Abstract

This paper constructed a stacked-autoencoder neural network model (SAE model) to estimate sea state bias (SSB) based on radar altimeter data. Six cycles of the geophysical data record (GDR) from Jason-1/2 radar altimeters were used as a training dataset, and the other 2 cycles of the GDR from Jason-1/2 were used for testing. The inputs to this SAE model include the significant wave height (SWH), wind speed (U), sea surface height (SSH), backscatter coefficient (σ0) and automatic gain control (AGC), and the model outputs the SSB. The model includes one input layer, three hidden layers and one output layer. The SSBs in the GDR of Jason-1/2 were obtained from a nonparametric model based on the SWH and U as input variables; thus, the model has high accuracy but low efficiency. The SSBs in the GDR of HY-2A were computed using a four-parameter parametric model that uses the SWH and U as input variables; therefore, this model’s computational speed is high but its accuracy is low. Thus, we used the HY-2A radar altimeter as an unseen validation dataset to evaluate the performance of the SAE model. Then, we analyzed the contrasting results of these methods, including the differences in the SSB, explained variance, residual error and operational efficiency. The results demonstrate not only that the accuracy of the SAE model is superior to that of the conventional parametric model but also that its operational efficiency is better than that of the nonparametric model.

Highlights

  • Satellite radar altimeters can quickly measure the global sea surface height (SSH) and invert geophysical information, such as the significant wave height (SWH) and wind speed (U) [1]

  • The SWH, U, SSH, σ0 and automatic gain control (AGC) values in the geophysical data record (GDR) were used as the model inputs, while the sea state bias (SSB) in the GDR was used as the desired model output when training the neural network

  • The trained SAE model was validated by HY-2A radar altimeter data

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Summary

Introduction

Satellite radar altimeters can quickly measure the global sea surface height (SSH) and invert geophysical information, such as the significant wave height (SWH) and wind speed (U) [1]. The accuracy of the SSB is limited because the parametric models use the modeling value obtained by the mismatch in the SSH at the cross point or collinearity data, and the assumed functional formula may be incorrect [3,4,5]. The true value of the SSB based on the results of the SSB nonparametric model in the Jason1/2 altimeter geophysical data record (GDR) is used during model training.

Results
Conclusion
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