Aerosol Retrievals from DSCOVR Measurements
Abstract
Atmospheric aerosols play a central role in the Earth's radiative budget. Together with various greenhouse gases, aerosols represent the most significant anthropogenic forcing responsible for climate change. However, uncertainties about the origin and composition of aerosol particles, their size distribution, concentration, spatial and temporal variability, make climate change prediction challenging. In order to quantify the influence of aerosols on the Earth's climate and to better validate climate models, information about their global abundance, properties and height distribution are needed. We use measurements of the Oxygen A and B bands from the Earth Polychromatic Imaging Camera (EPIC) onboard the Deep Space Climate Observatory (DSCOVR) to retrieve aerosol parameters such as optical depth, height and effective radius. Aerosol retrievals are ill-posed because of the large spatial and temporal variability in their composition and vertical distribution. We compare several retrieval methods and determine the optimum technique for the retrieval algorithm.
Additional Information
© 2018 IEEE. Part of this work was performed at the Jet Propulsion Laboratory, California Institute of Technology. This work was funded by the NASA Earth Science U.S. Participating Investigator program.Additional details
- Eprint ID
- 90786
- Resolver ID
- CaltechAUTHORS:20181109-084430672
- NASA/JPL/Caltech
- Created
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2018-11-13Created from EPrint's datestamp field
- Updated
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2021-11-16Created from EPrint's last_modified field
- Caltech groups
- Astronomy Department, Division of Geological and Planetary Sciences