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f | 1 | { | f | 1 | { |
2 | "author": "Wellmann, Marie-Constanze", | 2 | "author": "Wellmann, Marie-Constanze", | ||
3 | "author_email": "", | 3 | "author_email": "", | ||
4 | "creator_user_id": "17755db4-395a-4b3b-ac09-e8e3484ca700", | 4 | "creator_user_id": "17755db4-395a-4b3b-ac09-e8e3484ca700", | ||
5 | "doi": "10.35097/1523", | 5 | "doi": "10.35097/1523", | ||
6 | "doi_date_published": "2023", | 6 | "doi_date_published": "2023", | ||
7 | "doi_publisher": "", | 7 | "doi_publisher": "", | ||
8 | "doi_status": "True", | 8 | "doi_status": "True", | ||
9 | "groups": [], | 9 | "groups": [], | ||
10 | "id": "03ed9284-c8a2-4dbe-beea-d30fbc966aed", | 10 | "id": "03ed9284-c8a2-4dbe-beea-d30fbc966aed", | ||
11 | "isopen": false, | 11 | "isopen": false, | ||
12 | "license_id": "CC BY-SA 4.0 Attribution-ShareAlike", | 12 | "license_id": "CC BY-SA 4.0 Attribution-ShareAlike", | ||
13 | "license_title": "CC BY-SA 4.0 Attribution-ShareAlike", | 13 | "license_title": "CC BY-SA 4.0 Attribution-ShareAlike", | ||
14 | "metadata_created": "2023-08-04T08:50:58.965479", | 14 | "metadata_created": "2023-08-04T08:50:58.965479", | ||
t | 15 | "metadata_modified": "2023-08-04T08:52:08.785960", | t | 15 | "metadata_modified": "2023-08-04T08:53:42.292688", |
16 | "name": "rdr-doi-10-35097-1523", | 16 | "name": "rdr-doi-10-35097-1523", | ||
17 | "notes": "Abstract: This study aims to identify whether model | 17 | "notes": "Abstract: This study aims to identify whether model | ||
18 | parameters describing atmospheric conditions such as wind shear or | 18 | parameters describing atmospheric conditions such as wind shear or | ||
19 | model parameters related to cloud microphysics such as the fall | 19 | model parameters related to cloud microphysics such as the fall | ||
20 | velocity of hail lead to larger uncertainties in the prediction of | 20 | velocity of hail lead to larger uncertainties in the prediction of | ||
21 | deep convective clouds.\r\nIn an idealized setup of a cloud-resolving | 21 | deep convective clouds.\r\nIn an idealized setup of a cloud-resolving | ||
22 | model including a two-moment microphysics scheme we use the approach | 22 | model including a two-moment microphysics scheme we use the approach | ||
23 | of statistical emulation to allow for a Monte Carlo sampling of the | 23 | of statistical emulation to allow for a Monte Carlo sampling of the | ||
24 | parameter space, which enables a comprehensive sensitivity analysis. | 24 | parameter space, which enables a comprehensive sensitivity analysis. | ||
25 | We analyze the impact of three sets of input parameters (environmental | 25 | We analyze the impact of three sets of input parameters (environmental | ||
26 | conditions, microphysics, combined) on cloud properties (vertically | 26 | conditions, microphysics, combined) on cloud properties (vertically | ||
27 | integrated content of six hydrometeor classes), precipitation, the | 27 | integrated content of six hydrometeor classes), precipitation, the | ||
28 | size distribution of hail and diabatic heating rates. \r\nThis dataset | 28 | size distribution of hail and diabatic heating rates. \r\nThis dataset | ||
29 | contains the processed model output and the generated emulators when | 29 | contains the processed model output and the generated emulators when | ||
30 | the convection is triggered by a warm bubble.\r\nTechnicalRemarks: | 30 | the convection is triggered by a warm bubble.\r\nTechnicalRemarks: | ||
31 | There are three csv-files labeled \"InputDesign\" which give the input | 31 | There are three csv-files labeled \"InputDesign\" which give the input | ||
32 | combinations of parameters used for the COSMO simulations. The | 32 | combinations of parameters used for the COSMO simulations. The | ||
33 | remaining csv-files contain the processed model output | 33 | remaining csv-files contain the processed model output | ||
34 | (spatio-temporal means or maximum values) for output parameters of | 34 | (spatio-temporal means or maximum values) for output parameters of | ||
35 | interest. This dataset was used to train the emulators which are also | 35 | interest. This dataset was used to train the emulators which are also | ||
36 | included as R workspaces. The R package \"Sensitivity\" is necessary | 36 | included as R workspaces. The R package \"Sensitivity\" is necessary | ||
37 | to perform sensitivity analyses using the emulators.", | 37 | to perform sensitivity analyses using the emulators.", | ||
38 | "num_resources": 0, | 38 | "num_resources": 0, | ||
39 | "num_tags": 0, | 39 | "num_tags": 0, | ||
40 | "orcid": "", | 40 | "orcid": "", | ||
41 | "organization": { | 41 | "organization": { | ||
42 | "approval_status": "approved", | 42 | "approval_status": "approved", | ||
43 | "created": "2023-01-12T13:30:23.238233", | 43 | "created": "2023-01-12T13:30:23.238233", | ||
44 | "description": "RADAR (Research Data Repository) is a | 44 | "description": "RADAR (Research Data Repository) is a | ||
45 | cross-disciplinary repository for archiving and publishing research | 45 | cross-disciplinary repository for archiving and publishing research | ||
46 | data from completed scientific studies and projects. The focus is on | 46 | data from completed scientific studies and projects. The focus is on | ||
47 | research data from subjects that do not yet have their own | 47 | research data from subjects that do not yet have their own | ||
48 | discipline-specific infrastructures for research data management. ", | 48 | discipline-specific infrastructures for research data management. ", | ||
49 | "id": "013c89a9-383c-4200-8baa-0f78bf1d91f9", | 49 | "id": "013c89a9-383c-4200-8baa-0f78bf1d91f9", | ||
50 | "image_url": "radar-logo.svg", | 50 | "image_url": "radar-logo.svg", | ||
51 | "is_organization": true, | 51 | "is_organization": true, | ||
52 | "name": "radar", | 52 | "name": "radar", | ||
53 | "state": "active", | 53 | "state": "active", | ||
54 | "title": "RADAR", | 54 | "title": "RADAR", | ||
55 | "type": "organization" | 55 | "type": "organization" | ||
56 | }, | 56 | }, | ||
57 | "owner_org": "013c89a9-383c-4200-8baa-0f78bf1d91f9", | 57 | "owner_org": "013c89a9-383c-4200-8baa-0f78bf1d91f9", | ||
58 | "private": false, | 58 | "private": false, | ||
59 | "production_year": "2019", | 59 | "production_year": "2019", | ||
60 | "publication_year": "2023", | 60 | "publication_year": "2023", | ||
61 | "publishers": [ | 61 | "publishers": [ | ||
62 | { | 62 | { | ||
63 | "publisher": "Karlsruhe Institute of Technology" | 63 | "publisher": "Karlsruhe Institute of Technology" | ||
64 | } | 64 | } | ||
65 | ], | 65 | ], | ||
66 | "relationships_as_object": [], | 66 | "relationships_as_object": [], | ||
67 | "relationships_as_subject": [], | 67 | "relationships_as_subject": [], | ||
68 | "repository_name": "RADAR (Research Data Repository)", | 68 | "repository_name": "RADAR (Research Data Repository)", | ||
69 | "resources": [], | 69 | "resources": [], | ||
70 | "services_used_list": "", | 70 | "services_used_list": "", | ||
71 | "source_metadata_created": "2023", | 71 | "source_metadata_created": "2023", | ||
72 | "source_metadata_modified": "", | 72 | "source_metadata_modified": "", | ||
73 | "state": "active", | 73 | "state": "active", | ||
74 | "subject_areas": [ | 74 | "subject_areas": [ | ||
75 | { | 75 | { | ||
76 | "subject_area_additional": "", | 76 | "subject_area_additional": "", | ||
77 | "subject_area_name": "Geological Science" | 77 | "subject_area_name": "Geological Science" | ||
78 | } | 78 | } | ||
79 | ], | 79 | ], | ||
80 | "tags": [], | 80 | "tags": [], | ||
81 | "title": "Training data and emulators for the analysis of | 81 | "title": "Training data and emulators for the analysis of | ||
82 | sensitivity of deep convective clouds and hail to environmental | 82 | sensitivity of deep convective clouds and hail to environmental | ||
83 | conditions and microphysics (updated version)", | 83 | conditions and microphysics (updated version)", | ||
84 | "type": "vdataset", | 84 | "type": "vdataset", | ||
85 | "url": "https://doi.org/10.35097/1523" | 85 | "url": "https://doi.org/10.35097/1523" | ||
86 | } | 86 | } |