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f | 1 | { | f | 1 | { |
2 | "author": "Albern, Nicole", | 2 | "author": "Albern, Nicole", | ||
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": "10.35097/1217", | 5 | "doi": "10.35097/1217", | ||
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 | "extra_authors": [ | 9 | "extra_authors": [ | ||
10 | { | 10 | { | ||
11 | "extra_author": "Voigt, Aiko", | 11 | "extra_author": "Voigt, Aiko", | ||
12 | "orcid": "" | 12 | "orcid": "" | ||
13 | }, | 13 | }, | ||
14 | { | 14 | { | ||
15 | "extra_author": "Thompson, David W. J.", | 15 | "extra_author": "Thompson, David W. J.", | ||
16 | "orcid": "" | 16 | "orcid": "" | ||
17 | }, | 17 | }, | ||
18 | { | 18 | { | ||
19 | "extra_author": "Pinto, Joaquim G.", | 19 | "extra_author": "Pinto, Joaquim G.", | ||
20 | "orcid": "" | 20 | "orcid": "" | ||
21 | } | 21 | } | ||
22 | ], | 22 | ], | ||
23 | "groups": [], | 23 | "groups": [], | ||
24 | "id": "96fb9923-e96b-4e8a-9ed5-346f6906f698", | 24 | "id": "96fb9923-e96b-4e8a-9ed5-346f6906f698", | ||
25 | "isopen": false, | 25 | "isopen": false, | ||
26 | "license_id": "CC BY 4.0 Attribution", | 26 | "license_id": "CC BY 4.0 Attribution", | ||
27 | "license_title": "CC BY 4.0 Attribution", | 27 | "license_title": "CC BY 4.0 Attribution", | ||
28 | "metadata_created": "2023-08-04T08:50:20.543284", | 28 | "metadata_created": "2023-08-04T08:50:20.543284", | ||
t | 29 | "metadata_modified": "2023-08-04T09:04:05.043829", | t | 29 | "metadata_modified": "2023-08-04T09:28:58.719286", |
30 | "name": "rdr-doi-10-35097-1217", | 30 | "name": "rdr-doi-10-35097-1217", | ||
31 | "notes": "TechnicalRemarks: The simulations were performed with the | 31 | "notes": "TechnicalRemarks: The simulations were performed with the | ||
32 | atmospheric component of the ICON model. The model is run with the | 32 | atmospheric component of the ICON model. The model is run with the | ||
33 | physics package used for numerical weather prediction (version | 33 | physics package used for numerical weather prediction (version | ||
34 | 2.1.00). The simulations are performed in R2B04 horizontal resolution | 34 | 2.1.00). The simulations are performed in R2B04 horizontal resolution | ||
35 | (approximately 160km) with 47 levels extending up to 75km. A time step | 35 | (approximately 160km) with 47 levels extending up to 75km. A time step | ||
36 | of 720s is used.\r\nWe use a present-day setup and the cloud-locking | 36 | of 720s is used.\r\nWe use a present-day setup and the cloud-locking | ||
37 | method to determine the impact of regional cloud-radiative changes in | 37 | method to determine the impact of regional cloud-radiative changes in | ||
38 | the tropics, midlatitudes and polar region.\r\n\r\nThis data has to be | 38 | the tropics, midlatitudes and polar region.\r\n\r\nThis data has to be | ||
39 | used together with 10.5445/IR/1000094317 (ICON model simulations for | 39 | used together with 10.5445/IR/1000094317 (ICON model simulations for | ||
40 | publication \"Cloud-radiative impact on the regional responses of the | 40 | publication \"Cloud-radiative impact on the regional responses of the | ||
41 | midlatitude jet streams and storm tracks to global warming\") to | 41 | midlatitude jet streams and storm tracks to global warming\") to | ||
42 | determine both the role of global and regional cloud-radiative | 42 | determine both the role of global and regional cloud-radiative | ||
43 | changes.\r\n\r\nThe numbers after T (sea-surface temperature) and C | 43 | changes.\r\n\r\nThe numbers after T (sea-surface temperature) and C | ||
44 | (cloud-radiative properties) in the cloud-locked simulations are\r\n- | 44 | (cloud-radiative properties) in the cloud-locked simulations are\r\n- | ||
45 | 1 for the control simulation\r\n- 2 for the simulation with a uniform | 45 | 1 for the control simulation\r\n- 2 for the simulation with a uniform | ||
46 | SST increase.\r\n\r\nFor the regional cloud-radiative changes, the | 46 | SST increase.\r\n\r\nFor the regional cloud-radiative changes, the | ||
47 | number after C refers to the cloud-radiative properties in region | 47 | number after C refers to the cloud-radiative properties in region | ||
48 | reg\r\n- TR for tropics (30S-30N)\r\n- ML for midlatitudes (30N-60N, | 48 | reg\r\n- TR for tropics (30S-30N)\r\n- ML for midlatitudes (30N-60N, | ||
49 | 30S-60S)\r\n- PO for polar regions (60N-90N, 60S-90S)\r\n\r\nT1C2TR | 49 | 30S-60S)\r\n- PO for polar regions (60N-90N, 60S-90S)\r\n\r\nT1C2TR | ||
50 | means, for example, that we use C2 clouds in the tropics and C1 clouds | 50 | means, for example, that we use C2 clouds in the tropics and C1 clouds | ||
51 | in the midlatitudes and polar regions.\r\n\r\n# 4d (time-lev-lat-lon) | 51 | in the midlatitudes and polar regions.\r\n\r\n# 4d (time-lev-lat-lon) | ||
52 | data\r\n- ICON-NWP_AMIP_T?C?reg_3d_mm.nc\r\n\r\nThe files contain | 52 | data\r\n- ICON-NWP_AMIP_T?C?reg_3d_mm.nc\r\n\r\nThe files contain | ||
53 | monthly-mean data for 29 years.\r\n\r\n\r\n# storm track (lat-lon) | 53 | monthly-mean data for 29 years.\r\n\r\n\r\n# storm track (lat-lon) | ||
54 | data\r\n- st_ICON-NWP_AMIP_T?C?reg_geopot500.nc: time-mean storm track | 54 | data\r\n- st_ICON-NWP_AMIP_T?C?reg_geopot500.nc: time-mean storm track | ||
55 | (mean over all years)\r\n- st_T?C?reg_1980to2008.nc: time series of | 55 | (mean over all years)\r\n- st_T?C?reg_1980to2008.nc: time series of | ||
56 | annual-mean storm track data\r\n\r\n- | 56 | annual-mean storm track data\r\n\r\n- | ||
57 | st_ICON-NWP_AMIP_T?C?reg_geopot500_DJF.nc: time-mean storm track for | 57 | st_ICON-NWP_AMIP_T?C?reg_geopot500_DJF.nc: time-mean storm track for | ||
58 | DJF season (mean over all years)\r\n- st_T?C?reg_1980to2008_DJF.nc: | 58 | DJF season (mean over all years)\r\n- st_T?C?reg_1980to2008_DJF.nc: | ||
59 | time series of DJF storm track data\r\n\r\n-> analogously for MAM, | 59 | time series of DJF storm track data\r\n\r\n-> analogously for MAM, | ||
60 | JJA, SON\r\n\r\n\r\n# transient and stationary components of eddy | 60 | JJA, SON\r\n\r\n\r\n# transient and stationary components of eddy | ||
61 | momentum flux and eddy heat flux, (time-lev-lat-lon) | 61 | momentum flux and eddy heat flux, (time-lev-lat-lon) | ||
62 | data\r\nICON-NWP_AMIP_T?C?_vT_uv_stationary_transient_mm.nc (global | 62 | data\r\nICON-NWP_AMIP_T?C?_vT_uv_stationary_transient_mm.nc (global | ||
63 | cloud | 63 | cloud | ||
64 | changes)\r\nICON-NWP_AMIP_T?C?reg_vT_uv_stationary_transient_mm.nc | 64 | changes)\r\nICON-NWP_AMIP_T?C?reg_vT_uv_stationary_transient_mm.nc | ||
65 | (regional cloud changes)\r\n\r\nVariables:\r\n- vTtrans: eddy heat | 65 | (regional cloud changes)\r\n\r\nVariables:\r\n- vTtrans: eddy heat | ||
66 | flux, transient component\r\n- uvtrans: eddy momentum flux, transient | 66 | flux, transient component\r\n- uvtrans: eddy momentum flux, transient | ||
67 | component\r\n- vTstat: eddy heat flux, stationary component\r\n- | 67 | component\r\n- vTstat: eddy heat flux, stationary component\r\n- | ||
68 | uvstat: eddy momentum flux, stationary component\r\n\r\nThe files | 68 | uvstat: eddy momentum flux, stationary component\r\n\r\nThe files | ||
69 | contain monthly-mean data for 29 years.", | 69 | contain monthly-mean data for 29 years.", | ||
70 | "num_resources": 0, | 70 | "num_resources": 0, | ||
71 | "num_tags": 4, | 71 | "num_tags": 4, | ||
72 | "orcid": "", | 72 | "orcid": "", | ||
73 | "organization": { | 73 | "organization": { | ||
74 | "approval_status": "approved", | 74 | "approval_status": "approved", | ||
75 | "created": "2023-01-12T13:30:23.238233", | 75 | "created": "2023-01-12T13:30:23.238233", | ||
76 | "description": "RADAR (Research Data Repository) is a | 76 | "description": "RADAR (Research Data Repository) is a | ||
77 | cross-disciplinary repository for archiving and publishing research | 77 | cross-disciplinary repository for archiving and publishing research | ||
78 | data from completed scientific studies and projects. The focus is on | 78 | data from completed scientific studies and projects. The focus is on | ||
79 | research data from subjects that do not yet have their own | 79 | research data from subjects that do not yet have their own | ||
80 | discipline-specific infrastructures for research data management. ", | 80 | discipline-specific infrastructures for research data management. ", | ||
81 | "id": "013c89a9-383c-4200-8baa-0f78bf1d91f9", | 81 | "id": "013c89a9-383c-4200-8baa-0f78bf1d91f9", | ||
82 | "image_url": "radar-logo.svg", | 82 | "image_url": "radar-logo.svg", | ||
83 | "is_organization": true, | 83 | "is_organization": true, | ||
84 | "name": "radar", | 84 | "name": "radar", | ||
85 | "state": "active", | 85 | "state": "active", | ||
86 | "title": "RADAR", | 86 | "title": "RADAR", | ||
87 | "type": "organization" | 87 | "type": "organization" | ||
88 | }, | 88 | }, | ||
89 | "owner_org": "013c89a9-383c-4200-8baa-0f78bf1d91f9", | 89 | "owner_org": "013c89a9-383c-4200-8baa-0f78bf1d91f9", | ||
90 | "private": false, | 90 | "private": false, | ||
91 | "production_year": "2019", | 91 | "production_year": "2019", | ||
92 | "publication_year": "2023", | 92 | "publication_year": "2023", | ||
93 | "publishers": [ | 93 | "publishers": [ | ||
94 | { | 94 | { | ||
95 | "publisher": "Karlsruhe Institute of Technology" | 95 | "publisher": "Karlsruhe Institute of Technology" | ||
96 | } | 96 | } | ||
97 | ], | 97 | ], | ||
98 | "relationships_as_object": [], | 98 | "relationships_as_object": [], | ||
99 | "relationships_as_subject": [], | 99 | "relationships_as_subject": [], | ||
100 | "repository_name": "RADAR (Research Data Repository)", | 100 | "repository_name": "RADAR (Research Data Repository)", | ||
101 | "resources": [], | 101 | "resources": [], | ||
102 | "services_used_list": "", | 102 | "services_used_list": "", | ||
103 | "source_metadata_created": "2023", | 103 | "source_metadata_created": "2023", | ||
104 | "source_metadata_modified": "", | 104 | "source_metadata_modified": "", | ||
105 | "state": "active", | 105 | "state": "active", | ||
106 | "subject_areas": [ | 106 | "subject_areas": [ | ||
107 | { | 107 | { | ||
108 | "subject_area_additional": "", | 108 | "subject_area_additional": "", | ||
109 | "subject_area_name": "Geological Science" | 109 | "subject_area_name": "Geological Science" | ||
110 | } | 110 | } | ||
111 | ], | 111 | ], | ||
112 | "tags": [ | 112 | "tags": [ | ||
113 | { | 113 | { | ||
114 | "display_name": "ICON-NWP", | 114 | "display_name": "ICON-NWP", | ||
115 | "id": "ce7df5c3-20a0-4d23-8f87-9c4c927eeb8e", | 115 | "id": "ce7df5c3-20a0-4d23-8f87-9c4c927eeb8e", | ||
116 | "name": "ICON-NWP", | 116 | "name": "ICON-NWP", | ||
117 | "state": "active", | 117 | "state": "active", | ||
118 | "vocabulary_id": null | 118 | "vocabulary_id": null | ||
119 | }, | 119 | }, | ||
120 | { | 120 | { | ||
121 | "display_name": "climate change", | 121 | "display_name": "climate change", | ||
122 | "id": "6ca81aa5-bfe8-49d9-ac32-5be4ca6d3bc6", | 122 | "id": "6ca81aa5-bfe8-49d9-ac32-5be4ca6d3bc6", | ||
123 | "name": "climate change", | 123 | "name": "climate change", | ||
124 | "state": "active", | 124 | "state": "active", | ||
125 | "vocabulary_id": null | 125 | "vocabulary_id": null | ||
126 | }, | 126 | }, | ||
127 | { | 127 | { | ||
128 | "display_name": "cloud-radiative changes", | 128 | "display_name": "cloud-radiative changes", | ||
129 | "id": "d295e31d-f34f-4ccb-a688-c1d5befde76c", | 129 | "id": "d295e31d-f34f-4ccb-a688-c1d5befde76c", | ||
130 | "name": "cloud-radiative changes", | 130 | "name": "cloud-radiative changes", | ||
131 | "state": "active", | 131 | "state": "active", | ||
132 | "vocabulary_id": null | 132 | "vocabulary_id": null | ||
133 | }, | 133 | }, | ||
134 | { | 134 | { | ||
135 | "display_name": "midlatitude circulation", | 135 | "display_name": "midlatitude circulation", | ||
136 | "id": "a80c0209-0a0c-4faf-b585-ada99cae7335", | 136 | "id": "a80c0209-0a0c-4faf-b585-ada99cae7335", | ||
137 | "name": "midlatitude circulation", | 137 | "name": "midlatitude circulation", | ||
138 | "state": "active", | 138 | "state": "active", | ||
139 | "vocabulary_id": null | 139 | "vocabulary_id": null | ||
140 | } | 140 | } | ||
141 | ], | 141 | ], | ||
142 | "title": "Icon model simulations for publication \"the role of | 142 | "title": "Icon model simulations for publication \"the role of | ||
143 | tropical, midlatitude and polar cloud-radiative changes for the | 143 | tropical, midlatitude and polar cloud-radiative changes for the | ||
144 | midlatitude circulation response to global warming\"", | 144 | midlatitude circulation response to global warming\"", | ||
145 | "type": "vdataset", | 145 | "type": "vdataset", | ||
146 | "url": "https://doi.org/10.35097/1217" | 146 | "url": "https://doi.org/10.35097/1217" | ||
147 | } | 147 | } |