Estimation of oceanic whitecaps using high spatial-resolution optical remote sensing

  • role: First author第一作者
  • Affiliation:

    International Institute for Earth System Science, Nanjing University, Nanjing 210023, China

  • Email:Zhaobi1929@163.com
  • Introduction:E-mail Zhaobi1929@163.com
ZHAO Bi1,  
  • Affiliation:

    National Satellite Ocean Application Service, Beijing 100081, China

    Key Laboratory of Space Ocean Remote Sensing and Applications, Ministry of Natural Resources, Beijing 100081, China

DING Jing23,  
  • Affiliation:

    National Satellite Ocean Application Service, Beijing 100081, China

    Key Laboratory of Space Ocean Remote Sensing and Applications, Ministry of Natural Resources, Beijing 100081, China

LIU Jianqiang23,  
  • Affiliation:

    International Institute for Earth System Science, Nanjing University, Nanjing 210023, China

JIAO Junnan1,  
  • Affiliation:

    International Institute for Earth System Science, Nanjing University, Nanjing 210023, China

TANG Jun1,  
  • role: Corresponding author通信作者
  • Affiliation:

    International Institute for Earth System Science, Nanjing University, Nanjing 210023, China

  • Email:Luyc@nju.edu.cn
  • Introduction:E-mail Luyc@nju.edu.cn
LU Yingcheng1*

реферат

Oceanic whitecaps, generated from wind-wave breaking process, are the medium of air-sea exchange and the indicator of sea surface state. Due to the intense reflection and scattering of incident light, whitecaps can be effectively recognized and distinguished in in-situ photos or videos. Whitecap coverage (W), defined as the proportion of ocean surface covered by whitecaps, is an important parameter for the quantification of whitecaps. Of course, oceanic whitecaps can also be discriminated in high spatial resolution optical remote sensing images, such as Sentinel-2 MSI and Landsat-8 OLI data. This can provide a new research direction in marine environment observation, and may be further used for wind speed monitoring. However, how to estimate oceanic whitecap coverage from these optical remote sensing images is still a challenge. In this study, the formula of whitecap coverage is obtained by converting the form of radiative equation related with the constant and image reflectance of Sentinel-2 MSI data under some assumptions. The background signal of seawater and atmosphere was eliminated by data optimization, and the signal of whitecaps can be distinguished using regional filtering method. Then, whitecap coverage can be estimated. The identification and estimation results indicate that whitecap coverage derived from Sentinel-2 MSI images are consistent with previous studies using in situ observations in the order of magnitude, and can invert sea surface wind speed using a statistical model. Coarse spatial resolution wind speed images converted from MSI inversion were validated by ERA5 wind speed products from European Centre for Medium-Range Weather Forecasts (ECMWF). In addition, whitecap coverage can imply the modulation of other marine environmental dynamic factors (e.g., water mass, ocean fronts, ocean eddies and internal waves). Moreover, it should be noted that sunglint reflection is a non-negligible issue for optical remote sensing of oceanic whitecaps whose signal should be effectively eliminated. Examining the MSI-derived results to HY1-C/D CZI, it indicates that whitecaps can be identified in CZI images when wind speed is greater than 9 m/s, and the reflectance difference between whitecaps and background seawater is 5.8%—8.3%. We hope the above results can be used to improve the accuracy of atmospheric correction, and provide new reference for using high spatial resolution optical remote sensing in sea surface wind speed estimation and marine environmental dynamic factors monitoring. This will hopefully expand the research and application fields of ocean color remote sensing.

ключеви́че слова́

optical remote sensing;oceanic whitecaps;sunglint;HY-1C/D;Sentinel-2;MSI;CZI

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