Use a second-oder random walk with seasonal effects to model a main effect, or use multiple second-order random walks, each with their own seasonal effects, to model an interaction. A second-order random walk is effectively a random walk with drift where the drift term varies. It is typically used with main effects or interactions that involve time, where there are sustained trends upward or downward.
Usage
RW2_Seas(
n_seas,
s = 1,
sd_slope = 1,
s_seas = 0,
sd_seas = 1,
along = NULL,
zero_sum = FALSE
)
Arguments
- n_seas
Number of seasons
- s
Scale for prior for innovations in the random walk. Default is
1
.- sd_slope
Standard deviation for initial slope or random walk. Default is
1
.- s_seas
Scale for innovations in seasonal effects. Default is
0
.- sd_seas
Standard deviation for initial values of seasonal effects. Default is
1
.- along
Name of the variable to be used as the 'along' variable. Only used with interactions.
- zero_sum
If
TRUE
, values must sum to 0 within each combination of the 'by' variables. Default isFALSE
.
Details
If RW2_Seas()
is used with an interaction,
separate series are used for
the 'along' variable within
each combination of the
'by' variables.
Argument s
controls the size of innovations in the random walk.
Smaller values for s
tend to give smoother series.
Argument n_seas
controls the number of seasons
.
When using quarterly data, for instance,
n_seas
should be 4
, and when using
monthly data, n_seas
should be 12
.
By default, the magnitude of seasonal effects
is fixed. However, setting s_seas
to a value
greater than zero produces seasonal effects
that evolve over time.
Mathematical details
When RW2_Seas()
is used with a main effect,
$$\beta_j = \alpha_j + \lambda_j$$ $$\alpha_j \sim \text{N}(2 \alpha_{j-1} - \alpha_{j-2}, \tau^2)$$ $$\lambda_j \sim \text{N}(\lambda_{j-n}, \omega^2),$$
and when it is used with an interaction,
$$\beta_{u,v} = \alpha_{u,v} + \lambda_{u,v}$$ $$\alpha_{u,v} \sim \text{N}(2 \alpha_{u,v-1} - \alpha_{u,v-2}, \tau^2),$$ $$\lambda_{u,v} \sim \text{N}(\lambda_{u,v-n}, \omega^2)$$
where
\(\pmb{\beta}\) is the main effect or interaction;
\(\alpha_j\) or \(\alpha_{u,v}\) is an element of the random walk;
\(\lambda_j\) or \(\lambda_{u,v}\) is an element of the seasonal effect;
\(j\) denotes position within the main effect;
\(v\) denotes position within the 'along' variable of the interaction;
\(u\) denotes position within the 'by' variable(s) of the interaction; and
\(n\) is
n_seas
.
Parameter \(\omega\) has a half-normal prior
$$\omega \sim \text{N}^+(0, \text{s\_seas}^2),$$
where s_seas
is provided by the user. If
s_seas
is set to 0, then \(\omega\) is 0,
and the seasonal effects are fixed over time.
Parameter \(\tau\) has a half-normal prior
$$\tau \sim \text{N}^+(0, \text{s}^2),$$
where s
is provided by the user.
See also
RW2()
Second-order random walk, without seasonal effectRW_Seas()
Random walk, with seasonal effectpriors Overview of priors implemented in bage
set_prior()
Specify prior for intercept, main effect, or interaction
Examples
RW2_Seas(n_seas = 4) ## seasonal effects fixed
#> RW2_Seas(n_seas=4)
#> n_seas: 4
#> s: 1
#> sd_slope: 1
#> s_seas: 0
#> sd_seas: 1
#> along: NULL
#> zero_sum: FALSE
RW2_Seas(n_seas = 4, s_seas = 0.5) ## seasonal effects evolve
#> RW2_Seas(n_seas=4,s_seas=0.5)
#> n_seas: 4
#> s: 1
#> sd_slope: 1
#> s_seas: 0.5
#> sd_seas: 1
#> along: NULL
#> zero_sum: FALSE