Observation of surface radiation and turbulent flux on drift ice over the Arctic Ocean in summer 2016

Shen Hui; Yang Qinghua; Sun Qizhen; Sun Xiaoyu; Zhao Jiechen; Zhang Lin

doi:10.3969/j.issn.0253-4193.2019.03.002

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Shen Hui, Yang Qinghua, Sun Qizhen, Sun Xiaoyu, Zhao Jiechen, Zhang Lin. Observation of surface radiation and turbulent flux on drift ice over the Arctic Ocean in summer 2016[J]. Haiyang Xuebao, 2019, 41(3): 12-22. doi: 10.3969/j.issn.0253-4193.2019.03.002

Citation:

Shen Hui, Yang Qinghua, Sun Qizhen, Sun Xiaoyu, Zhao Jiechen, Zhang Lin. Observation of surface radiation and turbulent flux on drift ice over the Arctic Ocean in summer 2016[J]. Haiyang Xuebao, 2019, 41(3): 12-22. doi: 10.3969/j.issn.0253-4193.2019.03.002

Citation:

Shen Hui, Yang Qinghua, Sun Qizhen, Sun Xiaoyu, Zhao Jiechen, Zhang Lin. Observation of surface radiation and turbulent flux on drift ice over the Arctic Ocean in summer 2016[J]. Haiyang Xuebao, 2019, 41(3): 12-22. doi: 10.3969/j.issn.0253-4193.2019.03.002

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Observation of surface radiation and turbulent flux on drift ice over the Arctic Ocean in summer 2016

doi: 10.3969/j.issn.0253-4193.2019.03.002

1.
Key Laboratory of Research on Marine Hazards Forecasting, State Oceanic Administration, National Marine Environmental Forecasting Center, Beijing 100081, China
2.
Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies, School of Atmospheric Sciences, Sun Yat-sen University, Zhuhai 519082, China;Southern Laboratory of Ocean Science and Engineering(Zhuhai), Zhuhai 519082, China

Received Date: 2018-11-05
Rev Recd Date: 2018-12-04

Abstract

Abstract

The surface radiation and turbulent fluxes over 82°N drifting ice in the Arctic Ocean in summer were measured from August 7 to August 14 during the Chinese National Arctic Research Expedition in 2016 (CHINARE2016). The results show that the surface albedo of drifting ice range from 0.64 to 0.92 with an average of 0.78. Four different snow/ice albedo parameterizations (PW79, HIRHAM, ARCSYM and CCSM3) which are used in a variety of climate models are evaluated by comparing with the in-situ observations, the most complex CCSM3 scheme agreed best with the observations, but cannot well capture the rapid increasing of albedo which is induced by snowfall. The average sensible heat flux, latent heat flux and net radiation over the snow/ice surface are 1.73 W/m², 5.55 W/m² and 18.10 W/m², respectively. The melting rate of ice surface is (0.30±0.22) cm/d, which shows that the drifting ice is gaining heat and under rapidly melting. The average momentum flux over the ice surface is 0.098 (kg·m/s)/(m²·s). The momentum flux has a good correlation with the wind speed and the correlation coefficient reached 0.80.
- Arctic Ocean,
- turbulent flux,
- radiation,
- albedo,
- parameterization

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References(38)

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