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In the previous vignette we saw how to download and prepare OISST data. In this vignette we will use the subsetted data we downloaded (not global) for our example on how to detect MHWs in gridded data.
library(dplyr) # For basic data manipulation
library(ggplot2) # For visualising data
library(heatwaveR) # For detecting MHWs
library(tidync) # For easily dealing with NetCDF data
library(doParallel) # For parallel processing
Because we saved our data as an .Rds
file, loading it into R is easy.
<- readRDS("~/Desktop/OISST_vignette.Rds") OISST
dplyr
vs. plyr
When we want to make the same calculation across multiple groups of data within one dataframe we have two good options available to us. The first is to make use of the map()
suite of functions found in the purrr
package, and now implemented in dplyr
. This is a very fast tidyverse
friendly approach to splitting up tasks. The other good option is to go back in time a bit and use the ddply()
function from the plyr
package. This is arguably a better approach as it allows us to very easily use multiple cores to detect the MHWs. The problem with this approach is that one must never load the plyr
library directly as it has some fundamental inconsistencies with the tidyverse
. We will see below how to perform these two different techniques without causing ourselves any headaches.
It is a little clumsy to use multiple functions at once with the two methods so we will combine the calculations we want to make into one wrapper function.
<- function(df){
event_only # First calculate the climatologies
<- ts2clm(data = df, climatologyPeriod = c("1982-01-01", "2011-01-01"))
clim # Then the events
<- detect_event(data = clim)
event # Return only the event metric dataframe of results
return(event$event)
}
dplyr
methodThis method requires no special consideration and is performed just as any other friendly tidyverse
code chunk would be.
system.time(
# First we start by choosing the 'OISST' dataframe
<- OISST %>%
MHW_dplyr # Then we group the data by the 'lon' and 'lat' columns
group_by(lon, lat) %>%
# Then we run our MHW detecting function on each group
group_modify(~event_only(.x))
# ~123 seconds )
Running the above calculations with only one of the 2.8 GHz cores on a modern laptop took ~123 seconds. It must be noted however that a recent update to the dplyr
package now allows it to interrogate one’s computer to determine how many cores it has at it’s disposal. It then uses one core at full capacity and the other cores usually at half capacity.
plyr
techniqueThis method requires that we first tell our machine how many of its processor cores to give us for our calculation.
# NB: One should never use ALL available cores, save at least 1 for other essential tasks
# The computer I'm writing this vignette on has 8 cores, so I use 7 here
registerDoParallel(cores = 7)
# Detect events
system.time(
<- plyr::ddply(.data = OISST, .variables = c("lon", "lat"), .fun = event_only, .parallel = TRUE)
MHW_plyr # 33 seconds )
The plyr
technique took 33 seconds using seven cores. This technique is not seven times faster because when using multiple cores there is a certain amount of loss in efficiency due to the computer needing to remember which results are meant to go where so that it can stitch everything back together again for you. This takes very little memory, but over large jobs it can start to become problematic. Occasionally ‘slippage’ can occur as well where an entire task can be forgotten. This is very rare but does happen. This is partly what makes dplyr
a viable option as it does not have this problem. The other reason is that dplyr
performs more efficient calculations than plyr
. But what if we could have the best of both worlds?
As one may see above, running these calculations on a very large (or even global) gridded dataset can quickly become very heavy. While running these calculations myself on the global OISST dataset I have found that the fastest option is to combine the two options above. In my workflow I have saved each longitude segment of the global OISST dataset as separate files and use the dplyr
method on each individual file, while using the plyr
method to be running the multiple calculations on as many files as my core limit will allow. One may not do this the other way around and use dplyr
to run multiple plyr
calculations at once. This will confuse your computer and likely cause a stack overflow. Which sounds more fun than it actually is… as I have had to learn.
In order to happily combine these two options into one we will need to convert the dplyr
code we wrote above into it’s own wrapper function, which we will then call on a stack of files using the plyr
technique. Before we do that we must first create the aforementioned stack of files.
for(i in 1:length(unique(OISST$lon))){
<- OISST %>%
OISST_sub filter(lon == unique(lon)[i])
saveRDS(object = OISST_sub, file = paste0("~/Desktop/OISST_lon_",i,".Rds"))
}
This may initially seem like an unnecessary extra step, but when one is working with time series data it is necessary to have all of the dates at a given pixel loaded at once. Unless one is working from a server/virtual machine/supercomputer this means that one will often not be able to comfortably hold an entire grid for a study area in memory at once. Having the data accessible as thin strips like this makes life easier. And as we see in the code chunk below it also (arguably) allows us to perform the most efficient calculations on our data.
# The 'dplyr' wrapper function to pass to 'plyr'
<- function(file_name){
dplyr_wraper <- readRDS(file_name) %>%
MHW_dplyr group_by(lon, lat) %>%
group_modify(~event_only(.x))
}# Create a vector of the files we want to use
<- dir("~/Desktop", pattern = "OISST_lon_*", full.names = T)
OISST_files
# Use 'plyr' technique to run 'dplyr' technique with multiple cores
system.time(
<- plyr::ldply(OISST_files, .fun = dplyr_wraper, .parallel = T)
MHW_result # 31 seconds
)
# Save for later use as desired
saveRDS(MHW_result, "~/Desktop/MHW_result.Rds")
Even though this technique is not much faster computationally, it is much lighter on our memory (RAM) as it only loads one longitude slice of our data at a time. To maximise efficiency even further I would recommend writing out this full workflow in a stand-alone script and then running it using source()
directly from an R terminal. The gain in speed here appears nominal, but as one scales this up the speed boost becomes apparent.
As mentioned above, recent changes to how dplyr
interacts with one’s computer has perhaps slowed down the plyr
+ dplyr
workflow shown here. It may be now that simply using plyr
by itself is the better option. It depends on the number of cores and the amount of RAM that one has available.
Because of human-induced climate change, we anticipate that extreme events will occur more frequently and that they will become greater in intensity. Here we investigate this hypothesis by using gridded SST data, which is the only way that we can assess if this trend is unfolding across large ocean regions. Using the gridded 0.25 degree Reynolds OISST, we will detect marine heatwaves (MHWs) around South Africa by applying the detect_event()
function pixel-by-pixel to the data we downloaded in the previous vignette. After detecting the events, we will fit a generalised linear model (GLM) to each pixel to calculate rates of change in some MHW metrics, and then plot the estimated trends.
With our MHW detected we will now look at how to fit some GLMs to the results in order to determine long-term trends in MHW occurrence.
Up first we see how to calculate the number of events that occurred per pixel.
# summarise the number of unique longitude, latitude and year combination:
<- MHW_result %>%
OISST_n mutate(year = lubridate::year(date_start)) %>%
group_by(lon, lat, year) %>%
summarise(n = n(), .groups = "drop") %>%
group_by(lon, lat) %>%
::complete(year = c(1982:2019)) %>% # Note that these dates may differ
tidyrmutate(n = ifelse(is.na(n), 0, n))
head(OISST_n)
Then we specify the particulars of the GLM we are going to use.
<- function(ev) {
lin_fun <- glm(n ~ year, family = poisson(link = "log"), data = ev)
mod1 # extract slope coefficient and its p-value
<- data.frame(slope = summary(mod1)$coefficients[2,1],
tr p = summary(mod1)$coefficients[2,4])
return(tr)
}
Lastly we make the calculations.
<- plyr::ddply(OISST_n, c("lon", "lat"), lin_fun, .parallel = T)
OISST_nTrend $pval <- cut(OISST_nTrend$p, breaks = c(0, 0.001, 0.01, 0.05, 1))
OISST_nTrendhead(OISST_nTrend)
Let’s finish this vignette by visualising the long-term trends in the annual occurrence of MHWs per pixel in the chosen study area. First we will grab the base global map from the maps
package.
# The base map
<- ggplot2::fortify(maps::map(fill = TRUE, plot = FALSE)) %>%
map_base ::rename(lon = long) dplyr
Then we will create two maps that we will stick together using ggpubr
. The first map will show the slope of the count of events detected per year over time as shades of red, and the second map will show the significance (p-value) of these trends in shades of grey.
<- ggplot(OISST_nTrend, aes(x = lon, y = lat)) +
map_slope geom_rect(size = 0.2, fill = NA,
aes(xmin = lon - 0.1, xmax = lon + 0.1, ymin = lat - 0.1, ymax = lat + 0.1,
colour = pval)) +
geom_raster(aes(fill = slope), interpolate = FALSE, alpha = 0.9) +
scale_fill_gradient2(name = "count/year (slope)", high = "red", mid = "white",
low = "darkblue", midpoint = 0,
guide = guide_colourbar(direction = "horizontal",
title.position = "top")) +
scale_colour_manual(breaks = c("(0,0.001]", "(0.001,0.01]", "(0.01,0.05]", "(0.05,1]"),
values = c("firebrick1", "firebrick2", "firebrick3", "white"),
name = "p-value", guide = FALSE) +
geom_polygon(data = map_base, aes(group = group),
colour = NA, fill = "grey80") +
coord_fixed(ratio = 1, xlim = c(13.0, 23.0), ylim = c(-33, -42), expand = TRUE) +
labs(x = "", y = "") +
theme_bw() +
theme(legend.position = "bottom")
<- ggplot(OISST_nTrend, aes(x = lon, y = lat)) +
map_p geom_raster(aes(fill = pval), interpolate = FALSE) +
scale_fill_manual(breaks = c("(0,0.001]", "(0.001,0.01]", "(0.01,0.05]",
"(0.05,0.1]", "(0.1,0.5]", "(0.5,1]"),
values = c("black", "grey20", "grey40",
"grey80", "grey90", "white"),
name = "p-value",
guide = guide_legend(direction = "horizontal",
title.position = "top")) +
geom_polygon(data = map_base, aes(group = group),
colour = NA, fill = "grey80") +
coord_fixed(ratio = 1, xlim = c(13.0, 23.0), ylim = c(-33, -42), expand = TRUE) +
labs(x = "", y = "") +
theme_bw() +
theme(legend.position = "bottom")
<- ggpubr::ggarrange(map_slope, map_p, align = "hv")
map_both map_both
From the figure above we may see that the entire study area shows significant (p<= 0.05) increases in the count of MHWs per year. This is generally the case for the entire globe. Not shown here is the significant increase in the intensity of MHWs as well.
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