Generating a Long-Term Spatiotemporally Continuous Melt Pond Fraction Dataset for Arctic Sea Ice Using an Artificial Neural Network and a Statistical-Based Temporal Filter

被引:7
作者
Peng, Zeli [1 ]
Ding, Yinghui [1 ]
Qu, Ying [1 ]
Wang, Mengsi [1 ]
Li, Xijia [2 ]
机构
[1] Northeast Normal Univ, Sch Geog Sci, Key Lab Geog Proc & Ecol Secur Changbai Mt, Minist Educ, Changchun 130024, Peoples R China
[2] Jilin Jianzhu Univ, Sch Geomat & Prospecting Engn, Changchun 130119, Peoples R China
基金
中国国家自然科学基金;
关键词
melt pond fraction; sea ice; Arctic; artificial neural network; statistical-based temporal filter; MODIS; LAND-SURFACE ALBEDO; REFLECTIVE PROPERTIES; SPECTRAL ALBEDO; MERIS DATA; MODIS; ALGORITHM; RETRIEVAL; AERIAL; VALIDATION; COVERAGE;
D O I
10.3390/rs14184538
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The melt pond fraction (MPF) is an important geophysical parameter of climate and the surface energy budget, and many MPF datasets have been generated from satellite observations. However, the reliability of these datasets suffers from short temporal spans and data gaps. To improve the temporal span and spatiotemporal continuity, we generated a long-term spatiotemporally continuous MPF dataset for Arctic sea ice, which is called the Northeast Normal University-melt pond fraction (NENU-MPF), from Moderate Resolution Imaging Spectroradiometer (MODIS) data. First, the non-linear relationship between the MODIS reflectance/geometries and the MPF was constructed using a genetic algorithm optimized back-propagation neural network (GA-BPNN) model. Then, the data gaps were filled and smoothed using a statistical-based temporal filter. The results show that the GA-BPNN model can provide accurate estimations of the MPF (R-2 = 0.76, root mean square error (RMSE) = 0.05) and that the data gaps can be efficiently filled by the statistical-based temporal filter (RMSE = 0.047; bias = -0.022). The newly generated NENU-MPF dataset is consistent with the validation data and with published MPF datasets. Moreover, it has a longer temporal span and is much more spatiotemporally continuous; thus, it improves our knowledge of the long-term dynamics of the MPF over Arctic sea ice surfaces.
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页数:21
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