In pbs-assess/sdmTMB: Spatial and Spatiotemporal SPDE-Based GLMMs with 'TMB'
If the code in this vignette has not been evaluated, a rendered version is available on the documentation site under 'Articles'.
dplyr_installed <- require("dplyr", quietly = TRUE)
ggplot_installed <- require("ggplot2", quietly = TRUE)
sdmTMBextra_installed <- require("sdmTMBextra", quietly = TRUE)
pkgs <- dplyr_installed && ggplot_installed && sdmTMBextra_installed
EVAL <- identical(Sys.getenv("NOT_CRAN"), "true") && pkgs
knitr::opts_chunk$set(
collapse = TRUE,
comment = "#>",
fig.width = 7,
fig.asp = 0.618,
eval = EVAL,
purl = EVAL
)
library(ggplot2)
library(dplyr)
library(sdmTMB)
In this vignette, we describe the basic steps to fitting a spatial or spatiotemporal GLMM with sdmTMB. This type of model can be useful for (dynamic, i.e. changing through time) species distribution models and relative abundance index standardization among many other uses. See the model description for full model structure and equations.
We will use built-in package data for Pacific cod from a fisheries independent trawl survey.
- The density units are kg/km^2^ as calculated from catch biomass, net characteristics, and time on bottom.
- X and Y are coordinates in UTM zone 9. We could add these to a new dataset with
sdmTMB::add_utm_columns().
- Depth was centered and scaled by its standard deviation so that coefficient sizes weren't too big or small.
- There are columns for depth (
depth_scaled) and depth squared (depth_scaled2).
glimpse(pcod)
The most basic model structure possible in sdmTMB replicates a GLM as can be fit with glm() or a GLMM as can be fit with lme4 or glmmTMB, for example.
The spatial components in sdmTMB are included as random fields using a triangulated mesh with vertices, known as knots, used to approximate the spatial variability in observations.
Bilinear interpolation is used to approximate a continuous spatial field (Rue et al., 2009; Lindgren et al., 2011) from the estimated values of the spatial surface at these knot locations to other locations including those of actual observations.
These spatial random effects are assumed to be drawn from Gaussian Markov random fields (e.g., Cressie & Wikle, 2011; Lindgren et al., 2011) with covariance matrices that are constrained by Matérn covariance functions (Cressie & Wikle, 2011).
There are different options for creating the spatial mesh (see sdmTMB::make_mesh()).
We will start with a relatively coarse mesh for a balance between speed and accuracy (cutoff = 10, where cutoff is in the units of X and Y (km here) and represents the minimum distance between knots before a new mesh vertex is added).
Smaller values create meshes with more knots.
You will likely want to use a higher resolution mesh (more knots) in applied scenarios, but care must be taken to avoid overfitting.
The circles represent observations and the vertices are the knot locations.
mesh <- make_mesh(pcod, c("X", "Y"), cutoff = 10)
plot(mesh)
We will start with a logistic regression of Pacific cod presence in tows as a function of depth and depth squared. We will first use sdmTMB() without any spatial random effects (spatial = "off"):
m <- sdmTMB(
data = pcod,
formula = present ~ depth_scaled + depth_scaled2,
mesh = mesh, # can be omitted for a non-spatial model
family = binomial(link = "logit"),
spatial = "off"
)
m
AIC(m)
For comparison, here's the same model with glm():
m0 <- glm(
data = pcod,
formula = present ~ depth_scaled + depth_scaled2,
family = binomial(link = "logit")
)
summary(m0)
Notice that the AIC, log likelihood, parameter estimates, and standard errors are all identical.
Next, we can incorporate spatial random effects into the above model by changing spatial to "on" and see that this changes coefficient estimates:
m1 <- sdmTMB(
data = pcod,
formula = present ~ depth_scaled + depth_scaled2,
mesh = mesh,
family = binomial(link = "logit"),
spatial = "on"
)
m1
AIC(m1)
To add spatiotemporal random fields to this model, we need to include both the time argument that indicates what column of your data frame contains the time slices at which spatial random fields should be estimated (e.g., time = "year") and we need to choose whether these fields are independent and identically distributed (spatiotemporal = "IID"), first-order autoregressive (spatiotemporal = "AR1"), or as a random walk (spatiotemporal = "RW"). We will stick with IID for these examples.
m2 <- sdmTMB(
data = pcod,
formula = present ~ depth_scaled + depth_scaled2,
mesh = mesh,
family = binomial(link = "logit"),
spatial = "on",
time = "year",
spatiotemporal = "IID"
)
m2
We can also model biomass density using a Tweedie distribution. We'll switch to poly() notation to make some of the plotting easier.
m3 <- sdmTMB(
data = pcod,
formula = density ~ poly(log(depth), 2),
mesh = mesh,
family = tweedie(link = "log"),
spatial = "on",
time = "year",
spatiotemporal = "IID"
)
m3
Parameter estimates
We can view the confidence intervals on the fixed effects by using the tidy function:
tidy(m3, conf.int = TRUE)
And similarly for the random effect and variance parameters:
tidy(m3, "ran_pars", conf.int = TRUE)
Note that standard errors are not reported when coefficients are in log space, but the confidence intervals are reported. These parameters are defined as follows:
-
range: A derived parameter that defines the distance at which 2 points are effectively independent (actually about 13% correlated). If the share_range argument is changed to FALSE then the spatial and spatiotemporal ranges will be unique, otherwise the default is for both to share the same range.
-
phi: Observation error scale parameter (e.g., SD in Gaussian).
-
sigma_O: SD of the spatial process ("Omega").
-
sigma_E: SD of the spatiotemporal process ("Epsilon").
-
tweedie_p: Tweedie p (power) parameter; between 1 and 2.
If the model used AR1 spatiotemporal fields then:
rho: Spatiotemporal correlation between years; between -1 and 1.
If the model includes a spatial_varying predictor then:
sigma_Z: SD of spatially varying coefficient field ("Zeta").
Model diagnostics
We can inspect randomized quantile residuals:
pcod$resids <- residuals(m3) # randomized quantile residuals
qqnorm(pcod$resids)
qqline(pcod$resids)
ggplot(pcod, aes(X, Y, col = resids)) +
scale_colour_gradient2() +
geom_point() +
facet_wrap(~year) +
coord_fixed()
Those were fast to calculate but can look 'off' even when the model is consistent with the data.
MCMC-based residuals are more reliable but slow.
We can calculate them through some help from the sdmTMBextra package. https://github.com/pbs-assess/sdmTMBextra.
In practice you would like want more mcmc_iter and mcmc_warmup.
Total samples is mcmc_iter - mcmc_warmup.
We will also just use the spatial model here so the vignette builds quickly.
set.seed(123)
samps <- sdmTMBextra::predict_mle_mcmc(m3, mcmc_warmup = 100, mcmc_iter = 101)
r <- residuals(m3, "mle-mcmc", mcmc_samples = samps)
qqnorm(r)
qqline(r)
See ?residuals.sdmTMB().
Spatial predictions
Now, for the purposes of this example (e.g., visualization), we want to predict on a fine-scale grid on the entire survey domain. There is a grid built into the package for Queen Charlotte Sound named qcs_grid. Our prediction grid also needs to have all the covariates that we used in the model above.
glimpse(qcs_grid)
We can replicate our grid across all necessary years:
grid_yrs <- replicate_df(qcs_grid, "year", unique(pcod$year))
Now we will make the predictions on new data:
predictions <- predict(m3, newdata = grid_yrs)
Let's make a small function to help make maps.
plot_map <- function(dat, column) {
ggplot(dat, aes(X, Y, fill = {{ column }})) +
geom_raster() +
coord_fixed()
}
There are four kinds of predictions that we get out of the model.
First, we will show the predictions that incorporate all fixed effects and random effects:
plot_map(predictions, exp(est)) +
scale_fill_viridis_c(
trans = "sqrt",
# trim extreme high values to make spatial variation more visible
na.value = "yellow", limits = c(0, quantile(exp(predictions$est), 0.995))
) +
facet_wrap(~year) +
ggtitle("Prediction (fixed effects + all random effects)",
subtitle = paste("maximum estimated biomass density =", round(max(exp(predictions$est))))
)
We can also look at just the fixed effects, here only a quadratic effect of depth:
plot_map(predictions, exp(est_non_rf)) +
scale_fill_viridis_c(trans = "sqrt") +
ggtitle("Prediction (fixed effects only)")
We can look at the spatial random effects that represent consistent deviations in space through time that are not accounted for by our fixed effects.
In other words, these deviations represent consistent biotic and abiotic factors that are affecting biomass density but are not accounted for in the model.
plot_map(predictions, omega_s) +
scale_fill_gradient2() +
ggtitle("Spatial random effects only")
And finally we can look at the spatiotemporal random effects that represent deviation from the fixed effect predictions and the spatial random effect deviations.
These represent biotic and abiotic factors that are changing through time and are not accounted for in the model.
plot_map(predictions, epsilon_st) +
scale_fill_gradient2() +
facet_wrap(~year) +
ggtitle("Spatiotemporal random effects only")
We can also estimate the uncertainty in our spatiotemporal density predictions using simulations from the joint precision matrix by setting nsim > 0 in the predict function.
Here we generate 100 estimates and use apply() to calculate upper and lower confidence intervals, a standard deviation, and a coefficient of variation (CV).
sim <- predict(m3, newdata = grid_yrs, nsim = 100)
sim_last <- sim[grid_yrs$year == max(grid_yrs$year), ] # just plot last year
pred_last <- predictions[predictions$year == max(grid_yrs$year), ]
pred_last$lwr <- apply(exp(sim_last), 1, quantile, probs = 0.025)
pred_last$upr <- apply(exp(sim_last), 1, quantile, probs = 0.975)
pred_last$sd <- round(apply(exp(sim_last), 1, function(x) sd(x)), 2)
pred_last$cv <- round(apply(exp(sim_last), 1, function(x) sd(x) / mean(x)), 2)
Plot the CV on the estimates:
ggplot(pred_last, aes(X, Y, fill = cv)) +
geom_raster() +
scale_fill_viridis_c()
Conditional effects
We can visualize the conditional effect of any covariates by feeding simplified data frames to the predict function that fix covariate values we want fixed (e.g., at means) and vary parameters we want to visualize (across a range of values):
nd <- data.frame(
depth = seq(min(pcod$depth),
max(pcod$depth),
length.out = 100
),
year = 2015L # a chosen year
)
p <- predict(m3, newdata = nd, se_fit = TRUE, re_form = NA)
ggplot(p, aes(depth, exp(est),
ymin = exp(est - 1.96 * est_se),
ymax = exp(est + 1.96 * est_se)
)) +
geom_line() +
geom_ribbon(alpha = 0.4) +
scale_x_continuous() +
coord_cartesian(expand = F) +
labs(x = "Depth (m)", y = "Biomass density (kg/km2)")
We could also do this with the visreg package. This version is in link space and the residuals are partial randomized quantile residuals. See the scale argument in visreg for response scale plots.
visreg::visreg(m3, "depth")
Or the ggeffects package for a marginal effects plot. This will also be faster since it relies on the already estimated coefficients and variance-covariance matrix.
ggeffects::ggeffect(m3, "depth [0:500 by=1]") %>% plot()
Time-varying effects
We could also let the effect of depth vary through time.
In this example, it helps to give each year a separate mean effect (as.factor(year)).
The ~ 0 part of the formula omits the intercept.
For models like this that take longer to fit, we might want to set silent = FALSE so we can monitor progress.
m4 <- sdmTMB(
density ~ 0 + as.factor(year),
data = pcod,
time_varying = ~ 0 + depth_scaled + depth_scaled2,
mesh = mesh,
family = tweedie(link = "log"),
spatial = "on",
time = "year",
spatiotemporal = "IID"
)
m4
AIC(m4)
To plot these, we make a data frame that contains all combinations of the time-varying covariate and time. This is easily created using expand.grid() or tidyr::expand_grid().
nd <- expand.grid(
depth_scaled = seq(min(pcod$depth_scaled) + 0.2,
max(pcod$depth_scaled) - 0.2,
length.out = 50
),
year = unique(pcod$year) # all years
)
nd$depth_scaled2 <- nd$depth_scaled^2
p <- predict(m4, newdata = nd, se_fit = TRUE, re_form = NA)
ggplot(p, aes(depth_scaled, exp(est),
ymin = exp(est - 1.96 * est_se),
ymax = exp(est + 1.96 * est_se),
group = as.factor(year)
)) +
geom_line(aes(colour = year), lwd = 1) +
geom_ribbon(aes(fill = year), alpha = 0.1) +
scale_colour_viridis_c() +
scale_fill_viridis_c() +
scale_x_continuous(labels = function(x) round(exp(x * pcod$depth_sd[1] + pcod$depth_mean[1]))) +
coord_cartesian(expand = F) +
labs(x = "Depth (m)", y = "Biomass density (kg/km2)")
pbs-assess/sdmTMB documentation built on Dec. 20, 2024, 1:51 p.m.
R Package Documentation
Browse R Packages
We want your feedback!
Note that we can't provide technical support on individual packages. You should contact the package authors for that.
If the code in this vignette has not been evaluated, a rendered version is available on the documentation site under 'Articles'.
dplyr_installed <- require("dplyr", quietly = TRUE) ggplot_installed <- require("ggplot2", quietly = TRUE) sdmTMBextra_installed <- require("sdmTMBextra", quietly = TRUE) pkgs <- dplyr_installed && ggplot_installed && sdmTMBextra_installed EVAL <- identical(Sys.getenv("NOT_CRAN"), "true") && pkgs knitr::opts_chunk$set( collapse = TRUE, comment = "#>", fig.width = 7, fig.asp = 0.618, eval = EVAL, purl = EVAL )
library(ggplot2) library(dplyr) library(sdmTMB)
In this vignette, we describe the basic steps to fitting a spatial or spatiotemporal GLMM with sdmTMB. This type of model can be useful for (dynamic, i.e. changing through time) species distribution models and relative abundance index standardization among many other uses. See the model description for full model structure and equations.
We will use built-in package data for Pacific cod from a fisheries independent trawl survey.
- The density units are kg/km^2^ as calculated from catch biomass, net characteristics, and time on bottom.
- X and Y are coordinates in UTM zone 9. We could add these to a new dataset with
sdmTMB::add_utm_columns(). - Depth was centered and scaled by its standard deviation so that coefficient sizes weren't too big or small.
- There are columns for depth (
depth_scaled) and depth squared (depth_scaled2).
glimpse(pcod)
The most basic model structure possible in sdmTMB replicates a GLM as can be fit with glm() or a GLMM as can be fit with lme4 or glmmTMB, for example.
The spatial components in sdmTMB are included as random fields using a triangulated mesh with vertices, known as knots, used to approximate the spatial variability in observations.
Bilinear interpolation is used to approximate a continuous spatial field (Rue et al., 2009; Lindgren et al., 2011) from the estimated values of the spatial surface at these knot locations to other locations including those of actual observations.
These spatial random effects are assumed to be drawn from Gaussian Markov random fields (e.g., Cressie & Wikle, 2011; Lindgren et al., 2011) with covariance matrices that are constrained by Matérn covariance functions (Cressie & Wikle, 2011).
There are different options for creating the spatial mesh (see sdmTMB::make_mesh()).
We will start with a relatively coarse mesh for a balance between speed and accuracy (cutoff = 10, where cutoff is in the units of X and Y (km here) and represents the minimum distance between knots before a new mesh vertex is added).
Smaller values create meshes with more knots.
You will likely want to use a higher resolution mesh (more knots) in applied scenarios, but care must be taken to avoid overfitting.
The circles represent observations and the vertices are the knot locations.
mesh <- make_mesh(pcod, c("X", "Y"), cutoff = 10) plot(mesh)
We will start with a logistic regression of Pacific cod presence in tows as a function of depth and depth squared. We will first use sdmTMB() without any spatial random effects (spatial = "off"):
m <- sdmTMB( data = pcod, formula = present ~ depth_scaled + depth_scaled2, mesh = mesh, # can be omitted for a non-spatial model family = binomial(link = "logit"), spatial = "off" ) m AIC(m)
For comparison, here's the same model with glm():
m0 <- glm( data = pcod, formula = present ~ depth_scaled + depth_scaled2, family = binomial(link = "logit") ) summary(m0)
Notice that the AIC, log likelihood, parameter estimates, and standard errors are all identical.
Next, we can incorporate spatial random effects into the above model by changing spatial to "on" and see that this changes coefficient estimates:
m1 <- sdmTMB( data = pcod, formula = present ~ depth_scaled + depth_scaled2, mesh = mesh, family = binomial(link = "logit"), spatial = "on" ) m1 AIC(m1)
To add spatiotemporal random fields to this model, we need to include both the time argument that indicates what column of your data frame contains the time slices at which spatial random fields should be estimated (e.g., time = "year") and we need to choose whether these fields are independent and identically distributed (spatiotemporal = "IID"), first-order autoregressive (spatiotemporal = "AR1"), or as a random walk (spatiotemporal = "RW"). We will stick with IID for these examples.
m2 <- sdmTMB( data = pcod, formula = present ~ depth_scaled + depth_scaled2, mesh = mesh, family = binomial(link = "logit"), spatial = "on", time = "year", spatiotemporal = "IID" ) m2
We can also model biomass density using a Tweedie distribution. We'll switch to poly() notation to make some of the plotting easier.
m3 <- sdmTMB( data = pcod, formula = density ~ poly(log(depth), 2), mesh = mesh, family = tweedie(link = "log"), spatial = "on", time = "year", spatiotemporal = "IID" ) m3
Parameter estimates
We can view the confidence intervals on the fixed effects by using the tidy function:
tidy(m3, conf.int = TRUE)
And similarly for the random effect and variance parameters:
tidy(m3, "ran_pars", conf.int = TRUE)
Note that standard errors are not reported when coefficients are in log space, but the confidence intervals are reported. These parameters are defined as follows:
-
range: A derived parameter that defines the distance at which 2 points are effectively independent (actually about 13% correlated). If theshare_rangeargument is changed toFALSEthen the spatial and spatiotemporal ranges will be unique, otherwise the default is for both to share the same range. -
phi: Observation error scale parameter (e.g., SD in Gaussian). -
sigma_O: SD of the spatial process ("Omega"). -
sigma_E: SD of the spatiotemporal process ("Epsilon"). -
tweedie_p: Tweedie p (power) parameter; between 1 and 2.
If the model used AR1 spatiotemporal fields then:
rho: Spatiotemporal correlation between years; between -1 and 1.
If the model includes a spatial_varying predictor then:
sigma_Z: SD of spatially varying coefficient field ("Zeta").
Model diagnostics
We can inspect randomized quantile residuals:
pcod$resids <- residuals(m3) # randomized quantile residuals qqnorm(pcod$resids) qqline(pcod$resids) ggplot(pcod, aes(X, Y, col = resids)) + scale_colour_gradient2() + geom_point() + facet_wrap(~year) + coord_fixed()
Those were fast to calculate but can look 'off' even when the model is consistent with the data.
MCMC-based residuals are more reliable but slow.
We can calculate them through some help from the sdmTMBextra package. https://github.com/pbs-assess/sdmTMBextra.
In practice you would like want more mcmc_iter and mcmc_warmup.
Total samples is mcmc_iter - mcmc_warmup.
We will also just use the spatial model here so the vignette builds quickly.
set.seed(123) samps <- sdmTMBextra::predict_mle_mcmc(m3, mcmc_warmup = 100, mcmc_iter = 101) r <- residuals(m3, "mle-mcmc", mcmc_samples = samps) qqnorm(r) qqline(r)
See ?residuals.sdmTMB().
Spatial predictions
Now, for the purposes of this example (e.g., visualization), we want to predict on a fine-scale grid on the entire survey domain. There is a grid built into the package for Queen Charlotte Sound named qcs_grid. Our prediction grid also needs to have all the covariates that we used in the model above.
glimpse(qcs_grid)
We can replicate our grid across all necessary years:
grid_yrs <- replicate_df(qcs_grid, "year", unique(pcod$year))
Now we will make the predictions on new data:
predictions <- predict(m3, newdata = grid_yrs)
Let's make a small function to help make maps.
plot_map <- function(dat, column) { ggplot(dat, aes(X, Y, fill = {{ column }})) + geom_raster() + coord_fixed() }
There are four kinds of predictions that we get out of the model.
First, we will show the predictions that incorporate all fixed effects and random effects:
plot_map(predictions, exp(est)) + scale_fill_viridis_c( trans = "sqrt", # trim extreme high values to make spatial variation more visible na.value = "yellow", limits = c(0, quantile(exp(predictions$est), 0.995)) ) + facet_wrap(~year) + ggtitle("Prediction (fixed effects + all random effects)", subtitle = paste("maximum estimated biomass density =", round(max(exp(predictions$est)))) )
We can also look at just the fixed effects, here only a quadratic effect of depth:
plot_map(predictions, exp(est_non_rf)) + scale_fill_viridis_c(trans = "sqrt") + ggtitle("Prediction (fixed effects only)")
We can look at the spatial random effects that represent consistent deviations in space through time that are not accounted for by our fixed effects. In other words, these deviations represent consistent biotic and abiotic factors that are affecting biomass density but are not accounted for in the model.
plot_map(predictions, omega_s) + scale_fill_gradient2() + ggtitle("Spatial random effects only")
And finally we can look at the spatiotemporal random effects that represent deviation from the fixed effect predictions and the spatial random effect deviations. These represent biotic and abiotic factors that are changing through time and are not accounted for in the model.
plot_map(predictions, epsilon_st) + scale_fill_gradient2() + facet_wrap(~year) + ggtitle("Spatiotemporal random effects only")
We can also estimate the uncertainty in our spatiotemporal density predictions using simulations from the joint precision matrix by setting nsim > 0 in the predict function.
Here we generate 100 estimates and use apply() to calculate upper and lower confidence intervals, a standard deviation, and a coefficient of variation (CV).
sim <- predict(m3, newdata = grid_yrs, nsim = 100) sim_last <- sim[grid_yrs$year == max(grid_yrs$year), ] # just plot last year pred_last <- predictions[predictions$year == max(grid_yrs$year), ] pred_last$lwr <- apply(exp(sim_last), 1, quantile, probs = 0.025) pred_last$upr <- apply(exp(sim_last), 1, quantile, probs = 0.975) pred_last$sd <- round(apply(exp(sim_last), 1, function(x) sd(x)), 2) pred_last$cv <- round(apply(exp(sim_last), 1, function(x) sd(x) / mean(x)), 2)
Plot the CV on the estimates:
ggplot(pred_last, aes(X, Y, fill = cv)) + geom_raster() + scale_fill_viridis_c()
Conditional effects
We can visualize the conditional effect of any covariates by feeding simplified data frames to the predict function that fix covariate values we want fixed (e.g., at means) and vary parameters we want to visualize (across a range of values):
nd <- data.frame( depth = seq(min(pcod$depth), max(pcod$depth), length.out = 100 ), year = 2015L # a chosen year ) p <- predict(m3, newdata = nd, se_fit = TRUE, re_form = NA) ggplot(p, aes(depth, exp(est), ymin = exp(est - 1.96 * est_se), ymax = exp(est + 1.96 * est_se) )) + geom_line() + geom_ribbon(alpha = 0.4) + scale_x_continuous() + coord_cartesian(expand = F) + labs(x = "Depth (m)", y = "Biomass density (kg/km2)")
We could also do this with the visreg package. This version is in link space and the residuals are partial randomized quantile residuals. See the scale argument in visreg for response scale plots.
visreg::visreg(m3, "depth")
Or the ggeffects package for a marginal effects plot. This will also be faster since it relies on the already estimated coefficients and variance-covariance matrix.
ggeffects::ggeffect(m3, "depth [0:500 by=1]") %>% plot()
Time-varying effects
We could also let the effect of depth vary through time.
In this example, it helps to give each year a separate mean effect (as.factor(year)).
The ~ 0 part of the formula omits the intercept.
For models like this that take longer to fit, we might want to set silent = FALSE so we can monitor progress.
m4 <- sdmTMB( density ~ 0 + as.factor(year), data = pcod, time_varying = ~ 0 + depth_scaled + depth_scaled2, mesh = mesh, family = tweedie(link = "log"), spatial = "on", time = "year", spatiotemporal = "IID" ) m4 AIC(m4)
To plot these, we make a data frame that contains all combinations of the time-varying covariate and time. This is easily created using expand.grid() or tidyr::expand_grid().
nd <- expand.grid( depth_scaled = seq(min(pcod$depth_scaled) + 0.2, max(pcod$depth_scaled) - 0.2, length.out = 50 ), year = unique(pcod$year) # all years ) nd$depth_scaled2 <- nd$depth_scaled^2 p <- predict(m4, newdata = nd, se_fit = TRUE, re_form = NA) ggplot(p, aes(depth_scaled, exp(est), ymin = exp(est - 1.96 * est_se), ymax = exp(est + 1.96 * est_se), group = as.factor(year) )) + geom_line(aes(colour = year), lwd = 1) + geom_ribbon(aes(fill = year), alpha = 0.1) + scale_colour_viridis_c() + scale_fill_viridis_c() + scale_x_continuous(labels = function(x) round(exp(x * pcod$depth_sd[1] + pcod$depth_mean[1]))) + coord_cartesian(expand = F) + labs(x = "Depth (m)", y = "Biomass density (kg/km2)")
R Package Documentation
Browse R Packages
We want your feedback!
Note that we can't provide technical support on individual packages. You should contact the package authors for that.
Embedding an R snippet on your website
Add the following code to your website.
For more information on customizing the embed code, read Embedding Snippets.