dc.contributor.author
Docter, Nicole
dc.contributor.author
Hünerbein, Anja
dc.contributor.author
Donovan, David P.
dc.contributor.author
Preusker, Rene
dc.contributor.author
Fischer, Jürgen
dc.contributor.author
Meirink, Jan Fokke
dc.contributor.author
Stammes, Piet
dc.contributor.author
Eisinger, Michael
dc.date.accessioned
2024-05-06T10:42:06Z
dc.date.available
2024-05-06T10:42:06Z
dc.identifier.uri
https://refubium.fu-berlin.de/handle/fub188/43445
dc.identifier.uri
http://dx.doi.org/10.17169/refubium-43162
dc.description.abstract
The Multi-Spectral Imager (MSI) on board the Earth Cloud, Aerosol and Radiation Explorer (EarthCARE) will provide horizontal information about aerosols and clouds. These measurements are needed to extend vertical cloud and aerosol property information, which is obtained from EarthCARE's active sensors, in order to obtain a full three-dimensional view of cloud and aerosol conditions. Mesoscale weather systems, in particular, will be characterized. The discovery of a non-compliance of the MSI visible–near-infrared–shortwave infrared (VNS) camera’s visible (VIS) and shortwave infrared (SWIR1) channels regarding a spectral central wavelength (CWVL) shift across-track of up to 14 nm (VIS) and 20 nm (SWIR1) led to the need for an analysis regarding its impact on MSI Level-2A aerosol and cloud products. A significant influence of the spectral misalignment effect (SMILE) on MSI retrievals is identified due to the spectral variation in gas absorption, surface reflectance, and aerosol and cloud properties within the spectral ranges of these MSI bands. For example, the VIS channel is positioned in close proximity to the red edge of green vegetation and is impacted by residual absorption of water vapor and ozone. Small central wavelength variations introduce uncertainties due to the rapid change in surface reflectance for conditions with low optical thickness. The present central wavelength shift in the VIS towards shorter wavelengths than at nadir introduces a relative error in transmission of up to 3.3 % due to the increasing influence of water vapor and ozone absorption. We found relative errors in the top-of-atmosphere (TOA) signal due to the SMILE of up to 30 % for low optical thickness over a land surface in that band. Since the magnitude of the impact strongly depends on the underlying surface and atmospheric conditions, we conclude that accounting for the SMILE in Level-2 retrievals or correcting the Level-1 signal will improve MSI aerosol and cloud product quality.
en
dc.format.extent
13 Seiten
dc.rights
This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit https://creativecommons.org/licenses/by/4.0/
dc.rights.uri
https://creativecommons.org/licenses/by/4.0/
dc.subject
spectral misalignment effect
en
dc.subject.ddc
500 Naturwissenschaften und Mathematik::550 Geowissenschaften, Geologie::550 Geowissenschaften
dc.title
Assessment of the spectral misalignment effect (SMILE) on EarthCARE's Multi-Spectral Imager aerosol and cloud property retrievals
dc.type
Wissenschaftlicher Artikel
dc.date.updated
2024-04-27T05:57:04Z
dcterms.bibliographicCitation.doi
10.5194/amt-17-2507-2024
dcterms.bibliographicCitation.journaltitle
Atmospheric Measurement Techniques
dcterms.bibliographicCitation.number
8
dcterms.bibliographicCitation.originalpublishername
Copernicus Publications
dcterms.bibliographicCitation.originalpublisherplace
Göttingen, Germany
dcterms.bibliographicCitation.pagestart
2507
dcterms.bibliographicCitation.pageend
2519
dcterms.bibliographicCitation.volume
17
dcterms.bibliographicCitation.url
https://doi.org/10.5194/amt-17-2507-2024
refubium.affiliation
Geowissenschaften
refubium.affiliation.other
Institut für Meteorologie
refubium.note.author
Die Publikation wurde aus Open Access Publikationsgeldern der Freien Universität Berlin finanziert
de
refubium.resourceType.isindependentpub
no
dcterms.accessRights.openaire
open access
dcterms.isPartOf.eissn
1867-8548
refubium.resourceType.provider
DeepGreen