Project Details
Projekt Print View

S3-GEP: Scalable Spatiotemporal Statistics for Global Environmental Phenomena

Subject Area Geodesy, Photogrammetry, Remote Sensing, Geoinformatics, Cartography
Term from 2018 to 2024
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 396611854
 
Final Report Year 2024

Final Report Abstract

Today’s availability of large amounts of Earth observation data allows for complex analysis of environmental phenomena on a global scale. Satellite-based observations yield continuous global time series of the Earth’s surface and atmosphere. However, the practical application of complex statistical analysis of these data quickly results in methodological and technical difficulties. First, datasets are typically large in volume and have a complex structure (overlapping images, different pixel sizes and spatial reference systems, etc.). Second, common geostatistical models are computationally complex and have strict assumptions on variables that are not met on a global scale. As a result, researchers must invest a large amount of work into preprocessing and the potential of the data is not fully utilized. The project “scalable spatiotemporal statistics for global environmental phenomena” studied new ways to facilitate and scale-up the use of large multitemporal Earth observation data in statistical modeling. To facilitate the management of large satellite image time series, a new data representation as on-demand data cubes has been developed. Such data cubes allow for a scalable and more interactive use of large datasets while providing the flexibility to vary spatiotemporal resolution and/or study area. To make geostatistical analysis possible on such datasets on a global scale, spatiotemporal multiresolution approximations were developed. They allow for balancing computation times against prediction accuracy while being applicable in distributed computing environments. In a study on simulated data, we could considerably speed up typical interpolation tasks (speedup factor > 100) while increasing prediction errors (RMSE) by only 6.6% compared to traditional Kriging. To relax model assumptions on a global scale, we could integrate a kernel-convolution approach with spatially and/or temporally varying parameters of the covariance function. The project has furthermore taken up the impressive development of deep learning methods during the last years. We performed a study on how artificial neural network models based on partial convolutions can be used to fill gaps in atmospheric measurements. Results have not only shown promising computational properties and efficiency but also that such models are well suited for dynamic modeling in nowcasting applications.Methodological results have been published in articles and as open-source software. To demonstrate practical applications, study cases on different environmental variables (e.g. sea surface temperature, atmospheric carbon monoxide, land surface temperature) have been performed.

Publications

 
 

Additional Information

Textvergrößerung und Kontrastanpassung