• Many approaches we’ve talked about were forms of spatial regression

\[{ Y }_{ i }=\textbf{b}{ X }_{ i }+{ \phi }_{ i }+{ \varepsilon }_{ i }\]

• \(\phi\) is a vector of random effects describing a spatial field / process

• Is this a state space model?

• Instead of estimating giant covariance matrix describing \(\phi\),

• Estimate smaller random effects at a subset of points \(\phi^*\)

• Use some covariance kernel, and distances between points describing \(\phi\) and \(\phi^*\) to project estimates

• Can be done in ML or Bayesian framework, Latimer et al. 2009

• ‘glmmfields’ implements these models using Stan backend

• Easy to use formula syntax like gam() or spBayes()

• Allows spatial field to be modeled with Multivariate-T field, as alternative to Multivariate-Normal to better capture extremes

• Also includes lots of non-normal families for observation model

Let’s start with a simple model. This includes only 6 knots (probably way too few) and 100 iterations (too few!) for run time.

• Time set to NULL here to fit a model with constant spatial field

m <- glmmfields(Feb ~ 0, time = NULL,
 lat = "Latitude", lon = "Longitude", data = d,
 nknots = 6, iter = 100, chains = 2, seed = 1)

Ok, now let’s change the covariance function to matern, and estimate separate spatial fields by year.

• The ‘estimate_ar’ argument is important for determining whether the field is an AR(1) process or independent by year

m <- glmmfields(Feb ~ 0, time = "Water.Year",
 lat = "Latitude", lon = "Longitude", covariance="matern",
  data = d, nknots = 6, iter = 100, chains = 2, seed = 1,
  estimate_ar=FALSE)

Finally let’s include an example with modeling the spatial field as a Multivariate-t distribution

• We do this with the ‘estimate_df’ argument

m <- glmmfields(Feb ~ 0, time = "Water.Year",
 lat = "Latitude", lon = "Longitude", covariance="matern",
  data = d, nknots = 6, iter = 100, chains = 2, seed = 1,
  estimate_AR=FALSE, estimate_df= TRUE)

GP spatial models like glmmfields are extremely powerful

• May get overwhelmed by number of points

• Approaches to incorporate knots using sparse covariance matrices

• Integrated Nested Laplace Approximation - not on CRAN

• Some problems contain simple spatial structure

  • e.g. the harbor seal data in MARSS() with only 5 – 7 time series

• Others are much more complex

  • WA SWE data
  • Fisheries survey data (1000s of points)

• Including time-varying spatial fields becomes very computationally difficult

• Doing all of the above in a Bayesian setting can be prohibitive, but we can use Laplace approximation

• INLA meshes describe resolution of surface to estimate spatial process

INLA::meshbuilder

• How many points fall on vertices?
• Is the boundary area large enough?
• Choosing this must be done very carefully!

• Estimates seems similar to those from gls() and spBayes()
• Year included as numeric here (not significant)
• Alternatively, we can include year in spatial field
• Year can also be included as factor

• Start with the built in make_mesh function

snow_spde <- make_mesh(d, c("Longitude", "Latitude"), n_knots=50)
plot(snow_spde)

## Estimation in INLA

• Can be slow for very large models
  • but can also generate approximate Bayesian estimates
• Alternatively using automatic differentiation / TMB to maximize likelihood
  • VAST
  • sdmTMB

• This would fit a model with static spatial field

fit <- sdmTMB(Feb ~ 1, spde = snow_spde, data=d)

• Versus this one, where the field is independent by year

fit <- sdmTMB(Feb ~ 1, spde = snow_spde, time="Water.Year",data=d)

fit <- sdmTMB(Feb ~ 1, spde = snow_spde, data=d)
qqnorm(residuals(fit))

Lindgren 2013

Lindgren & Rue 2015

INLA book

Kristensen et al. 2016