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Towards a semi-empirical model of the sea ice thickness based on hyperspectral remote sensing in the Bohai Sea

机译:基于高光谱遥感的渤海海冰厚度半经验模型

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摘要

Sea ice thickness is one of the most important input parameters for the prevention and mitigation of sea ice disasters and the prediction of local sea environments and climates. Estimating the sea ice thickness is currently the most important issue in the study of sea ice remote sensing. With the Bohai Sea as the study area, a semi-empirical model of the sea ice thickness (SEMSIT) that can be used to estimate the thickness of first-year ice based on existing water depth estimation models and hyperspectral remote sensing data according to an optical radiative transfer process in sea ice is proposed. In the model, the absorption and scattering properties of sea ice in different bands (spectral dimension information) are utilized. An integrated attenuation coefficient at the pixel level is estimated using the height of the reflectance peak at 1 088 nm. In addition, the surface reflectance of sea ice at the pixel level is estimated using the 1 550–1 750 nm band reflectance. The model is used to estimate the sea ice thickness with Hyperion images. The first validation results suggest that the proposed model and parameterization scheme can effectively reduce the estimation error associated with the sea ice thickness that is caused by temporal and spatial heterogeneities in the integrated attenuation coefficient and sea ice surface. A practical semi-empirical model and parameterization scheme that may be feasible for the sea ice thickness estimation using hyperspectral remote sensing data are potentially provided.
机译:海冰厚度是预防和减轻海冰灾害以及预测当地海洋环境和气候的最重要输入参数之一。目前,估计海冰厚度是海冰遥感研究中最重要的问题。以渤海为研究区域,可根据现有的水深估算模型和高光谱遥感数据,根据海冰厚度(SEMSIT)的半经验模型来估算第一年冰的厚度。提出了海冰的光辐射传递过程。在该模型中,利用了不同波段中海冰的吸收和散射特性(光谱尺寸信息)。使用1 088 nm处反射峰的高度估算像素级的积分衰减系数。另外,使用1 550–1 750 nm波段的反射率估算像素级海冰的表面反射率。该模型用于通过Hyperion图像估算海冰厚度。初步验证结果表明,所提出的模型和参数化方案可以有效地减少与海冰厚度相关的估计误差,该误差是由综合衰减系数和海冰表面的时间和空间异质性引起的。潜在地提供了一种实用的半经验模型和参数化方案,该方案对于使用高光谱遥感数据进行海冰厚度估算可能是可行的。

著录项

  • 来源
    《海洋学报(英文版)》 |2017年第1期|80-89|共10页
  • 作者单位

    National Marine Environmental Monitoring Center, State 0ceanic Administration, Dalian 116023, China;

    State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing 100875, China;

    Key Laboratory of Spatial Active 0pto-electronic Techniques, Shanghai Institute of Technical Physics, Chinese Academy of Sciences, Shanghai 200083, China;

    Key Laboratory of Spatial Active 0pto-electronic Techniques, Shanghai Institute of Technical Physics, Chinese Academy of Sciences, Shanghai 200083, China;

  • 收录信息 中国科学引文数据库(CSCD);中国科技论文与引文数据库(CSTPCD);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
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  • 入库时间 2022-08-19 03:57:49
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