Abstract

The formation and distribution of melt ponds have an important influence on the Arctic climate. Therefore, it is necessary to obtain more accurate information on melt ponds on Arctic sea ice by remote sensing. The present large-scale melt pond products, especially the melt pond fraction (MPF), still require verification, and using very high resolution optical satellite remote sensing data is a good way to verify the large-scale retrieval of MPF products. Unlike most MPF algorithms using very high resolution data, the LinearPolar algorithm using Sentinel-2 data considers the albedo of melt ponds unfixed. In this paper, by selecting the best band combination, we applied this algorithm to Landsat 8 (L8) data. Moreover, Sentinel-2 data, as well as support vector machine (SVM) and iterative self-organizing data analysis technique (ISODATA) algorithms, are used as the comparison and verification data. The results show that the recognition accuracy of the LinearPolar algorithm for melt ponds is higher than that of previous algorithms. The overall accuracy and kappa coefficient results achieved by using the LinearPolar algorithm with L8 and Sentinel-2A (S2), the SVM algorithm, and the ISODATA algorithm are 95.38% and 0.88, 94.73% and 0.86, and 92.40%and 0.80, respectively, which are much higher than those of principal component analysis (PCA) and Markus algorithms. The mean MPF (10.0%) obtained from 80 cases from L8 data based on the LinearPolar algorithm is much closer to Sentinel-2 (10.9%) than the Markus (5.0%) and PCA algorithms (4.2%), with a mean MPF difference of only 0.9%, and the correlation coefficients of the two MPFs are as high as 0.95. The overall relative error of the LinearPolar algorithm is 53.5% and 46.4% lower than that of the Markus and PCA algorithms, respectively, and the root mean square error (RMSE) is 30.9% and 27.4% lower than that of the Markus and PCA algorithms, respectively. In the cases without obvious melt ponds, the relative error is reduced more than that of those with obvious melt ponds because the LinearPolar algorithm can identify 100% of dark melt ponds and relatively small melt ponds, and the latter contributes more to the reduction in the relative error of MPF retrieval. With a wider range and longer time series, the MPF from Landsat data are more efficient than those from Sentinel-2 for verifying large-scale MPF products or obtaining long-term monitoring of a fixed area.

Highlights

  • Classification of S2 interpolated onto the Landsat 8 (L8) grid; (d) the iterative self-organizing data analysis technique (ISODATA) classification of S2; (e) the ISODATA classification of S2 interpolated onto the L8 grid; (f) the melt pond fraction (MPF) of S2 using LinearPolar algorithm; (g) the result of (f) interpolated on the L8 grid; the MPF of L8 using (h) the Markus algorithm; (i) principal component analysis (PCA); and (j) the LinearPolar algorithm

  • The MPF retrieval data of S2 using the LinearPolar algorithm are shown in Figure 6(f1–f5), and Figure 6(g1–g5) shows the interpolation of Figure 6(f1–f5) onto the L8 grid

  • The results of S2 retrieval, support vector machine (SVM) classification, and ISODATA classification are used as verification data to calculate the classification accuracy of the results of L8 using three retrieval algorithms

Read more

Summary

Introduction

Melt ponds are some of the most common phenomena on the surface of Arctic sea ice in warm seasons and generally form in late May and refreeze during late August and early September [1]. The distribution and variability of melt ponds have an important influence on the Arctic climate through sea ice albedo feedback [2]. It has been shown that the melt pond fraction (MPF) of the Arctic in spring can effectively predict the September minimum sea ice extent [3,4,5], which leads to enhancements in the seasonal forecasting ability of the summer sea ice extent. Accurately obtaining the MPF is extremely vital for understanding and predicting Arctic sea ice changes

Objectives
Methods
Results
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call