Krause 2008 - Experiments and Empirical Findings

Summary

Two real datasets (Intel Berkeley temperature, Pacific Northwest precipitation) support five findings: nonstationary GPs beat stationary ones; GP-based placements beat the disk model; MI beats entropy and A-, D-, E-optimal design on prediction error; greedy MI is near-optimal and beats random plus exchange heuristics; lazy evaluation and truncated kernels give large speedups at little cost. Figures are plotted, not tabulated, so quantitative claims below are the ones the text states.

Overview

Datasets (9.1). Temperature: 46 sensors of the Intel Berkeley network (Fig. 1a); training data at 30-second intervals over 3 consecutive days from 28 Feb 2004; test data the following two days. Precipitation: daily rainfall 1949-1994 in Washington and Oregon (Widmann and Bretherton 1999), 167 equal-area regions about 50 km apart; log-transformed, daily mean removed, rainy days only; first two thirds training, last third test. Covariance estimated from training data and regularised by independent measurement noise (chosen by cross-validation). Error bars are not reported because temporally correlated samples make them overconfident.

Main Content

SectionComparisonFinding (as stated)
9.2Stationary (isotropic exponential, bandwidth from least-squares variogram) vs nonstationary (Nott-Dunsmuir) GPs, learned from a growing initial deployment (Fig. 9)Nonstationary GP from 10 sensors matches stationary from 40 (temperature); nonstationary from 20 sensors beats stationary from 160 (precipitation). RMS converges to the empirical-covariance placement as the initial deployment grows.
9.3Disk model (radius m, chosen so 20 sensors just cover the space) vs GP-MI placements (Fig. 10)The geometric criterion “performs poorly” relative to model-based ones; empirical-covariance placement is best, nonstationary close behind.
9.4MI vs entropy on morning (8-9 am) and noon (12-1 pm) models and a whole-day model (Figs 11-13)MI “in almost all cases” gives better RMS/log-likelihood with fewer sensors; on precipitation “often several sensors would have to be additionally placed for entropy to reach the same level”. Entropy places sensors near the border (Fig. 11); with 22 sensors MI concentrates on the top and bottom sides where the field is most complex and yields lower predicted variance almost everywhere (Fig. 13).
9.5MI vs classical A-, D-, E-optimal design (12 target locations ; model ) (Fig. 14)MI has the least RMS error on the targets except at a single sensor; E-optimal is comparable to entropy; D and A are worse. On a precipitation subsample a classical criterion slightly outperforms MI, but for the full 167 locations MI wins. Running times: entropy fastest, truncated MI () next; untruncated MI is 3x faster than (fractional) D-optimal and 24x faster than A-optimal.
9.6Greedy vs random, hill-climbing with pairwise exchange (PE), and MIP bounds (Figs 5, 15, 16)Greedy beats the max of 100 random placements; greedy, greedy+PE and random+PE rarely differ (one size-12 case where random+PE edges greedy); greedy within 5% of optimum on 16 nodes; lazy evaluation cuts MI computations from 7125 to 1172 (41.3 s to 8.7 s) for 50 precipitation sensors.
9.7Local kernels (Figs 17-19)Truncation (text) or (caption) balances time and RMS; 7x7 grid with bandwidth 0.1..12.8: local and Gaussian kernels give very similar placements.

Observation in the paper that matters for decisions: placements chosen on an estimated model are evaluated by RMS on held-out data, not on the model they were optimised against, so the comparison is honest about model misspecification.

Examples

Reproducing the qualitative MI-versus-entropy contrast on synthetic data takes a few lines (see Krause 2008 - Greedy Algorithm and the 1-1 over e Guarantee): entropy picks the endpoints of the grid; MI does not.

Connections

See Also