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CNRS Laboratoire de Meteorologie Physique - Laboratoire de Glaciologie
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An integrating nephelometer (TSI 3563) to determine aerosol back scattering coefficient. These measurements include the aerosol back scattering coefficient at three wavelengths (450, 550 and 700 nm) since 2006.
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Measurements of aerosol-size distributions at the NCO-P (or Nepal Climate Observatory at Pyramid) site were continuously performed by using the scanning mobility particles sizer (SMPS) technique. The dataset is available at http://www.rrcap.unep.org/abc/data/abc/index.html.
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Aerosol total and back scattering are derived by an integrating nephelometer (model TSI 3563),at three wavelengths (450, 550 and 700 nm) installed in 25 March 2006.
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At the Nepal Climate Observatory - Pyramid, aerosol total and back scattering coefficients at three wavelengths (450, 550 and 700 nm) are derived by an integrating nephelometer (model TSI 3563). The integrating nephelometer is a high-sensitivity device capable of measuring the scattering properties of aerosol particles. The nephelometer measures the light scattered by the aerosol and then subtracting light scattered by the walls of the measurement chamber, light scattered by the gas, and electronic noise inherent in the detectors.
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A three wavelength integrating nephelometer to determine aerosol total and back scattering coefficients.
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At the Nepal Climate Observatory - Pyramid, aerosol total and back scattering coefficients at three wavelengths (450, 550 and 700 nm) are derived by an integrating nephelometer (model TSI 3563).
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At the Nepal Climate Observatory - Pyramid, aerosol total and back scattering coefficients at three wavelengths (450, 550 and 700 nm) are derived by an integrating nephelometer (model TSI 3563).
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The integrating nephelometer (model TSI 3563) is a high-sensitivity device capable of measuring the scattering properties of aerosol particles. The nephelometer measures the light scattered by the aerosol and then subtracting light scattered by the walls of the measurement chamber, light scattered by the gas, and electronic noise inherent in the detectors.
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Measurements of aerosol-size distributions at the NCO-P (or Nepal Climate Observatory at Pyramid) site were continuously performed by using the scanning mobility particles sizer (SMPS) technique.
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Measurements of aerosol-size distributions at the NCO-P (or Nepal Climate Observatory at Pyramid) site were continuously performed by using the scanning mobility particles sizer (SMPS) technique.