Cloudnet IWC during PS106 ...
The dataset contains daily nc-files of the Cloudnet ice water content during Polarstern cruise PS106 based on:- 35.5 GHz Cloud radar MIRA.The data is retrieved using the instrument synergystic approach Cloudnet (Illingworth, 2007 doi:10.1175/BAMS-88-6-883 ).This variable was calculated from the 35.5...
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Online Access: | https://dx.doi.org/10.1594/pangaea.919452 https://doi.pangaea.de/10.1594/PANGAEA.919452 |
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ftdatacite:10.1594/pangaea.919452 2024-09-09T19:25:45+00:00 Cloudnet IWC during PS106 ... Griesche, Hannes Seifert, Patric Engelmann, Ronny Radenz, Martin Bühl, Johannes 2020 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.919452 https://doi.pangaea.de/10.1594/PANGAEA.919452 en eng PANGAEA https://dx.doi.org/10.5194/amt-2019-434 https://dx.doi.org/10.1594/pangaea.900246 https://dx.doi.org/10.1175/jam2340.1 https://dx.doi.org/10.1175/bams-88-6-883 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Cloudnet OCEANET-ATMOSPHERE PASCAL Polarstern PS106 TROPOS Event label DATE/TIME File name File format File size Uniform resource locator/link to file Cloud Radar PS106/1 Arctic Amplification AC3 Dataset dataset 2020 ftdatacite https://doi.org/10.1594/pangaea.91945210.5194/amt-2019-43410.1594/pangaea.90024610.1175/jam2340.110.1175/bams-88-6-883 2024-07-03T13:11:36Z The dataset contains daily nc-files of the Cloudnet ice water content during Polarstern cruise PS106 based on:- 35.5 GHz Cloud radar MIRA.The data is retrieved using the instrument synergystic approach Cloudnet (Illingworth, 2007 doi:10.1175/BAMS-88-6-883 ).This variable was calculated from the 35.5-GHz radar reflectivity factor after correction for gaseous attenuation, and temperature taken from a forecast model, using the following empirical formula:log10(iwc[g m-3]) = 0.000242Z[dBZ]T[degC] + 0.0699Z[dBZ] + -0.0186T[degC] + -1.63 (Hogan, 2006 doi:10.1175/JAM2340.1 ).In this formula Z is taken to be defined such that all frequencies of radar would measure the same Z in Rayleigh scattering ice. However, the radar is more likely to have been calibrated such that all frequencies would measure the same Z in Rayleigh scattering liquid cloud at 0 degrees C. The measured Z is therefore multiplied by|K(liquid,0degC,35GHz)|^2/0.93 = 0.9441before applying this formula.The formula has been used where the ... : This is an updated version of this data set: https://doi.pangaea.de/10.1594/PANGAEA.900246 ... Dataset Arctic DataCite Arctic |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Cloudnet OCEANET-ATMOSPHERE PASCAL Polarstern PS106 TROPOS Event label DATE/TIME File name File format File size Uniform resource locator/link to file Cloud Radar PS106/1 Arctic Amplification AC3 |
spellingShingle |
Cloudnet OCEANET-ATMOSPHERE PASCAL Polarstern PS106 TROPOS Event label DATE/TIME File name File format File size Uniform resource locator/link to file Cloud Radar PS106/1 Arctic Amplification AC3 Griesche, Hannes Seifert, Patric Engelmann, Ronny Radenz, Martin Bühl, Johannes Cloudnet IWC during PS106 ... |
topic_facet |
Cloudnet OCEANET-ATMOSPHERE PASCAL Polarstern PS106 TROPOS Event label DATE/TIME File name File format File size Uniform resource locator/link to file Cloud Radar PS106/1 Arctic Amplification AC3 |
description |
The dataset contains daily nc-files of the Cloudnet ice water content during Polarstern cruise PS106 based on:- 35.5 GHz Cloud radar MIRA.The data is retrieved using the instrument synergystic approach Cloudnet (Illingworth, 2007 doi:10.1175/BAMS-88-6-883 ).This variable was calculated from the 35.5-GHz radar reflectivity factor after correction for gaseous attenuation, and temperature taken from a forecast model, using the following empirical formula:log10(iwc[g m-3]) = 0.000242Z[dBZ]T[degC] + 0.0699Z[dBZ] + -0.0186T[degC] + -1.63 (Hogan, 2006 doi:10.1175/JAM2340.1 ).In this formula Z is taken to be defined such that all frequencies of radar would measure the same Z in Rayleigh scattering ice. However, the radar is more likely to have been calibrated such that all frequencies would measure the same Z in Rayleigh scattering liquid cloud at 0 degrees C. The measured Z is therefore multiplied by|K(liquid,0degC,35GHz)|^2/0.93 = 0.9441before applying this formula.The formula has been used where the ... : This is an updated version of this data set: https://doi.pangaea.de/10.1594/PANGAEA.900246 ... |
format |
Dataset |
author |
Griesche, Hannes Seifert, Patric Engelmann, Ronny Radenz, Martin Bühl, Johannes |
author_facet |
Griesche, Hannes Seifert, Patric Engelmann, Ronny Radenz, Martin Bühl, Johannes |
author_sort |
Griesche, Hannes |
title |
Cloudnet IWC during PS106 ... |
title_short |
Cloudnet IWC during PS106 ... |
title_full |
Cloudnet IWC during PS106 ... |
title_fullStr |
Cloudnet IWC during PS106 ... |
title_full_unstemmed |
Cloudnet IWC during PS106 ... |
title_sort |
cloudnet iwc during ps106 ... |
publisher |
PANGAEA |
publishDate |
2020 |
url |
https://dx.doi.org/10.1594/pangaea.919452 https://doi.pangaea.de/10.1594/PANGAEA.919452 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_relation |
https://dx.doi.org/10.5194/amt-2019-434 https://dx.doi.org/10.1594/pangaea.900246 https://dx.doi.org/10.1175/jam2340.1 https://dx.doi.org/10.1175/bams-88-6-883 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.91945210.5194/amt-2019-43410.1594/pangaea.90024610.1175/jam2340.110.1175/bams-88-6-883 |
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1809895484309897216 |