Cloud optical thickness, cloud particle effective radius, and effective snow grain size retrieved from airborne spectral reflectivity measurements on 2012-04-29 (VERDI 2012) over the Beaufort Sea ...
SMART uses two separte spectrometer to cover the solar spectral range. To overcome differences in the timing of both components, a running mean (5 sec) was applied to the reflectivity time series in the retrieval algorithm. Therefore, cloud optical thickness, cloud particle size and snow grain size...
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ftdatacite:10.1594/pangaea.882978 2023-10-01T03:54:08+02:00 Cloud optical thickness, cloud particle effective radius, and effective snow grain size retrieved from airborne spectral reflectivity measurements on 2012-04-29 (VERDI 2012) over the Beaufort Sea ... Ehrlich, André Bierwirth, Eike Istomina, Larysa Wendisch, Manfred 2017 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.882978 https://doi.pangaea.de/10.1594/PANGAEA.882978 en eng PANGAEA https://store.pangaea.de/Publications/EhrlichA-etal_2017/Snow_Cloud_Retrieval_120429.na https://dx.doi.org/10.1594/pangaea.882979 https://dx.doi.org/10.5194/amt-10-3215-2017 https://store.pangaea.de/Publications/EhrlichA-etal_2017/Snow_Cloud_Retrieval_120429.na Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Time in seconds DATE/TIME LATITUDE LONGITUDE Height above sea level Solar zenith angle Reflectance Flag Cloud optical thickness Cloud particle radius Snow grain size Error Aircraft Spectral modular airborne radiation measurement system SMART Moderate-resolution imaging spectroradiometer MODIS VERDI_2012 POLAR 5 Arctic Amplification AC3 Dataset dataset 2017 ftdatacite https://doi.org/10.1594/pangaea.88297810.1594/pangaea.88297910.5194/amt-10-3215-2017 2023-09-04T14:52:34Z SMART uses two separte spectrometer to cover the solar spectral range. To overcome differences in the timing of both components, a running mean (5 sec) was applied to the reflectivity time series in the retrieval algorithm. Therefore, cloud optical thickness, cloud particle size and snow grain size are smoothed as well while the reflectivity time series are provided as raw data without running mean.MODIS cloud products were selected and averaged for an area of 5x5 pixel with the aircraft observations centered in this area.tau_MODIS: MODIS cloud product Collection 6: Cloud Optical Thickness (dimensionless) two-channel retrieval using band 7(2.1 µm) and band 6(1.6 µm) from best points: not failed in any way, not marked for clear sky restoraltau_MODIS_16: MODIS cloud product Collection 6: Cloud Optical Thickness (dimensionless) two-channel retrieval using band 7(2.1 µm) and either band 1(0.65 µm) , 2(0.86 µm) , or 5(1.2 µm) (specified in Quality_Assurance_1km) from best points: not failed in any way, not marked ... Dataset Arctic Beaufort Sea DataCite Metadata Store (German National Library of Science and Technology) Arctic |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Time in seconds DATE/TIME LATITUDE LONGITUDE Height above sea level Solar zenith angle Reflectance Flag Cloud optical thickness Cloud particle radius Snow grain size Error Aircraft Spectral modular airborne radiation measurement system SMART Moderate-resolution imaging spectroradiometer MODIS VERDI_2012 POLAR 5 Arctic Amplification AC3 |
spellingShingle |
Time in seconds DATE/TIME LATITUDE LONGITUDE Height above sea level Solar zenith angle Reflectance Flag Cloud optical thickness Cloud particle radius Snow grain size Error Aircraft Spectral modular airborne radiation measurement system SMART Moderate-resolution imaging spectroradiometer MODIS VERDI_2012 POLAR 5 Arctic Amplification AC3 Ehrlich, André Bierwirth, Eike Istomina, Larysa Wendisch, Manfred Cloud optical thickness, cloud particle effective radius, and effective snow grain size retrieved from airborne spectral reflectivity measurements on 2012-04-29 (VERDI 2012) over the Beaufort Sea ... |
topic_facet |
Time in seconds DATE/TIME LATITUDE LONGITUDE Height above sea level Solar zenith angle Reflectance Flag Cloud optical thickness Cloud particle radius Snow grain size Error Aircraft Spectral modular airborne radiation measurement system SMART Moderate-resolution imaging spectroradiometer MODIS VERDI_2012 POLAR 5 Arctic Amplification AC3 |
description |
SMART uses two separte spectrometer to cover the solar spectral range. To overcome differences in the timing of both components, a running mean (5 sec) was applied to the reflectivity time series in the retrieval algorithm. Therefore, cloud optical thickness, cloud particle size and snow grain size are smoothed as well while the reflectivity time series are provided as raw data without running mean.MODIS cloud products were selected and averaged for an area of 5x5 pixel with the aircraft observations centered in this area.tau_MODIS: MODIS cloud product Collection 6: Cloud Optical Thickness (dimensionless) two-channel retrieval using band 7(2.1 µm) and band 6(1.6 µm) from best points: not failed in any way, not marked for clear sky restoraltau_MODIS_16: MODIS cloud product Collection 6: Cloud Optical Thickness (dimensionless) two-channel retrieval using band 7(2.1 µm) and either band 1(0.65 µm) , 2(0.86 µm) , or 5(1.2 µm) (specified in Quality_Assurance_1km) from best points: not failed in any way, not marked ... |
format |
Dataset |
author |
Ehrlich, André Bierwirth, Eike Istomina, Larysa Wendisch, Manfred |
author_facet |
Ehrlich, André Bierwirth, Eike Istomina, Larysa Wendisch, Manfred |
author_sort |
Ehrlich, André |
title |
Cloud optical thickness, cloud particle effective radius, and effective snow grain size retrieved from airborne spectral reflectivity measurements on 2012-04-29 (VERDI 2012) over the Beaufort Sea ... |
title_short |
Cloud optical thickness, cloud particle effective radius, and effective snow grain size retrieved from airborne spectral reflectivity measurements on 2012-04-29 (VERDI 2012) over the Beaufort Sea ... |
title_full |
Cloud optical thickness, cloud particle effective radius, and effective snow grain size retrieved from airborne spectral reflectivity measurements on 2012-04-29 (VERDI 2012) over the Beaufort Sea ... |
title_fullStr |
Cloud optical thickness, cloud particle effective radius, and effective snow grain size retrieved from airborne spectral reflectivity measurements on 2012-04-29 (VERDI 2012) over the Beaufort Sea ... |
title_full_unstemmed |
Cloud optical thickness, cloud particle effective radius, and effective snow grain size retrieved from airborne spectral reflectivity measurements on 2012-04-29 (VERDI 2012) over the Beaufort Sea ... |
title_sort |
cloud optical thickness, cloud particle effective radius, and effective snow grain size retrieved from airborne spectral reflectivity measurements on 2012-04-29 (verdi 2012) over the beaufort sea ... |
publisher |
PANGAEA |
publishDate |
2017 |
url |
https://dx.doi.org/10.1594/pangaea.882978 https://doi.pangaea.de/10.1594/PANGAEA.882978 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Beaufort Sea |
genre_facet |
Arctic Beaufort Sea |
op_relation |
https://store.pangaea.de/Publications/EhrlichA-etal_2017/Snow_Cloud_Retrieval_120429.na https://dx.doi.org/10.1594/pangaea.882979 https://dx.doi.org/10.5194/amt-10-3215-2017 https://store.pangaea.de/Publications/EhrlichA-etal_2017/Snow_Cloud_Retrieval_120429.na |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.88297810.1594/pangaea.88297910.5194/amt-10-3215-2017 |
_version_ |
1778521513923706880 |