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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >A global comparison of carbon monoxide profiles and column amounts from Tropospheric Emission Spectrometer (TES) and Measurements of Pollution in the Troposphere (MOPITT)
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A global comparison of carbon monoxide profiles and column amounts from Tropospheric Emission Spectrometer (TES) and Measurements of Pollution in the Troposphere (MOPITT)

机译:对流层发射光谱仪(TES)和对流层污染测量(MOPITT)的一氧化碳分布图和柱量的全球比较

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摘要

In this study, we compare carbon monoxide (CO) products from the Measurements of Pollution in the Troposphere (MOPITT) and Tropospheric Emission Spectrometer (TES) and investigate the possible causes of the differences between retrievals for these two data sets. Direct comparisons of CO retrievals for July 2006 show that TES CO concentrations are consistently biased lower than those of MOPITT by 25 ppbv near the surface and by 20 ppbv at 150 hPa, primarily due to different a priori profiles and covariance matrices used in the TES and MOPITT CO retrievals. To reduce the effects of different a priori constraints, we apply TES a priori profiles and covariance matrices to a modified MOPITT retrieval algorithm. The mean TES-MOPITT CO difference decreases from —25 to —10 ppbv near the surface. To further account for retrieval smoothing errors due to different TES and MOPITT averaging kernels, TES averaging kernels are used to smooth MOPITT CO profiles to derive TES-equivalent CO profiles. Compared to these, TES CO profiles are biased 1 ppbv lower near the surface and 4-9 ppbv lower in the troposphere, and the mean absolute TES and TES-equivalent CO column difference is less than 6.5%. The mean TES and MOPITT CO differences due to smoothing errors are close to zero, and the remaining bias is primarily due to the combined effects of radiance biases, forward model errors, and the spatial and temporal mismatches of TES and MOPITT pixels.
机译:在这项研究中,我们比较了来自对流层污染测量(MOPITT)和对流层排放光谱仪(TES)的一氧化碳(CO)产品,并研究了这两个数据集检索之间差异的可能原因。对2006年7月的CO取回量的直接比较表明,TES CO的浓度始终比MOPITT低20 ppbv靠近地表,在150 hPa时降低20 ppbv,这主要是由于TES和CO中使用的先验分布和协方差矩阵不同MOPITT CO检索。为了减少不同先验约束的影响,我们将TES先验分布图和协方差矩阵应用于经过修改的MOPITT检索算法。 TES-MOPITT CO的平均差在地表附近从-25 ppbv减小。为了进一步解决由于不同的TES和MOPITT平均内核导致的检索平滑误差,使用TES平均内核对MOPITT CO轮廓进行平滑以导出TES等效CO轮廓。相比之下,TES CO剖面在地表附近低1 ppbv,在对流层中低4-9 ppbv,平均TES和TES等效CO柱的平均绝对差小于6.5%。由于平滑误差导致的TES和MOPITT CO平均差接近于零,而剩余的偏差主要是由于辐射偏差,正向模型误差以及TES和MOPITT像素的空间和时间不匹配的综合影响。

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