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7 results for “Absorbing aerosol”

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zenodo44/100

Spectral Effects of Absorbing Aerosols on Backscattered UV Radiation

<p>Satellite measurements of backscattered UV radiation are sensitive to the presence of UV-absorbing aerosols in the atmosphere. These measurements are commonly used for determining the concentration of atmospheric trace gases such as O<sub>3</sub>, SO<sub>2</sub>, and H<sub>2</sub>CO.</p> <p>The theoretical results in this dataset describe the effects of UV-absorbing mineral dust and carbonaceous smoke aerosols on these backscatter satellite measurements between 300-400 nm. The information provided is independent of any specific trace gas retrieval algorithm and does not require detailed a priori knowledge of aerosol and surface properties.</p> <p>The results are derived from the analysis of the radiative transfer model simulations performed with the optical property data used in the Ozone Monitoring Instrument (OMI) UV aerosol retrieval algorithm, OMAERUV. Results from this algorithm have been validated with Aerosol Robotic Network (AERONET) observations (Jethva &amp; Torres, 2011; Torres et al., 2018).</p> <p>This dataset is associated with the following publication:</p> <p>Jethva, H., Haffner, D.,&nbsp;Bhartia, P. K., &amp; Torres, O. (2022). Estimating Spectral Effects of Absorbing Aerosols on Backscattered UV Radiation, Earth Space Sci., Accepted.</p>

opencc-by-4.0Sep 2022View details →
zenodo36/100

Diurnal cycle of the semi-direct effect from a persistent absorbing aerosol layer over marine stratocumulus in large-eddy simulations: supporting dataset

<p>Relevant data for reproducing figures and tables from Herbert et al.,&nbsp;2020, Atmospheric Chemistry and Physics: &quot;Diurnal cycle of the semi-direct effect from a persistent absorbing aerosol layer over marine stratocumulus in large-eddy simulations&quot;.</p> <p>The tar file contains the relevant netcdf files that contain simulation output from the MET&nbsp;Office large eddy model (LEM). Each netcdf file corresponds to a single model setup and experiment - details of which can be found within the published manuscript.&nbsp;Information concerning&nbsp;the LEM, and details on how to obtain access to the code,&nbsp;can be found at&nbsp;http://appconv.metoffice.com/LEM/index.html.</p> <p>The file &#39;relevant_information.pdf&#39; contains two tables. The first provides the names of each netcdf file that was used to produce each figure in the manuscript. The second provides the metadata for the netcdf variables that were used to produce the figures and tables.</p> <p>The netcdf filename provides information on the experiment setup as follows:</p> <p>run-identifier-number _ length-of-run _ AOD-of-layer _ GAP-between-cloud-and-layer _ THICKNESS-of-layer _ &#39;bigarray&#39; _ special-setups-for-sensitivity-experiments</p> <p>For example,&nbsp;r1360_8day_transient_aod02_0dz_250th_bigarray_nodrizz is run number r1360, simulating 8 days, with the aerosol layer properties AOD=0.2, cloud-to-aerosol gap of 0m, layer thickness of 250m, in the sensitivity setup where precipitation has been switched off.</p>

opencc-by-4.0Jan 2020View details →
zenodo36/100

Absorbing Aerosol Optical Central Height (AOCH) retrieved from TROPOMI with UIowa's AOCH-O2AB algorithm

<p>Absorbing Aerosol Optical Centroid Height (AOCH) retrieved from TROPOMI with UIowa&rsquo;s AOCH-O<sub>2</sub>AB algorithm. Dataset for analyzing dust and smoke cases over Asia during 2021-2023.</p> <p>More information about this dataset can be found in:&nbsp;</p> <p>Chen, X., Wang, J., Xu, X. G., Zhou, M., Zhang, H. X., Garcia, L. C., Colarco, P. R., Janz, S. J., Yorks, J., McGill, M., Reid, J. S., de Graaf, M., and Kondragunta, S.: First retrieval of absorbing aerosol height over dark target using TROPOMI oxygen B band: Algorithm development and application for surface particulate matter estimates, Remote Sensing of Environment, 265, 18,&nbsp;<a href="https://doi.org/10.1016/j.rse.2021.112674">https://doi.org/10.1016/j.rse.2021.112674</a>, 2021.</p>

opencc-by-4.0Dec 2023View details →
dryad36/100

Fractional change of scattering and absorbing aerosols contributes to Northern Hemisphere Hadley Circulation expansion

Open the record for dataset details and reuse information.

publicNov 2024View details →
nasa28/100

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.

restrictednotspecifiedApr 2025View details →
zenodo24/100

Supporting data for ''Strong control of effective radiative forcing by the spatial pattern of absorbing aerosol"

<p>Supporting data for our Nature Climate Change study. We provide a subset of:</p> <p>&nbsp;- 2D, monthly fields</p> <p>&nbsp;- time-averaged 3D fields</p> <p>&nbsp;- a numpy/text file which is needed to identify the different aerosol plume experiments</p> <p>&nbsp;</p> <p>Please see the README for more information on the outputs, accessing specific plume experiments,&nbsp;and the&nbsp;data post-processing we conducted.</p>

opencc-by-4.0Apr 2022View details →
zenodo24/100

Code & Data for Ying et al. Fractional change of scattering and absorbing aerosols contributes to Northern Hemisphere Hadley Circulation expansion

<p>The attached files contain data used for the figures in the main text of Ying et al. Fractional change of scattering and absorbing aerosols contributes to Northern Hemisphere Hadley Circulation expansion.</p> <p>Data includes the edge and strength of Hadley Circulation simulated by CESM as well as derived from ERA5 and MERRA-2 based on multiple matrix, AOD and SSA as well as zonal-mean meteorological fields differences between CESM simulations, and data derived from CMIP6 hist-aer simulations.</p> <p>Code includes the matlab function to solve the Kuo-Eliassen equation and calculate linear trends based on Sen's Slope and significant test based on Mann-Kendall test.</p>

opencc-by-4.0Aug 2024View details →

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