Changes
On December 3, 2022 at 10:30:47 AM UTC, seanh:
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Moved CASIWAL Presentation NO.7 from organization Aerospace Information Research Institute, CAS to organization JRC-AO
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8 | "description": "Youth Group on Cryosphere | 8 | "description": "Youth Group on Cryosphere | ||
9 | Air-Snow-Ice-Water-Land (CASIWAL) interactions, observation, modeling, | 9 | Air-Snow-Ice-Water-Land (CASIWAL) interactions, observation, modeling, | ||
10 | and process seminar series initiated by the cooperation with Polar and | 10 | and process seminar series initiated by the cooperation with Polar and | ||
11 | Cryosphere. | 11 | Cryosphere. | ||
12 | 62a5\u544a\u4fe1\u606f\uff1ahttp://115.29.142.79/group/casiwal\u3002", | 12 | 62a5\u544a\u4fe1\u606f\uff1ahttp://115.29.142.79/group/casiwal\u3002", | ||
13 | "display_name": "Cryosphere Air-Snow-Ice-Water-Land (CASIWAL)", | 13 | "display_name": "Cryosphere Air-Snow-Ice-Water-Land (CASIWAL)", | ||
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17 | "name": "casiwal", | 17 | "name": "casiwal", | ||
18 | "title": "Cryosphere Air-Snow-Ice-Water-Land (CASIWAL)" | 18 | "title": "Cryosphere Air-Snow-Ice-Water-Land (CASIWAL)" | ||
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n | 28 | "metadata_modified": "2022-12-03T10:20:03.088731", | n | 28 | "metadata_modified": "2022-12-03T10:30:47.829219", |
29 | "name": "casiwal_7th", | 29 | "name": "casiwal_7th", | ||
30 | "notes": "Abstract:\r\nVariations in Arctic sea ice are not only | 30 | "notes": "Abstract:\r\nVariations in Arctic sea ice are not only | ||
31 | apparent in the extent and thickness but also in its inter nal | 31 | apparent in the extent and thickness but also in its inter nal | ||
32 | properties.The microstructure of summer Arctic sea ice changes | 32 | properties.The microstructure of summer Arctic sea ice changes | ||
33 | simultaneously due to vary ing external forcing,ice ageand extended | 33 | simultaneously due to vary ing external forcing,ice ageand extended | ||
34 | melting seasons that affect its optical properties Thus, knowledge of | 34 | melting seasons that affect its optical properties Thus, knowledge of | ||
35 | the role ofinternal variations on the partitioning ofincident solar | 35 | the role ofinternal variations on the partitioning ofincident solar | ||
36 | shortwave radiation within the ice and upper ocean is important.We | 36 | shortwave radiation within the ice and upper ocean is important.We | ||
37 | investigated the sensitivity of the opti- cal properties of summer ice | 37 | investigated the sensitivity of the opti- cal properties of summer ice | ||
38 | on ice microstructures.The results show that gas bubbles are the | 38 | on ice microstructures.The results show that gas bubbles are the | ||
39 | predominant scatterers within sea ice.Their effects on the scattering | 39 | predominant scatterers within sea ice.Their effects on the scattering | ||
40 | coefficient and ice albedo are 5 and 20 times stronger, | 40 | coefficient and ice albedo are 5 and 20 times stronger, | ||
41 | respectively,than the effect of brine pockets\r\nSea ice cores sampled | 41 | respectively,than the effect of brine pockets\r\nSea ice cores sampled | ||
42 | in the Pacific Sector of the Arctic during the summers of 2008 to 2016 | 42 | in the Pacific Sector of the Arctic during the summers of 2008 to 2016 | ||
43 | were used to estimate the variations in the inherent optical | 43 | were used to estimate the variations in the inherent optical | ||
44 | properties(IOPs ofice and further effects on the radiation budget of | 44 | properties(IOPs ofice and further effects on the radiation budget of | ||
45 | sea iceThe modeled results reveal that variations in ice IOPs of | 45 | sea iceThe modeled results reveal that variations in ice IOPs of | ||
46 | different ice layers are different.These variations are related to the | 46 | different ice layers are different.These variations are related to the | ||
47 | increasing air temperature and decreasing ice ages.At the Arctic basin | 47 | increasing air temperature and decreasing ice ages.At the Arctic basin | ||
48 | scalethe changing OPs ofice greatly changed the amount of solar | 48 | scalethe changing OPs ofice greatly changed the amount of solar | ||
49 | radiation transmitted to the upper ocean even when a constant ice | 49 | radiation transmitted to the upper ocean even when a constant ice | ||
50 | thickness was assumed. especially in marginal ice zonesimplying | 50 | thickness was assumed. especially in marginal ice zonesimplying | ||
51 | different sea ice bottom melt.These find ings revealed the important | 51 | different sea ice bottom melt.These find ings revealed the important | ||
52 | role of the microstructure ofice in affecting the radiation budget of | 52 | role of the microstructure ofice in affecting the radiation budget of | ||
53 | Arctic sea ice.\r\nThis work has been | 53 | Arctic sea ice.\r\nThis work has been | ||
54 | published:https://doi.org/103389/fmars2022.861994 Short-bio:\r\nMiao | 54 | published:https://doi.org/103389/fmars2022.861994 Short-bio:\r\nMiao | ||
55 | YU is a PhD candidate from the Dalian University | 55 | YU is a PhD candidate from the Dalian University | ||
56 | ofTechnology(Supervisor Peng LU) His research interests are the | 56 | ofTechnology(Supervisor Peng LU) His research interests are the | ||
57 | changes in sea ice on different scales and understanding the corre | 57 | changes in sea ice on different scales and understanding the corre | ||
58 | sponding physical processes. The recent study is focused on the | 58 | sponding physical processes. The recent study is focused on the | ||
59 | effects of changing ice micro- structure on ice optical properties.", | 59 | effects of changing ice micro- structure on ice optical properties.", | ||
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61 | "num_tags": 0, | 61 | "num_tags": 0, | ||
62 | "organization": { | 62 | "organization": { | ||
63 | "approval_status": "approved", | 63 | "approval_status": "approved", | ||
n | 64 | "created": "2020-04-30T11:11:08.802657", | n | 64 | "created": "2022-12-03T18:28:36.501371", |
65 | "description": "Aerospace Information Research Institute (AIR) | 65 | "description": "The JRC-AO, Joint Research Center for Arctic | ||
66 | under the Chinese Academy of Sciences (CAS) was established in July | 66 | Observations, is a joint research center for the collabration effort | ||
67 | 2017, following the approval for consolidation of three CAS | 67 | by AIR-CAS, and ASC FMI.", | ||
68 | institutes: the Institute of Electronics (IECAS), the Institute of | 68 | "id": "01f3a7d5-4715-4bd1-886a-4e1c800be33e", | ||
69 | Remote Sensing and Digital Earth (RADI), and the Academy of | 69 | "image_url": "2022-12-03-102836.49099620221203182535.png", | ||
70 | Opto-Electronics (AOE) at CAS President Board Meeting. The merger is | ||||
71 | the outcome of CAS efforts towards reformation of its R&D system to | ||||
72 | meet future R&D challenges and to better meet the national demands.", | ||||
73 | "id": "c25dce84-97be-4153-8b90-d38f9ab73e5f", | ||||
74 | "image_url": "2021-05-18-080509.992585AIRlogo.png", | ||||
75 | "is_organization": true, | 70 | "is_organization": true, | ||
n | 76 | "name": "air", | n | 71 | "name": "jrc-ao_", |
77 | "state": "active", | 72 | "state": "active", | ||
n | 78 | "title": "Aerospace Information Research Institute, CAS", | n | 73 | "title": "JRC-AO", |
79 | "type": "organization" | 74 | "type": "organization" | ||
80 | }, | 75 | }, | ||
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112 | "title": "CASIWAL Presentation NO.7", | 107 | "title": "CASIWAL Presentation NO.7", | ||
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