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Data-driven Warping of Gaussian Processes for Spatial Interpolation of Skewed Data
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<p>Gaussian processes are a flexible machine learning framework that can be used for spatial interpolation and space-time prediction as well. Gaussian process regression (GPR) is quite similar to the geostatistical kriging method.&#160; It encompasses various types of kriging (e.g., simple, ordinary, universal and regression kriging).&#160; In addition, it is formulated in an inherently Bayesian framework which allows taking into account a priori beliefs regarding the distribution of the model&#8217;s hyper-parameters. Thus, it also incorporates Bayesian versions of kriging [1]. &#160;GPR is based on the assumption that the stochastic component of the observations follows a Gaussian distribution.&#160; However, this is not the case for various environmental variables (e.g., amount of precipitation, hydraulic conductivity, wind speed), which follow skewed probability distributions.&#160; The skewness is handled within the geostatistical framework using nonlinear transforms such that the marginal distribution of the data in the latent space becomes normal.&#160; This procedure is known as Gaussian anamorphosis in geostatistics.&#160; In the context of GPR, the term warped Gaussian process is used to denote the nonlinear transformation of the observations [2].&#160; &#160;Gaussian anamorphosis (warping) is usually implemented using explicit, monotonically increasing nonlinear functions.&#160; A different approach involves generating the warping function with the help of the empirically estimated cumulative probability distribution of the data.&#160; This approach provides flexibility because the transformation is data-driven (non-parametric) and is thus not constrained by specific functional forms.&#160; Furthermore, the cumulative distribution function of the data can be accurately estimated using smoothing kernels [3].&#160; We investigate warped Gaussian process regression using synthetic datasets and precipitation reanalysis data from the Mediterranean island of Crete. Cross validation analysis is used to establish the advantages of non-parametric warping for the interpolation of incomplete data. We demonstrate that warped GPR equipped with data-driven warping provides enhanced flexibility compared to "bare" GPR and can lead to improved predictive accuracy for non-Gaussian data. &#160;</p><p>Keywords: Gaussian processes, Mediterranean island, non-Gaussian, warping, precipitation</p><p>Funding: This research is co-financed by Greece and the European Union (European Social Fund- ESF) through the Operational Programme &#171;Human Resources Development, Education and Lifelong Learning 2014-2020&#187;in the context of the project &#8220;Gaussian Anamorphosis with Kernel Estimators for Spatially Distributed Data and Time Series and Applications in the Analysis of Precipitation&#8221; (MIS 5052133).</p><p><strong>References</strong></p><p>[1] T. Hristopulos, 2020. Random Fields for Spatial Data Modeling. Springer Netherlands, http://dx.doi.org/10.1007/978-94-024-1918-4.</p><p>[2] Snelson, E., Rasmussen, C.E. and Ghahramani, Z., 2004. Warped Gaussian processes. <em>Advances in neural information processing systems</em>, <em>16</em>, pp.337-344.</p><p>[3] Pavlides, A., Agou, V., and Hristopulos, D. T., 2021. Non-parametric Kernel-Based Estimation of Probability Distributions for Precipitation Modeling. <em>arXiv preprint arXiv:2109.09961</em>.</p>
Title: Data-driven Warping of Gaussian Processes for Spatial Interpolation of Skewed Data
Description:
<p>Gaussian processes are a flexible machine learning framework that can be used for spatial interpolation and space-time prediction as well.
Gaussian process regression (GPR) is quite similar to the geostatistical kriging method.
&#160; It encompasses various types of kriging (e.
g.
, simple, ordinary, universal and regression kriging).
&#160; In addition, it is formulated in an inherently Bayesian framework which allows taking into account a priori beliefs regarding the distribution of the model&#8217;s hyper-parameters.
Thus, it also incorporates Bayesian versions of kriging [1].
&#160;GPR is based on the assumption that the stochastic component of the observations follows a Gaussian distribution.
&#160; However, this is not the case for various environmental variables (e.
g.
, amount of precipitation, hydraulic conductivity, wind speed), which follow skewed probability distributions.
&#160; The skewness is handled within the geostatistical framework using nonlinear transforms such that the marginal distribution of the data in the latent space becomes normal.
&#160; This procedure is known as Gaussian anamorphosis in geostatistics.
&#160; In the context of GPR, the term warped Gaussian process is used to denote the nonlinear transformation of the observations [2].
&#160; &#160;Gaussian anamorphosis (warping) is usually implemented using explicit, monotonically increasing nonlinear functions.
&#160; A different approach involves generating the warping function with the help of the empirically estimated cumulative probability distribution of the data.
&#160; This approach provides flexibility because the transformation is data-driven (non-parametric) and is thus not constrained by specific functional forms.
&#160; Furthermore, the cumulative distribution function of the data can be accurately estimated using smoothing kernels [3].
&#160; We investigate warped Gaussian process regression using synthetic datasets and precipitation reanalysis data from the Mediterranean island of Crete.
Cross validation analysis is used to establish the advantages of non-parametric warping for the interpolation of incomplete data.
We demonstrate that warped GPR equipped with data-driven warping provides enhanced flexibility compared to "bare" GPR and can lead to improved predictive accuracy for non-Gaussian data.
&#160;</p><p>Keywords: Gaussian processes, Mediterranean island, non-Gaussian, warping, precipitation</p><p>Funding: This research is co-financed by Greece and the European Union (European Social Fund- ESF) through the Operational Programme &#171;Human Resources Development, Education and Lifelong Learning 2014-2020&#187;in the context of the project &#8220;Gaussian Anamorphosis with Kernel Estimators for Spatially Distributed Data and Time Series and Applications in the Analysis of Precipitation&#8221; (MIS 5052133).
</p><p><strong>References</strong></p><p>[1] T.
Hristopulos, 2020.
Random Fields for Spatial Data Modeling.
Springer Netherlands, http://dx.
doi.
org/10.
1007/978-94-024-1918-4.
</p><p>[2] Snelson, E.
, Rasmussen, C.
E.
and Ghahramani, Z.
, 2004.
Warped Gaussian processes.
<em>Advances in neural information processing systems</em>, <em>16</em>, pp.
337-344.
</p><p>[3] Pavlides, A.
, Agou, V.
, and Hristopulos, D.
T.
, 2021.
Non-parametric Kernel-Based Estimation of Probability Distributions for Precipitation Modeling.
<em>arXiv preprint arXiv:2109.
09961</em>.
</p>.
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