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Lucke, Johannes; Moser, Manuel; De La Torre Castro, Elena; Mayer, Johanna; Voigt, Christiane (2023): Backscatter Cloud Probe with Polarization Detection [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.963614

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Abstract:
This dataset contains the processed and raw data collected with the Backscatter Cloud Probe with Polarization Detection during the HALO-AC³ campaign in March and April 2022 with the Polar 6 Aircraft out of Longyearbyen, Svalbard. The dataset contains two kinds of data. Data to which no inversion procedure has been applied and data to which the inversion procedure has been applied. The inversion procedure is applied to account for an uneven intensity of the laser beam across the sample area and resulting undersizing effects. The inversion procedure has been discussed in Lucke et al. (2023) (doi.org/10.4271/2023-01-1485) and Beswick et al. (2014) (doi.org/10.5194/amt-7-1443-2014). All quantities which carry the suffix inv are based on the inverted data, all other properties are not. It should be noted, that the necessity of the inversion procedure remains unclear (see the previously mentioned publications). The inversion procedure could only be applied when more than 2000 particles were present over a 5 second interval. When this was not the case, the inverted data are 9999.999. The inverted data are therefore also computed from a 5s rolling average. The measurements of the BCPD are likely severely influenced by inertial separation effects, due to the proximity of the BCPD sample area to the fuselage (approx. 3cm). When ice particles are present, shattering occurs on the fuselage and artificially increases the ice number concentration. The number of ice and liquid particles listed in this data set can be useful for assessing the presence of ice and liquid particles. To estimate the number of liquid and ice particles more than 100 particles are required over a 5s interval. When this is not the case, the data are 9999.999. The number of ice and liquid particles were computed as rolling averages over 5s intervals. The sample area in case no inversion procedure is applied is 0.273 square millimeters.
Keyword(s):
Backscatter Cloud Probe with Polarization Detection; HALO-(AC)³; mixed-phase clouds; Particle size distributions; Phase differentiation; Svalbard
Related to:
Beswick, K; Baumgardner, Darrel; Gallagher, Martin W; Volz-Thomas, A; Nedelec, P; Wang, K-Y; Lance, S (2014): The backscatter cloud probe – a compact low-profile autonomous optical spectrometer. Atmospheric Measurement Techniques, 7(5), 1443-1457, https://doi.org/10.5194/amt-7-1443-2014
Lucke, Johannes; Jurkat, Tina; Baumgardner, Darrel; Kalinka, Frank; Moser, Manuel; De La Torre Castro, Elena; Voigt, Christiane (2023): Characterization of Atmospheric Icing Conditions during the HALO-(AC) 3 Campaign with the Nevzorov Probe and the Backscatter Cloud Probe with Polarization Detection. International Conference on Icing of Aircraft, Engines, and Structures, Technical Paper, 2023-01-1485, https://doi.org/10.4271/2023-01-1485
Funding:
Horizon 2020 (H2020), grant/award no. 824253: SENS4ICE
Coverage:
Median Latitude: 78.239504 * Median Longitude: 15.106434 * South-bound Latitude: 78.091476 * West-bound Longitude: 6.004681 * North-bound Latitude: 78.246003 * East-bound Longitude: 15.503320
Date/Time Start: 2022-03-20T10:39:14 * Date/Time End: 2022-04-10T14:13:58
Event(s):
P6_231_HALO_2022_2203200401 (HALO-AC3_20220320_P6_RF01)  * Latitude Start: 78.245964 * Longitude Start: 15.502078 * Latitude End: 78.245980 * Longitude End: 15.501922 * Date/Time Start: 2022-03-20T10:39:14 * Date/Time End: 2022-03-20T16:03:13 * Location: Arctic * Campaign: P6-231_HALO_2022 (HALO - (AC)3) * Basis: POLAR 6 * Method/Device: Aircraft (AC)
P6_231_HALO_2022_2203220501 (HALO-AC3_20220322_P6_RF02)  * Latitude Start: 78.245998 * Longitude Start: 15.501904 * Latitude End: 78.245946 * Longitude End: 15.502071 * Date/Time Start: 2022-03-22T10:15:37 * Date/Time End: 2022-03-22T16:40:35 * Location: Arctic * Campaign: P6-231_HALO_2022 (HALO - (AC)3) * Basis: POLAR 6 * Method/Device: Aircraft (AC)
P6_231_HALO_2022_2203260702 (HALO-AC3_20220326_P6_RF04)  * Latitude Start: 78.245984 * Longitude Start: 15.501844 * Latitude End: 78.245704 * Longitude End: 15.503320 * Date/Time Start: 2022-03-26T12:09:03 * Date/Time End: 2022-03-26T17:12:02 * Location: Arctic * Campaign: P6-231_HALO_2022 (HALO - (AC)3) * Basis: POLAR 6 * Method/Device: Aircraft (AC)
Comment:
During RF03 there was a malfunction with the BCPD, hence no data is available for that flight.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Event labelEventLucke, Johannes
Date/Time of eventDate/TimeLucke, Johannes
netCDF filenetCDFLucke, JohannesBackscatter Cloud Probe with Polarization Detection (BCPD)
netCDF file (File Size)netCDF (Size)BytesLucke, JohannesBackscatter Cloud Probe with Polarization Detection (BCPD)
Status:
Curation Level: Basic curation (CurationLevelB)
Size:
12 data points

Data

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Event

Date/Time

netCDF

netCDF (Size) [Bytes]
P6_231_HALO_2022_2203200401 2022-03-20BCPD_HALO-AC3_polar6_20220320_RF01.nc16.4 MBytes
P6_231_HALO_2022_2203220501 2022-03-22BCPD_HALO-AC3_polar6_20220322_RF02.nc19.3 MBytes
P6_231_HALO_2022_2203260702 2022-03-26BCPD_HALO-AC3_polar6_20220326_RF04.nc8.4 MBytes
P6_231_HALO_2022_2203280801 2022-03-28BCPD_HALO-AC3_polar6_20220328_RF05.nc16.2 MBytes
P6_231_HALO_2022_2203290901 2022-03-29BCPD_HALO-AC3_polar6_20220329_RF06.nc19.7 MBytes
P6_231_HALO_2022_2203301001 2022-03-30BCPD_HALO-AC3_polar6_20220330_RF07.nc17.3 MBytes
P6_231_HALO_2022_2204011101 2022-04-01BCPD_HALO-AC3_polar6_20220401_RF08.nc17.9 MBytes
P6_231_HALO_2022_2204041201 2022-04-04BCPD_HALO-AC3_polar6_20220404_RF09.nc14.9 MBytes
P6_231_HALO_2022_2204051301 2022-04-05BCPD_HALO-AC3_polar6_20220405_RF10.nc15.8 MBytes
P6_231_HALO_2022_2204081401 2022-04-08BCPD_HALO-AC3_polar6_20220408_RF11.nc18.8 MBytes
P6_231_HALO_2022_2204091501 2022-04-09BCPD_HALO-AC3_polar6_20220409_RF12.nc16.8 MBytes
P6_231_HALO_2022_2204101601 2022-04-10BCPD_HALO-AC3_polar6_20220410_RF13.nc17.4 MBytes