Titlebook: Aerosol Remote Sensing; Jacqueline Lenoble,Lorraine Remer,Didier Tanre Book 2013 Springer Verlag Berlin Heidelberg 2013 Aerosol optics.Det

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Introduction,l, they are abundant only after major volcanic eruptions, and they are mainly formed by gas-toparticle conversion. Although much less numerous than tropospheric aerosols, they may have an important impact, due to their long residence time and to their spread all around the globe.

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Passive shortwave remote sensing from the Ground,y of ground-based aerosol remote sensing networks, leaving the formalism of the retrievals and inversions to the previous chapters. Not described in detail in this book are methods to retrieve trace gas measurements using absorption features measured by groundbased sensors, even though the history o

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Introduction,days, or the well-defined plumes of particles that rise out of a burning fire. These particles can be either natural (lofted desert and soil dust, sea salt particles, volcanic emissions, wildfire smoke, biogenic emissions) or anthropogenic (industrial emissions, biomass burning for agriculture, or l

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History of passive remote sensing of aerosol from space,s of orbiting spacecraft in the early 1960s (Lazarev et al., 1987). From these photographs we could see for the first time the bluish haze that covered polluted regions and the dust emitted from deserts. The pictures showed that these hazes were inhomogeneous and temporally inconsistent, but quantit

Accommodation

Recent instruments and algorithms for passive shortwave remote sensing,in Chapter 7: occultation methods, dark target approaches, and spectral ultra-violet (UV) algorithms. Beginning in the 1970s, these techniques have been applied to instruments flown on a series of different satellite platforms and have produced important time series of aerosol parameters that span d