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On October 16, 2023 at 6:31:25 AM UTC, seanh:
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2 | "author": "", | 2 | "author": "", | ||
3 | "author_email": "", | 3 | "author_email": "", | ||
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15 | "name": "cnisde", | ||||
16 | "title": | ||||
17 | "CNISDE\u6570\u5b57\u6781\u5730\u4e13\u59d4\u5458\u4f1a" | ||||
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10 | "license_title": "", | 23 | "license_title": "", | ||
11 | "maintainer": "", | 24 | "maintainer": "", | ||
12 | "maintainer_email": "", | 25 | "maintainer_email": "", | ||
13 | "metadata_created": "2023-10-16T06:22:33.954097", | 26 | "metadata_created": "2023-10-16T06:22:33.954097", | ||
t | 14 | "metadata_modified": "2023-10-16T06:30:00.835274", | t | 27 | "metadata_modified": "2023-10-16T06:31:25.473403", |
15 | "name": "cnisde_21st", | 28 | "name": "cnisde_21st", | ||
16 | "notes": "Short bio:\r\nXianda Gong received his Ph.D. degree in | 29 | "notes": "Short bio:\r\nXianda Gong received his Ph.D. degree in | ||
17 | Meteorology from the Leibniz Institute for Tropospheric Research in | 30 | Meteorology from the Leibniz Institute for Tropospheric Research in | ||
18 | 2020. He then worked as a Postdoctoral Research Associate at | 31 | 2020. He then worked as a Postdoctoral Research Associate at | ||
19 | Washington University in St. Louis. He joined Westlake University as a | 32 | Washington University in St. Louis. He joined Westlake University as a | ||
20 | principle investigator in 2023. The research focus of Gong\u2019s | 33 | principle investigator in 2023. The research focus of Gong\u2019s | ||
21 | group is to quantify the effects of atmospheric aerosols on radiation, | 34 | group is to quantify the effects of atmospheric aerosols on radiation, | ||
22 | clouds, and climate in remote marine environments and polar regions. | 35 | clouds, and climate in remote marine environments and polar regions. | ||
23 | Dr. Gong has published 18 peer-reviewed papers in journals such as | 36 | Dr. Gong has published 18 peer-reviewed papers in journals such as | ||
24 | Nature Geoscience, Bulletin of American Meteorology Society, | 37 | Nature Geoscience, Bulletin of American Meteorology Society, | ||
25 | Atmospheric Chemistry and Physics, etc.\r\nAbstract:\r\nThe Arctic | 38 | Atmospheric Chemistry and Physics, etc.\r\nAbstract:\r\nThe Arctic | ||
26 | warms nearly four times faster than the global average, and aerosols | 39 | warms nearly four times faster than the global average, and aerosols | ||
27 | play an increasingly important role in Arctic climate change. Here we | 40 | play an increasingly important role in Arctic climate change. Here we | ||
28 | present observational evidence of abundant sea salt aerosol production | 41 | present observational evidence of abundant sea salt aerosol production | ||
29 | from blowing snow in the central Arctic. Blowing snow was observed | 42 | from blowing snow in the central Arctic. Blowing snow was observed | ||
30 | more than 20% of the time from November to April. The sublimation of | 43 | more than 20% of the time from November to April. The sublimation of | ||
31 | blowing snow generates high concentrations of fine-mode sea salt | 44 | blowing snow generates high concentrations of fine-mode sea salt | ||
32 | aerosol (diameter below 300\u2009nm), enhancing cloud condensation | 45 | aerosol (diameter below 300\u2009nm), enhancing cloud condensation | ||
33 | nuclei concentrations up to tenfold above background levels. Using a | 46 | nuclei concentrations up to tenfold above background levels. Using a | ||
34 | global chemical transport model, we estimate that from November to | 47 | global chemical transport model, we estimate that from November to | ||
35 | April north of 70\u00b0\u2009N, sea salt aerosol produced from blowing | 48 | April north of 70\u00b0\u2009N, sea salt aerosol produced from blowing | ||
36 | snow accounts for about 27.6% of the total particle number, and the | 49 | snow accounts for about 27.6% of the total particle number, and the | ||
37 | sea salt aerosol increases the longwave emissivity of clouds, leading | 50 | sea salt aerosol increases the longwave emissivity of clouds, leading | ||
38 | to a calculated surface warming of | 51 | to a calculated surface warming of | ||
39 | +2.30\u2009W\u2009m\u22122\u00a0under cloudy sky conditions.", | 52 | +2.30\u2009W\u2009m\u22122\u00a0under cloudy sky conditions.", | ||
40 | "num_resources": 0, | 53 | "num_resources": 0, | ||
41 | "num_tags": 0, | 54 | "num_tags": 0, | ||
42 | "organization": { | 55 | "organization": { | ||
43 | "approval_status": "approved", | 56 | "approval_status": "approved", | ||
44 | "created": "2022-12-03T18:02:48.312360", | 57 | "created": "2022-12-03T18:02:48.312360", | ||
45 | "description": | 58 | "description": | ||
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54 | "is_organization": true, | 67 | "is_organization": true, | ||
55 | "name": "cnisde_", | 68 | "name": "cnisde_", | ||
56 | "state": "active", | 69 | "state": "active", | ||
57 | "title": "CNISDE\u6570\u5b57\u6781\u5730\u4e13\u59d4\u5458\u4f1a", | 70 | "title": "CNISDE\u6570\u5b57\u6781\u5730\u4e13\u59d4\u5458\u4f1a", | ||
58 | "type": "organization" | 71 | "type": "organization" | ||
59 | }, | 72 | }, | ||
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61 | "private": false, | 74 | "private": false, | ||
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63 | "relationships_as_subject": [], | 76 | "relationships_as_subject": [], | ||
64 | "resources": [], | 77 | "resources": [], | ||
65 | "state": "draft", | 78 | "state": "draft", | ||
66 | "tags": [], | 79 | "tags": [], | ||
67 | "title": | 80 | "title": | ||
68 | 1\u4e00\u671f\uff08\u5bab\u5148\u8fbe-\u897f\u6e56\u5927\u5b66\uff09", | 81 | 1\u4e00\u671f\uff08\u5bab\u5148\u8fbe-\u897f\u6e56\u5927\u5b66\uff09", | ||
69 | "type": "dataset", | 82 | "type": "dataset", | ||
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71 | "version": "" | 84 | "version": "" | ||
72 | } | 85 | } |