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2013
DOI: 10.1016/j.atmosenv.2013.05.051
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Emissions estimation from satellite retrievals: A review of current capability

Abstract: h i g h l i g h t s Comprehensive review of studies of satellite data applied to emissions estimation. Overview of retrievals for eight major tropospheric air pollutants. Techniques to enhance the usefulness of satellite retrievals. Identification of target source categories for satellite data application. Recommendations on ways to improve the usability of satellite retrievals.

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Cited by 349 publications
(217 citation statements)
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References 332 publications
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“…[7,23]), provided real time NO 2 forecasts are available at TEMPO processing time. The resultant TEMPO NO 2 will offer a powerful constraint on NO x emissions [72,100].…”
Section: Trace Gas Column Measurementsmentioning
confidence: 99%
“…[7,23]), provided real time NO 2 forecasts are available at TEMPO processing time. The resultant TEMPO NO 2 will offer a powerful constraint on NO x emissions [72,100].…”
Section: Trace Gas Column Measurementsmentioning
confidence: 99%
“…NO x emissions have been assessed using satellite measurements of integrated NO 2 column concentrations (see review by Streets et al, 2013). These assessments require that a chemical transport model be used to transform emissions into the quantities observed in the measurement (NO 2 column concentrations), but the approach has been widely used to estimate trends in emissions.…”
Section: Zavala Et Al 2015amentioning
confidence: 99%
“…The association of human activity with the presence of tropospheric aerosols is well established from both ground-based (Jimenez et al 2009;Yoon et al 2016) and space-based observations (Streets et al 2013;Yoon et al 2014;He et al 2016;McLinden et al 2016). Yet, quantification of the RF of climate due to tropospheric aerosols continues to pose a scientific challenge due to the inability to precisely define numerical values of both the direct modulation of RF by anthropogenic aerosols (Myhre 2009;Kahn 2012;Bond et al 2013) and the changes in RF driven by the effect of aerosols on clouds (Morgan et al 2006;Carslaw et al 2013).…”
Section: Aerosolsmentioning
confidence: 99%
“…As a consequence, movements are underway throughout the world to reduce both the direct emission of aerosols as well as the emission of aerosol precursors. Reductions in the abundance of tropospheric aerosols and aerosol precursors, in response to air quality legislation motivated by public health concerns, have been readily observed by space-borne 33 Atmospheric abundance of NF 3 peaked at 0.0012 ppb in late 2011 (Arnold et al 2012) and radiative efficiency is 0.2 W m −2 ppb −1 (Table 8. instrumentation throughout the world (Streets et al 2013;Yoon et al 2014;He et al 2016). As such, the climate system is presently transitioning from an era where the cooling of climate due to aerosols may have had close to comparable strength as GHG induced warming to an era where the radiative warming due to GHGs will dominate aerosol cooling (Smith and Bond 2014).…”
Section: Aerosolsmentioning
confidence: 99%