2011
DOI: 10.5194/acp-11-1659-2011
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Assessing the regional surface influence through Backward Lagrangian Dispersion Models for aircraft CO<sub>2</sub> vertical profiles observations in NE Spain

Abstract: Abstract. In this study the differences in the measured atmospheric CO 2 mixing ratio at three aircraft profiling sites in NE Spain separated by 60 km are analyzed in regard to

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Cited by 3 publications
(4 citation statements)
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“…Fluxes of CH 4 obtained by this analysis have been compared with GHGs emission inventories results, such as the EDGAR map (EDGAR [13]) and with results obtained in past studies using the same RTM method. Footprint analysis performed with FLEXPART model v8.2 (Stohl et al [14]; Font et al [15]) at 300m a.g.l. and with ECMWF data were used in order to calculate the catchment areas of methane for episode included in the RTM analysis.…”
Section: Introductionmentioning
confidence: 99%
“…Fluxes of CH 4 obtained by this analysis have been compared with GHGs emission inventories results, such as the EDGAR map (EDGAR [13]) and with results obtained in past studies using the same RTM method. Footprint analysis performed with FLEXPART model v8.2 (Stohl et al [14]; Font et al [15]) at 300m a.g.l. and with ECMWF data were used in order to calculate the catchment areas of methane for episode included in the RTM analysis.…”
Section: Introductionmentioning
confidence: 99%
“…Previous studies demonstrated that with aircraft profiling measurements at a certain time interval (e.g., morning and afternoon), surface flux can be calculated as temporal change of CO 2 amount in the CBL unless advective contribution from a distant source is large [ Shashkov et al ., ]. Such profile measurements at different time frames are not available in our data over DEL; however, it is inferred that CO 2 variation in the CBL, which is represented by Δ V CO2 in this study, is under dominant influence of local to regional scale (10 1 –10 3 km) surface fluxes [ Shashkov et al ., ; Font et al ., ]. In our present study, the Δ V CO2 variability in the CBL is influenced by two major local fluxes: the urban emission from Delhi and the agricultural ecosystem exchange around Delhi.…”
Section: Resultsmentioning
confidence: 71%
“…The unique vertical profiles obtained over Delhi constitute a good example. One possible future application is to quantify CO 2 emissions from worldwide megacities by optimizing emission estimates with the CONTRAIL CO 2 data over airports, since variations of atmospheric trace gases in the CBL are dominantly caused by local to regional fluxes as shown in this study and previously [ Font et al ., ; Boschetti et al ., ].…”
Section: Resultsmentioning
confidence: 99%
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