| Literature DB >> 30393385 |
Alexander Marshak1, Jay Herman2, Adam Szabo1, Karin Blank1, Alexander Cede3, Simon Carn4, Igor Geogdzhayev5, Dong Huang6, Liang-Kang Huang6, Yuri Knyazikhin7, Matthew Kowalewski8, Nickolay Krotkov1, Alexei Lyapustin1, Richard McPeters1, Omar Torres1, Yuekui Yang1.
Abstract
The NOAA Deep Space Climate Observatory (DSCOVR) spacecraft was launched on February 11, 2015, and in June 2015 achieved its orbit at the first Lagrange point or L1, 1.5 million km from Earth towards the Sun. There are two NASA Earth observing instruments onboard: the Earth Polychromatic Imaging Camera (EPIC) and the National Institute of Standards and Technology Advanced Radiometer (NISTAR). The purpose of this paper is to describe various capabilities of the DSCOVR/EPIC instrument. EPIC views the entire sunlit Earth from sunrise to sunset at the backscattering direction (scattering angles between 168.5° and 175.5°) with 10 narrowband filters: 317, 325, 340, 388, 443, 552, 680, 688, 764 and 779 nm. We discuss a number of pre-processingsteps necessary for EPIC calibration including the geolocation algorithm and the radiometric calibration for each wavelength channel in terms of EPIC counts/second for conversion to reflectance units. The principal EPIC products are total ozone O3amount, scene reflectivity, erythemal irradiance, UV aerosol properties, sulfur dioxide SO2 for volcanic eruptions, surface spectral reflectance, vegetation properties, and cloud products including cloud height. Finally, we describe the observation of horizontally oriented ice crystals in clouds and the unexpected use of the O2 B-band absorption for vegetation properties.Entities:
Year: 2018 PMID: 30393385 PMCID: PMC6208167 DOI: 10.1175/BAMS-D-17-0223.1
Source DB: PubMed Journal: Bull Am Meteorol Soc ISSN: 0003-0007 Impact factor: 8.766