rerddap is a general purpose R client for working with ERDDAP servers. ERDDAP is a web service developed by Bob Simons of NOAA. At the time of this writing, there are over sixty ERDDAP servers (though not all are public facing) providing access to literally petabytes of data and model output relevant to oceanography, meteorology, fisheries and marine mammals, among other areas. ERDDAP is a simple to use, RESTful web service, that allows data to be subsetted and returned in a variety of formats.
This vignette goes over some of the nuts and bolts of using the rerddap package, and shows the power of the combination of the rerddap package with ERDDAP servers. Some of the examples are taken from the xtractomatic package (available from CRAN - https://cran.r-project.org/package=xtractomatic), and some from the rerddapXtracto package available on Github (https://github.com/rmendels/rerddapXtracto), but reworked to use rerddap directly. Other examples are new to this vignette, and include both gridded and non-gridded datasets from several ERDDAPs.
The first step is to install the rerddap package, the stable version is available from CRAN:
install.packages("rerddap")
or the development version can be installed from GitHub:
devtools::install_github("ropensci/rerddap")
and to load the library:
library("rerddap")
Besides rerddap the following libraries are used in this vignette:
library("akima")
library("dplyr")
library("ggplot2")
library("mapdata")
library("ncdf4")
library("plot3D")
Code chunks are always given with the required libraries so that the chunks are more standalone in nature. Many of the plots use the cmocean colormaps designed by Kristen Thyng (see http://matplotlib.org/cmocean/ and https://github.com/matplotlib/cmocean). These colormaps were initally developed for Python, but a version of the colormaps is used in the oce package by Dan Kelley and Clark Richards and that is what is used here.
rerddap functionsThe complete list of rerddap functions can be seen by looking at he rerddap package help:
?rerddap
and selecting the index of the package. The main functions used here are:
rerddap knows about - server()ed_search(query, page = NULL, page_size = NULL, which = "griddap", url = eurl(), ...)ed_datasets(which = "tabledap", url = eurl())info(datasetid, url = eurl(), ...)griddap(x, ..., fields = "all", stride = 1, fmt = "nc", url = eurl(), store = disk(), read = TRUE, callopts = list())tabledap(x, ..., fields = NULL, distinct = FALSE, orderby = NULL, orderbymax = NULL, orderbymin = NULL, orderbyminmax = NULL, units = NULL, url = eurl(), store = disk(), callopts = list())Be careful when using the functions ed_search() and ed_datasets(). The default ERDDAP has over 9,000 datasets, most of which are grids, so that a list of all the gridded datasets can be quite long. A seemly reasonable search:
whichSST <- ed_search(query = "SST")
returns about 1000 responses. The more focused query:
whichSST <- ed_search(query = "SST MODIS")
still returns 172 responses. If the simple search doesn't narrow things enough, look at the advanced search function ed_search_adv().
The first way to find a dataset is to browse the builtin web page for a particular ERDDAP server.
A list of some of the public available ERDDAP servers can be obtained from the rerddap command:
servers()
#> name
#> 1 Marine Domain Awareness (MDA) - Italy
#> 2 Marine Institute - Ireland
#> 3 CoastWatch Caribbean/Gulf of Mexico Node
#> 4 CoastWatch West Coast Node
#> 5 NOAA IOOS CeNCOOS (Central and Northern California Ocean Observing System)
#> 6 NOAA IOOS NERACOOS (Northeastern Regional Association of Coastal and Ocean Observing Systems)
#> 7 NOAA IOOS NGDAC (National Glider Data Assembly Center)
#> 8 NOAA IOOS PacIOOS (Pacific Islands Ocean Observing System) at the University of Hawaii (UH)
#> 9 NOAA IOOS SECOORA (Southeast Coastal Ocean Observing Regional Association)
#> 10 NOAA NCEI (National Centers for Environmental Information) / NCDDC
#> 11 NOAA OSMC (Observing System Monitoring Center)
#> 12 NOAA UAF (Unified Access Framework)
#> 13 ONC (Ocean Networks Canada)
#> 14 UC Davis BML (University of California at Davis, Bodega Marine Laboratory)
#> 15 R.Tech Engineering
#> 16 French Research Institute for the Exploitation of the Sea
#> url
#> 1 https://bluehub.jrc.ec.europa.eu/erddap/
#> 2 http://erddap.marine.ie/erddap/
#> 3 http://cwcgom.aoml.noaa.gov/erddap/
#> 4 https://coastwatch.pfeg.noaa.gov/erddap/
#> 5 http://erddap.axiomalaska.com/erddap/
#> 6 http://www.neracoos.org/erddap/
#> 7 http://data.ioos.us/gliders/erddap/
#> 8 http://oos.soest.hawaii.edu/erddap/
#> 9 http://129.252.139.124/erddap/
#> 10 http://ecowatch.ncddc.noaa.gov/erddap/
#> 11 http://osmc.noaa.gov/erddap/
#> 12 https://upwell.pfeg.noaa.gov/erddap/
#> 13 http://dap.onc.uvic.ca/erddap/
#> 14 http://bmlsc.ucdavis.edu:8080/erddap/
#> 15 http://meteo.rtech.fr/erddap/
#> 16 http://www.ifremer.fr/erddap/index.html
The second way to find and obtain the desired data is to use functions in rerddap. The basic steps are:
rerddap::servers(), rerddap::ed_search(), rerddap::ed_datasets() ).rerddap::info() )rerddap::griddap() or rerddap::tabledap() ).We discuss each of these steps in more detail, and then look at some realistic uses of the package.
This may seem to be a strange step in the process, but it is important because many of the datasets are high-resolution, and data requests can get very large, very quickly. As an example, based on a real use case. The MUR SST ( Multi-scale Ultra-high Resolution (MUR) SST Analysis fv04.1, see https://coastwatch.pfeg.noaa.gov/erddap/griddap/jplMURSST41.html ) is a daily, high-quality, high-resolution sea surface temperature product. The user wanted the MUR data for a 2x2-degree box, daily for a year. That seems innocuous enough. Except that MURsst is at a one-hundreth of degree resolution. If we assume just a binary representation of the data, assuming 8-bytes per value, and do the math:
100*100*4*8*365
#> [1] 116800000
Yes, 116,800,000 bytes or roughly 115MB for that request. Morever the user wanted the data as a .csv file, which usually makes the resulting file 8-10 times larger, so now we are over a 1GB for the request. Even more so, there are four parameters in that dataset, and in rerddap::griddap() if “fields” is not specified, all fields are downloaded, therefore the resulting files will be four times as large as given above.
So the gist of this is to think about your request before you make it. Do a little mental math to get a rough estimate of the size of the download. There are times receiving the data as a .csv file is convenient, but make certain the request will not be too large. For larger requests, obtain the data as netCDF files. By default, rerddap::griddap() “melts”“ the data into a dataframe, so a .csv only provides a small convenience. But for really large downloads, you should select the option in rerddap::griddap() to not read in the data, and use instead the netcdf4 package to read in the data, as this allows for only reading in parts of the data at a time. Below we provide a brief tutorial on reading in data using the ncdf4 package.
One of the main advantages of a service such as ERDDAP is that you only need to download the subset of the data you desire, rather than the entire dataset, which is both convenient and essential for large datasets. The underlying data model in ERDDAP is quite simple - everything is either a (multi-dimensional) grid (think R array) or a table (think a simple spreadsheet or data table). Grids are subsetted using the function griddap() and tables are subset using the function tabledap().
If you know the datasetID of the data you are after, and are unsure if it is a grid or a table, there are several ways to find out. We will look at two datasets, 'jplMURSST41' and 'siocalcofiHydroCasts'. The first method is to use the rerddap function browse()
browse('jplMURSST41')
browse('siocalcofiHydroCasts')
which brings up information on the datasets in the browser, in the first case the "data” link is under “griddap”, the second is under “tabledap”.
The other method is to use the rerddap function info:
info('jplMURSST41')
#> <ERDDAP info> jplMURSST41
#> Dimensions (range):
#> time: (2002-06-01T09:00:00Z, 2017-05-10T09:00:00Z)
#> latitude: (-89.99, 89.99)
#> longitude: (-179.99, 180.0)
#> Variables:
#> analysed_sst:
#> Units: degree_C
#> analysis_error:
#> Units: degree_C
#> mask:
#> sea_ice_fraction:
#> Units: fraction
info('siocalcofiHydroCasts')
#> <ERDDAP info> siocalcofiHydroCasts
#> Variables:
#> ac_line:
#> ac_sta:
#> barometer:
#> Units: millibars
#> bottom_d:
#> Units: meters
#> cast_id:
#> civil_t:
#> Units: seconds since 1970-01-01T00:00:00Z
#> cloud_amt:
#> Units: oktas
#> cloud_typ:
#> cruise_id:
#> cruz_leg:
#> cruz_num:
#> cruz_sta:
#> cst_cnt:
#> data_or:
#> data_type:
#> date:
#> dbsta_id:
#> distance:
#> dry_t:
#> Units: degree C
#> event_num:
#> forelu:
#> Units: Forel-Ule scale
#> inc_end:
#> Units: seconds since 1970-01-01T00:00:00Z
#> inc_str:
#> Units: seconds since 1970-01-01T00:00:00Z
#> intc14:
#> Units: milligrams Carbon per square meter
#> intchl:
#> julian_date:
#> julian_day:
#> latitude:
#> Range: 18.417, 47.917
#> Units: degrees_north
#> latitude_degrees:
#> latitude_hemisphere:
#> latitude_minutes:
#> longitude:
#> Range: -164.083, -105.967
#> Units: degrees_east
#> longitude_degrees:
#> longitude_hemisphere:
#> longitude_minutes:
#> month:
#> Range: 1, 12
#> order_occ:
#> orig_sta_id:
#> pst_lan:
#> Units: seconds since 1970-01-01T00:00:00Z
#> quarter:
#> rpt_line:
#> rpt_sta:
#> secchi:
#> Units: meters
#> ship_code:
#> ship_name:
#> st_line:
#> st_station:
#> sta_code:
#> sta_id:
#> time:
#> Range: -6.5759508E8, 1.423140778E9
#> Units: seconds since 1970-01-01T00:00:00Z
#> time_ascii:
#> timezone:
#> visibility:
#> wave_dir:
#> Units: degrees
#> wave_ht:
#> Units: feet
#> wave_prd:
#> Units: seconds
#> wea:
#> wet_t:
#> Units: degree C
#> wind_dir:
#> Units: degrees
#> wind_spd:
#> Units: knots
#> year:
#> Range: 1949, 2015
Notice the information on 'jplMURSST41' lists the dimensions (that is a grid) while that of 'siocalcofiHydroCasts' does not (that is a table).
Like an R array, ERDDAP grids are subsetted by setting limits on the dimension variables, the difference being that a subset is defined in coordinate space (latitude values, longitude values, time values) rather than array space as is done with R arrays. Thus for 'jplMURSST41' if the desired area of the data extract is latitude limits of (22N, 51N), longitude limits of (140W, 105W), and with time limits of (2017-01-01, 2017-01-02) the following would be passed to the function griddap():
latitude = c(22., 51.)
longitude = c(-140., -105)
time = c("2017-01-01", "2017-01-02")
A full griddap() request to retrieve “analysed_sst” with these constraints would be:
sstInfo <- info('jplMURSST41')
murSST <- griddap(sstInfo, latitude = c(22., 51.), longitude = c(-140., -105), time = c("2017-01-01", "2017-01-02"), fields = 'analysed_sst')
Strides allow to retrieve data within a coordinate bound only at every “n” values, where “n” is an integer - think of the “by” part of the R function seq(). This is useful say for a monthly dataset where only the December values are desired, or you want to subsample a very high resolution dataset. The default is a stride of 1 for all dimensions. If you want to change the stride value in any dimension, then the value must be given for all dimensions. So in the previous example, if only every fifth longitude is desired, the call would be:
murSST <- griddap(sstInfo, latitude = c(22., 51.), longitude = c(-140., -105), time = c("2017-01-01", "2017-01-02"), stride = c(1,1,5), fields = 'analysed_sst')
Strides are done in array space, not in coordinate space - so it is not skipping say a number of degrees of longitude, but is skipping a number of values of the array index - if longitude is thought of as an array, then every fifth value is used. There are many cases where having strides work in coordinate space would be handy, but it can cause a lot of problems. Consider the case where neither the starting longitude, nor the ending longitude in the request lie on the actual data grid, and the stride is in coordinate units in such a way that no value requested actually lies on an actual grid value. This would be equivalent to the more complicated problem of data regridding and data interpolation.
When ERDDAP receives a request where the bounds are not on the actual dataset grid, ERDDAP finds the closest values on the grid to the requested bounds, and returns those points and all grid points in between. If a stride is added of a value greater than one but resricted to array space, this guarantees that every value returned lies on the dataset grid.
Tables in ERDDAP are subset by using “constraint expressions” on any variable in the table. The valid operators are =, != (not equals), =~ (a regular expression test), <, <=, >, and >=. The constraint is constructed as the parameter on the left, value on the right, and the operator in the middle, all within a set of quotes. For example, if in the SWFSC/FRD trawl catch data (datasetID 'FRDCPSTrawlLHHaulCatch'), only sardines for 2010 were desired, the following constraints would be set in the tabledap() call:
'time>=2010-01-01'
'time<=2010-12-31'
'scientific_name="Sardinops sagax"'
Note that in tabledap() character strings usually must be passed as “double-quoted”, as seen in the example with the scientific name. A full tabledap() request to retrieve 'latitude', 'longitude', 'time', 'scientific_name', and 'subsample_count' with these constraints would be:
CPSinfo <- info('FRDCPSTrawlLHHaulCatch')
sardines <- tabledap(CPSinfo, fields = c('latitude', 'longitude', 'time', 'scientific_name', 'subsample_count'), 'time>=2010-01-01', 'time<=2010-12-31', 'scientific_name="Sardinops sagax"' )
MUR (Multi-scale Ultra-high Resolution) is an analyzed SST product at 0.01-degree resolution going back to 2002, providing one of the longest satellite based time series at such high resolution (see https://podaac.jpl.nasa.gov/dataset/MUR-JPL-L4-GLOB-v4.1). The latest data available for a region off the west coast can be extracted and plotted by:
require("ggplot2")
require("mapdata")
require("rerddap")
sstInfo <- info('jplMURSST41')
# get latest daily sst
murSST <- griddap(sstInfo, latitude = c(22., 51.), longitude = c(-140., -105), time = c('last','last'), fields = 'analysed_sst')
mycolor <- colors$temperature
w <- map_data("worldHires", ylim = c(22., 51.), xlim = c(-140, -105))
ggplot(data = murSST$data, aes(x = lon, y = lat, fill = analysed_sst)) +
geom_polygon(data = w, aes(x = long, y = lat, group = group), fill = "grey80") +
geom_raster(interpolate = FALSE) +
scale_fill_gradientn(colours = mycolor, na.value = NA) +
theme_bw() + ylab("latitude") + xlab("longitude") +
coord_fixed(1.3, xlim = c(-140, -105), ylim = c(22., 51.)) + ggtitle("Latest MUR SST")
VIIRS (Visible Infrared Imaging Radiometer Suite) is a scanning radiometer, that collects visible and infrared imagery and radiometric measurements of the land, atmosphere, cryosphere, and oceans. VIIRS data is used to measure cloud and aerosol properties, ocean color, sea and land surface temperature, ice motion and temperature, fires, and Earth's albedo. Both NASA and NOAA provide VIIRS-based high resolution SST and chlorophyll products.
ERD provides a 3-day composite SST product at 750 meter resolution developed from a real-time NOAA product. The most recent values can be obtained by setting “time” to be “last”. (Note that R sees the latitude-longitude grid as slightly uneven (even though it is in fact even), and that produces artificial lines in ggplot2::geom_raster(). In order to remove those lines, the latitude-longitude grid is remapped to an evenly-space grid.)
require("ggplot2")
require("mapdata")
require("rerddap")
sstInfo <- info('erdVHsstaWS3day')
# get latest 3-day composite sst
viirsSST <- griddap(sstInfo, latitude = c(41., 31.), longitude = c(-128., -115), time = c('last','last'), fields = 'sst')
# remap latitiudes and longitudes to even grid
myLats <- unique(viirsSST$data$lat)
myLons <- unique(viirsSST$data$lon)
myLats <- seq(range(myLats)[1], range(myLats)[2], length.out = length(myLats))
myLons <- seq(range(myLons)[1], range(myLons)[2], length.out = length(myLons))
# melt these out to full grid
mapFrame <- expand.grid(x = myLons, y = myLats)
mapFrame$y <- rev(mapFrame$y)
# form a frame with the new values and the data
tempFrame <- data.frame(sst = viirsSST$data$sst, lat = mapFrame$y, lon = mapFrame$x)
mycolor <- colors$temperature
w <- map_data("worldHires", ylim = c(30., 42.), xlim = c(-128, -114))
ggplot(data = tempFrame, aes(x = lon, y = lat, fill = sst)) +
geom_polygon(data = w, aes(x = long, y = lat, group = group), fill = "grey80") +
geom_raster(interpolate = FALSE) +
scale_fill_gradientn(colours = mycolor, na.value = NA) +
theme_bw() + ylab("latitude") + xlab("longitude") +
coord_fixed(1.3, xlim = c(-128, -114), ylim = c(30., 42.)) + ggtitle("Latest VIIRS 3-day SST")
A time series from the same dataset at a given location, here (36., -126.):
require("ggplot2")
require("rerddap")
viirsSST1 <- griddap(sstInfo, latitude = c(36., 36.),
longitude = c(-126., -126.),
time = c('2015-01-01','2015-12-31'), fields = 'sst')
tempTime <- as.Date(viirsSST1$data$time, origin = '1970-01-01', tz = "GMT")
tempFrame <- data.frame(time = tempTime, sst = viirsSST1$data$sst)
ggplot(tempFrame, aes(time, sst)) +
geom_line() +
theme_bw() +
ylab("sst") +
ggtitle("VIIRS SST at (36N, 126W)")
A similar 3-day composite for chloropyll for the same region from a scientific quality product developed by NOAA:
require("ggplot2")
require("mapdata")
require("rerddap")
chlaInfo <- info('erdVHNchla3day')
viirsCHLA <- griddap(chlaInfo, latitude = c(41., 31.),
longitude = c(-128., -115), time = c('last','last'),
fields = 'chla')
# get latest 3-day composite sst
mycolor <- colors$chlorophyll
w <- map_data("worldHires", ylim = c(30., 42.), xlim = c(-128, -114))
ggplot(data = viirsCHLA$data, aes(x = lon, y = lat, fill = log(chla))) +
geom_polygon(data = w, aes(x = long, y = lat, group = group), fill = "grey80") +
geom_raster(interpolate = FALSE) +
scale_fill_gradientn(colours = mycolor, na.value = NA) +
theme_bw() + ylab("latitude") + xlab("longitude") +
coord_fixed(1.3, xlim = c(-128, -114), ylim = c(30., 42.)) +
ggtitle("Latest VIIRS 3-day Chla")
#> Warning: Removed 1781323 rows containing missing values (geom_raster).
This is an example of an extract from a 4-D dataset (results from the “Simple Ocean Data Assimilation (SODA)” model - see http://www.atmos.umd.edu/~ocean/), and illustrate the case where the z-coordinate does not have the default name “altitude”. Water temperature at 70m depth is extracted for the North Pacific Ocean.
require("rerddap")
dataInfo <- rerddap::info('hawaii_d90f_20ee_c4cb')
xpos <- c(135.25, 240.25)
ypos <- c(20.25, 60.25)
zpos <- c(70.02, 70.02)
tpos <- c('2010-12-15', '2010-12-15')
soda70 <- griddap(dataInfo, longitude = xpos, latitude = ypos,
time = tpos, depth = zpos, fields = 'temp' )
str(soda70$data)
#> 'data.frame': 17091 obs. of 4 variables:
#> $ time: chr "2010-12-15T00:00:00Z" "2010-12-15T00:00:00Z" "2010-12-15T00:00:00Z" "2010-12-15T00:00:00Z" ...
#> $ lat : num 20.2 20.2 20.2 20.2 20.2 ...
#> $ lon : num 135 136 136 137 137 ...
#> $ temp: num 27.1 27.1 27.5 27.8 28.2 ...
Since the data cross the dateline, it is necessary to use the new “world2Hires” continental outlines in the package mapdata which is Pacific Ocean centered. Unfortunatley there is a small problem where the outlines from certain countries wrap and mistakenly appear in plots, and those countries must be removed, see code below.
require("ggplot2")
require("mapdata")
xlim <- c(135, 240)
ylim <- c(20, 60)
my.col <- colors$temperature
## Must do a kludge to remove countries that wrap and mess up the plot
w1 <- map("world2Hires", xlim = c(135, 240), ylim = c(20, 60), fill = TRUE, plot = FALSE)
remove <- c("UK:Great Britain", "France", "Spain", "Algeria", "Mali", "Burkina Faso", "Ghana", "Togo")
w <- map_data("world2Hires", regions = w1$names[!(w1$names %in% remove)], ylim = ylim, xlim = xlim)
myplot <- ggplot() +
geom_raster(data = soda70$data, aes(x = lon, y = lat, fill = temp), interpolate = FALSE) +
geom_polygon(data = w, aes(x = long, y = lat, group = group), fill = "grey80") +
theme_bw() + scale_fill_gradientn(colours = my.col, na.value = NA, limits = c(-3,30), name = "temperature") +
ylab("latitude") + xlab("longitude") +
coord_fixed(1.3, xlim = xlim, ylim = ylim) +
ggtitle(paste("70m temperature ", soda70$data$time[1]))
myplot
The Irish Marine Institute has an ERDDAP server at http://erddap.marine.ie/erddap. Among other datasets, they have hourly output from a model of the North Altantic ocean, with a variety of ocean related parameters, see http://erddap.marine.ie/erddap/griddap/IMI_NEATL.html. To obtain the latest sea surface salinity for the domain of the model:
require("rerddap")
urlBase <- "http://erddap.marine.ie/erddap/"
parameter <- "sea_surface_salinity"
sssTimes <- c("last", "last")
sssLats <- c(48.00625, 57.50625)
sssLons <- c(-17.99375, -1.00625)
dataInfo <- rerddap::info("IMI_NEATL", url = urlBase)
NAtlSSS <- griddap(dataInfo, longitude = sssLons, latitude = sssLats, time = sssTimes, fields = parameter, url = urlBase)
str(NAtlSSS$data)
#> 'data.frame': 1034960 obs. of 4 variables:
#> $ time : chr "2017-05-14T00:00:00Z" "2017-05-14T00:00:00Z" "2017-05-14T00:00:00Z" "2017-05-14T00:00:00Z" ...
#> $ lat : num 48 48 48 48 48 ...
#> $ lon : num -18 -18 -18 -18 -17.9 ...
#> $ sea_surface_salinity: num 35.6 35.6 35.6 35.6 35.6 ...
and the extracted data plotted:
require("ggplot2")
require("mapdata")
xlim <- c(-17.99375, -1.00625)
ylim <- c(48.00625, 57.50625)
my.col <- colors$salinity
w <- map_data("worldHires", ylim = ylim, xlim = xlim)
myplot <- ggplot() +
geom_raster(data = NAtlSSS$data, aes(x = lon, y = lat, fill = sea_surface_salinity), interpolate = FALSE) +
geom_polygon(data = w, aes(x = long, y = lat, group = group), fill = "grey80") +
theme_bw() + scale_fill_gradientn(colours = my.col, na.value = NA, limits = c(34, 36), name = "salinity") +
ylab("latitude") + xlab("longitude") +
coord_fixed(1.3, xlim = xlim, ylim = ylim) +
ggtitle(paste("salinity", NAtlSSS$data$time[1]))
myplot
The French agency IFREMER also has an ERDDAP server. Here salinity data at 75 meters from “Global Ocean, Coriolis Observation Re-Analysis CORA4.1” model off the west coast of the United States is extracted and plotted.
require("rerddap")
urlBase <- "http://www.ifremer.fr/erddap/"
parameter <- "PSAL"
ifrTimes <- c("2013-05-15", "2013-05-15")
ifrLats <- c(30., 50.)
ifrLons <- c(-140., -110.)
ifrDepth <- c(75., 75.)
dataInfo <- rerddap::info("ifremer_tds0_6080_109e_ed80", url = urlBase)
ifrPSAL <- griddap(dataInfo, longitude = ifrLons, latitude = ifrLats, time = ifrTimes, depth = ifrDepth, fields = parameter, url = urlBase)
str(ifrPSAL$data)
#> 'data.frame': 3294 obs. of 4 variables:
#> $ time: chr "2013-05-15T00:00:00Z" "2013-05-15T00:00:00Z" "2013-05-15T00:00:00Z" "2013-05-15T00:00:00Z" ...
#> $ lat : num 30 30 30 30 30 ...
#> $ lon : num -140 -140 -139 -138 -138 ...
#> $ PSAL: num 34.9 34.9 34.9 34.9 34.9 ...
The ggplot2 function geom_raster() is not designed for unevenly spaced coordinates, as are the latitudes from this model. The function interp() from the package akima is used to interpolate the data which are then plotted.
## ggplot2 has trouble with unequal y's
require("akima")
require("dplyr")
require("ggplot2")
require("mapdata")
xlim <- c(-140, -110)
ylim <- c(30, 51)
## ggplot2 has trouble with unequal y's
my.col <- colors$salinity
tempData1 <- ifrPSAL$data$PSAL
tempData <- array(tempData1 , 61 * 54)
tempFrame <- data.frame(x = ifrPSAL$data$lon, y = ifrPSAL$data$lat)
tempFrame$temp <- tempData
tempFrame1 <- dplyr::filter(tempFrame, !is.nan(temp))
myinterp <- akima::interp(tempFrame1$x, tempFrame1$y, tempFrame1$temp, xo = seq(min(tempFrame1$x), max(tempFrame1$x), length = 61), yo = seq(min(tempFrame1$y), max(tempFrame1$y), length = 54))
myinterp1 <- expand.grid(x = myinterp$x, y = myinterp$y)
myinterp1$temp <- array(myinterp$z, 61 * 54)
w <- map_data("worldHires", ylim = ylim, xlim = xlim)
myplot <- ggplot() +
geom_raster(data = myinterp1, aes(x = x, y = y, fill = temp), interpolate = FALSE) +
geom_polygon(data = w, aes(x = long, y = lat, group = group), fill = "grey80") +
theme_bw() + scale_fill_gradientn(colours = my.col, na.value = NA, limits = c(32, 35), name = "salinity") +
ylab("latitude") + xlab("longitude") +
coord_fixed(1.3, xlim = xlim, ylim = ylim) + ggtitle(paste("salinity at 75 meters",ifrPSAL$data$time[1] ))
myplot
CalCOFI (California Cooperative Oceanic Fisheries Investigations - http://www.calcofi.org) is a multi-agency partnership formed in 1949 to investigate the collapse of the sardine population off California. The organization's members are from NOAA Fisheries Service, Scripps Institution of Oceanography, and California Department of Fish and Wildlife. The scope of this research has evolved into the study of marine ecosystems off California and the management of its fisheries resources. The nearly complete CalCOFI data, both physical and biological, are available through ERDDAP.
The following example is a modification of a script developed by Dr. Andrew Leising of the Southwest Fisheries Science Center. The original script has been used to automate the generation of several yearly reports about the California Current Ecosystem. The script gets chlorophyll data and a measure of primary productivity from the hydrocasts,and then calculates a seasoanlly adjusted chlorophyll anomaly as well as a seasonally adjusted primary productivity anomaly. The first step is to get the information about the particular dataset:
require("rerddap")
hydroInfo <- info('siocalcofiHydroCasts')
and then get the desired data from 1984 through 2014:
require("rerddap")
calcofi.df <- tabledap(hydroInfo, fields = c('cst_cnt', 'date', 'year', 'month', 'julian_date', 'julian_day', 'rpt_line', 'rpt_sta', 'cruz_num', 'intchl', 'intc14', 'time'), 'time>=1984-01-01T00:00:00Z', 'time<=2014-04-17T05:35:00Z')
str(calcofi.df)
#> Classes 'tabledap' and 'data.frame': 11072 obs. of 12 variables:
#> $ cst_cnt : int 22522 22523 22524 22525 22526 22527 22528 22529 22530 22531 ...
#> $ date : chr "01/04/1984" "01/05/1984" "01/05/1984" "01/05/1984" ...
#> $ year : int 1984 1984 1984 1984 1984 1984 1984 1984 1984 1984 ...
#> $ month : int 1 1 1 1 1 1 1 1 1 1 ...
#> $ julian_date: int 30685 30686 30686 30686 30686 30686 30687 30687 30687 30687 ...
#> $ julian_day : int 4 5 5 5 5 5 6 6 6 6 ...
#> $ rpt_line : num 93.3 90 90 90 90 90 90 90 90 90 ...
#> $ rpt_sta : num 29 35 30 28 32 37 53 53 53 53 ...
#> $ cruz_num : chr "8401" "8401" "8401" "8401" ...
#> $ intchl : num NaN 30.3 27.9 29.9 39.3 36.7 30.3 30.6 21.3 31.1 ...
#> $ intc14 : chr "NaN" "NaN" "NaN" "NaN" ...
#> $ time : chr "1984-01-04T22:08:00Z" "1984-01-05T03:20:00Z" "1984-01-05T09:03:00Z" "1984-01-05T12:26:00Z" ...
#> - attr(*, "datasetid")= chr "siocalcofiHydroCasts"
#> - attr(*, "path")= chr "/Users/sacmac/Library/Caches/R/rerddap/a7a35af414deaac89811bf13fc934978.csv"
#> - attr(*, "url")= chr "https://upwell.pfeg.noaa.gov/erddap/tabledap/siocalcofiHydroCasts.csv?cst_cnt,date,year,month,julian_date,julia"| __truncated__
Both “intchl” and “intC14” are returned as character strings, and are easier to work with as numbers:
calcofi.df$cruz_num <- as.numeric(calcofi.df$cruz_num)
#> Warning: NAs introduced by coercion
calcofi.df$intc14 <- as.numeric(calcofi.df$intc14)
calcofi.df$time <- as.Date(calcofi.df$time, origin = '1970-01-01', tz = "GMT")
At this point the requested data are in the R workspace - the rest of the code performs the calculations to derive the seasonally adjusted values and plot them.
require("dplyr")
# calculate cruise means
by_cruznum <- group_by(calcofi.df, cruz_num)
tempData <- select(by_cruznum, year, month, cruz_num, intchl, intc14)
CruiseMeans <- summarize(by_cruznum, cruisechl = mean(intchl, na.rm = TRUE), cruisepp = mean(intc14, na.rm = TRUE), year = median(year, na.rm = TRUE), month = median(month, na.rm = TRUE))
tempTimes <- paste0(CruiseMeans$year,'-',CruiseMeans$month,'-1')
cruisetimes <- as.Date(tempTimes, origin = '1970-01-01', tz = "GMT")
CruiseMeans$cruisetimes <- cruisetimes
# calculate monthly "climatologies"
byMonth <- group_by(CruiseMeans, month)
climate <- summarize(byMonth, ppClimate = mean(cruisepp, na.rm = TRUE), chlaClimate = mean(cruisechl, na.rm = TRUE))
# calculate anomalies
CruiseMeans$chlanom <- CruiseMeans$cruisechl - climate$chlaClimate[CruiseMeans$month]
CruiseMeans$ppanom <- CruiseMeans$cruisepp - climate$ppClimate[CruiseMeans$month]
# calculate mean yearly anomaly
byYear <- select(CruiseMeans, year)
tempData <- select(CruiseMeans, year, chlanom, ppanom )
byYear <- group_by(tempData, year)
yearlyAnom <- summarize(byYear, ppYrAnom = mean(ppanom, na.rm = TRUE), chlYrAnom = mean(chlanom, na.rm = TRUE))
yearlyAnom$year <- ISOdate(yearlyAnom$year, 01, 01, hour = 0)
ggplot(yearlyAnom, aes(year, chlYrAnom)) + geom_line() +
theme_bw() + ggtitle('yearly chla anom')
ggplot(yearlyAnom, aes(year, ppYrAnom)) + geom_line() +
theme_bw() + ggtitle('yearly pp anom')
The CPS (Coastal Pelagic Species) Trawl Life History Length Frequency Data contains the length distribution of a subset of individuals from a species (mainly non-target) caught during SWFSC-FRD fishery independent trawl surveys of coastal pelagic species. Measured lengths for indicated length type (fork, standard, total, or mantle) were grouped in 10 mm bins (identified by the midpoint of the length class) and counts are recorded by sex.
The number and location of sardines (Sardinops sagax) in the tows in March 2010 and 2011 are extracted, and compared with monthly SST from satellites. First, query the ERDDAP server to see if CPS Trawl data are available through the ERDDAP server, and if so, obtain the datasetID for the dataset.
require("rerddap")
CPSquery <- ed_search(query = 'CPS Trawl')
CPSquery$alldata[[1]]$summary
#> [1] "Weight in kilograms for all species (identified to lowest taxonomic criteria) caught during SWFSC-FRD fishery independent surveys (including DEPM, ATM, SaKe) of coastal pelagic species using mid-water trawls (with most tows performed near the surface) at position and times listed. Additional information for a subset of individuals from some species can be found in either CPS Trawl Life History Length Frequency or the CPS Trawl Life History Specimen datasets.\n\ncdm_data_type = Point\nVARIABLES:\ncruise\nship\nhaul (Haul Number)\ncollection\nlatitude (Start Latitude, degrees_north)\nlongitude (Start Longitude, degrees_east)\nstop_latitude\nstop_longitude\ntime (Equilibrium Time, seconds since 1970-01-01T00:00:00Z)\nhaulback_time (Haul Back Time, seconds since 1970-01-01T00:00:00Z)\nsurface_temp (Surface Temperature, degree C)\nsurface_temp_method (Surface Temperature Method)\nship_spd_through_water (Ship Speed Through Water, knot)\nitis_tsn (ItisTSN)\nscientific_name\nsubsample_count\nsubsample_weight (kg)\nremaining_weight (kg)\n"
CPSquery$alldata[[1]]$tabledap
#> [1] "https://upwell.pfeg.noaa.gov/erddap/tabledap/FRDCPSTrawlLHHaulCatch"
CPSquery$alldata[[1]]$dataset_id
#> [1] "FRDCPSTrawlLHHaulCatch"
Then get the information for the CPS dataset:
require("rerddap")
(CPSinfo <- info('FRDCPSTrawlLHHaulCatch'))
#> <ERDDAP info> FRDCPSTrawlLHHaulCatch
#> Variables:
#> collection:
#> Range: 2003, 3623
#> cruise:
#> Range: 200307, 201604
#> haul:
#> Range: 1, 160
#> haulback_time:
#> Range: -6.5759508E8, 1.3977129E9
#> Units: seconds since 1970-01-01T00:00:00Z
#> itis_tsn:
#> latitude:
#> Range: 30.7001, 54.3997
#> Units: degrees_north
#> longitude:
#> Range: -134.0793, -117.3796
#> Units: degrees_east
#> remaining_weight:
#> Units: kg
#> scientific_name:
#> ship:
#> ship_spd_through_water:
#> Units: knot
#> stop_latitude:
#> Range: 30.6663, 51.0923
#> stop_longitude:
#> Range: -132.184, -117.4116
#> subsample_count:
#> subsample_weight:
#> Units: kg
#> surface_temp:
#> Units: degree C
#> surface_temp_method:
#> time:
#> Range: 1.05771978E9, 1.4613093E9
#> Units: seconds since 1970-01-01T00:00:00Z
extract the desired CPS data:
require("dplyr")
require("rerddap")
sardines <- tabledap(CPSinfo, fields = c('latitude', 'longitude', 'time', 'scientific_name', 'subsample_count'), 'time>=2010-01-01', 'time<=2012-01-01', 'scientific_name="Sardinops sagax"' )
sardines$time <- as.Date(sardines$time, origin = '1970-01-01', tz = "GMT")
sardines$latitude <- as.numeric(sardines$latitude)
sardines$longitude <- as.numeric(sardines$longitude)
sardine2010 <- filter(sardines, time < as.Date('2010-12-01'))
and plot the data versus monthly SST values:
# get the dataset info
sstInfo <- info('erdMWsstdmday')
# get 201004 monthly sst
sst201004 <- griddap('erdMWsstdmday', latitude = c(22., 51.), longitude = c(220., 255), time = c('2010-04-16','2010-04-16'), fields = 'sst')
# get 201104 monthly sst
sst201104 <- griddap('erdMWsstdmday', latitude = c(22., 51.), longitude = c(220., 255), time = c('2011-04-16','2011-04-16'), fields = 'sst')
# get polygons of coast for this area
w <- map_data("worldHires", ylim = c(22., 51.), xlim = c(220 - 360, 250 - 360))
# plot 201004 sst on the map
sardine2010 <- filter(sardines, time < as.Date('2010-12-01', origin = '1970-01-01', tz = "GMT"))
sardine2011 <- filter(sardines, time > as.Date('2010-12-01', origin = '1970-01-01', tz = "GMT"))
mycolor <- colors$temperature
p1 <- ggplot() +
geom_polygon(data = w, aes(x = long, y = lat, group = group), fill = "grey80") +
geom_raster(data = sst201004$data, aes(x = lon - 360, y = lat, fill = sst), interpolate = FALSE) +
scale_fill_gradientn(colours = mycolor, na.value = NA, limits = c(5,30)) +
theme_bw() + ylab("latitude") + xlab("longitude") +
coord_fixed(1.3, xlim = c(220 - 360, 250 - 360), ylim = c(22., 51.))
# plot 201104 sst on the map
p2 <- ggplot() +
geom_polygon(data = w, aes(x = long, y = lat, group = group), fill = "grey80") +
geom_raster(data = sst201104$data, aes(x = lon - 360, y = lat, fill = sst), interpolate = FALSE) +
geom_point(data = sardine2011, aes(x = longitude, y = latitude, colour = subsample_count)) +
scale_fill_gradientn(colours = mycolor, na.value = NA, limits = c(5,30)) +
theme_bw() + ylab("latitude") + xlab("longitude") +
coord_fixed(1.3, xlim = c(220 - 360, 250 - 360), ylim = c(22., 51.))
p1 + geom_point(data = sardine2010, aes(x = longitude, y = latitude, colour = subsample_count)) + scale_colour_gradient(space = "Lab", na.value = NA, limits = c(0,80))
p2 + geom_point(data = sardine2011, aes(x = longitude, y = latitude, colour = subsample_count)) + scale_colour_gradient(space = "Lab", na.value = NA, limits = c(0,80))
Also of interest is the distribution of sardines through the years:
sardinops <- tabledap(CPSinfo, fields = c('longitude', 'latitude', 'time'), 'scientific_name="Sardinops sagax"')
sardinops$time <- as.Date(sardinops$time, origin = '1970-01-01', tz = "GMT")
sardinops$year <- as.factor(format(sardinops$time, '%Y'))
sardinops$latitude <- as.numeric(sardinops$latitude)
sardinops$longitude <- as.numeric(sardinops$longitude)
xlim <- c(-135, -110)
ylim <- c(30, 51)
coast <- map_data("worldHires", ylim = ylim, xlim = xlim)
ggplot() +
geom_point(data = sardinops, aes(x = longitude, y = latitude, colour = year)) +
geom_polygon(data = coast, aes(x = long, y = lat, group = group), fill = "grey80") +
theme_bw() + ylab("latitude") + xlab("longitude") +
coord_fixed(1.3, xlim = xlim, ylim = ylim) +
ggtitle("Location of sardines by year in EPM Trawls")
NOAA's National Data Buoy Center (NDBC) collects world-wide data from buoys in the ocean. ERDDAP can be searched for the location of all buoys in a bounding box with latitudes(37N, 47N) and longitudes (124W, 121W) and the results plotted:
# get location and station ID of NDBC buoys in a region
BuoysInfo <- info('cwwcNDBCMet')
locationBuoys <- tabledap(BuoysInfo, distinct = TRUE, fields = c("station", "longitude", "latitude"), "longitude>=-124", "longitude<=-121", "latitude>=37", "latitude<=47")
locationBuoys$latitude <- as.numeric(locationBuoys$latitude)
locationBuoys$longitude <- as.numeric(locationBuoys$longitude)
xlim <- c(-130, -110)
ylim <- c(35, 50)
coast <- map_data("worldHires", ylim = ylim, xlim = xlim)
ggplot() +
geom_point(data = locationBuoys, aes(x = longitude , y = latitude, colour = factor(station) )) +
geom_polygon(data = coast, aes(x = long, y = lat, group = group), fill = "grey80") +
theme_bw() + ylab("latitude") + xlab("longitude") +
coord_fixed(1.3, xlim = xlim, ylim = ylim) +
ggtitle("Location of buoys in given region")
Looking at wind speed for 2012 for station “46012”
buoyData <- tabledap(BuoysInfo, fields = c("time", "wspd"), 'station="46012"', 'time>=2012-01-01', 'time<=2013-01-01')
buoyData$wspd <- as.numeric(buoyData$wspd)
buoyData$time <- as.Date(buoyData$time, origin = '1970-01-01', tz = "GMT")
ggplot(buoyData, aes(time, wspd)) +
geom_line() +
theme_bw() +
ylab("wind speed") +
ggtitle("Wind Speed in 2012 from buoy 46012 ")
The mission of the IOOS Glider DAC is to provide glider operators with a simple process for submitting glider data sets to a centralized location, enabling the data to be visualized, analyzed, widely distributed via existing web services and the Global Telecommunications System (GTS) and archived at the National Centers for Environmental Information (NCEI).
The IOOS Glider Dac is accessible through rerddap (http://data.ioos.us/gliders/erddap/). Extracting and plotting salinity from part of the path of one glider deployed by the Scripps Institution of Oceanography:
urlBase <- "https://data.ioos.us/gliders/erddap/"
gliderInfo <- info("sp064-20161214T1913", url = urlBase)
glider <- tabledap(gliderInfo, fields = c("longitude", "latitude", "depth", "salinity"), 'time>=2016-12-14', 'time<=2016-12-23', url = urlBase)
glider$longitude <- as.numeric(glider$longitude)
glider$latitude <- as.numeric(glider$latitude)
glider$depth <- as.numeric(glider$depth)
require("plot3D")
scatter3D(x = glider$longitude , y = glider$latitude , z = -glider$depth, colvar = glider$salinity, col = colors$salinity, phi = 40, theta = 25, bty = "g", type = "p",
ticktype = "detailed", pch = 10, clim = c(33.2,34.31), clab = 'Salinity',
xlab = "longitude", ylab = "latitude", zlab = "depth",
cex = c(0.5, 1, 1.5))