| Analyses of structure of planetary boundary layer in ice camp over Arctic ocean |
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| 引用本文： | 卞林根,陆龙骅,张占海,程斌,逯昌贵. Analyses of structure of planetary boundary layer in ice camp over Arctic ocean[J]. 极地研究(英文版), 2007, 18(1): 8-17 |
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| 作者姓名： | 卞林根 陆龙骅 张占海 程斌 逯昌贵 |
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| 作者单位： | Chinese Academy of Meteorological Sciences，Chinese Academy of Meteorological Sciences，Polar Research Institute of China，Finish Institute of Marine Research Helsinki FIN-00931，Filnand，Chinese Academy of Meteorological Sciences，Beijing 100081，China，Beijing 100081，China，Shanghai 200136，China，Beijing 100081，China |
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| 摘 要： | The vertical structure of Planetary boundary layer over Arctic floating ice is presented by using about 50 atmospheric profiles and relevant data sounded at an ice station over Arctic Ocean from 22 August to 3 September,2003.It shows that the height of the convective boundary layer in day is greater than that of the stability boundary layer in night.The boundary layer can be described as vertical structures of stability,instability and multipling The interaction between relative warm and wet down draft air from up level and cool air of surface layer is significant,which causes stronger wind shear,temperature and humidity inversion with typical wind shear of 10 m/s/100 m,intensity of temperature inversion of 8 ℃/100 m.While the larger pack ice is broken by such process,new ice free area in the high latitudes of arctic ocean.The interactions between air/ice/water are enhanced.The fact helps to understanding characteristics of atmospheric boundary layer and its effect in Arctic floating ice region.
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Analyses of structure of planetary boundary layer in ice camp over Arctic ocean |
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| Bian Lingen,Lu Longhua,Zhang Zhanhai,Cheng Bin,Lu changgui. Analyses of structure of planetary boundary layer in ice camp over Arctic ocean[J]. Chinese Journal of Polar Science, 2007, 18(1): 8-17 |
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| Authors: | Bian Lingen Lu Longhua Zhang Zhanhai Cheng Bin Lu changgui |
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| Abstract: | The vertical structure of Planetary boundary layer over Arctic floating ice is presented by using about 50 atmospheric profiles and relevant data sounded at an ice station over Arctic Ocean from 22 August to 3 September, 2003. It shows that the height of the convective boundary layer in day is greater than that of the stability boundary layer in night. The boundary layer can be described as vertical structures of stability, instability and multipling The interaction between relative warm and wet down draft air from up level and cool air of surface layer is significant, which causes stronger wind shear, temperature and humidity inversion with typical wind shear of 10 m/s/100 m, intensity of temperature inversion of 8 ℃/100 m. While the larger pack ice is broken by such process, new ice free area in the high latitudes of arctic ocean. The interactions between air/ice/water are enhanced. The fact helps to understanding characteristics of atmospheric boundary layer and its effect in Arctic floating ice region. |
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| Keywords: | Arctic Ocean atmospheric profile sounding boundary layer structure Arctic ocean camp planetary boundary layer structure fact understanding characteristics atmospheric boundary layer effect region water interactions free area high pack ice process intensity temperature inversion humidity |
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