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f | 1 | { | f | 1 | { |
2 | "author": "Deetz, Konrad", | 2 | "author": "Deetz, Konrad", | ||
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": "10.35097/1113", | 5 | "doi": "10.35097/1113", | ||
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": "86cf8f68-27d7-486c-9f7a-d337d1d969b4", | 10 | "id": "86cf8f68-27d7-486c-9f7a-d337d1d969b4", | ||
11 | "isopen": false, | 11 | "isopen": false, | ||
12 | "license_id": "CC BY 4.0 Attribution", | 12 | "license_id": "CC BY 4.0 Attribution", | ||
13 | "license_title": "CC BY 4.0 Attribution", | 13 | "license_title": "CC BY 4.0 Attribution", | ||
14 | "metadata_created": "2023-08-04T08:50:06.029840", | 14 | "metadata_created": "2023-08-04T08:50:06.029840", | ||
t | 15 | "metadata_modified": "2023-08-04T08:51:45.771455", | t | 15 | "metadata_modified": "2023-08-04T08:53:16.202483", |
16 | "name": "rdr-doi-10-35097-1113", | 16 | "name": "rdr-doi-10-35097-1113", | ||
17 | "notes": "Abstract: By using COSMO-ART, highly resolved process | 17 | "notes": "Abstract: By using COSMO-ART, highly resolved process | ||
18 | study simulations for 2-3 July 2016 are conducted to assess the | 18 | study simulations for 2-3 July 2016 are conducted to assess the | ||
19 | aerosol effect on the meteorological conditions of southern West | 19 | aerosol effect on the meteorological conditions of southern West | ||
20 | Africa. The meteorological phenomenon Evening Monsoon Flow Enhancement | 20 | Africa. The meteorological phenomenon Evening Monsoon Flow Enhancement | ||
21 | (EMFE) is identified as highly susceptible to the aerosol direct | 21 | (EMFE) is identified as highly susceptible to the aerosol direct | ||
22 | effect, leading to a spatial shift of the EMFE front. In a second | 22 | effect, leading to a spatial shift of the EMFE front. In a second | ||
23 | aerosol feedback chain the aerosol variation leads to a temporal shift | 23 | aerosol feedback chain the aerosol variation leads to a temporal shift | ||
24 | of the stratus-to-cumulus transition.\r\nAbstract: By using COSMO-ART, | 24 | of the stratus-to-cumulus transition.\r\nAbstract: By using COSMO-ART, | ||
25 | highly resolved process study simulations for 2-3 July 2016 are | 25 | highly resolved process study simulations for 2-3 July 2016 are | ||
26 | conducted to assess the aerosol effect on the meteorological | 26 | conducted to assess the aerosol effect on the meteorological | ||
27 | conditions of southern West Africa. The meteorological phenomenon | 27 | conditions of southern West Africa. The meteorological phenomenon | ||
28 | Evening Monsoon Flow Enhancement (EMFE) is identified as highly | 28 | Evening Monsoon Flow Enhancement (EMFE) is identified as highly | ||
29 | susceptible to the aerosol direct effect, leading to a spatial shift | 29 | susceptible to the aerosol direct effect, leading to a spatial shift | ||
30 | of the EMFE front. In a second aerosol feedback chain the aerosol | 30 | of the EMFE front. In a second aerosol feedback chain the aerosol | ||
31 | variation leads to a temporal shift of the stratus-to-cumulus | 31 | variation leads to a temporal shift of the stratus-to-cumulus | ||
32 | transition.\r\nTechnicalRemarks: Dieser Datensatz nimmt Bezug auf die | 32 | transition.\r\nTechnicalRemarks: Dieser Datensatz nimmt Bezug auf die | ||
33 | bei KIT Scientific Publishing (KSP) ver\u00f6ffentlichte Dissertation | 33 | bei KIT Scientific Publishing (KSP) ver\u00f6ffentlichte Dissertation | ||
34 | von Konrad Deetz (https://publikationen.bibliothek.kit.edu/1000077925, | 34 | von Konrad Deetz (https://publikationen.bibliothek.kit.edu/1000077925, | ||
35 | ISBN: 978-3-7315-0744-4, DOI: 10.5445/KSP/1000077925), mit der | 35 | ISBN: 978-3-7315-0744-4, DOI: 10.5445/KSP/1000077925), mit der | ||
36 | Absicht, die Reproduzierbarkeit der Ergebnisse zu gew\u00e4hrleisten | 36 | Absicht, die Reproduzierbarkeit der Ergebnisse zu gew\u00e4hrleisten | ||
37 | und eine Langzeitarchivierung sicher zu stellen.\r\nDer Datensatz | 37 | und eine Langzeitarchivierung sicher zu stellen.\r\nDer Datensatz | ||
38 | enth\u00e4lt alle Abbildungen der Dissertation sowie die Skripte | 38 | enth\u00e4lt alle Abbildungen der Dissertation sowie die Skripte | ||
39 | (Programmiersprache R) zur Erstellung dieser Abbildungen. Die | 39 | (Programmiersprache R) zur Erstellung dieser Abbildungen. Die | ||
40 | Modelldaten, auf denen die Abbildungen beruhen, sind nicht enthalten, | 40 | Modelldaten, auf denen die Abbildungen beruhen, sind nicht enthalten, | ||
41 | da der Datenumfang (mehrere Terabyte) dies nicht zul\u00e4sst. Die | 41 | da der Datenumfang (mehrere Terabyte) dies nicht zul\u00e4sst. Die | ||
42 | Modelldaten sind in der Large Scale Data Facility (LSDF) des Steinbuch | 42 | Modelldaten sind in der Large Scale Data Facility (LSDF) des Steinbuch | ||
43 | Centre for Computing (SCC) archiviert und k\u00f6nnen bei Bedarf | 43 | Centre for Computing (SCC) archiviert und k\u00f6nnen bei Bedarf | ||
44 | bereitgestellt werden. Zur Modellevaluierung wurden in der | 44 | bereitgestellt werden. Zur Modellevaluierung wurden in der | ||
45 | Dissertation auch Messdaten verwendet, die im Rahmen von DACCIWA | 45 | Dissertation auch Messdaten verwendet, die im Rahmen von DACCIWA | ||
46 | (Dynamics-aerosol-chemistry-cloud interactions in West Africa) | 46 | (Dynamics-aerosol-chemistry-cloud interactions in West Africa) | ||
47 | erstellt wurden. (Messdaten werden \u00fcber die Datenbank | 47 | erstellt wurden. (Messdaten werden \u00fcber die Datenbank | ||
48 | http://baobab.sedoo.fr/ bereitgestellt. Zugriff erteilt die | 48 | http://baobab.sedoo.fr/ bereitgestellt. Zugriff erteilt die | ||
49 | Administration von DACCIWA.)\r\nDer Datensatz enth\u00e4lt die Ordner | 49 | Administration von DACCIWA.)\r\nDer Datensatz enth\u00e4lt die Ordner | ||
50 | D1 (Domain 1, \u201eCONTINENTAL\u201c), D2 (Domain 2, | 50 | D1 (Domain 1, \u201eCONTINENTAL\u201c), D2 (Domain 2, | ||
51 | \u201eSWA\u201c), D3 (Domain 3, \u201eREGIONAL\u201c) und | 51 | \u201eSWA\u201c), D3 (Domain 3, \u201eREGIONAL\u201c) und | ||
52 | \u201emodel_framework\u201c. Die Namen der Unterordner enthalten die | 52 | \u201emodel_framework\u201c. Die Namen der Unterordner enthalten die | ||
53 | Abbildungsnummern, wie sie auch in der Dissertation verwendet werden. | 53 | Abbildungsnummern, wie sie auch in der Dissertation verwendet werden. | ||
54 | Bei R\u00fcckfragen kann man sich an den Autoren wenden.\r\n\r\nThis | 54 | Bei R\u00fcckfragen kann man sich an den Autoren wenden.\r\n\r\nThis | ||
55 | dataset refers to the dissertation published in KIT Scientific | 55 | dataset refers to the dissertation published in KIT Scientific | ||
56 | Publishing (KSP) by Konrad Deetz | 56 | Publishing (KSP) by Konrad Deetz | ||
57 | (https://publikationen.bibliothek.kit.edu/1000077925, ISBN: | 57 | (https://publikationen.bibliothek.kit.edu/1000077925, ISBN: | ||
58 | 978-3-7315-0744-4, DOI: 10.5445/KSP/\r\n1000077925). With that, the | 58 | 978-3-7315-0744-4, DOI: 10.5445/KSP/\r\n1000077925). With that, the | ||
59 | reproducibility of the results and the long-term archiving will be | 59 | reproducibility of the results and the long-term archiving will be | ||
60 | ensured.\r\nThe dataset contains all figures of the dissertation as | 60 | ensured.\r\nThe dataset contains all figures of the dissertation as | ||
61 | well as the scripts (programming language R) to create these figures. | 61 | well as the scripts (programming language R) to create these figures. | ||
62 | The model output, related to these figures, is not included, due to | 62 | The model output, related to these figures, is not included, due to | ||
63 | the amount of data (several terabyte). The model output is archived in | 63 | the amount of data (several terabyte). The model output is archived in | ||
64 | the Large Scale Data Facility (LSDF) of the Steinbuch Centre for | 64 | the Large Scale Data Facility (LSDF) of the Steinbuch Centre for | ||
65 | Computing (SCC) and can be made available on demand. For the model | 65 | Computing (SCC) and can be made available on demand. For the model | ||
66 | evaluation also measurements were used, obtained in the framework of | 66 | evaluation also measurements were used, obtained in the framework of | ||
67 | DACCIWA (Dynamics-aerosol-chemistry-cloud interactions in West | 67 | DACCIWA (Dynamics-aerosol-chemistry-cloud interactions in West | ||
68 | Africa). (Measurements are provided via the database | 68 | Africa). (Measurements are provided via the database | ||
69 | http://baobab.sedoo.fr/. Access is provided via the DACCIWA | 69 | http://baobab.sedoo.fr/. Access is provided via the DACCIWA | ||
70 | administration.)\r\nThe dataset contains the directories D1 (Domain 1, | 70 | administration.)\r\nThe dataset contains the directories D1 (Domain 1, | ||
71 | \u201eCONTINENTAL\u201c), D2 (Domain 2, \u201eSWA\u201c), D3 (Domain | 71 | \u201eCONTINENTAL\u201c), D2 (Domain 2, \u201eSWA\u201c), D3 (Domain | ||
72 | 3, \u201eREGIONAL\u201c) and \u201emodel_framework\u201c. The | 72 | 3, \u201eREGIONAL\u201c) and \u201emodel_framework\u201c. The | ||
73 | subdirectory names contain the figure numbers as used in the | 73 | subdirectory names contain the figure numbers as used in the | ||
74 | dissertation. In case of questions please contact the | 74 | dissertation. In case of questions please contact the | ||
75 | author.\r\n\r\nKonrad Deetz, 22 March 2018", | 75 | author.\r\n\r\nKonrad Deetz, 22 March 2018", | ||
76 | "num_resources": 0, | 76 | "num_resources": 0, | ||
77 | "num_tags": 5, | 77 | "num_tags": 5, | ||
78 | "orcid": "", | 78 | "orcid": "", | ||
79 | "organization": { | 79 | "organization": { | ||
80 | "approval_status": "approved", | 80 | "approval_status": "approved", | ||
81 | "created": "2023-01-12T13:30:23.238233", | 81 | "created": "2023-01-12T13:30:23.238233", | ||
82 | "description": "RADAR (Research Data Repository) is a | 82 | "description": "RADAR (Research Data Repository) is a | ||
83 | cross-disciplinary repository for archiving and publishing research | 83 | cross-disciplinary repository for archiving and publishing research | ||
84 | data from completed scientific studies and projects. The focus is on | 84 | data from completed scientific studies and projects. The focus is on | ||
85 | research data from subjects that do not yet have their own | 85 | research data from subjects that do not yet have their own | ||
86 | discipline-specific infrastructures for research data management. ", | 86 | discipline-specific infrastructures for research data management. ", | ||
87 | "id": "013c89a9-383c-4200-8baa-0f78bf1d91f9", | 87 | "id": "013c89a9-383c-4200-8baa-0f78bf1d91f9", | ||
88 | "image_url": "radar-logo.svg", | 88 | "image_url": "radar-logo.svg", | ||
89 | "is_organization": true, | 89 | "is_organization": true, | ||
90 | "name": "radar", | 90 | "name": "radar", | ||
91 | "state": "active", | 91 | "state": "active", | ||
92 | "title": "RADAR", | 92 | "title": "RADAR", | ||
93 | "type": "organization" | 93 | "type": "organization" | ||
94 | }, | 94 | }, | ||
95 | "owner_org": "013c89a9-383c-4200-8baa-0f78bf1d91f9", | 95 | "owner_org": "013c89a9-383c-4200-8baa-0f78bf1d91f9", | ||
96 | "private": false, | 96 | "private": false, | ||
97 | "production_year": "2017", | 97 | "production_year": "2017", | ||
98 | "publication_year": "2023", | 98 | "publication_year": "2023", | ||
99 | "publishers": [ | 99 | "publishers": [ | ||
100 | { | 100 | { | ||
101 | "publisher": "Karlsruhe Institute of Technology" | 101 | "publisher": "Karlsruhe Institute of Technology" | ||
102 | } | 102 | } | ||
103 | ], | 103 | ], | ||
104 | "relationships_as_object": [], | 104 | "relationships_as_object": [], | ||
105 | "relationships_as_subject": [], | 105 | "relationships_as_subject": [], | ||
106 | "repository_name": "RADAR (Research Data Repository)", | 106 | "repository_name": "RADAR (Research Data Repository)", | ||
107 | "resources": [], | 107 | "resources": [], | ||
108 | "services_used_list": "", | 108 | "services_used_list": "", | ||
109 | "source_metadata_created": "2023", | 109 | "source_metadata_created": "2023", | ||
110 | "source_metadata_modified": "", | 110 | "source_metadata_modified": "", | ||
111 | "state": "active", | 111 | "state": "active", | ||
112 | "subject_areas": [ | 112 | "subject_areas": [ | ||
113 | { | 113 | { | ||
114 | "subject_area_additional": "", | 114 | "subject_area_additional": "", | ||
115 | "subject_area_name": "Geological Science" | 115 | "subject_area_name": "Geological Science" | ||
116 | } | 116 | } | ||
117 | ], | 117 | ], | ||
118 | "tags": [ | 118 | "tags": [ | ||
119 | { | 119 | { | ||
120 | "display_name": "COSMO-ART", | 120 | "display_name": "COSMO-ART", | ||
121 | "id": "1f282b8c-33f5-47ee-b4aa-f77110cbd4cd", | 121 | "id": "1f282b8c-33f5-47ee-b4aa-f77110cbd4cd", | ||
122 | "name": "COSMO-ART", | 122 | "name": "COSMO-ART", | ||
123 | "state": "active", | 123 | "state": "active", | ||
124 | "vocabulary_id": null | 124 | "vocabulary_id": null | ||
125 | }, | 125 | }, | ||
126 | { | 126 | { | ||
127 | "display_name": "West African monsoon", | 127 | "display_name": "West African monsoon", | ||
128 | "id": "bd6d8f95-8b20-46ec-938a-0722950ec4be", | 128 | "id": "bd6d8f95-8b20-46ec-938a-0722950ec4be", | ||
129 | "name": "West African monsoon", | 129 | "name": "West African monsoon", | ||
130 | "state": "active", | 130 | "state": "active", | ||
131 | "vocabulary_id": null | 131 | "vocabulary_id": null | ||
132 | }, | 132 | }, | ||
133 | { | 133 | { | ||
134 | "display_name": "aerosol", | 134 | "display_name": "aerosol", | ||
135 | "id": "0eb4ce61-429a-4793-8eab-ea2768af4c87", | 135 | "id": "0eb4ce61-429a-4793-8eab-ea2768af4c87", | ||
136 | "name": "aerosol", | 136 | "name": "aerosol", | ||
137 | "state": "active", | 137 | "state": "active", | ||
138 | "vocabulary_id": null | 138 | "vocabulary_id": null | ||
139 | }, | 139 | }, | ||
140 | { | 140 | { | ||
141 | "display_name": "clouds", | 141 | "display_name": "clouds", | ||
142 | "id": "b7433580-b55f-473a-8776-0ee0152a3de1", | 142 | "id": "b7433580-b55f-473a-8776-0ee0152a3de1", | ||
143 | "name": "clouds", | 143 | "name": "clouds", | ||
144 | "state": "active", | 144 | "state": "active", | ||
145 | "vocabulary_id": null | 145 | "vocabulary_id": null | ||
146 | }, | 146 | }, | ||
147 | { | 147 | { | ||
148 | "display_name": "nocturnal stratus", | 148 | "display_name": "nocturnal stratus", | ||
149 | "id": "24095bc9-951b-41bd-9de9-b4702f8c5c5f", | 149 | "id": "24095bc9-951b-41bd-9de9-b4702f8c5c5f", | ||
150 | "name": "nocturnal stratus", | 150 | "name": "nocturnal stratus", | ||
151 | "state": "active", | 151 | "state": "active", | ||
152 | "vocabulary_id": null | 152 | "vocabulary_id": null | ||
153 | } | 153 | } | ||
154 | ], | 154 | ], | ||
155 | "title": "Assessing the aerosol impact on southern west african | 155 | "title": "Assessing the aerosol impact on southern west african | ||
156 | clouds and atmospheric dynamics (dataset)", | 156 | clouds and atmospheric dynamics (dataset)", | ||
157 | "type": "vdataset", | 157 | "type": "vdataset", | ||
158 | "url": "https://doi.org/10.35097/1113" | 158 | "url": "https://doi.org/10.35097/1113" | ||
159 | } | 159 | } |