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基于光谱特征的HY-1C/D卫星赤潮探测方法

王义衎 刘荣杰 刘建强 丁静 叶小敏 赵鑫 宋冬梅 马毅

王义衎,刘荣杰,刘建强,等. 基于光谱特征的HY-1C/D卫星赤潮探测方法−以红夜光藻为例[J]. 海洋学报,2023,45(12):166–178 doi: 10.12284/hyxb2023179
引用本文: 王义衎,刘荣杰,刘建强,等. 基于光谱特征的HY-1C/D卫星赤潮探测方法−以红夜光藻为例[J]. 海洋学报,2023,45(12):166–178 doi: 10.12284/hyxb2023179
Wang Yikan,Liu Rongjie,Liu Jianqiang, et al. Detection method of red tide based on the spectral features from HY-1C/D satellite: Take red Noctiluca scintillans blooms as an example[J]. Haiyang Xuebao,2023, 45(12):166–178 doi: 10.12284/hyxb2023179
Citation: Wang Yikan,Liu Rongjie,Liu Jianqiang, et al. Detection method of red tide based on the spectral features from HY-1C/D satellite: Take red Noctiluca scintillans blooms as an example[J]. Haiyang Xuebao,2023, 45(12):166–178 doi: 10.12284/hyxb2023179

基于光谱特征的HY-1C/D卫星赤潮探测方法以红夜光藻为例

doi: 10.12284/hyxb2023179
基金项目: 国家重点研发计划项目(2022YFC3105101);国家自然科学基金重大项目(61890964);中韩海洋科学共同研究中心项目(PI-2022-1)。
详细信息
    作者简介:

    王义衎(1999—),女,山东省潍坊市人,主要从事赤潮遥感探测研究。E-mail:wangyikan@126.com

    通讯作者:

    刘荣杰(1981—),男,副研究员,主要从事海洋光学遥感方面研究。E-mail:liurj@fio.org.cn

  • 中图分类号: P714+.5

Detection method of red tide based on the spectral features from HY-1C/D satellite: Take red Noctiluca scintillans blooms as an example

  • 摘要: 红夜光藻是我国主要的赤潮优势种,在渤海、黄海、东海和南海均有发生。近年来,红夜光藻赤潮发生频率明显上升,监测需求迫切。但红夜光藻赤潮发生具有分布范围广、变化速度快、多呈条带状分布的特点,其探测对卫星影像空间分辨率、覆盖范围和重访周期要求高。虽然水色卫星在赤潮监测中发挥了重要作用,但其空间分辨率低,无法准确探测条带状分布的红夜光藻赤潮。海洋一号C、D(HY-1C/D)卫星搭载的海岸带成像仪(Coastal Zone Imager,CZI)以其高空间分辨率、大幅宽和短重访周期的优势,被越来越多地用于赤潮监测。现有的红夜光藻赤潮HY-1C/D CZI探测模型大多基于深度学习方法,需要大量赤潮样本,但赤潮样本获取困难,影响模型的精度。因此,本文以2022年3月发生在广东省汕尾市红海湾的红夜光藻赤潮为例,分析了红夜光藻赤潮光谱特征,基于红夜光藻赤潮在红光和近红外波段的高反射特性和浑浊水体在绿光波段的高反射特性,构建了一个面向HY-1C/D CZI的红夜光藻赤潮探测方法。实验结果表明,该方法可以有效地探测赤潮,并避免浑浊水体的干扰,精确率和F1-Score达到89.72%和0.90。而且,该方法具有较好的适用性,可适用于不同海洋环境、不同宽波段卫星传感器的红夜光藻赤潮探测。
  • 图  1  HY-1C/D CZI、GF-1 WFV光谱响应函数

    Fig.  1  Spectral response functions of HY-1C/D CZI and GF-1 WFV

    图  2  不同卫星传感器数据覆盖范围

    Fig.  2  Data coverage of different satellite sensors

    图  3  不同类型水体样本分布示意图与光谱曲线

    Fig.  3  Schematic distribution and spectral curves of different types of water bodies

    图  4  红光波段基线差示意图

    Fig.  4  Schematic of the baseline difference in the red band

    图  5  红光波段基线差值统计结果

    Fig.  5  Statistical results of the values of the baseline difference in the red band

    图  6  绿光波段基线差的示意图与统计结果

    Fig.  6  Schematic and statistical results of the baseline difference in the green band

    图  7  不同倍数加和局部赤潮探测结果

    Fig.  7  Local red tide detection results of different multiplicative summation

    图  8  不同倍数加和赤潮探测精度

    Fig.  8  Accuracy of red tide detection by different multiplicative summation

    图  9  基于光谱特征的赤潮探测方法流程图

    Fig.  9  Flowchart of red tide detection method based on spectral features

    图  10  HY-1C/D CZI影像赤潮探测结果(红色表示赤潮)

    Fig.  10  HY-1C/D CZI image red tide detection results (red indicates red tide)

    图  11  HY-1C/D CZI影像局部赤潮探测结果(红色表示赤潮)

    Fig.  11  Local red tide detection results of HY-1C/D CZI image (red indicates red tide)

    图  12  浑浊水体区域赤潮探测结果(红色表示赤潮)

    Fig.  12  Red tide detection results in turbid water areas (red indicates red tide)

    图  13  不同赤潮探测方法结果对比(红色表示赤潮)

    Fig.  13  Comparison of results of different red tide detection methods (red indicates red tide)

    图  14  不同赤潮探测方法局部赤潮探测结果(红色表示赤潮)

    Fig.  14  Local red tide detection results of different red tide detection methods (red indicates red tide)

    图  15  不同海洋环境HY-1C CZI影像赤潮探测结果(红色表示赤潮)

    Fig.  15  Red tide detection results of HY-1C CZI images in different marine environments (red indicates red tide)

    图  16  有无薄云覆盖下不同类型水体光谱曲线

    Fig.  16  Spectral curves of different types of water bodies with and without thin cloud cover

    图  17  GF-1 WFV影像赤潮探测结果(红色表示赤潮)

    Fig.  17  GF-1 WFV image red tide detection results (red indicates red tide)

    图  18  归一化处理前后不同类型水体光谱曲线

    Fig.  18  Spectral curves of different types of water bodies before and after normalization

    表  1  HY-1C/D CZI和GF-1 WFV卫星传感器参数

    Tab.  1  HY-1C/D CZI and GF-1 WFV satellite sensor parameters

    传感器 波段 光谱范围/
    nm
    中心波长/
    nm
    空间分辨率/
    m
    幅宽/
    km
    重访周期/
    d
    HY-1C/D CZI 1 420~500 460 50 950 3
    2 520~600 560 50 950 3
    3 610~690 650 50 950 3
    4 760~890 825 50 950 3
    GF-1 WFV 1 450~520 485 16 800 4
    2 520~600 560 16 800 4
    3 630~690 660 16 800 4
    4 760~900 830 16 800 4
    下载: 导出CSV

    表  2  所用卫星影像详细信息

    Tab.  2  Detailed information of satellite images used

    传感器 成像时间 纬度 经度 覆盖区域
    HY-1D CZI 2022年3月13日 19° 29' 44"~24° 33' 38"N 108° 00' 00"~118° 09' 04"E 广东红海湾
    HY-1C CZI 2022年3月14日 19° 39' 52"~24° 44' 10"N 110° 10' 55"~120° 18' 59"E 广东红海湾
    2020年8月17日 31° 38' 33"~34° 44' 11"N 124° 14' 34"~135° 27' 05"E 东海
    2021年2月14日 16° 50' 08"~21° 52' 53"N 105° 48' 27"~115° 37' 30"E 广西北部湾
    GF-1 WFV 2022年3月13日 21° 48' 09"~24° 03' 14"N 114° 34' 08"~117° 12' 22"E 广东红海湾
    下载: 导出CSV

    表  3  不同方法赤潮探测精度

    Tab.  3  Accuracy of red tide detection by different methods

    方法 总体精度/% 精确率/% 召回率/% F1-Score Kappa系数
    RTSI 98.42 89.72 90.16 0.90 0.89
    GF1_RI 97.02 81.90 79.76 0.81 0.79
    下载: 导出CSV
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  • 收稿日期:  2023-05-12
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