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首页> 外文期刊>Atmospheric chemistry and physics >Comparing the CarbonTracker and TM5-4DVar data assimilation systems for CO2 surface flux inversions
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Comparing the CarbonTracker and TM5-4DVar data assimilation systems for CO2 surface flux inversions

机译:比较CarbonTracker和TM5-4DVAR数据同化系统进行二氧化碳表面磁通反转

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摘要

Data assimilation systems allow for estimating surface fluxes of greenhouse gases from atmospheric concentration measurements. Good knowledge about fluxes is essential to understand how climate change affects ecosystems and to characterize feedback mechanisms. Based on the assimilation of more than 1 year of atmospheric in situ concentration measurements, we compare the performance of two established data assimilation models, CarbonTracker and TM5-4DVar (Transport Model 5 - Four-Dimensional Variational model), for CO2 flux estimation. CarbonTracker uses an ensemble Kalman filter method to optimize fluxes on ecoregions. TM5-4DVar employs a 4-D variational method and optimizes fluxes on a 6 degrees x 4 degrees longitude-latitude grid. Harmonizing the input data allows for analyzing the strengths and weaknesses of the two approaches by direct comparison of the modeled concentrations and the estimated fluxes. We further assess the sensitivity of the two approaches to the density of observations and operational parameters such as the length of the assimilation time window.
机译:数据同化系统允许估计来自大气浓度测量的温室气体的表面磁通量。良好的关于助势的了解对于了解气候变化如何影响生态系统以及表征反馈机制是必不可少的。基于同化超过1年的大气浓度测量,我们比较两种建立的数据同化模型,CarbonTracker和TM5-4DVAR(传输模型5 - 四维变分模型)的性能,用于CO2通量估计。 CarbonTracker使用集合Kalman滤波器方法来优化Ecoregions上的助熔剂。 TM5-4DVAR采用4-D变分方法,并在6度x 4度经度纬度网格上优化助熔剂。协调输入数据允许通过直接比较建模浓度和估计的助熔剂来分析两种方法的强度和弱点。我们进一步评估了两种方法对观测密度和操作参数的敏感性,例如同化时间窗口的长度。

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