Academic Journal

Assessment of the spectral misalignment effect (SMILE) on EarthCARE's Multi-Spectral Imager aerosol and cloud property retrievals

التفاصيل البيبلوغرافية
العنوان: Assessment of the spectral misalignment effect (SMILE) on EarthCARE's Multi-Spectral Imager aerosol and cloud property retrievals
المؤلفون: N. Docter, A. Hünerbein, D. P. Donovan, R. Preusker, J. Fischer, J. F. Meirink, P. Stammes, M. Eisinger
المصدر: Atmospheric Measurement Techniques, Vol 17, Pp 2507-2519 (2024)
بيانات النشر: Copernicus Publications, 2024.
سنة النشر: 2024
المجموعة: LCC:Environmental engineering
LCC:Earthwork. Foundations
مصطلحات موضوعية: Environmental engineering, TA170-171, Earthwork. Foundations, TA715-787
الوصف: 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.
نوع الوثيقة: article
وصف الملف: electronic resource
اللغة: English
تدمد: 1867-1381
1867-8548
Relation: https://amt.copernicus.org/articles/17/2507/2024/amt-17-2507-2024.pdf; https://doaj.org/toc/1867-1381; https://doaj.org/toc/1867-8548
DOI: 10.5194/amt-17-2507-2024
URL الوصول: https://doaj.org/article/95cae0a1f37842c6bcce2e7cc1310b01
رقم الانضمام: edsdoj.95cae0a1f37842c6bcce2e7cc1310b01
قاعدة البيانات: Directory of Open Access Journals
الوصف
تدمد:18671381
18678548
DOI:10.5194/amt-17-2507-2024