cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.927237
title: Measurements of wind, temperature, pressure and humidity during lead-parallel flight 20130326_SP50326h02_45505-45594 with POLAR 5

description: The data collection consists of the airborne measurements obtained in the framework of the AWI-campaign "SpringTime Atmospheric Boundary Layer Experiment" (STABLE) that are used as supplement for the study by Michaelis et al. (2020). The measurements were performed in the atmospheric boundary layer near three different leads in the Arctic Marginal Sea Ice Zone north and northwest of Svalbard on 10, 25 and 26 March 2013. All cases represent conditions of a nearly lead-perpendicular convective flow over the leads.This data set contains the lead-parallel flight legs performed at different distances to the upwind lead edge at different altitudes, either above the lead or further downwind. Mean distance to upwind lead edge: 0.7 km
DOI: 10.1594/pangaea.927238
title: Measurements of wind, temperature, pressure and humidity during lead-parallel flight 20130326_SP50326h03_45715-45831 with POLAR 5

description: The data collection consists of the airborne measurements obtained in the framework of the AWI-campaign "SpringTime Atmospheric Boundary Layer Experiment" (STABLE) that are used as supplement for the study by Michaelis et al. (2020). The measurements were performed in the atmospheric boundary layer near three different leads in the Arctic Marginal Sea Ice Zone north and northwest of Svalbard on 10, 25 and 26 March 2013. All cases represent conditions of a nearly lead-perpendicular convective flow over the leads.This data set contains the lead-parallel flight legs performed at different distances to the upwind lead edge at different altitudes, either above the lead or further downwind. Mean distance to upwind lead edge: 1.5 km.
DOI: 10.1594/pangaea.927239
title: Measurements of wind, temperature, pressure and humidity during lead-parallel flight 20130326_SP50326h04_45966-46088 with POLAR 5

description: The data collection consists of the airborne measurements obtained in the framework of the AWI-campaign "SpringTime Atmospheric Boundary Layer Experiment" (STABLE) that are used as supplement for the study by Michaelis et al. (2020). The measurements were performed in the atmospheric boundary layer near three different leads in the Arctic Marginal Sea Ice Zone north and northwest of Svalbard on 10, 25 and 26 March 2013. All cases represent conditions of a nearly lead-perpendicular convective flow over the leads.This data set contains the lead-parallel flight legs performed at different distances to the upwind lead edge at different altitudes, either above the lead or further downwind. Mean distance to upwind lead edge: 1.5 km.
DOI: 10.1594/pangaea.927245
title: Measurements of wind, temperature, pressure and humidity during lead-parallel flight 20130326_SP50326h05_46203-46308 with POLAR 5

description: The data collection consists of the airborne measurements obtained in the framework of the AWI-campaign "SpringTime Atmospheric Boundary Layer Experiment" (STABLE) that are used as supplement for the study by Michaelis et al. (2020). The measurements were performed in the atmospheric boundary layer near three different leads in the Arctic Marginal Sea Ice Zone north and northwest of Svalbard on 10, 25 and 26 March 2013. All cases represent conditions of a nearly lead-perpendicular convective flow over the leads.This data set contains the lead-parallel flight legs performed at different distances to the upwind lead edge at different altitudes, either above the lead or further downwind. Mean distance to upwind lead edge: 1.5 km.
DOI: 10.1594/pangaea.927246
title: Measurements of wind, temperature, pressure and humidity during lead-parallel flight 20130326_SP50326h06_46457-46568 with POLAR 5

description: The data collection consists of the airborne measurements obtained in the framework of the AWI-campaign "SpringTime Atmospheric Boundary Layer Experiment" (STABLE) that are used as supplement for the study by Michaelis et al. (2020). The measurements were performed in the atmospheric boundary layer near three different leads in the Arctic Marginal Sea Ice Zone north and northwest of Svalbard on 10, 25 and 26 March 2013. All cases represent conditions of a nearly lead-perpendicular convective flow over the leads.This data set contains the lead-parallel flight legs performed at different distances to the upwind lead edge at different altitudes, either above the lead or further downwind. Mean distance to upwind lead edge: 1.5 km.
DOI: 10.1594/pangaea.927247
title: Measurements of wind, temperature, pressure and humidity during lead-parallel flight 20130326_SP50326h07_46725-46833 with POLAR 5

description: The data collection consists of the airborne measurements obtained in the framework of the AWI-campaign "SpringTime Atmospheric Boundary Layer Experiment" (STABLE) that are used as supplement for the study by Michaelis et al. (2020). The measurements were performed in the atmospheric boundary layer near three different leads in the Arctic Marginal Sea Ice Zone north and northwest of Svalbard on 10, 25 and 26 March 2013. All cases represent conditions of a nearly lead-perpendicular convective flow over the leads.This data set contains the lead-parallel flight legs performed at different distances to the upwind lead edge at different altitudes, either above the lead or further downwind. Mean distance to upwind lead edge: 1.5 km.
DOI: 10.1594/pangaea.927248
title: Measurements of wind, temperature, pressure and humidity during lead-parallel flight 20130326_SP50326h09_46944-47090 with POLAR 5

description: The data collection consists of the airborne measurements obtained in the framework of the AWI-campaign "SpringTime Atmospheric Boundary Layer Experiment" (STABLE) that are used as supplement for the study by Michaelis et al. (2020). The measurements were performed in the atmospheric boundary layer near three different leads in the Arctic Marginal Sea Ice Zone north and northwest of Svalbard on 10, 25 and 26 March 2013. All cases represent conditions of a nearly lead-perpendicular convective flow over the leads.This data set contains the lead-parallel flight legs performed at different distances to the upwind lead edge at different altitudes, either above the lead or further downwind. Mean distance to upwind lead edge: 3.0 km.
DOI: 10.1594/pangaea.927250
title: Measurements of wind, temperature, pressure and humidity during lead-parallel flight 20130326_SP50326h10_47265-47383 with POLAR 5

description: The data collection consists of the airborne measurements obtained in the framework of the AWI-campaign "SpringTime Atmospheric Boundary Layer Experiment" (STABLE) that are used as supplement for the study by Michaelis et al. (2020). The measurements were performed in the atmospheric boundary layer near three different leads in the Arctic Marginal Sea Ice Zone north and northwest of Svalbard on 10, 25 and 26 March 2013. All cases represent conditions of a nearly lead-perpendicular convective flow over the leads.This data set contains the lead-parallel flight legs performed at different distances to the upwind lead edge at different altitudes, either above the lead or further downwind. Mean distance to upwind lead edge: 3.0 km.
DOI: 10.1594/pangaea.927251
title: Measurements of wind, temperature, pressure and humidity during lead-parallel flight 20130326_SP50326h11_47559-47676 with POLAR 5

description: The data collection consists of the airborne measurements obtained in the framework of the AWI-campaign "SpringTime Atmospheric Boundary Layer Experiment" (STABLE) that are used as supplement for the study by Michaelis et al. (2020). The measurements were performed in the atmospheric boundary layer near three different leads in the Arctic Marginal Sea Ice Zone north and northwest of Svalbard on 10, 25 and 26 March 2013. All cases represent conditions of a nearly lead-perpendicular convective flow over the leads.This data set contains the lead-parallel flight legs performed at different distances to the upwind lead edge at different altitudes, either above the lead or further downwind. Mean distance to upwind lead edge: 3.0 km.
DOI: 10.1594/pangaea.927252
title: Measurements of wind, temperature, pressure and humidity during lead-parallel flight 20130326_SP50326h12_47826-47950 with POLAR 5

description: The data collection consists of the airborne measurements obtained in the framework of the AWI-campaign "SpringTime Atmospheric Boundary Layer Experiment" (STABLE) that are used as supplement for the study by Michaelis et al. (2020). The measurements were performed in the atmospheric boundary layer near three different leads in the Arctic Marginal Sea Ice Zone north and northwest of Svalbard on 10, 25 and 26 March 2013. All cases represent conditions of a nearly lead-perpendicular convective flow over the leads.This data set contains the lead-parallel flight legs performed at different distances to the upwind lead edge at different altitudes, either above the lead or further downwind. Mean distance to upwind lead edge: 3.0 km.
DOI: 10.1594/pangaea.927253
title: Measurements of wind, temperature, pressure and humidity during lead-parallel flight 20130326_SP50326h13_48125-48235 with POLAR 5

description: The data collection consists of the airborne measurements obtained in the framework of the AWI-campaign "SpringTime Atmospheric Boundary Layer Experiment" (STABLE) that are used as supplement for the study by Michaelis et al. (2020). The measurements were performed in the atmospheric boundary layer near three different leads in the Arctic Marginal Sea Ice Zone north and northwest of Svalbard on 10, 25 and 26 March 2013. All cases represent conditions of a nearly lead-perpendicular convective flow over the leads.This data set contains the lead-parallel flight legs performed at different distances to the upwind lead edge at different altitudes, either above the lead or further downwind. Mean distance to upwind lead edge: 3.0 km.
DOI: 10.1594/pangaea.927254
title: Measurements of wind, temperature, pressure and humidity during lead-parallel flight 20130326_SP50326h14_48352-48490 with POLAR 5

description: The data collection consists of the airborne measurements obtained in the framework of the AWI-campaign "SpringTime Atmospheric Boundary Layer Experiment" (STABLE) that are used as supplement for the study by Michaelis et al. (2020). The measurements were performed in the atmospheric boundary layer near three different leads in the Arctic Marginal Sea Ice Zone north and northwest of Svalbard on 10, 25 and 26 March 2013. All cases represent conditions of a nearly lead-perpendicular convective flow over the leads.This data set contains the lead-parallel flight legs performed at different distances to the upwind lead edge at different altitudes, either above the lead or further downwind. Mean distance to upwind lead edge: 4.3 km.
DOI: 10.1594/pangaea.927255
title: Measurements of wind, temperature, pressure and humidity during lead-parallel flight 20130326_SP50326h15_48678-48824 with POLAR 5

description: The data collection consists of the airborne measurements obtained in the framework of the AWI-campaign "SpringTime Atmospheric Boundary Layer Experiment" (STABLE) that are used as supplement for the study by Michaelis et al. (2020). The measurements were performed in the atmospheric boundary layer near three different leads in the Arctic Marginal Sea Ice Zone north and northwest of Svalbard on 10, 25 and 26 March 2013. All cases represent conditions of a nearly lead-perpendicular convective flow over the leads.This data set contains the lead-parallel flight legs performed at different distances to the upwind lead edge at different altitudes, either above the lead or further downwind. Mean distance to upwind lead edge: 4.3 km.
DOI: 10.1594/pangaea.927257
title: Measurements of wind, temperature, pressure and humidity during lead-parallel flight 20130326_SP50326h16_48967-49120 with POLAR 5

description: The data collection consists of the airborne measurements obtained in the framework of the AWI-campaign "SpringTime Atmospheric Boundary Layer Experiment" (STABLE) that are used as supplement for the study by Michaelis et al. (2020). The measurements were performed in the atmospheric boundary layer near three different leads in the Arctic Marginal Sea Ice Zone north and northwest of Svalbard on 10, 25 and 26 March 2013. All cases represent conditions of a nearly lead-perpendicular convective flow over the leads.This data set contains the lead-parallel flight legs performed at different distances to the upwind lead edge at different altitudes, either above the lead or further downwind. Mean distance to upwind lead edge: 4.3 km.
DOI: 10.1594/pangaea.927258
title: Measurements of wind, temperature, pressure and humidity during lead-parallel flight 20130326_SP50326h17_49295-49425 with POLAR 5

description: The data collection consists of the airborne measurements obtained in the framework of the AWI-campaign "SpringTime Atmospheric Boundary Layer Experiment" (STABLE) that are used as supplement for the study by Michaelis et al. (2020). The measurements were performed in the atmospheric boundary layer near three different leads in the Arctic Marginal Sea Ice Zone north and northwest of Svalbard on 10, 25 and 26 March 2013. All cases represent conditions of a nearly lead-perpendicular convective flow over the leads.This data set contains the lead-parallel flight legs performed at different distances to the upwind lead edge at different altitudes, either above the lead or further downwind. Mean distance to upwind lead edge: 4.3 km.
DOI: 10.1594/pangaea.927298
title: Measurements of wind, temperature, pressure and humidity during cross-lead flight zz1_20130310_cross-lead_SP50310h17_54271-55000_p5

description: The data collection consists of the airborne measurements obtained in the framework of the AWI-campaign "SpringTime Atmospheric Boundary Layer Experiment" (STABLE) that are used as supplement for the study by Michaelis et al. (2020). The measurements were performed in the atmospheric boundary layer near three different leads in the Arctic Marginal Sea Ice Zone north and northwest of Svalbard on 10, 25 and 26 March 2013. All cases represent conditions of a nearly lead-perpendicular convective flow over the leads.This data set contains the cross-lead flight data: a low-level horizontal flight leg performed across the lead along the mean wind direction.
DOI: 10.1594/pangaea.927299
title: Measurements of wind, temperature, pressure and humidity during cross-lead flight zz1_20130325_cross-lead_SP50325h01_43682-44220_p5

description: The data collection consists of the airborne measurements obtained in the framework of the AWI-campaign "SpringTime Atmospheric Boundary Layer Experiment" (STABLE) that are used as supplement for the study by Michaelis et al. (2020). The measurements were performed in the atmospheric boundary layer near three different leads in the Arctic Marginal Sea Ice Zone north and northwest of Svalbard on 10, 25 and 26 March 2013. All cases represent conditions of a nearly lead-perpendicular convective flow over the leads.This data set contains the cross-lead flight data: a low-level horizontal flight leg performed across the lead along the mean wind direction.
DOI: 10.1594/pangaea.927300
title: Measurements of wind, temperature, pressure and humidity during cross-lead flight zz1_20130326_cross-lead_SP50326h01_44143-44668_p5

description: The data collection consists of the airborne measurements obtained in the framework of the AWI-campaign "SpringTime Atmospheric Boundary Layer Experiment" (STABLE) that are used as supplement for the study by Michaelis et al. (2020). The measurements were performed in the atmospheric boundary layer near three different leads in the Arctic Marginal Sea Ice Zone north and northwest of Svalbard on 10, 25 and 26 March 2013. All cases represent conditions of a nearly lead-perpendicular convective flow over the leads.This data set contains the cross-lead flight data: a low-level horizontal flight leg performed across the lead along the mean wind direction.
DOI: 10.1594/pangaea.929319
title: Master track from POLAR 5 flight P5_200_ANT_2015_2016_1509240101 in 1 sec resolution (zipped, 53 kBytes)
DOI: 10.1594/pangaea.929320
title: Master track from POLAR 5 flight P5_200_ANT_2015_2016_1512140201 in 1 sec resolution (zipped, 48 kBytes)
DOI: 10.1594/pangaea.929321
title: Master track from POLAR 5 flight P5_200_ANT_2015_2016_1512150301 in 1 sec resolution (zipped, 39 kBytes)
DOI: 10.1594/pangaea.929322
title: Master track from POLAR 5 flight P5_200_ANT_2015_2016_1512150401 in 1 sec resolution (zipped, 186 kBytes)
DOI: 10.1594/pangaea.929324
title: Master track from POLAR 5 flight P5_200_ANT_2015_2016_1512180601 in 1 sec resolution (zipped, 186 kBytes)
DOI: 10.1594/pangaea.929325
title: Master track from POLAR 5 flight P5_200_ANT_2015_2016_1512190701 in 1 sec resolution (zipped, 182 kBytes)
DOI: 10.1594/pangaea.929326
title: Master track from POLAR 5 flight P5_200_ANT_2015_2016_1512230901 in 1 sec resolution (zipped, 185 kBytes)
DOI: 10.1594/pangaea.929327
title: Master track from POLAR 5 flight P5_200_ANT_2015_2016_1512241001 in 1 sec resolution (zipped, 190 kBytes)
DOI: 10.1594/pangaea.929328
title: Master track from POLAR 5 flight P5_200_ANT_2015_2016_1512271101 in 1 sec resolution (zipped, 196 kBytes)
DOI: 10.1594/pangaea.929330
title: Master track from POLAR 5 flight P5_200_ANT_2015_2016_1512291301 in 1 sec resolution (zipped, 150 kBytes)
DOI: 10.1594/pangaea.929331
title: Master track from POLAR 5 flight P5_200_ANT_2015_2016_1601021401 in 1 sec resolution (zipped, 188 kBytes)
DOI: 10.1594/pangaea.929332
title: Master track from POLAR 5 flight P5_200_ANT_2015_2016_1601031501 in 1 sec resolution (zipped, 166 kBytes)
DOI: 10.1594/pangaea.929333
title: Master track from POLAR 5 flight P5_200_ANT_2015_2016_1601041601 in 1 sec resolution (zipped, 94 kBytes)
DOI: 10.1594/pangaea.929334
title: Master track from POLAR 5 flight P5_200_ANT_2015_2016_1512160501 in 1 sec resolution (zipped, 135 kBytes)
DOI: 10.1594/pangaea.929335
title: Master track from POLAR 5 flight P5_200_ANT_2015_2016_1512281201 in 1 sec resolution (zipped, 189 kBytes)
DOI: 10.1594/pangaea.929340
title: Master tracks in different resolutions from POLAR 5 flight P5_200_ANT_2015_2016_1509240101
DOI: 10.1594/pangaea.929341
title: Master tracks in different resolutions from POLAR 5 flight P5_200_ANT_2015_2016_1512140201
DOI: 10.1594/pangaea.929342
title: Master tracks in different resolutions from POLAR 5 flight P5_200_ANT_2015_2016_1512150301
DOI: 10.1594/pangaea.929343
title: Master tracks in different resolutions from POLAR 5 flight P5_200_ANT_2015_2016_1512150401
DOI: 10.1594/pangaea.929344
title: Master tracks in different resolutions from POLAR 5 flight P5_200_ANT_2015_2016_1512160501
DOI: 10.1594/pangaea.929345
title: Master tracks in different resolutions from POLAR 5 flight P5_200_ANT_2015_2016_1512180601
DOI: 10.1594/pangaea.929346
title: Master tracks in different resolutions from POLAR 5 flight P5_200_ANT_2015_2016_1512190701
DOI: 10.1594/pangaea.929347
title: Master tracks in different resolutions from POLAR 5 flight P5_200_ANT_2015_2016_1512230901
DOI: 10.1594/pangaea.929348
title: Master tracks in different resolutions from POLAR 5 flight P5_200_ANT_2015_2016_1512241001
DOI: 10.1594/pangaea.929349
title: Master tracks in different resolutions from POLAR 5 flight P5_200_ANT_2015_2016_1512271101
DOI: 10.1594/pangaea.929350
title: Master tracks in different resolutions from POLAR 5 flight P5_200_ANT_2015_2016_1512281201
DOI: 10.25402/pgs.20746831.v1
title: Detection of relevant pharmacogenetic information through exome sequencing in oncology: Supplementary tables

description: Background: Germline sequencing of individual genomes can detect alleles responsible for adverse drug
reactions (ADRs) in relation to chemotherapy, targeted agents, antiemetics or pain treatment. Materials
& methods: To evaluate the interest of such pharmacogenetic information, the authors retrospectively
analyzed genes known to have an impact on cancer therapy in a cohort of 445 solid cancers patients.
Results: Six patients treated with 5-fluorouracil carrying one DPYD variant classified as 1A showed
decreased drug mean clearance (p = 0.01). Regarding CYP2D6, all patients (n = 5) with predicted CYP2D6
poor or ultra-rapid metabolizer status experienced adverse drug reactions related to opioid therapy.
Conclusion: Genomic germline sequencing performed for theragnostic issues in patients with a solid
tumor, can provide relevant information about common pharmacogenetic alleles.
DOI: 10.1594/pangaea.929351
title: Master tracks in different resolutions from POLAR 5 flight P5_200_ANT_2015_2016_1512291301
DOI: 10.1594/pangaea.929352
title: Master tracks in different resolutions from POLAR 5 flight P5_200_ANT_2015_2016_1601021401
DOI: 10.1594/pangaea.929353
title: Master tracks in different resolutions from POLAR 5 flight P5_200_ANT_2015_2016_1601031501
DOI: 10.1594/pangaea.929354
title: Master tracks in different resolutions from POLAR 5 flight P5_200_ANT_2015_2016_1601041601
DOI: 10.1594/pangaea.930932
title: Spectral solar cloud top and surface radiance measured by airborne spectral imaging during the AFLUX campaign in 2019

description: Hyperspectral fields of visible and near infrared cloud top and surface radiance observed by AISA Eagle (1024 spatial pixels and 504 spectral channels between 400 and 993 nm) and AISA Hawk (384 spatial pixels and 384 spectral channels between 931 and 2545 nm) during the Airborne measurements of radiative and turbulent FLUXes of energy and momentum in the Arctic boundary layer (AFLUX) campaign in March/April 2019.
DOI: 10.1594/pangaea.930746
title: Footprints of MACS aerial images from POLAR 6 ThawTrend_Air_2019 flight campaign in northern Alaska

description: This datasets contains the footprints of the DLR MACS (Modular Aerial Camera System) acquisitions (RGB + NIR) during the AWI ThawTrendAir2019 campaign on POLAR 6 from 10 July until 1 August 2019. This mission was based in Utkiagvik/Barrow, Alaska, USA. The aerial images were acquired to map permafrost related land cover and landforms in very high resolution and to create multi-spectral orthomosaics and digital surface models (DSM) across the Arctic Coastal Plain (North Slope) of Alaska. The acquired datasets cover grids of specific targets (e.g. coastal erosion, fire scars, permafrost degradation) as well as transects.The footprint files were created to search for data availability and data selection purposes. Data were extracted from raw MACS files using DLR MACS-BOX Mosaica Software and processed with custom python scripts (https://github.com/awi-response/MACS_tools).
description: General File Information (please see further details: Footprints of MACS aerial images from POLAR 6 ThawTrend_Air_2019 flight campaign in northern Alaska - data description):EPSG: 4326File format: ESRI ShapefileVector Type: PolygonDataset #1: ThawTrendAir2019_MACS_footprints_dissolved.zipDissolved footprint of the entire mission. This dataset can be used to find areas with image acquisitions.Dataset #2: ThawTrendAir2019_MACS_footprints_datasets.zipDissolved footprints of sub-missions/projects. Each feature contains the sub-mission name.Dataset #3: ThawTrendAir2019_MACS_footprints_scenes.zipIndividual image footprints of the entire mission including individual image metadata.