Changes
On October 16, 2023 at 6:31:33 AM UTC, seanh:
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Added resource 宫先达.png to 数字极地报告_第二十一期(宫先达-西湖大学)
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28 | "name": "cnisde_21st", | 28 | "name": "cnisde_21st", | ||
29 | "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 | ||
30 | Meteorology from the Leibniz Institute for Tropospheric Research in | 30 | Meteorology from the Leibniz Institute for Tropospheric Research in | ||
31 | 2020. He then worked as a Postdoctoral Research Associate at | 31 | 2020. He then worked as a Postdoctoral Research Associate at | ||
32 | Washington University in St. Louis. He joined Westlake University as a | 32 | Washington University in St. Louis. He joined Westlake University as a | ||
33 | principle investigator in 2023. The research focus of Gong\u2019s | 33 | principle investigator in 2023. The research focus of Gong\u2019s | ||
34 | group is to quantify the effects of atmospheric aerosols on radiation, | 34 | group is to quantify the effects of atmospheric aerosols on radiation, | ||
35 | clouds, and climate in remote marine environments and polar regions. | 35 | clouds, and climate in remote marine environments and polar regions. | ||
36 | 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 | ||
37 | Nature Geoscience, Bulletin of American Meteorology Society, | 37 | Nature Geoscience, Bulletin of American Meteorology Society, | ||
38 | Atmospheric Chemistry and Physics, etc.\r\nAbstract:\r\nThe Arctic | 38 | Atmospheric Chemistry and Physics, etc.\r\nAbstract:\r\nThe Arctic | ||
39 | warms nearly four times faster than the global average, and aerosols | 39 | warms nearly four times faster than the global average, and aerosols | ||
40 | play an increasingly important role in Arctic climate change. Here we | 40 | play an increasingly important role in Arctic climate change. Here we | ||
41 | present observational evidence of abundant sea salt aerosol production | 41 | present observational evidence of abundant sea salt aerosol production | ||
42 | from blowing snow in the central Arctic. Blowing snow was observed | 42 | from blowing snow in the central Arctic. Blowing snow was observed | ||
43 | 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 | ||
44 | blowing snow generates high concentrations of fine-mode sea salt | 44 | blowing snow generates high concentrations of fine-mode sea salt | ||
45 | aerosol (diameter below 300\u2009nm), enhancing cloud condensation | 45 | aerosol (diameter below 300\u2009nm), enhancing cloud condensation | ||
46 | nuclei concentrations up to tenfold above background levels. Using a | 46 | nuclei concentrations up to tenfold above background levels. Using a | ||
47 | global chemical transport model, we estimate that from November to | 47 | global chemical transport model, we estimate that from November to | ||
48 | 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 | ||
49 | 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 | ||
50 | sea salt aerosol increases the longwave emissivity of clouds, leading | 50 | sea salt aerosol increases the longwave emissivity of clouds, leading | ||
51 | to a calculated surface warming of | 51 | to a calculated surface warming of | ||
52 | +2.30\u2009W\u2009m\u22122\u00a0under cloudy sky conditions.", | 52 | +2.30\u2009W\u2009m\u22122\u00a0under cloudy sky conditions.", | ||
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