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2 results for “Light absorbing particles”
Global climatology of light-absorbing particle deposition on snow
<p><strong>Description</strong></p> <p>Light-absorbing particles (LAPs) deposited at the snow surface significantly reduce its albedo and strongly affect the snow melt dynamics. To better quantify the spatial variability of LAP deposition on snow, Gaillard et al. (2024) have generated a global climatology of LAP deposition on snow. It combines a climatological dataset of LAP deposition rates (Black Carbon (BC) and dust) over the period 1979-2015 (Zhao et al., 2018) with a global dataset of snow cover (Romanov, 2017) to obtain a climatology of LAP deposition rates on snow. The climatology is accompanied by the 25th and 75th percentiles of LAP deposition rates on snow to quantify the inter-annual variability of LAP deposition on snow. </p> <p>The data are distributed in a NetCDF file (<em>climato_tot_publish_v2.nc</em>). More details about the dataset and the file format are given in the file <em>readme_climatology_v2.pdf</em>. </p> <p> </p>
ATom: Light-Absorbing Metallic Aerosols, Single Particle Soot Photometer, 2016-2018
This dataset provides mass mixing ratios and number density of light-absorbing metallic aerosols (LAM) in the size range 180-1290 nm obtained with the NOAA Single Particle Soot Photometer (SP2) during the four deployments of the NASA Atmospheric Tomography (ATom) airborne mission from 2016-2018. The NOAA SP2 detects light absorbing aerosols, such as black carbon (BC), via laser-induced incandescence to provide real-time in situ quantification of refractory aerosol mass and number density. The percent of LAM aerosols attributed to anthropogenic iron oxides (FeOx) by mass is also provided.
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