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Absorption of sunlight by dust as inferred from satellite and ground-based remote sensing

TLDR
In this paper, the authors used satellite spectral measurements and ground-based sky measurements to demonstrate that Saharan dust absorption of solar radiation is several times smaller than the current international standards.
Abstract
Dust absorption of solar radiation is not well known due to limitations in the accuracy of in situ measurements. Here we report two new independent remote sensing techniques that provide sensitive measurements of dust absorption. One uses satellite spectral measurements, the second ground based sky measurements. Both techniques demonstrate that Saharan dust absorption of solar radiation is several times smaller than the current international standards. For example, at wavelength of 0.64 µm the dust single scattering albedo is reported here as 0.97±0.02 rather than 0.87±0.04 in recent review.

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Global and regional climate changes due to black carbon

TL;DR: The second most important contribution to anthropogenic climate warming, after carbon dioxide emissions, was made by black carbon emissions as mentioned in this paper, which is an efficient absorbing agent of solar irradiation that is preferentially emitted in the tropics and can form atmospheric brown clouds in mixture with other aerosols.
Journal ArticleDOI

Variability of Absorption and Optical Properties of Key Aerosol Types Observed in Worldwide Locations

TL;DR: In this paper, the AERONET network of ground-based radiometers were used to remotely sense the aerosol absorption and other optical properties in several key locations, and the results showed robust differentiation in both the magnitude and spectral dependence of the absorption, a property driving aerosol climate forcing.
Journal ArticleDOI

Light Absorption by Carbonaceous Particles: An Investigative Review

TL;DR: The optical properties of light-absorbing, carbonaceous substance often called "soot", "black carbon", or "carbon black" have been the subject of some debate as discussed by the authors.
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A satellite view of aerosols in the climate system

TL;DR: Increases in aerosol concentration and changes in their composition, driven by industrialization and an expanding population, may adversely affect the Earth's climate and water supply.
References
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Journal ArticleDOI

Radiative forcing and climate response

TL;DR: This paper examined the sensitivity of a climate model to a wide range of radiative forcings, including changes of solar irradiance, atmospheric CO2, O3, CFCs, clouds, aerosols, surface albedo, and a "ghost" forcing introduced at arbitrary heights, latitudes, longitudes, seasons, and times of day.
Journal ArticleDOI

Accuracy assessments of aerosol optical properties retrieved from Aerosol Robotic Network (AERONET) Sun and sky radiance measurements

TL;DR: In this article, a new inversion concept for simultaneously retrieving aerosol size distribution, complex refractive index, and single scattering albedo from spectral measurements of direct and diffuse radiation was proposed.
Journal ArticleDOI

The influence on climate forcing of mineral aerosols from disturbed soils

TL;DR: In this article, the authors used a radiative transfer model embedded in a general circulation model to find that dust from disturbed soils causes a decrease of the net surface radiation forcing of about lWm-2, accompanied by increased atmospheric heating.
Journal ArticleDOI

Direct radiative forcing by anthropogenic airborne mineral aerosols

TL;DR: In this article, the global mean direct solar radiative forcing by anthropogenically generated mineral aerosols may be comparable to the direct solar forcing by other anthropogenic aerosols, and the net regional forcing by mineral aerosol can greatly exceed the regional forcing of sulfate aerosol and can even be comparable with the net forcing by clouds.
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Q1. What contributions have the authors mentioned in the paper "Absorption of sunlight by dust as inferred from satellite and gound-based remote sensing" ?

Here the authors report two new independent remote sensing techniques that provide sensitive measurements of dust absorption. For example, at wavelength of 0. 64 pm the dust single scattering albedo is reported here as 0. 97kO. 02 rather than 0. 8710. 04 in recent review.