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タイトルSpatial Variability of Trace Gases During DISCOVER-AQ: Planning for Geostationary Observations of Atmospheric Composition
本文(外部サイト)http://hdl.handle.net/2060/20150023592
著者(英)Diskin, G.; Weinheimer, A.; Fried, A.; Follette-Cook, Melanie B.; Crawford, J.; Appel, W.; Pickering, K.; Pfister, G.; Loughner, C.
著者所属(英)NASA Goddard Space Flight Center
発行日2015-12-14
言語eng
内容記述Results from an in-depth analysis of trace gas variability in MD indicated that the variability in this region was large enough to be observable by a TEMPO-like instrument. The variability observed in MD is relatively similar to the other three campaigns with a few exceptions: CO variability in CA was much higher than in the other regions; HCHO variability in CA and CO was much lower; MD showed the lowest variability in NO2All model simulations do a reasonable job simulating O3 variability. For CO, the CACO simulations largely under over estimate the variability in the observations. The variability in HCHO is underestimated for every campaign. NO2 variability is slightly overestimated in MD, more so in CO. The TX simulation underestimates the variability in each trace gas. This is most likely due to missing emissions sources (C. Loughner, manuscript in preparation).Future Work: Where reasonable, we will use these model outputs to further explore the resolvability from space of these key trace gases using analyses of tropospheric column amounts relative to satellite precision requirements, similar to Follette-Cook et al. (2015).
NASA分類Environment Pollution; Earth Resources and Remote Sensing
レポートNOA11G - 0132
GSFC-E-DAA-TN28873
権利Copyright, Distribution as joint owner in the copyright


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