Changes
On January 21, 2022 at 1:38:42 PM UTC, Yubao Qiu:
-
Changed title to CAIW交流报告_第三期 (previously 海冰汽交流报告_第三期)
f | 1 | { | f | 1 | { |
2 | "author": "", | 2 | "author": "", | ||
3 | "author_email": "", | 3 | "author_email": "", | ||
4 | "creator_user_id": "2e9fa41b-0394-4070-98d0-205f79d5738b", | 4 | "creator_user_id": "2e9fa41b-0394-4070-98d0-205f79d5738b", | ||
5 | "extras": [], | 5 | "extras": [], | ||
6 | "groups": [ | 6 | "groups": [ | ||
7 | { | 7 | { | ||
n | 8 | "description": "", | n | 8 | "description": "Cryosphere Air-Ice-Water (CAIW) interactions, |
9 | "display_name": "\u4e2d\u82ac\u5408\u4f5c\u4ea4\u6d41", | 9 | observation, modeling and process investigation seminar series | ||
10 | 8c\u8fc7\u7a0b\u7814\u7a76\u53ca\u5b66\u672f\u601d\u60f3\u4ea4\u6d41", | ||||
11 | "display_name": "Cryosphere Air-Ice-Water (CAIW)", | ||||
10 | "id": "300150f1-0aaf-42b4-8022-3dfca52e8b66", | 12 | "id": "300150f1-0aaf-42b4-8022-3dfca52e8b66", | ||
11 | "image_display_url": | 13 | "image_display_url": | ||
n | 12 | "http://115.29.142.79/uploads/group/2022-01-20-012230.388144logo.jpg", | n | 14 | 5.29.142.79/uploads/group/2022-01-21-132035.27590220220121211935.png", |
13 | "name": "zhongfen", | 15 | "name": "zhongfen", | ||
n | 14 | "title": "\u4e2d\u82ac\u5408\u4f5c\u4ea4\u6d41" | n | 16 | "title": "Cryosphere Air-Ice-Water (CAIW)" |
15 | } | 17 | } | ||
16 | ], | 18 | ], | ||
17 | "id": "e1994fce-fc42-4ceb-bb9c-e0b2d60edc6f", | 19 | "id": "e1994fce-fc42-4ceb-bb9c-e0b2d60edc6f", | ||
18 | "isopen": false, | 20 | "isopen": false, | ||
19 | "license_id": "", | 21 | "license_id": "", | ||
20 | "license_title": "", | 22 | "license_title": "", | ||
21 | "maintainer": "", | 23 | "maintainer": "", | ||
22 | "maintainer_email": "", | 24 | "maintainer_email": "", | ||
23 | "metadata_created": "2022-01-20T03:32:20.410837", | 25 | "metadata_created": "2022-01-20T03:32:20.410837", | ||
n | 24 | "metadata_modified": "2022-01-21T13:15:34.105988", | n | 26 | "metadata_modified": "2022-01-21T13:38:42.524462", |
25 | "name": "zhongfen_3th", | 27 | "name": "zhongfen_3th", | ||
26 | "notes": "Abstract:\r\n\r\nStrong offshore wind events (SOWEs) occur | 28 | "notes": "Abstract:\r\n\r\nStrong offshore wind events (SOWEs) occur | ||
27 | frequently near the Antarctic coast during austral winter. These wind | 29 | frequently near the Antarctic coast during austral winter. These wind | ||
28 | events are typically associated with passage of synoptic- or | 30 | events are typically associated with passage of synoptic- or | ||
29 | meso-scale cyclones, which interact with the katabatic wind field and | 31 | meso-scale cyclones, which interact with the katabatic wind field and | ||
30 | affect sea ice and oceanic processes in coastal polynyas. Based on | 32 | affect sea ice and oceanic processes in coastal polynyas. Based on | ||
31 | numerical simulations from the coupled Finite Element Sea-ice Ocean | 33 | numerical simulations from the coupled Finite Element Sea-ice Ocean | ||
32 | Model (FESOM) driven by the CORE-II forcing, coastal polynyas along | 34 | Model (FESOM) driven by the CORE-II forcing, coastal polynyas along | ||
33 | the East Antarctica coast are selected to examine the response of sea | 35 | the East Antarctica coast are selected to examine the response of sea | ||
34 | ice and oceanic properties to SOWEs. In these polynyas, the southern | 36 | ice and oceanic properties to SOWEs. In these polynyas, the southern | ||
35 | or western flanks of cyclones play a crucial role in increasing the | 37 | or western flanks of cyclones play a crucial role in increasing the | ||
36 | offshore winds depending on the local topography. During SOWEs, the | 38 | offshore winds depending on the local topography. During SOWEs, the | ||
37 | offshore component of sea ice velocity increased apparently, which is | 39 | offshore component of sea ice velocity increased apparently, which is | ||
38 | followed by dramatic decrease in sea ice concentration and increase of | 40 | followed by dramatic decrease in sea ice concentration and increase of | ||
39 | sea ice production by up to two to four folds. Formation of high | 41 | sea ice production by up to two to four folds. Formation of high | ||
40 | salinity shelf water (HSSW) is detected in the coastal regions from | 42 | salinity shelf water (HSSW) is detected in the coastal regions from | ||
41 | surface to 800 m layers after several days of the SOWEs. HSSW | 43 | surface to 800 m layers after several days of the SOWEs. HSSW | ||
42 | formation averaged over winter is notably greater in years with longer | 44 | formation averaged over winter is notably greater in years with longer | ||
43 | duration of SOWEs. \r\nThe response of sea ice and water mass to meso- | 45 | duration of SOWEs. \r\nThe response of sea ice and water mass to meso- | ||
44 | and synoptic-scale cyclones are also investigated for the Ross Ice | 46 | and synoptic-scale cyclones are also investigated for the Ross Ice | ||
45 | Shelf Polynya (RISP) based on a numerical model targeted on the Ross | 47 | Shelf Polynya (RISP) based on a numerical model targeted on the Ross | ||
46 | Sea. During the passage of mesoscale cyclones, sea ice production | 48 | Sea. During the passage of mesoscale cyclones, sea ice production | ||
47 | (SIP) increased rapidly over the western side of RISP but decreased | 49 | (SIP) increased rapidly over the western side of RISP but decreased | ||
48 | over the eastern side of RISP resulting from the different branches of | 50 | over the eastern side of RISP resulting from the different branches of | ||
49 | cyclones. When synoptic-scale cyclones prevailed over this region, | 51 | cyclones. When synoptic-scale cyclones prevailed over this region, | ||
50 | increased SIP values emerged over nearly the entire RISP. Under the | 52 | increased SIP values emerged over nearly the entire RISP. Under the | ||
51 | two types of cyclones, HSSW formation is detected when there is a | 53 | two types of cyclones, HSSW formation is detected when there is a | ||
52 | notable increase in SIP in the coastal regions. Enhancement in the | 54 | notable increase in SIP in the coastal regions. Enhancement in the | ||
53 | HSSW formation is mainly observed over the western side of RISP, which | 55 | HSSW formation is mainly observed over the western side of RISP, which | ||
54 | could persistent for 12\u201348 hours after the passage of the | 56 | could persistent for 12\u201348 hours after the passage of the | ||
55 | cyclones. \r\nShort-bio:\r\nXiaoqiao Wang is a PhD candidate from the | 57 | cyclones. \r\nShort-bio:\r\nXiaoqiao Wang is a PhD candidate from the | ||
56 | School of Oceanography, Shanghai Jiao Tong University (supervisor: | 58 | School of Oceanography, Shanghai Jiao Tong University (supervisor: | ||
57 | Zhaoru Zhang). Now, she is visiting the Institute for Atmospheric and | 59 | Zhaoru Zhang). Now, she is visiting the Institute for Atmospheric and | ||
58 | Earth System Research at the University of Helsinki (supervisor: | 60 | Earth System Research at the University of Helsinki (supervisor: | ||
59 | Petteri Uotila). Her research is focused on the impacts of synoptic- | 61 | Petteri Uotila). Her research is focused on the impacts of synoptic- | ||
60 | and meso-scale atmospheric forcing on sea ice and water mass processes | 62 | and meso-scale atmospheric forcing on sea ice and water mass processes | ||
61 | in Antarctic coastal polynyas.", | 63 | in Antarctic coastal polynyas.", | ||
62 | "num_resources": 1, | 64 | "num_resources": 1, | ||
63 | "num_tags": 0, | 65 | "num_tags": 0, | ||
64 | "organization": { | 66 | "organization": { | ||
65 | "approval_status": "approved", | 67 | "approval_status": "approved", | ||
66 | "created": "2020-04-30T11:11:08.802657", | 68 | "created": "2020-04-30T11:11:08.802657", | ||
67 | "description": "Aerospace Information Research Institute (AIR) | 69 | "description": "Aerospace Information Research Institute (AIR) | ||
68 | under the Chinese Academy of Sciences (CAS) was established in July | 70 | under the Chinese Academy of Sciences (CAS) was established in July | ||
69 | 2017, following the approval for consolidation of three CAS | 71 | 2017, following the approval for consolidation of three CAS | ||
70 | institutes: the Institute of Electronics (IECAS), the Institute of | 72 | institutes: the Institute of Electronics (IECAS), the Institute of | ||
71 | Remote Sensing and Digital Earth (RADI), and the Academy of | 73 | Remote Sensing and Digital Earth (RADI), and the Academy of | ||
72 | Opto-Electronics (AOE) at CAS President Board Meeting. The merger is | 74 | Opto-Electronics (AOE) at CAS President Board Meeting. The merger is | ||
73 | the outcome of CAS efforts towards reformation of its R&D system to | 75 | the outcome of CAS efforts towards reformation of its R&D system to | ||
74 | meet future R&D challenges and to better meet the national demands.", | 76 | meet future R&D challenges and to better meet the national demands.", | ||
75 | "id": "c25dce84-97be-4153-8b90-d38f9ab73e5f", | 77 | "id": "c25dce84-97be-4153-8b90-d38f9ab73e5f", | ||
76 | "image_url": "2021-05-18-080509.992585AIRlogo.png", | 78 | "image_url": "2021-05-18-080509.992585AIRlogo.png", | ||
77 | "is_organization": true, | 79 | "is_organization": true, | ||
78 | "name": "air", | 80 | "name": "air", | ||
79 | "state": "active", | 81 | "state": "active", | ||
80 | "title": "Aerospace Information Research Institute, CAS", | 82 | "title": "Aerospace Information Research Institute, CAS", | ||
81 | "type": "organization" | 83 | "type": "organization" | ||
82 | }, | 84 | }, | ||
83 | "owner_org": "c25dce84-97be-4153-8b90-d38f9ab73e5f", | 85 | "owner_org": "c25dce84-97be-4153-8b90-d38f9ab73e5f", | ||
84 | "private": false, | 86 | "private": false, | ||
85 | "relationships_as_object": [], | 87 | "relationships_as_object": [], | ||
86 | "relationships_as_subject": [], | 88 | "relationships_as_subject": [], | ||
87 | "resources": [ | 89 | "resources": [ | ||
88 | { | 90 | { | ||
89 | "cache_last_updated": null, | 91 | "cache_last_updated": null, | ||
90 | "cache_url": null, | 92 | "cache_url": null, | ||
91 | "created": "2022-01-20T03:32:32.896183", | 93 | "created": "2022-01-20T03:32:32.896183", | ||
92 | "datastore_active": false, | 94 | "datastore_active": false, | ||
93 | "description": "", | 95 | "description": "", | ||
94 | "format": "JPEG", | 96 | "format": "JPEG", | ||
95 | "hash": "", | 97 | "hash": "", | ||
96 | "id": "bed490a2-773c-4d6a-b88c-a0b62b08f337", | 98 | "id": "bed490a2-773c-4d6a-b88c-a0b62b08f337", | ||
97 | "last_modified": "2022-01-20T03:32:32.882771", | 99 | "last_modified": "2022-01-20T03:32:32.882771", | ||
98 | "metadata_modified": "2022-01-20T03:32:33.107838", | 100 | "metadata_modified": "2022-01-20T03:32:33.107838", | ||
99 | "mimetype": "image/jpeg", | 101 | "mimetype": "image/jpeg", | ||
100 | "mimetype_inner": null, | 102 | "mimetype_inner": null, | ||
101 | "name": | 103 | "name": | ||
102 | "20211221-\u738b\u5c0f\u4e54\u4e2d\u82ac\u4f1a\u8bae.jpg", | 104 | "20211221-\u738b\u5c0f\u4e54\u4e2d\u82ac\u4f1a\u8bae.jpg", | ||
103 | "package_id": "e1994fce-fc42-4ceb-bb9c-e0b2d60edc6f", | 105 | "package_id": "e1994fce-fc42-4ceb-bb9c-e0b2d60edc6f", | ||
104 | "position": 0, | 106 | "position": 0, | ||
105 | "resource_type": null, | 107 | "resource_type": null, | ||
106 | "size": 4805815, | 108 | "size": 4805815, | ||
107 | "state": "active", | 109 | "state": "active", | ||
108 | "url": | 110 | "url": | ||
109 | resource/bed490a2-773c-4d6a-b88c-a0b62b08f337/download/20211221-.jpg", | 111 | resource/bed490a2-773c-4d6a-b88c-a0b62b08f337/download/20211221-.jpg", | ||
110 | "url_type": "upload" | 112 | "url_type": "upload" | ||
111 | } | 113 | } | ||
112 | ], | 114 | ], | ||
113 | "state": "active", | 115 | "state": "active", | ||
114 | "tags": [], | 116 | "tags": [], | ||
t | 115 | "title": | t | 117 | "title": "CAIW\u4ea4\u6d41\u62a5\u544a_\u7b2c\u4e09\u671f", |
116 | "\u6d77\u51b0\u6c7d\u4ea4\u6d41\u62a5\u544a_\u7b2c\u4e09\u671f", | ||||
117 | "type": "dataset", | 118 | "type": "dataset", | ||
118 | "url": "", | 119 | "url": "", | ||
119 | "version": "" | 120 | "version": "" | ||
120 | } | 121 | } |