropical areas was found to have the highest uncertainty in the analyzed historical climate datasets, we test whether simulation results could be improved by a correction of the tested shortwave radiation for tropical areas using a new radiation product from the International Satellite Cloud Climatology Project (ISCCP). A large improvement (up to 48%) in simulated GPP magnitude was observed with bias corrected shortwave radiation, as well as an increase in spatio-temporal agreement between the simulated GPP and observation-based GPP. This study conducts a spatial inter-comparison and quantification of the performances of climate datasets and can thereby facilitate the selection of climate forcing data over any given study area for modelling purposes.
机译:生物地球化学模型使用通过不同方法(例如基于观测数据的内插或重新分析或本文的混合)得出的气象强迫数据来模拟生态系统过程,例如总初级生产力(GPP)。这项研究评估了不同的广泛使用的气候数据集对模拟总初级生产力的影响,并评估了它们是否适合从独立GPP数据中绘制出的全球和区域碳循环。我们使用六个历史气候数据集(CRU,CRUNCEP,ECMWF,NCEP,PRINCETON和WFDEI)用生物地球化学模型LPJ-GUESS模拟GPP。使用基于观测值的GPP产品评估仿真的GPP,该产品是从涡动协方差测量结果与遥感数据相结合得出的。我们的结果表明,所有测试数据集在全球范围内均产生了相对相似的GPP模拟,与基于观测的数据相当吻合,模拟与观测之间的差异介于-50至60 gm -2 yr之间 -1 。但是,所有模拟都显示出对GPP的强烈低估(范围从-533到-870 gm -2 yr -1 ),并且时间一致性低(r <0.4)热带地区的观测。由于在分析的历史气候数据集中发现热带地区的短波辐射具有最高的不确定性,因此我们测试了是否可以通过使用国际卫星云的新辐射产品对热带地区的短波辐射进行校正来改善模拟结果气候学项目(ISCCP)。通过偏置校正的短波辐射,可以观察到模拟GPP幅度有很大的提高(高达48%),并且模拟GPP和基于观测的GPP之间的时空一致性也有所提高。这项研究对气候数据集的性能进行了空间比对和量化,从而可以促进在任何给定研究区域内为模型目的选择气候强迫数据。

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