首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Comparing mass balance and adjoint methods for inverse modeling of nitrogen dioxide columns for global nitrogen oxide emissions
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Comparing mass balance and adjoint methods for inverse modeling of nitrogen dioxide columns for global nitrogen oxide emissions

机译:对全球氮氧化物排放氮二氧化氮柱逆建模的质量平衡和伴随方法

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摘要

Satellite observations offer information applicable to top-down constraints on emission inventories through inverse modeling. Here we compare two methods of inverse modeling for emissions of nitrogen oxides (NO_x) from nitrogen dioxide (NO_2) columns using the GEOS-Chem chemical transport model and its adjoint. We treat the adjoint-based 4D-Var modeling approach for estimating top-down emissions as a benchmark against which to evaluate variations on the mass balance method. We use synthetic NO_2 columns generated from known NO_x emissions to serve as "truth." We find that error in mass balance inversions can be reduced by up to a factor of 2 with an iterative process that uses finite difference calculations of the local sensitivity of NO_2 columns to a change in emissions. In a simplified experiment to recover local emission perturbations, horizontal smearing effects due to NO_x transport are better resolved by the adjoint approach than by mass balance. For more complex emission changes, or at finer resolution, the iterative finite difference mass balance and adjoint methods produce similar global top-down inventories when inverting hourly synthetic observations, both reducing the a priori error by factors of 3-4. Inversions of simulated satellite observations from low Earth and geostationary orbits also indicate that both the mass balance and adjoint inversions produce similar results, reducing a priori error by a factor of 3. As the iterative finite difference mass balance method provides similar accuracy as the adjoint method, it offers the prospect of accurately estimating top-down NO_x emissions using models that do not have an adjoint.
机译:卫星观察通过反向建模提供适用于对排放清单的自上而下限制的信息。在这里,我们使用Geos-Chem化学传输模型及其伴随的二氧化氮(NO_2)柱的氮氧化物(NO_X)排放两种反向建模的两种反向建模方法。我们对基于伴随的4D-VAR建模方法进行估算,以估计自上而下的排放作为评估质量平衡方法的变化的基准。我们使用从已知的NO_X排放中生成的合成NO_2列作为“真理”。我们发现可以通过最多为2的因子减小与一个反复的过程中质量平衡倒置该误差NO_2列到在排放的变化的局部灵敏度的用途有限差分计算。在简化的实验中以回收局部排放扰动,通过伴随方法而不是质量平衡,更好地解决了由于NO_X传输引起的水平涂抹效果。为了更复杂的排放变化,或更精细的分辨率,迭代有限差分质量平衡和伴随方式在反转每小时合成观察时会产生类似的全球自上而下库存,两者都通过3-4的因素来减少先验误差。来自低地球和地球静止轨道的模拟卫星观测的逆转,也表明质量平衡和伴随反转都产生了类似的结果,减少了优先误差。随着迭代有限差分质量平衡方法提供类似的准确性作为伴随方法。 ,它提供了使用没有伴随的模型准确地估算自上而下的NO_X排放的前景。

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