Parallel Approximation of the Maximum Likelihood Estimation for the Prediction of Large-Scale Geostatistics Simulations

Parallel Approximation of the Maximum Likelihood Estimation for the Prediction of Large-Scale Geostatistics Simulations

Parallel Approximation of the Maximum Likelihood Estimation for the Prediction of Large-Scale Geostatistics Simulations Sameh Abdulah, Hatem Ltaief, Ying Sun, Marc G. Genton, and David E. Keyes Extreme Computing Research Center Computer, Electrical, and Mathematical Sciences and Engineering Division, King Abdullah University of Science Technology, Thuwal, Saudi Arabia. [email protected], [email protected], [email protected], [email protected], [email protected]. Abstract—Maximum likelihood estimation is an important Equations (PDEs) to estimate conditions at specific output statistical technique for estimating missing data, for example points based on semi-empirical models and assimilated mea- in climate and environmental applications, which are usually surements. This conventional approach translates the original large and feature data points that are irregularly spaced. In particular, the Gaussian log-likelihood function is the de facto big data problem into a large-scale simulation problem, solved model, which operates on the resulting sizable dense covariance globally, en route to particular quantities of interest, and it matrix. The advent of high performance systems with advanced relies on PDE solvers to extract performance from the targeted computing power and memory capacity have enabled full sim- architectures. ulations only for rather small dimensional climate problems, An alternative available in many use cases is to estimate solved at the machine precision accuracy. The challenge for high dimensional problems lies in the computation requirements missing quantities of interest from a statistical model. Until of the log-likelihood function, which necessitates O(n2) storage recently, the computation used in statistical models, like using and O(n3) operations, where n represents the number of given field data to estimate parameters of a Gaussian log-likelihood spatial locations. This prohibitive computational cost may be function and then evaluating that distribution to estimate reduced by using approximation techniques that not only enable phenomena where field data are not available, was intractable large-scale simulations otherwise intractable, but also maintain the accuracy and the fidelity of the spatial statistics model. for very large meteorological and environmental datasets. This In this paper, we extend the Exascale GeoStatistics software is due to the arithmetic complexity, for which a key step framework (i.e., ExaGeoStat1) to support the Tile Low-Rank grows as the cube of the problem size [1], i.e., increasing the (TLR) approximation technique, which exploits the data sparsity problem size by a factor of 10 requires 1; 000X more work of the dense covariance matrix by compressing the off-diagonal (and 100X more memory). Therefore, the existing hardware tiles up to a user-defined accuracy threshold. The underlying linear algebra operations may then be carried out on this landscape with its limited memory capacity, and even with data compression format, which may ultimately reduce the its high thread concurrency, still appears unfriendly for large- arithmetic complexity of the maximum likelihood estimation scale simulations due to the aforementioned curse of dimen- and the corresponding memory footprint. Performance results sionality [2]. Piggybacking on the renaissance in hierarchically of TLR-based computations on shared and distributed-memory low rank computational linear algebra, we propose to exploit systems attain up to 13X and 5X speedups, respectively, compared to full accuracy simulations using synthetic and real datasets (up data sparsity in the resulting, apparently dense, covariance arXiv:1804.09137v2 [cs.NA] 28 May 2018 to 2M), while ensuring adequate prediction accuracy. matrix by compressing the off-diagonal blocks up to a specific Index Terms—massively parallel algorithms, machine learning application-dependent accuracy. algorithms, applied computing mathematics and statistics, max- This work leverages our Exascale GeoStatistics software imum likelihood optimization, geo-statistics applications framework (ExaGeoStat [2]) in the context of climate and environmental simulations, which calculates the core statistical I. INTRODUCTION operation, i.e., the Maximum Likelihood Estimation (MLE), Current massively parallel systems provide unprecedented up to the machine precision accuracy for only rather small spa- computing power with up to millions of execution threads. tial datasets. ExaGeoStat relies on the asynchronous task- This hardware technology evolution comes at the expense of based dense linear algebra library Chameleon [3] associated a limited memory capacity per core, which may prevent sim- with the dynamic runtime system StarPU [4] to exploit the ulations of big data problems. In particular, climate/weather underlying computing power toward large-scale systems. simulations usually rely on a complex set of Partial Differential However, herein, we reduce the memory footprint and the arithmetic complexity of the MLE to alleviate the dimension- 1https://github.com/ecrc/exageostat ality bottleneck. We employ the Tile Low-Rank (TLR) data format for the compression, as implemented in the Hierarchical covariance functions. Section V describes the Tile Low-Rank Computations on Manycore Architectures (HiCMA2) numeri- (TLR) approximation technique and the HiCMA TLR approx- cal library. HiCMA relies on task-based programming model imation library and its integration into the ExaGeoStat and is deployed on shared [5] and distributed-memory sys- framework. Section VI highlights the ExaGeoStat frame- tems [6] via StarPU. The asynchronous execution achieved work with its software stack. Section VII defines both the via StarPU is even more critical for HiCMA’s workload, synthetic datasets and the two climate datasets obtained from characterized by lower arithmetic intensity, since it permits large geographic regions, i.e., the Mississippi River Basin to mitigate the latency overhead engendered by the data and the Middle-East region that are used to evaluate the movement. proposed TLR method. Performance results and accuracy analysis are presented in Section VIII, using both synthetic and A. Contributions real environmental datasets, and we conclude in Section IX. The contributions of this paper are sixfold. II. RELATED WORK • We propose an accurate and amenable MLE framework using TLR-based approximation format to reduce the Approximation techniques to reduce arithmetic complexities prohibitive complexity of the apparently dense covariance and memory footprint for large-scale climate and environmen- matrix computation. tal applications are well-established in the literature. Sun et • We provide a TLR solution for the prediction operation al. [7] have discussed several of these methods such as Kalman to impute values related to non-sampled locations. filtering [8], moving averages [9], Gaussian predictive pro- • We demonstrate the applicability of our approximation cesses [10], fixed-rank kriging [11], covariance tapering [12], technique on both synthetic (up to 1M locations) and real [13], and low-rank splines [14]. All these methods depend on datasets (i.e., soil moisture from the Mississippi Basin low-rank models, where a latent process is used with lower area and wind speed from the Middle East area). dimension, and eventually result in a low-rank representation • We port the ExaGeoStat simulation framework to a of the covariance matrix. Although these methods propose myriad of shared and distributed-memory systems using several possibilities to reduce the complexity of generating and a single source code to enhance user productivity, thanks computing the domain covariance matrix, several restrictions to its modular software stack. limit their functionality [15], [16]. • We conduct a comprehensive performance evaluation to On the other hand, low-rank off-diagonal matrix approx- highlight the effectiveness of the TLR-based approxi- imation techniques have gained a lot of attention to cope mation method compared to the original full accuracy with covariance matrices of high dimension. In the liter- approach. The experimental platforms include shared- ature, these are commonly referred as hierarchical matri- memory Intel Xeon Haswell / Broadwell / KNL / Skylake ces or H-matrices [17], [18]. The development of various high-end HPC servers and the distributed-memory Cray data compression techniques such as Hierarchically Semi- XC40 Shaheen-2 supercomputer. Separable (HSS) [19], H2-matrices [20]–[22], Hierarchically • We perform a thorough qualitative analysis to assess the Off-Diagonal Low-Rank (HODLR) [23], Block/Tile Low- accuracy of the estimation of the Matern´ covariance pa- Rank (BLR/TLR) [5], [6], [24], [25] increases their impact on rameters as well as the prediction operation. Performance a wide range of scientific applications. Each of the aforemen- results of TLR-based MLE computations on shared and tioned data compression formats has pros and cons in terms of distributed-memory systems achieve up to 13X and 5X arithmetic complexity, memory footprint and efficient parallel speedups, respectively, compared to full machine pre- implementation, depending on the application operator. We cision accuracy using synthetic and real environmental have chosen to rely on TLR data compression format, as datasets (up to 2M), without compromising the prediction implemented in the HiCMA library. TLR may not be the quality. best in terms of theoretical bounds for asymptotic sizes.

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