Machine Learning for Polar Regions Workshop presentation at
Lamont-Doherty Earth Observatory (virtual), Friday 17 Jun 2022, 15:15-15:30 (UTC)
by Wei Ji Leong & Huw Horgan
P.S. Slides are at https://hackmd.io/@weiji14/2022ML4Polar
Going from a 1km resolution BEDMAP2 to a higher (250m) spatial resolution bed topography would enable us to:
Cumulatively, this will lead to more accurate sea level rise projections!
Ice-penetrating radar surveys, accurate but limited spatial coverage
Figure showing Radio-echo-sounding datasets around Antarctica from Gardner et al. 2018
Hillshade Map of the Reference Elevation Model of Antarctica (REMA) from Howat et al. 2018
Given high resolution surface datasets + prior knowledge of bed, model learns to predict high resolution bed topography
High resolution groundtruth areas provide 'answer' to train the neural network.
X(Surface inputs) -- function(X) --> Y(Groundtruth bed)
Apply trained model to fill in gaps where there is few/no survey data
X(Surface inputs) -- function(X) --> Y(High Resolution Bed)
Super-Resolution is one of these hard problems, how do we produce a realistic high resolution image from a low resolution image.
Why? Because GANs can drive the reconstruction towards a more 'natural' look, compared to standard ConvNets that simply reduce the Mean Squared Error (MSE) loss.
Two competing neural networks working to improve image's finer details
Generator (artist) learns to produce better image to convince Discriminator, Discriminator (teacher) points out where image is incorrect
2016-2017: Super Resolution Generative Adversarial Network (SRGAN) by Ledig et al., 2017
Generator-Discriminator GAN models have parallels with Actor-Critic models in Reinforcement Learning.
Pan-sharpening is a classic (remote-sensing) example. Given a high resolution panchromatic band and low resolution RGB bands -> produce a 'super resolution' RGB image.
Figure showing pan-sharpened results using PSGAN from Liu et al., 2018
Model adapted from ESRGAN and built using Chainer (Python deep learning library)
Example over Pine Island Glacier.
DeepBedMap_DEM (purple) features more fine-scale (<10km) bumps and troughs, and higher roughness values (mean standard deviation of about 40m), similar to the ground truth (orange)
To optimize the ESRGAN model's performance, a Bayesian approach (Tree-Structured Parzen Estimator) was used to narrow down our hyperparameter search space.
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HyperBand used to prune unpromising trials.
Main 'hyperparameters' tuned (in rough order of priority) were:
Learning rate (1.7e-4, 2e-4 to 1e-4); Residual scaling factor (0.2, 0.1 to 0.5); Training epochs (~140, 90 to 150); Number of Residual-in-Residual Dense Blocks (12, 8 to 14); Mini-batch size (128, 64 or 128)
P.S. Slides are at https://hackmd.io/@weiji14/2022ML4Polar and DeepBedMap paper is at https://doi.org/10.5194/tc-14-3687-2020. Or check out the repo at https://github.com/weiji14/deepbedmap.
Fretwell, P., Pritchard, H. D., Vaughan, D. G., Bamber, J. L., Barrand, N. E., Bell, R., … Zirizzotti, A. (2013). Bedmap2: improved ice bed, surface and thickness datasets for Antarctica. The Cryosphere, 7(1), 375–393. https://doi.org/10.5194/tc-7-375-2013
Gardner, A. S., Moholdt, G., Scambos, T., Fahnstock, M., Ligtenberg, S., van den Broeke, M., & Nilsson, J. (2018). Increased West Antarctic and unchanged East Antarctic ice discharge over the last 7 years. The Cryosphere, 12(2), 521–547. https://doi.org/10.5194/tc-12-521-2018
Howat, Ian, Morin, Paul, Porter, Claire, & Noh, Myong-Jong. (2018). The Reference Elevation Model of Antarctica [Data set]. Harvard Dataverse. https://doi.org/10.7910/DVN/SAIK8B
Ledig, C., Theis, L., Huszar, F., Caballero, J., Cunningham, A., Acosta, A., Aitken, A., Tejani, A., Totz, J., Wang, Z., & Shi, W. (2017). Photo-Realistic Single Image Super-Resolution Using a Generative Adversarial Network. 2017 IEEE Conference on Computer Vision and Pattern Recognition (CVPR), 105–114. https://doi.org/10.1109/CVPR.2017.19
Leong, W. J., & Horgan, H. J. (2020). DeepBedMap: A deep neural network for resolving the bed topography of Antarctica. The Cryosphere, 14(11), 3687–3705. https://doi.org/10.5194/tc-14-3687-2020
Morlighem, M., Rignot, E., Binder, T., Blankenship, D., Drews, R., Eagles, G., Eisen, O., Ferraccioli, F., Forsberg, R., Fretwell, P., Goel, V., Greenbaum, J. S., Gudmundsson, G. H., Guo, J., Helm, V., Hofstede, C., Howat, I., Humbert, A., Jokat, W., … Young, D. A. (2019). Deep glacial troughs and stabilizing ridges unveiled beneath the margins of the Antarctic ice sheet. Nature Geoscience, 13(2), 132–137. https://doi.org/10.1038/s41561-019-0510-8
Wang, X., Yu, K., Wu, S., Gu, J., Liu, Y., Dong, C., … Tang, X. (2018). ESRGAN: Enhanced Super-Resolution Generative Adversarial Networks. ArXiv:1809.00219 [Cs]. Retrieved from http://arxiv.org/abs/1809.00219