Sea ice in the Arctic Ocean plays an important role in the global climate change, and its quick change and impact are the scientists' focus all over the world. The spectra of different kinds of sea ice were measured with portable ASD FieldSpec 3 spectrometer during the long-term ice station of the 4th Chinese national Arctic Expedition in 2010, and the spectral features were analyzed systematically. The results indicated that the reflectance of sea ice covered by snow is the highest one, naked sea ice the second, and melted sea ice the lowest. Peak and valley characteristics of spectrum curves of sea ice covered by thick snow, thin snow, wet snow and snow crystal are very significant, and the reflectance basically decreases with the wavelength increasing. The rules of reflectance change with wavelength of natural sea ice, white ice and blue ice are basically same, the reflectance of them is medium, and that of grey ice is far lower than natural sea ice, white ice and blue ice. It is very significant for scientific research to analyze the spectral features of sea ice in the Arctic Ocean and to implement the quantitative remote sensing of sea ice, and to further analyze its response to the global warming.%北极海冰对全球气候变化有着举足轻重的作用,它的快速变化及其影响是国内外关注的焦点.采用ASD FieldSpec 3便携式地物光谱仪,在2010年中国第4次北极科学考察的长期冰站观测期间对不同类型的海冰进行了野外光谱测量,系统分析了光谱特征.结果表明积雪覆盖海冰的光谱反射率最高,裸露海冰其次,表层消融的海冰(有融池)最低.厚雪、薄雪、湿雪、雪晶的光谱曲线峰谷特征明显,基本都随波长的增加反射率降低.天然海冰、白冰、蓝冰的反射率随波长的变化基本一致,反射率居于中等,灰冰的反射率远低于天然海冰、白冰和蓝冰.分析北极海冰的波谱特性,探索北极海冰的定量遥感研究,进而分析其对全球变暖的响应,具有重要的科学意义.
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