knitr::opts_chunk$set( collapse = TRUE, comment = "#>" )
pastclim
is on CRAN, and the easiest way to install it is with:
install.packages("pastclim")
If you want the latest development version, you can get it from GitHub.
To install from GitHub, you will need to use devtools
; if you haven't
done so already, install it from CRAN with
install.packages("devtools")
. Also, note that the dev
version of
pastclim
tracks changes in the dev
version of terra
, so you will
need to upgrade to both:
install.packages("terra", repos = "https://rspatial.r-universe.dev") devtools::install_github("EvolEcolGroup/pastclim", ref = "dev")
On its dedicated website,
you can find Articles giving you a step-by-step overview of the
package,
and a
cheatsheet.
There is also a version
of the site updated for the dev
version (on the top left, the version
number is in red, and will be in the format x.x.x.9xxx, indicating it is
a development version).
If you want to build the vignette directly in R
when installing
pastclim
from GitHub, you can :
devtools::install_github("EvolEcolGroup/pastclim", ref = "dev", build_vignettes = TRUE )
And read it directly in R with:
vignette("pastclim_overview", package = "pastclim")
Depending on the operating system you use, you might need additional packages to build a vignette.
You will need to download climatic reconstructions before being able to
do any real work with pastclim
.
Pastclim currently includes data from Beyer et al 2020 (Beyer2020, a reconstruction
of climate based on the HadCM3 model for the last 120k years), Krapp
et al 2021 (Krapp2021, which covers the last 800k years with a statistical emulator of HadCM3),
Barreto et al 2023 (Barreto2023), covering the last 5M years using the PALEO-PGEM emulator), the CHELSA-TraCE21k, covering the last 21k years at high spatial and temporal resolution (CHELSA_trace21k_0.5m_vsi),
the HYDE3.3 database of land use reconstructions for the last 10k years (HYDE_3.3_baseline)
the paleoclim dataset, a selected few time steps over the last 120k years at various resolutions (paleoclim_RESm),
and the WorldClim and CHELSA data (WorldClim_2.1_ and CHELSA_2.1_, present, and future projections with a number of models and
emission scenarios). More information on each of these
datasets can be found
here, or using the help
page for a given dataset.
For detailed instructions on how to use the WorldClim and CHELSA datasets for present and future reconstructions can be found in this article
There are also instructions on how to build and use custom
datasets,
but you will need some
familiarity with handling netcdf
files.
A list of all datasets available can be obtained by typing:
library(pastclim) get_available_datasets()
Please be aware that using any dataset made available to pastclim
will
require to cite both pastclim
as well as the original publication
presenting the dataset. The reference to cite for pastclim
can be
obtained by typing
citation("pastclim")
while the reference associated to any dataset of choice (in this case "Beyer2020") is displayed together with the general information on that dataset through the command:
help("Beyer2020")
pastclim:::get_dataset_info(dataset = "Beyer2020")
For the datasets available in pastclim
, there are functions that help
you download the data and choose the variables. When you start
pastclim
for the first time, you will need to set the path where
reconstructions are stored using set_data_path
. By default, the
package data path will be used:
library(pastclim) set_data_path()
library(pastclim) set_data_path(on_CRAN = TRUE)
#> The data_path will be set to /home/andrea/.local/share/R/pastclim. #> A copy of the Example dataset will be copied there. #> This path will be saved by pastclim for future use. #> Proceed? #> #> 1: Yes #> 2: No
Press 1 if you are happy with the offered choices, and pastclim
will
remember your data path in future sessions. Note that your data path
will look different than in this example, as it depends on your user
name and operating system.
If you prefer using a custom path (e.g. in "\~/my_reconstructions"), it can be set with:
set_data_path(path_to_nc = "~/my_reconstructions")
The package includes a small dataset, Example, that we will use in this vignette but is not suitable for running real analyses; the real datasets are large (from 100s of Mb to a few Gb), and you will need to specify what you want to download (see below).
Let us start by inspecting the Example dataset. We can get a list of variables available for this dataset with:
get_vars_for_dataset(dataset = "Example")
and the available time steps can be obtained with:
get_time_bp_steps(dataset = "Example")
We can also query the resolution of this dataset:
get_resolution(dataset = "Example")
so, the *Example" dataset only has a resolution of 1x1 degree.
For Beyer2020 and Krapp2021, you can get a list of available variables for each dataset with:
get_vars_for_dataset(dataset = "Beyer2020")
and
get_vars_for_dataset(dataset = "Krapp2021")
Note that, by default, only annual variables are shown. To see the available monthly variables, simply use:
get_vars_for_dataset(dataset = "Beyer2020", annual = FALSE, monthly = TRUE)
For monthly variables, months are coded as "_xx" at the end of the variable names; e.g. "temperature_02" is the mean monthly temperature for February. A more thorough description of each variable (including the units) can be obtained with:
get_vars_for_dataset(dataset = "Example", details = TRUE)
You will not be able to get the available time steps until you download
the dataset. pastclim
offers an interface to download the necessary
files into your data path.
To inspect which datasets and variables have already been downloaded in the data path, we can use:
get_downloaded_datasets()
Let's now download bio01 and bio05 for the Beyer2020 dataset (this
operation might take several minutes, as the datasets are large; R
will pause until the download is complete):
download_dataset(dataset = "Beyer2020", bio_variables = c("bio01", "bio05"))
Note that multiple variables can be packed together into a single file,
so get_downloaded_datasets()
might list more variables than the ones
that we chose to download (it depends on the dataset).
When upgrading pastclim
, new version of various datasets might become
available. This will make the previously downloaded datasets obsolete,
and you might suddenly be told by pastclim
that some variables have to
be re-downloaded. This can lead to the accumulation of old datasets in
your data path. The function clean_data_path()
can be used to delete
old files that are no longer needed.
Often we want to get the climate for specific locations. We can do so by
using the function location_slice
. With this function, we will get
slices of climate for the times relevant to the locations of interest.
Let us consider five possible locations of interest: Iho Eleru (a Late Stone Age inland site in Nigeria), La Riera (a Late Palaeolithic coastal site on Spain), Chalki (a Mesolithic site on a Greek island), Oronsay (a Mesolithic site in the Scottish Hebrides), and Atlantis (the fabled submersed city mentioned by Plato). For each site we have a date (realistic, but made up) that we are interested in associating with climatic reconstructions.
locations <- data.frame( name = c("Iho Eleru", "La Riera", "Chalki", "Oronsay", "Atlantis"), longitude = c(5, -4, 27, -6, -24), latitude = c(7, 44, 36, 56, 31), time_bp = c(-11200, -18738, -10227, -10200, -11600) ) locations
And extract their climatic conditions for bio01 and bio12:
location_slice( x = locations, bio_variables = c("bio01", "bio12"), dataset = "Example", nn_interpol = FALSE )
pastclim
finds the closest time step (slice) available for a given
date, and outputs the slice used in column time_bp_slice
(the
Example dataset that we use in this vignette has a temporal resolution
of only 5k years).
Note that Chalki and Atlantis are not available (we get NA) for the
appropriate time steps. This occurs when a location, in the
reconstructions, was either under water or ice, and so pastclim
can
not return any estimate. In some instances, this is due to the
discretisation of space in the raster. We can interpolate climate among
the nearest neighbours, thus using climate reconstructions for
neighbouring pixels if the location is just off one or more land pixels:
location_slice( x = locations, bio_variables = c("bio01", "bio12"), dataset = "Example", nn_interpol = TRUE )
For Chalki, we can see that the problem is indeed that, since it is a
small island, it is not well represented in the reconstructions (bear in
mind that the Example
dataset is very coarse in spatial resolution),
and so we can reconstruct some appropriate climate by interpolating.
Atlantis, on the other hand, is the middle of the ocean, and so there is
no information on what the climate might have been before became
submerged (assuming it ever existed...). Note that nn_interpol = TRUE
is the default for this function.
Sometimes, we want to get a time series of climatic reconstructions, thus allowing us to see how climate changed over time:
locations_ts <- location_series( x = locations, bio_variables = c("bio01", "bio12"), dataset = "Example" )
The resulting dataframe can be subsetted to get the time series for each location (the small Example dataset only contains 5 time slices):
subset(locations_ts, name == "Iho Eleru")
Also note that for some locations, climate can be available only for certain time steps, depending on sea level and ice sheet extent. This is the case for Oronsay:
subset(locations_ts, name == "Oronsay")
We can quickly plot bio01
through time for the locations:
library(ggplot2) ggplot(data = locations_ts, aes(x = time_bp, y = bio01, group = name)) + geom_line(aes(col = name)) + geom_point(aes(col = name))
As expected, we don't have data for Atlantis (as it is always
underwater), but we also fail to retrieve data for Chalki. This is
because location_series
does not interpolate from nearest neighbours
by default (so, it differs from location_slice
in behaviour). The
rationale for this behaviour is that we are interested in whether some
locations might end up underwater, and so we do not want to grab climate
estimates if they have been submerged. However, in some cases (as for
Chalki) it might be necessary to allow for interpolation.
Pretty labels for environmental variables can be generated with
var_labels
:
library(ggplot2) ggplot(data = locations_ts, aes(x = time_bp, y = bio01, group = name)) + geom_line(aes(col = name)) + geom_point(aes(col = name)) + labs( y = var_labels("bio01", dataset = "Example", abbreviated = TRUE), x = "time BP (yr)" )
Note that these climatic reconstructions were extracted from the
Example
dataset, which is very coarse, so they should not be used to
base any real inference about their environmental conditions. But note
also that higher resolution is not always better. It is important to
consider the appropriate spatial scale that is relevant to the question
at hand. Sometimes, it might be necessary to downscale the simulations
(see section at the end of this vignette), or in other cases we might
want to get estimates to cover an area around the specific location
(e.g. if we are comparing to proxies that capture the climatology of a
broad area, such as certain sediment cores that capture pollen from the
broader region). location_slice
and location_series
can provide mean
estimates for areas around the location coordinates by setting the
buffer
parameter (see the help pages of those functions for details).
Instead of focussing on specific locations, we might want to look at a whole region. For a given time step, we can extract a slice of climate with
climate_20k <- region_slice( time_bp = -20000, bio_variables = c("bio01", "bio10", "bio12"), dataset = "Example" )
This returns a raster (technically a SpatRaster
object as defined in
the terra
library, meaning that we can perform all standard terra
raster operations on this object). To interact with SpatRaster
objects, you will need to have the library terra
loaded (otherwise you
might get errors as the correct method is not found, e.g. when
plotting). pastclim
automatically loads terra
, so you should be able
to work with terra
objects without any problem:
climate_20k
and plot these three variables (the layers of the raster):
terra::plot(climate_20k)
We can add more informative labels with var_labels
:
terra::plot(climate_20k, main = var_labels(climate_20k, dataset = "Example", abbreviated = TRUE) )
It is possible to also load a time series of rasters with the function
region_series
. In this case, the function returns a
SpatRasterDataset
, with each variable as a sub-dataset:
climate_region <- region_series( time_bp = list(min = -15000, max = 0), bio_variables = c("bio01", "bio10", "bio12"), dataset = "Example" ) climate_region
Each of these sub-dataset is a SpatRaster
, with time steps as layers:
climate_region$bio01
Note that terra
stores dates in years as AD, not BP. You can inspect
the times in years BP with:
time_bp(climate_region)
We can then plot the time series of a given variable (we relabel the plots to use years bp):
terra::plot(climate_region$bio01, main = time_bp(climate_region))
To plot all climate variables for a given time step, we can slice the time series:
slice_10k <- slice_region_series(climate_region, time_bp = -10000) terra::plot(slice_10k)
Instead of giving a minimum and maximum time step, you can also provide
specific time steps to region_series
. Note that pastclim
has a
function to get a vector of the time steps for a given MIS in a dataset.
For example, for MIS 1, we get:
mis1_steps <- get_mis_time_steps(mis = 1, dataset = "Example") mis1_steps
Which we can then use:
climate_mis1 <- region_series( time_bp = mis1_steps, bio_variables = c("bio01", "bio10", "bio12"), dataset = "Example" ) climate_mis1
Often we want to focus a given region. There are a number of preset
rectangular extents in pastclim
:
names(region_extent)
We can get the corners of the European extent:
region_extent$Europe
And then we can extract climate only for Europe by setting ext
in
region_slice
:
europe_climate_20k <- region_slice( time_bp = -20000, bio_variables = c("bio01", "bio10", "bio12"), dataset = "Example", ext = region_extent$Europe ) terra::plot(europe_climate_20k)
As we can see in the plot, cutting Europe using a rectangular shape
keeps a portion of Northern Africa in the map. pastclim
includes a
number of pre-generated masks for the main continental masses, stored in
the dataset region_outline
in an sf::sfc
object. We can get a list
with:
names(region_outline)
We can then use the function crop
within region_slice
to only keep
the area within the desired outline.
europe_climate_20k <- region_slice( time_bp = -20000, bio_variables = c("bio01", "bio10", "bio12"), dataset = "Example", crop = region_outline$Europe ) terra::plot(europe_climate_20k)
We can combine multiple regions together. For example, we can crop to Africa and Eurasia by unioning the two individual outlines:
library(sf) afr_eurasia <- sf::st_union(region_outline$Africa, region_outline$Eurasia) climate_20k_afr_eurasia <- region_slice( time_bp = -20000, bio_variables = c("bio01", "bio10", "bio12"), dataset = "Example", crop = afr_eurasia ) terra::plot(climate_20k_afr_eurasia)
Note that outlines that cross the antimeridian are split into multiple
polygons (so that they can be used without projecting the rasters). For
Eurasia, we have the eastern end of Siberia on the left hand side of the
plot. continent_outlines_union
provides the same outlines as single
polygons (in case you want to use a projection).
You can also use your own custom outline (i.e. a polygon, coded as a
terra::vect
object) as a mask to limit the area covered by the raster.
Note that you need to reuse the first vertex as the last vertex, to
close the polygon:
custom_vec <- terra::vect("POLYGON ((0 70, 25 70, 50 80, 170 80, 170 10, 119 2.4, 119 0.8, 116 -7.6, 114 -12, 100 -40, -25 -40, -25 64, 0 70))") climate_20k_custom <- region_slice( time_bp = -20000, bio_variables = c("bio01", "bio10", "bio12"), dataset = "Example", crop = custom_vec ) terra::plot(climate_20k_custom)
region_series
takes the same ext
and crop
options as
region_slice
to limit the extent of the climatic reconstructions.
The Beyer2020 and Krapp2021 datasets include a categorical variable detailing the extension of biomes.
get_biome_classes("Example")
We can get the biome for 20k years ago and plot it with:
biome_20k <- region_slice( time_bp = -20000, bio_variables = c("biome"), dataset = "Example" ) plot(biome_20k)
Note that the legend is massive. When plotting multiple time slices, it is best
to use legned=FALSE
in the plotting statement to avoid having the legend.
If we need to plot the extent of a specific biome, for example the
desert, we can simply set the other levels to NA:
biome_20k$desert <- biome_20k$biome biome_20k$desert[biome_20k$desert != 21] <- NA terra::plot(biome_20k$desert)
The climate reconstructions do not show areas under permanent ice. Ice sheets are stored as class 28 in the "biome" variable. We can retrieve directly the ice and land (all other biome categories) masks with:
ice_mask <- get_ice_mask(-20000, dataset = "Example") land_mask <- get_land_mask(-20000, dataset = "Example") terra::plot(c(ice_mask, land_mask))
We can also add the ice sheets to plots of climatic variables. First, we need to turn the ice mask into polygons:
ice_mask_vect <- as.polygons(ice_mask)
We can then add the polygons to each layer (i.e. variable) of climate
slice with the following code (note that, to add the polygons to every
panel of the figure, we need to create a function that is used as an
argument for fun
within plot
):
plot(climate_20k, fun = function() polys(ice_mask_vect, col = "gray", lwd = 0.5) )
In some other cases, we have multiple time points of the same variable and we want to see how the ice sheets change:
europe_climate <- region_series( time_bp = c(-20000, -15000, -10000, 0), bio_variables = c("bio01"), dataset = "Example", ext = region_extent$Europe ) ice_masks <- get_ice_mask(c(-20000, -15000, -10000, 0), dataset = "Example" ) ice_poly_list <- lapply(ice_masks, as.polygons) plot(europe_climate$bio01, main = time_bp(europe_climate), fun = function(i) { polys(ice_poly_list[[i]], col = "gray", lwd = 0.5 ) } )
Note that to add the ice sheets in this instance, we build a function that takes a single parameter i which is the index of the image (i.e. i from 1 to 4 in the plot above) and use it to subset the list of ice outlines.
Sometimes it is interesting to measure the distance from the coastline
(e.g. when modelling species that rely on brackish water, or to
determine the distance from marine resources in archaeology). In
pastclim
, we can use use distance_from_sea
, which accounts for sea
level change based on the landmask:
distances_sea <- distance_from_sea(time_bp = c(-20000, 0), dataset = "Example") distances_sea_australia <- crop(distances_sea, terra::ext(100, 170, -60, 20)) plot(distances_sea_australia, main = time_bp(distances_sea_australia))
To plot locations on region plots, we first need to create a
SpatVector
object from the dataframe of metadata, specifying the names
of the columns with the x and y coordinates:
locations_vect <- vect(locations, geom = c("longitude", "latitude")) locations_vect
We can then add it to a climate slice with the following code (note
that, to add the points to every panel of the figure, we need to create
a function that is used as an argument for fun
within plot
):
plot(europe_climate_20k, fun = function() points(locations_vect, col = "red", cex = 2) )
Only the points within the extent of the region will be plotted (so, in this case, only the European locations).
We can combine ice sheets and locations in a single plot:
plot(europe_climate_20k, fun = function() { polys(ice_mask_vect, col = "gray", lwd = 0.5) points(locations_vect, col = "red", cex = 2) } )
In many studies, we want to set the environmental conditions at a given set of location within the background for that time period. Let us start by visualising the background for the time step of interest with a PCA:
bio_vars <- c("bio01", "bio10", "bio12") climate_10k <- region_slice(-10000, bio_variables = bio_vars, dataset = "Example" ) climate_values_10k <- df_from_region_slice(climate_10k) climate_10k_pca <- prcomp(climate_values_10k[, bio_vars], scale = TRUE, center = TRUE ) plot(climate_10k_pca$x[, 2] ~ climate_10k_pca$x[, 1], pch = 20, col = "lightgray", xlab = "PC1", ylab = "PC2" )
We can now get the climatic conditions for the locations at this time step and compute the PCA scores based on the axes we defined on the background:
locations_10k <- data.frame( longitude = c(0, 90, 20, 5), latitude = c(20, 45, 50, 47), time_bp = c(-9932, -9753, -10084, -10249) ) climate_loc_10k <- location_slice( x = locations_10k[, c("longitude", "latitude")], time_bp = locations_10k$time_bp, bio_variables = bio_vars, dataset = "Example" ) locations_10k_pca_scores <- predict(climate_10k_pca, newdata = climate_loc_10k[, bio_vars] )
And now we can plot the points on top of the background
plot(climate_10k_pca$x[, 2] ~ climate_10k_pca$x[, 1], pch = 20, col = "lightgray", xlab = "PC1", ylab = "PC2" ) points(locations_10k_pca_scores, pch = 20, col = "red")
If we want to pool the background from multiple time steps, we can
simple use region_series
to get a series, and then transform it into a
data frame with df_from_region_series
.
In some instances (e.g. when the underlying raster is too large to handle),
it might be desirable to sample the background instead of using all values. If
we are interested in a single time step, we can simply
generate the raster for the time slice of interest, and use
sample_region_slice
:
climate_20k <- region_slice( time_bp = -20000, bio_variables = c("bio01", "bio10"), dataset = "Example" ) this_sample <- sample_region_slice(climate_20k, size = 100) head(this_sample)
If we have samples from multiple time steps, we need to sample the background proportionally to the number of points in each time step. So, for example, if we wanted 30 samples from 20k years ago and 50 samples from 10k years ago:
climate_ts <- region_series( time_bp = c(-20000, -10000), bio_variables = c("bio01", "bio10", "bio12"), dataset = "Example", ext = terra::ext(region_extent$Europe) ) sampled_climate <- sample_region_series(climate_ts, size = c(3, 5)) sampled_climate
We could then use these data to build a PCA.
pastclim
does not contain built-in code to change the spatial
resolution of the climatic reconstructions, but it is possible to
downscale the data by using the relevant function from the terra
package.
At first we will need to extract a region and time of choice, in this case Europe 10,000 years ago
europe_10k <- region_slice( dataset = "Example", bio_variables = c("bio01"), time_bp = -10000, ext = region_extent$Europe ) terra::plot(europe_10k)
We can then downscale using the disagg()
function from the terra
package, requiring an aggregation factor expressed as number of cells in
each direction (horizontally, vertically, and, if needed, over layers).
In the example below we used 25 both horizontally and vertically, using
bilinear interpolation.
europe_ds <- terra::disagg(europe_10k, fact = 25, method = "bilinear") terra::plot(europe_ds)
Note that, whilst we have smoothed the climate, the land mask has not changed, and thus it still has very blocky edges.
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