Cloud top heights and aerosol layer properties from EarthCARE lidar observations: the A-CTH and A-ALD products
<p>The high-spectral-resolution Atmospheric Lidar (ATLID) on the Earth Cloud, Aerosol and Radiation Explorer (EarthCARE) provides vertically resolved information on aerosols and clouds with unprecedented accuracy. Together with the Cloud Profiling Radar (CPR), the Multi-Spectral Imager (MSI),...
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2023-09-01
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| Series: | Atmospheric Measurement Techniques |
| Online Access: | https://amt.copernicus.org/articles/16/4031/2023/amt-16-4031-2023.pdf |
| _version_ | 1797690598533103616 |
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| author | U. Wandinger M. Haarig H. Baars D. Donovan G.-J. van Zadelhoff |
| author_facet | U. Wandinger M. Haarig H. Baars D. Donovan G.-J. van Zadelhoff |
| author_sort | U. Wandinger |
| collection | DOAJ |
| description | <p>The high-spectral-resolution Atmospheric Lidar (ATLID) on the Earth Cloud, Aerosol and Radiation Explorer (EarthCARE)
provides vertically resolved information on aerosols and clouds with unprecedented accuracy. Together with the Cloud Profiling Radar (CPR), the Multi-Spectral Imager (MSI), and the Broad-Band Radiometer (BBR) on the same platform, it allows for a new synergistic view on atmospheric processes related to the interaction of aerosols, clouds, precipitation, and radiation at the global scale.
This paper describes the algorithms for the determination of cloud top height and aerosol layer information from ATLID Level 1b (L1b) and Level 2a (L2a) input data. The ATLID L2a Cloud Top Height (A-CTH) and Aerosol Layer Descriptor (A-ALD) products are developed to ensure the provision of atmospheric layer products in continuation of the heritage from the Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO). Moreover, the products serve as input for synergistic algorithms that make use of data from ATLID and MSI. Therefore, the products are provided on the EarthCARE joint standard grid (JSG).
A wavelet covariance transform (WCT) method with flexible thresholds is applied to determine layer boundaries from the ATLID Mie co-polar signal.
Strong features detected with a horizontal resolution of 1 JSG pixel (approximately 1 km) or 11 JSG pixels are classified as thick or thin clouds, respectively. The top height of the uppermost cloud layer together with information on cloud layering are stored in the A-CTH product for further use in the generation of the ATLID-MSI Cloud Top Height (AM-CTH) synergy product. Aerosol layers are detected as weaker features at a resolution of 11 JSG pixels. Layer-mean optical properties are calculated from the ATLID L2a Extinction, Backscatter and Depolarization (A-EBD) product and stored in the A-ALD product, which also contains the aerosol optical thickness (AOT) of each layer, the stratospheric AOT, and the AOT of the entire atmospheric column. The latter parameter is used to produce the synergistic ATLID-MSI Aerosol Column Descriptor (AM-ACD) later in the processing chain. Several quality criteria are applied in the generation of A-CTH and A-ALD, and respective information is stored in the products. The functionality and performance of the algorithms are demonstrated by applying them to common EarthCARE test scenes. Conclusions are drawn for the application to real-world data and the validation of the products after the launch of EarthCARE.</p> |
| first_indexed | 2024-03-12T02:01:36Z |
| format | Article |
| id | doaj.art-c59d4523fd1044078f3cd265cbd41ff4 |
| institution | Directory Open Access Journal |
| issn | 1867-1381 1867-8548 |
| language | English |
| last_indexed | 2024-03-12T02:01:36Z |
| publishDate | 2023-09-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | Atmospheric Measurement Techniques |
| spelling | doaj.art-c59d4523fd1044078f3cd265cbd41ff42023-09-07T12:47:09ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482023-09-01164031405210.5194/amt-16-4031-2023Cloud top heights and aerosol layer properties from EarthCARE lidar observations: the A-CTH and A-ALD productsU. Wandinger0M. Haarig1H. Baars2D. Donovan3G.-J. van Zadelhoff4Leibniz Institute for Tropospheric Research, Leipzig, GermanyLeibniz Institute for Tropospheric Research, Leipzig, GermanyLeibniz Institute for Tropospheric Research, Leipzig, GermanyRoyal Netherlands Meteorological Institute, De Bilt, the NetherlandsRoyal Netherlands Meteorological Institute, De Bilt, the Netherlands<p>The high-spectral-resolution Atmospheric Lidar (ATLID) on the Earth Cloud, Aerosol and Radiation Explorer (EarthCARE) provides vertically resolved information on aerosols and clouds with unprecedented accuracy. Together with the Cloud Profiling Radar (CPR), the Multi-Spectral Imager (MSI), and the Broad-Band Radiometer (BBR) on the same platform, it allows for a new synergistic view on atmospheric processes related to the interaction of aerosols, clouds, precipitation, and radiation at the global scale. This paper describes the algorithms for the determination of cloud top height and aerosol layer information from ATLID Level 1b (L1b) and Level 2a (L2a) input data. The ATLID L2a Cloud Top Height (A-CTH) and Aerosol Layer Descriptor (A-ALD) products are developed to ensure the provision of atmospheric layer products in continuation of the heritage from the Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO). Moreover, the products serve as input for synergistic algorithms that make use of data from ATLID and MSI. Therefore, the products are provided on the EarthCARE joint standard grid (JSG). A wavelet covariance transform (WCT) method with flexible thresholds is applied to determine layer boundaries from the ATLID Mie co-polar signal. Strong features detected with a horizontal resolution of 1 JSG pixel (approximately 1 km) or 11 JSG pixels are classified as thick or thin clouds, respectively. The top height of the uppermost cloud layer together with information on cloud layering are stored in the A-CTH product for further use in the generation of the ATLID-MSI Cloud Top Height (AM-CTH) synergy product. Aerosol layers are detected as weaker features at a resolution of 11 JSG pixels. Layer-mean optical properties are calculated from the ATLID L2a Extinction, Backscatter and Depolarization (A-EBD) product and stored in the A-ALD product, which also contains the aerosol optical thickness (AOT) of each layer, the stratospheric AOT, and the AOT of the entire atmospheric column. The latter parameter is used to produce the synergistic ATLID-MSI Aerosol Column Descriptor (AM-ACD) later in the processing chain. Several quality criteria are applied in the generation of A-CTH and A-ALD, and respective information is stored in the products. The functionality and performance of the algorithms are demonstrated by applying them to common EarthCARE test scenes. Conclusions are drawn for the application to real-world data and the validation of the products after the launch of EarthCARE.</p>https://amt.copernicus.org/articles/16/4031/2023/amt-16-4031-2023.pdf |
| spellingShingle | U. Wandinger M. Haarig H. Baars D. Donovan G.-J. van Zadelhoff Cloud top heights and aerosol layer properties from EarthCARE lidar observations: the A-CTH and A-ALD products Atmospheric Measurement Techniques |
| title | Cloud top heights and aerosol layer properties from EarthCARE lidar observations: the A-CTH and A-ALD products |
| title_full | Cloud top heights and aerosol layer properties from EarthCARE lidar observations: the A-CTH and A-ALD products |
| title_fullStr | Cloud top heights and aerosol layer properties from EarthCARE lidar observations: the A-CTH and A-ALD products |
| title_full_unstemmed | Cloud top heights and aerosol layer properties from EarthCARE lidar observations: the A-CTH and A-ALD products |
| title_short | Cloud top heights and aerosol layer properties from EarthCARE lidar observations: the A-CTH and A-ALD products |
| title_sort | cloud top heights and aerosol layer properties from earthcare lidar observations the a cth and a ald products |
| url | https://amt.copernicus.org/articles/16/4031/2023/amt-16-4031-2023.pdf |
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