Abstract

Environmental monitoring using satellite remote sensing is challenging because of data gaps in eddy-covariance (EC)-based in situ flux tower observations. In this study, we obtain the latent heat flux (LE) from an EC station and perform gap filling using two deep learning methods (two-dimensional convolutional neural network (CNN) and long short-term memory (LSTM) neural networks) and two machine learning (ML) models (support vector machine (SVM), and random forest (RF)), and we investigate their accuracies and uncertainties. The average model performance based on ~25 input and hysteresis combinations show that the mean absolute error is in an acceptable range (34.9 to 38.5 Wm−2), which indicates a marginal difference among the performances of the four models. In fact, the model performance is ranked in the following order: SVM > CNN > RF > LSTM. We conduct a robust analysis of variance and post-hoc tests, which yielded statistically insignificant results (p-value ranging from 0.28 to 0.76). This indicates that the distribution of means is equal within groups and among pairs, thereby implying similar performances among the four models. The time-series analysis and Taylor diagram indicate that the improved two-dimensional CNN captures the temporal trend of LE the best, i.e., with a Pearson’s correlation of >0.87 and a normalized standard deviation of ~0.86, which are similar to those of in situ datasets, thereby demonstrating its superiority over other models. The factor elimination analysis reveals that the CNN performs better when specific meteorological factors are removed from the training stage. Additionally, a strong coupling between the hysteresis time factor and the accuracy of the ML models is observed.

Highlights

  • IntroductionThe development of reliable and long-term Latent heat flux (LE) fluxes is vital for climate adaptation strategies [3] as well as disaster risk reduction plans [4], and it is one of the sustainable development goals of the United Nations initiative for global geospatial information management [5]

  • Latent heat flux (LE) is an important hydro-meteorological variable in the investigation of climate change, hydrological cycle intensification, and plant–atmosphere interactions [1,2].The development of reliable and long-term LE fluxes is vital for climate adaptation strategies [3] as well as disaster risk reduction plans [4], and it is one of the sustainable development goals of the United Nations initiative for global geospatial information management [5]

  • For the generation of an optimal input combination for training the two deep-learningbased models (CNN and long short-term memory (LSTM)) and two machine learning (ML)-based models (SVM and RF), we adopted an iterative approach as a function of mean absolute error (MAE)

Read more

Summary

Introduction

The development of reliable and long-term LE fluxes is vital for climate adaptation strategies [3] as well as disaster risk reduction plans [4], and it is one of the sustainable development goals of the United Nations initiative for global geospatial information management [5]. LE is defined as the sum of outgoing turbulent heat fluxes in the form of transpiration from plant canopies and evaporation from the soil surface [6]. In terms of global outgoing turbulent heat fluxes, LE contributes the most significantly among the components of the water cycle, as well as provides a linkage among water, energy, and the carbon cycle [7,8,9]. Owing to spatial heterogeneity in the land surface, the accurate quantification of LE is challenging [12,13]

Objectives
Methods
Results
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