Atmospheric aerosols directly affect climate by scattering and absorbing radiation. The magnitude of the impact is dependent upon the wavelength of light, but is often estimated near 550 nm. When light scattering and absorption by aerosols is approximated, the wavelength dependence of the refractive index for specific components is lost. As a result, climate models would have inherent uncertainties for aerosol contributions to radiative forcing when considering the entire solar spectrum. An aerosol extinction differential optical absorption spectrometer has been developed to directly measure aerosol extinction at mid-ultraviolet to near infrared wavelengths. The instrument consists of a spectrometer coupled to a closed White-type multi-pass ...
Abstract. Aerosol intensive optical properties like the Ångström exponents for aerosol light extinct...
The wavelength-dependence of aerosol absorption optical depth (AAOD) is generally represented in ter...
Deriving absorption coefficients from Aethalometer attenuation data requires different corrections t...
Atmospheric aerosols directly affect climate by scattering and absorbing radiation. The magnitude of...
Atmospheric aerosols directly affect climate by scattering and absorbing radiation. The magnitude of...
Atmospheric aerosols directly affect climate by scattering and absorbing incident solar radiation. T...
Atmospheric aerosols directly affect climate by scattering and absorbing incident solar radiation. T...
Atmospheric aerosols directly affect climate by scattering and absorbing incident solar radiation. T...
International audienceWe have determined the solar spectral absorption optical depth of atmospheric ...
International audienceWe have determined the solar spectral absorption optical depth of atmospheric ...
Atmospheric aerosols play an important part in the Earth's energy budget by scattering and absorbing...
Aerosols influence the Earth's radiative budget by scattering and absorbing incoming solar radiation...
Atmospheric aerosol absorption properties play a key role on the Earth radiation balance. Although ...
The role of atmospheric aerosols in earth’s radiative balance is crucial. A thorough knowledge about...
The interaction between aerosols and sun light plays an important role in the radiative balance of E...
Abstract. Aerosol intensive optical properties like the Ångström exponents for aerosol light extinct...
The wavelength-dependence of aerosol absorption optical depth (AAOD) is generally represented in ter...
Deriving absorption coefficients from Aethalometer attenuation data requires different corrections t...
Atmospheric aerosols directly affect climate by scattering and absorbing radiation. The magnitude of...
Atmospheric aerosols directly affect climate by scattering and absorbing radiation. The magnitude of...
Atmospheric aerosols directly affect climate by scattering and absorbing incident solar radiation. T...
Atmospheric aerosols directly affect climate by scattering and absorbing incident solar radiation. T...
Atmospheric aerosols directly affect climate by scattering and absorbing incident solar radiation. T...
International audienceWe have determined the solar spectral absorption optical depth of atmospheric ...
International audienceWe have determined the solar spectral absorption optical depth of atmospheric ...
Atmospheric aerosols play an important part in the Earth's energy budget by scattering and absorbing...
Aerosols influence the Earth's radiative budget by scattering and absorbing incoming solar radiation...
Atmospheric aerosol absorption properties play a key role on the Earth radiation balance. Although ...
The role of atmospheric aerosols in earth’s radiative balance is crucial. A thorough knowledge about...
The interaction between aerosols and sun light plays an important role in the radiative balance of E...
Abstract. Aerosol intensive optical properties like the Ångström exponents for aerosol light extinct...
The wavelength-dependence of aerosol absorption optical depth (AAOD) is generally represented in ter...
Deriving absorption coefficients from Aethalometer attenuation data requires different corrections t...