View source: R/geom_streamline.R
geom_streamline | R Documentation |
Streamlines are paths that are always tangential to a vector field. In the case of a steady field, it's identical to the path of a massless particle that moves with the "flow".
geom_streamline(
mapping = NULL,
data = NULL,
stat = "streamline",
position = "identity",
...,
L = 5,
min.L = 0,
res = 1,
S = NULL,
dt = NULL,
xwrap = NULL,
ywrap = NULL,
skip = 1,
skip.x = skip,
skip.y = skip,
n = NULL,
nx = n,
ny = n,
jitter = 1,
jitter.x = jitter,
jitter.y = jitter,
arrow.angle = 6,
arrow.length = 0.5,
arrow.ends = "last",
arrow.type = "closed",
arrow = grid::arrow(arrow.angle, grid::unit(arrow.length, "lines"), ends = arrow.ends,
type = arrow.type),
lineend = "butt",
na.rm = TRUE,
show.legend = NA,
inherit.aes = TRUE
)
stat_streamline(
mapping = NULL,
data = NULL,
geom = "streamline",
position = "identity",
...,
L = 5,
min.L = 0,
res = 1,
S = NULL,
dt = NULL,
xwrap = NULL,
ywrap = NULL,
skip = 1,
skip.x = skip,
skip.y = skip,
n = NULL,
nx = n,
ny = n,
jitter = 1,
jitter.x = jitter,
jitter.y = jitter,
arrow.angle = 6,
arrow.length = 0.5,
arrow.ends = "last",
arrow.type = "closed",
arrow = grid::arrow(arrow.angle, grid::unit(arrow.length, "lines"), ends = arrow.ends,
type = arrow.type),
lineend = "butt",
na.rm = TRUE,
show.legend = NA,
inherit.aes = TRUE
)
mapping |
Set of aesthetic mappings created by |
data |
The data to be displayed in this layer. There are three options: If A A |
stat |
The statistical transformation to use on the data for this layer.
When using a
|
position |
A position adjustment to use on the data for this layer. This
can be used in various ways, including to prevent overplotting and
improving the display. The
|
... |
Other arguments passed on to
|
L |
typical length of a streamline in x and y units |
min.L |
minimum length of segments to show |
res |
resolution parameter (higher numbers increases the resolution) |
S |
optional numeric number of timesteps for integration |
dt |
optional numeric size "timestep" for integration |
xwrap , ywrap |
vector of length two used to wrap the circular dimension. |
skip , skip.x , skip.y |
numeric specifying number of gridpoints not to draw in the x and y direction |
n , nx , ny |
optional numeric indicating the number of points to draw in the
x and y direction (replaces |
jitter , jitter.x , jitter.y |
amount of jitter of the starting points |
arrow.length , arrow.angle , arrow.ends , arrow.type |
parameters passed to grid::arrow |
arrow |
specification for arrow heads, as created by |
lineend |
Line end style (round, butt, square). |
na.rm |
If |
show.legend |
logical. Should this layer be included in the legends?
|
inherit.aes |
If |
geom |
The geometric object to use to display the data for this layer.
When using a
|
Streamlines are computed by simple integration with a forward Euler method.
By default, stat_streamline()
computes dt
and S
from L
, res
,
the resolution of the grid and the mean magnitude of the field. S
is
then defined as the number of steps necessary to make a streamline of length
L
under an uniform mean field and dt
is chosen so that each step is no
larger than the resolution of the data (divided by the res
parameter). Be
aware that this rule of thumb might fail in field with very skewed distribution
of magnitudes.
Alternatively, L
and/or res
are ignored if S
and/or dt
are specified
explicitly. This not only makes it possible to fine-tune the result but also
divorces the integration parameters from the properties of the data and makes
it possible to compare streamlines between different fields.
The starting grid is a semi regular grid defined, either by the resolution of the
field and the skip.x
and skip.y
parameters o the nx
and ny
parameters,
jittered by an amount proportional to the resolution of the data and the
jitter.x
and jitter.y
parameters.
It might be important that the units of the vector field are compatible to the units
of the x and y dimensions. For example, passing dx
and dy
in m/s on a
longitude-latitude grid will might misleading results (see spherical).
Missing values are not permitted and the field must be defined on a regular grid, for now.
stat_streamline
understands the following aesthetics (required aesthetics are in bold)
x
y
dx
dy
alpha
colour
linetype
size
step in the simulation
dx at each location of the streamline
dy at each location of the streamline
Other ggplot2 helpers:
MakeBreaks()
,
WrapCircular()
,
geom_arrow()
,
geom_contour2()
,
geom_contour_fill()
,
geom_label_contour()
,
geom_relief()
,
guide_colourstrip()
,
map_labels
,
reverselog_trans()
,
scale_divergent
,
scale_longitude
,
stat_na()
,
stat_subset()
## Not run:
library(data.table)
library(ggplot2)
data(geopotential)
geopotential <- copy(geopotential)[date == date[1]]
geopotential[, gh.z := Anomaly(gh), by = .(lat)]
geopotential[, c("u", "v") := GeostrophicWind(gh.z, lon, lat)]
(g <- ggplot(geopotential, aes(lon, lat)) +
geom_contour2(aes(z = gh.z), xwrap = c(0, 360)) +
geom_streamline(aes(dx = dlon(u, lat), dy = dlat(v)), L = 60,
xwrap = c(0, 360)))
# The circular parameter is particularly important for polar coordinates
g + coord_polar()
# If u and v are not converted into degrees/second, the resulting
# streamlines have problems, specially near the pole.
ggplot(geopotential, aes(lon, lat)) +
geom_contour(aes(z = gh.z)) +
geom_streamline(aes(dx = u, dy = v), L = 50)
# The step variable can be mapped to size or alpha to
# get cute "drops". It's important to note that after_stat(dx) (the calculated variable)
# is NOT the same as dx (from the data).
ggplot(geopotential, aes(lon, lat)) +
geom_streamline(aes(dx = dlon(u, lat), dy = dlat(v), alpha = after_stat(step),
color = sqrt(after_stat(dx^2) + after_stat(dy^2)),
size = after_stat(step)),
L = 40, xwrap = c(0, 360), res = 2, arrow = NULL,
lineend = "round") +
scale_size(range = c(0, 0.6))
# Using topographic information to simulate "rivers" from slope
topo <- GetTopography(295, -55+360, -30, -42, res = 1/20) # needs internet!
topo[, c("dx", "dy") := Derivate(h ~ lon + lat)]
topo[h <= 0, c("dx", "dy") := 0]
# See how in this example the integration step is too coarse in the
# western montanous region where the slope is much higher than in the
# flatlands of La Pampa at in the east.
ggplot(topo, aes(lon, lat)) +
geom_relief(aes(z = h), interpolate = TRUE, data = topo[h >= 0]) +
geom_contour(aes(z = h), breaks = 0, color = "black") +
geom_streamline(aes(dx = -dx, dy = -dy), L = 10, skip = 3, arrow = NULL,
color = "#4658BD") +
coord_quickmap()
## End(Not run)
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