edu.ucar.opensky::articles:22524 UCAR/NCAR - Library OpenSky Support PO Box 3000 Boulder CO 80307-3000 opensky@ucar.edu http://opensky.ucar.edu/ homepage pointOfContact 2025-12-25T15:34:07.392841 ISO 19115-2 Geographic Information - Metadata - Part 2: Extensions for Imagery and Gridded Data ISO 19115-2:2009(E) https://n2t.org/ark:/85065/d73n26fp Evolution of DARDAR-CLOUD ice cloud retrievals: New parameters and impacts on the retrieved microphysical properties 2019-05-16T00:00:00Z publication https://n2t.org/ark:/85065/d73n26fp https://doi.org/10.5194/amt-12-2819-2019 Cazenave, Q. author Ceccaldi, M. author Delanoë, J. author Pelon, J. author Groß, S. author Heymsfield, Andrew J. author UCAR/NCAR - Library publisher In this paper we present the latest refinements brought to the DARDAR-CLOUD product, which contains ice cloud microphysical properties retrieved from the cloud radar and lidar measurements from the A-Train mission. Based on a large dataset of in situ ice cloud measurements, the parameterizations used in the microphysical model of the algorithm - i.e. the normalized particle size distribution, the mass-size relationship, and the parameterization of the a priori value of the normalized number concentration as a function of temperature - were assessed and refined to better fit the measurements, keeping the same formalism as proposed in DARDAR basis papers. Additionally, in regions where lidar measurements are available, the lidar ratio retrieved for ice clouds is shown to be well constrained by the lidar-radar synergy. Using this information, the parameterization of the lidar ratio was also refined, and the new retrieval equals on average 35 +/- 10 sr in the temperature range between 60 and -20 degrees C. The impact of those changes on the retrieved ice cloud properties is presented in terms of ice water content (IWC) and effective radius. Overall, IWC values from the new DARDAR-CLOUD product are on average 16% smaller than the previous version, leading to a 24% reduction in the ice water path. In parallel, the retrieved effective radii increase by 5% to 40 %, depending on temperature and the availability of the instruments, with an average difference of +15 %. Modifications of the microphysical model strongly affect the ice water content retrievals with differences that were found to range from -50% to +40 %, depending on temperature and the availability of the instruments. The largest differences are found for the warmest temperatures (between -20 and 0 degrees C) in regions where the cloud microphysical processes are more complex and where the retrieval is almost exclusively based on radar-only measurements. The new lidar ratio values lead to a reduction of IWC at cold temperatures, the difference between the two versions increasing from around 0% at -30 degrees C to 70% below -80 degrees C, whereas effective radii are not impacted. UCAR/NCAR - Library OpenSky Support PO Box 3000 Boulder CO 80307-3000 opensky@ucar.edu http://opensky.ucar.edu/ homepage pointOfContact PDF Text theme Resource Type 2016-01-01T00:00:00Z publication Copyright 2019 Author(s). This work is licensed under a Creative Commons Attribution 4.0 International license. None eng geoscientificInformation