通过改进云检测增强MOPITT数据覆盖

H. Marey, J. Drummond, Dylan B. A. Jones, H. Worden, M. Deeter, J. Gille, D. Mao
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摘要

摘要自2000年3月以来,对流层污染测量(MOPITT)卫星仪器一直在测量全球对流层一氧化碳(CO),提供了从太空几乎连续的最长CO记录。在其长期任务期间,数据处理算法已得到更新,以提高CO检索的质量和对流层下层的敏感性。目前,MOPITT的检索仅用于晴空观测或低云上的海洋场景。与所有观测到的辐射相比,在90°S-90°N和60°S-60°N之间,成功的恢复率分别约为30%和40%。空间季节变化表明,一些地方的MOPITT数据覆盖率在夏季可达30%,但在冬季,由于云量的显著增加,这一数字可能下降到10%以下。因此,我们研究了现有的MOPITT云检测算法,并考虑了增加数据覆盖率的方法。通过关闭云检测方案来修改MOPITT CO总列(TC)数据,以允许CO检索结果,而不管其云状态如何。在选定的日子对标准CO TC产品(云过滤)和非标准产品(非云屏蔽)进行分析。结果表明,在非掩膜CO产品中经常观察到一些在标准产品中不存在的相干结构,这些结构可能是实际的CO特征。对中分辨率成像光谱仪(MODIS)的云高度和云掩模产品以及MOPITT云标志描述符进行了相应的分析,以了解这些明显的物理CO特征所存在的云条件。结果表明,在标准产品中有大量低云CO回收被拒绝。这些缺失的区域与在非掩膜CO产品中检测到的相干模式相匹配。在红外大气探测干涉仪(IASI) CO TC产品中也多次看到这些结构,表明实际的CO羽流。利用Terra卫星上的多角度成像光谱辐射计(MISR)数据与MODIS进行云高比较。MODIS和MISR云高数据的比较表明,两者的一致性非常显著,这对于将MODIS云高纳入MOPITT云检测方案的可能性是令人鼓舞的。对MODIS云高潜在利用的全球评估的统计表明,当在检索中纳入高度小于2公里的云高时,MOPITT数据显著增加。但是,必须定义和制定质量指标,以确保足够的检索质量。
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Enhanced MOPITT data coverage through cloud detection improvement
Abstract. The Measurements of Pollution in the Troposphere (MOPITT) satellite instrument has been measuring global tropospheric carbon monoxide (CO) since March 2000, providing the longest nearly continuous record of CO from space. During its long mission the data processing algorithms have been updated to improve the quality of CO retrievals and the sensitivity to the lower troposphere. Currently, MOPITT retrievals are only performed for clear-sky observations or over low clouds for ocean scenes. Compared to all observed radiances, successful retrieval rates are about 30 % and 40 % between 90° S–90° N and 60° S–60° N, respectively. Spatial seasonal variations show that while MOPITT data coverage in some places reaches 30 % in summer, this number can drop to less than 10 % in winter due to significantly increased cloud cover. Therefore, we investigate the current MOPITT cloud detection algorithm and consider approaches to increase the data coverage. The MOPITT CO total column (TC) data were modified by turning off the cloud detection scheme to allow a CO retrieval result regardless of their cloud status. Analyses of the standard CO TC product (cloud filtered) and non-standard product (non-cloud masked) were conducted for selected days. Results showed some coherent structures that were observed frequently in the non-masked CO product that were not present in the standard product and could potentially be actual CO features. A corresponding analysis of Moderate Resolution Imaging Spectroradiometer(MODIS) cloud height and cloud mask products along with MOPITT cloud flag descriptors was conducted in order to understand the cloud conditions present for these apparently physical CO features. Results show that a significant number of low cloud CO retrievals were rejected in the standard product. Those missing areas match the coherent patterns that were detected in the non-masked CO product. Many times, these structures were also seen in the Infrared Atmospheric Sounding Interferometer (IASI) CO TC product indicating actual CO plumes. Multi-angle Imaging SpectroRadiometer (MISR) data on the Terra satellite were also employed for cloud height comparison with MODIS. Comparisons of MODIS and MISR cloud height data indicate remarkable agreement which is encouraging for the possibility of incorporating MODIS cloud height in the MOPITT cloud detection scheme. Statistics of the global assessment of the potential use of MODIS cloud height shows that MOPITT data increases significantly when cloud heights less than 2 km in height are incorporated in the retrievals. However quality indices should be defined and produced to ensure sufficient retrieval quality.
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