Changes
On December 3, 2022 at 10:20:03 AM UTC,
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Changed title to CASIWAL Presentation NO.7 (previously CAIW交流报告_第七期)
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Moved CASIWAL Presentation NO.7 from http://115.29.142.79/dataset/zhongfen_7th to http://115.29.142.79/dataset/casiwal_7th
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| 7 | { | ||||
| 8 | "description": "Youth Group on Cryosphere | ||||
| 9 | Air-Snow-Ice-Water-Land (CASIWAL) interactions, observation, modeling, | ||||
| 10 | and process seminar series initiated by the cooperation with Polar and | ||||
| 11 | Cryosphere. | ||||
| 12 | 62a5\u544a\u4fe1\u606f\uff1ahttp://115.29.142.79/group/casiwal\u3002", | ||||
| 13 | "display_name": "Cryosphere Air-Snow-Ice-Water-Land (CASIWAL)", | ||||
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| 16 | 5.29.142.79/uploads/group/2022-01-21-132035.27590220220121211935.png", | ||||
| 17 | "name": "casiwal", | ||||
| 18 | "title": "Cryosphere Air-Snow-Ice-Water-Land (CASIWAL)" | ||||
| 19 | } | ||||
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| 13 | "metadata_created": "2022-11-02T13:15:42.925328", | 27 | "metadata_created": "2022-11-02T13:15:42.925328", | ||
| n | 14 | "metadata_modified": "2022-11-02T13:16:13.002002", | n | 28 | "metadata_modified": "2022-12-03T10:20:03.088731", |
| 15 | "name": "zhongfen_7th", | 29 | "name": "casiwal_7th", | ||
| 16 | "notes": "Abstract:\r\nVariations in Arctic sea ice are not only | 30 | "notes": "Abstract:\r\nVariations in Arctic sea ice are not only | ||
| 17 | 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 | ||
| 18 | properties.The microstructure of summer Arctic sea ice changes | 32 | properties.The microstructure of summer Arctic sea ice changes | ||
| 19 | simultaneously due to vary ing external forcing,ice ageand extended | 33 | simultaneously due to vary ing external forcing,ice ageand extended | ||
| 20 | melting seasons that affect its optical properties Thus, knowledge of | 34 | melting seasons that affect its optical properties Thus, knowledge of | ||
| 21 | the role ofinternal variations on the partitioning ofincident solar | 35 | the role ofinternal variations on the partitioning ofincident solar | ||
| 22 | shortwave radiation within the ice and upper ocean is important.We | 36 | shortwave radiation within the ice and upper ocean is important.We | ||
| 23 | investigated the sensitivity of the opti- cal properties of summer ice | 37 | investigated the sensitivity of the opti- cal properties of summer ice | ||
| 24 | on ice microstructures.The results show that gas bubbles are the | 38 | on ice microstructures.The results show that gas bubbles are the | ||
| 25 | predominant scatterers within sea ice.Their effects on the scattering | 39 | predominant scatterers within sea ice.Their effects on the scattering | ||
| 26 | coefficient and ice albedo are 5 and 20 times stronger, | 40 | coefficient and ice albedo are 5 and 20 times stronger, | ||
| 27 | 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 | ||
| 28 | 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 | ||
| 29 | were used to estimate the variations in the inherent optical | 43 | were used to estimate the variations in the inherent optical | ||
| 30 | properties(IOPs ofice and further effects on the radiation budget of | 44 | properties(IOPs ofice and further effects on the radiation budget of | ||
| 31 | sea iceThe modeled results reveal that variations in ice IOPs of | 45 | sea iceThe modeled results reveal that variations in ice IOPs of | ||
| 32 | different ice layers are different.These variations are related to the | 46 | different ice layers are different.These variations are related to the | ||
| 33 | increasing air temperature and decreasing ice ages.At the Arctic basin | 47 | increasing air temperature and decreasing ice ages.At the Arctic basin | ||
| 34 | scalethe changing OPs ofice greatly changed the amount of solar | 48 | scalethe changing OPs ofice greatly changed the amount of solar | ||
| 35 | radiation transmitted to the upper ocean even when a constant ice | 49 | radiation transmitted to the upper ocean even when a constant ice | ||
| 36 | thickness was assumed. especially in marginal ice zonesimplying | 50 | thickness was assumed. especially in marginal ice zonesimplying | ||
| 37 | different sea ice bottom melt.These find ings revealed the important | 51 | different sea ice bottom melt.These find ings revealed the important | ||
| 38 | role of the microstructure ofice in affecting the radiation budget of | 52 | role of the microstructure ofice in affecting the radiation budget of | ||
| 39 | Arctic sea ice.\r\nThis work has been | 53 | Arctic sea ice.\r\nThis work has been | ||
| 40 | published:https://doi.org/103389/fmars2022.861994 Short-bio:\r\nMiao | 54 | published:https://doi.org/103389/fmars2022.861994 Short-bio:\r\nMiao | ||
| 41 | YU is a PhD candidate from the Dalian University | 55 | YU is a PhD candidate from the Dalian University | ||
| 42 | ofTechnology(Supervisor Peng LU) His research interests are the | 56 | ofTechnology(Supervisor Peng LU) His research interests are the | ||
| 43 | changes in sea ice on different scales and understanding the corre | 57 | changes in sea ice on different scales and understanding the corre | ||
| 44 | sponding physical processes. The recent study is focused on the | 58 | sponding physical processes. The recent study is focused on the | ||
| 45 | 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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| 48 | "organization": { | 62 | "organization": { | ||
| 49 | "approval_status": "approved", | 63 | "approval_status": "approved", | ||
| 50 | "created": "2020-04-30T11:11:08.802657", | 64 | "created": "2020-04-30T11:11:08.802657", | ||
| 51 | "description": "Aerospace Information Research Institute (AIR) | 65 | "description": "Aerospace Information Research Institute (AIR) | ||
| 52 | under the Chinese Academy of Sciences (CAS) was established in July | 66 | under the Chinese Academy of Sciences (CAS) was established in July | ||
| 53 | 2017, following the approval for consolidation of three CAS | 67 | 2017, following the approval for consolidation of three CAS | ||
| 54 | institutes: the Institute of Electronics (IECAS), the Institute of | 68 | institutes: the Institute of Electronics (IECAS), the Institute of | ||
| 55 | Remote Sensing and Digital Earth (RADI), and the Academy of | 69 | Remote Sensing and Digital Earth (RADI), and the Academy of | ||
| 56 | Opto-Electronics (AOE) at CAS President Board Meeting. The merger is | 70 | Opto-Electronics (AOE) at CAS President Board Meeting. The merger is | ||
| 57 | the outcome of CAS efforts towards reformation of its R&D system to | 71 | the outcome of CAS efforts towards reformation of its R&D system to | ||
| 58 | meet future R&D challenges and to better meet the national demands.", | 72 | meet future R&D challenges and to better meet the national demands.", | ||
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| 60 | "image_url": "2021-05-18-080509.992585AIRlogo.png", | 74 | "image_url": "2021-05-18-080509.992585AIRlogo.png", | ||
| 61 | "is_organization": true, | 75 | "is_organization": true, | ||
| 62 | "name": "air", | 76 | "name": "air", | ||
| 63 | "state": "active", | 77 | "state": "active", | ||
| 64 | "title": "Aerospace Information Research Institute, CAS", | 78 | "title": "Aerospace Information Research Institute, CAS", | ||
| 65 | "type": "organization" | 79 | "type": "organization" | ||
| 66 | }, | 80 | }, | ||
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| t | 98 | "title": "CAIW\u4ea4\u6d41\u62a5\u544a_\u7b2c\u4e03\u671f", | t | 112 | "title": "CASIWAL Presentation NO.7", |
| 99 | "type": "dataset", | 113 | "type": "dataset", | ||
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| 102 | } | 116 | } |
