首页|基于PlanetScope光学小卫星与ICESat-2激光测高数据的极地冰盖冰面湖水深遥感反演

基于PlanetScope光学小卫星与ICESat-2激光测高数据的极地冰盖冰面湖水深遥感反演

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每年消融期,冰面湖广泛分布于极地冰盖表面,能够存储大量冰面融水,但部分冰面湖底部破裂后会输送融水进入冰盖底部,从而影响冰盖运动与稳定性.因此,准确测算冰面湖水深信息,进而估算冰面湖体积及其动态变化,对于理解极地冰盖水文过程具有重要意义.然而,实地测量冰面湖深度难度大、成本高、覆盖范围小,通过中低空间分辨率光学遥感影像构建的冰面湖水深反演模型精度不足.该研究综合PlanetScope SuperDove光学小卫星8波段遥感影像(空间分辨率为3 m)与ICESat-2激光测高数据反演冰面湖水深.首先,通过自适应核密度估计分离并拟合湖面与湖底ICESat-2激光测高点云,进而获取冰面湖水深观测结果;其次,利用最佳波段比值分析Planet-Scope影像不同波段(组合)与ICESat-2水深数据的相关关系,构建二次函数、指数函数、幂函数与对数函数4种冰面湖水深反演经验公式;最后,选择4个具有同时期PlanetScope和ICESat-2数据覆盖的冰面湖,测试冰面湖水深遥感反演的精度.结果表明PlanetScope绿光I波段是冰面湖水深反演最佳波段,单波段反射率与冰面湖水深相关性最强(R2=0.94),水深反演精度最高(均方根误差为1.0 m,相对均方根误差为0.15).研究揭示了综合主被动卫星数据分析极地冰盖水文过程的良好潜力.
Remote sensing-based bathymetry retrieval of supraglacial lakes on polar ice sheets using images from small optical satellite PlanetScope and ICESat-2 laser altimetry data
During the melt season,supraglacial lakes are widely distributed across polar ice sheets,storing large amounts of surface meltwater.When some of these supraglacial lakes rupture at the bottom,the released meltwater infiltrates ice sheets,affecting their movement and stability.Therefore,accurate bathymetry retrieval of supraglacial lakes and estimating the volume of supraglacial lakes are significant for understanding the hydrological processes of polar ice sheets.However,field measurement of supraglacial lake depth is difficult,costly,and small-scale.Meanwhile,the bathymetry models derived from optical satellite images with low to medium spatial resolutions are insufficiently accurate.Given these,this study conducted the bathymetry retrieval of supraglacial lakes based on eight-band remote sensing images from the small-size optical satellite PlanetScope SuperDove(spatial resolution:3 m)and ICESat-2 laser altimetry data.First,the ICESat-2 laser altimetry point clouds data for the lake surface and bottom were separated and modeled using adaptive kernel density estimation to derive lake depth observations.Second,Optimal Band Ratio Analysis(OBRA)was used to examine the correlations between various bands of PlanetScope images(and combinations thereof)and ICESat-2 bathymetry data,leading to the development of four kinds of empirical formulas for the bathymetry retrieval of supraglacial lakes:quadratic,exponential,power,and logarithmic functions.Then,four supraglacial lakes covered by concurrent PlanetScope and ICESat-2 data were selected to test the retrieval accuracy.The results indicate that the Green Ⅰ band of PlanetScope is the most favorable for the bathymetry retrieval,demonstrating the strongest correlation with the ICESat-2 derived depths(R2=0.94)and the highest inversion accuracy(RMSE=1.0 m,RRMSE=0.15).The study reveals that integrating active and passive satellite data has great potential for analyzing hydrological processes in polar ice sheets.

supraglacial lakePlanetScopeICESat-2bathymetry

朱雨欣、满梦甜、王裕涵、陈定华、杨康

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南京大学地理与海洋科学学院,南京 210023

江苏省地理信息技术重点实验室,南京 210023

中国南海研究协同创新中心,南京 210023

冰面湖 PlanetScope ICESat-2 水深反演

2024

自然资源遥感
中国国土资源航空物探遥感中心

自然资源遥感

CSTPCD北大核心
影响因子:1.275
ISSN:2097-034X
年,卷(期):2024.36(4)