Edited by Jemma Stachelek: 04 August, 2021

Introduction

This package contains functions to assist in the processing and exploration of data from monitoring programs for aquatic ecosystems. The name wq stands for water quality. Although our own interest is in aquatic ecology, almost all of the functions should be useful for time series analysis regardless of the subject matter. The package is intended for programs that sample approximately monthly at discrete stations, a feature of many legacy data sets.

The functions are summarized in the diagram above, which illustrates a typical sequence of analysis that could be facilitated by the package when the data are in a data frame or time series. The functions associated with each step of the sequence are listed below their corresponding step. First, we might want to derive additional variables of interest. A few functions are provided here for variables common to water monitoring data. Next, we generate time series from the data in a two-stage process: the data.frame is first converted into a standardized form (with wqData) and then another function (tsMake) is applied to this new data object to generate the series. This two-stage process is not necessary, and – as implied in the diagram – you can skip it by using time series that already exist or that you construct in another way. But it has advantages when you’re constructing many different kinds of series from a data set, especially one that is unbalanced with respect to place and time. There are also a few special methods available to summarize this new data object. Next, we may need to reshape the time series in various ways for further analysis, perhaps also imputing missing values. Finally, we analyze the data to extract patterns using special plots, trend tests, and other approaches.

We illustrate some of the steps in the diagram using the accompanying data set sfbay.

library(wql)

Preparing data from an external file

Our starting point is a comma-delimited file downloaded on 2009-11-17 from the U.S. Geological Survey’s water quality data set for San Francisco Bay. The downloaded file, sfbay.csv, starts with a row of variable names followed by a row of units, so the first two lines are skipped during import and simpler variable names are substituted for the originals. Also, only a subset of stations and years is used in order to keep sfbay.csv small:

sfbay <- read.csv("sfbay.csv", header = FALSE, as.is = TRUE,
skip = 2)
names(sfbay) <- c('date', 'time', 'stn', 'depth', 'chl', 'dox',
'spm', 'ext', 'sal', 'temp', 'nox', 'nhx')
sfbay <- subset(sfbay, stn %in% c(21, 24, 27, 30, 32, 36) &
substring(date, 7, 10) %in% 1985:2004)

The resulting data frame sfbay is provided as part of the package, and its contents are explained in the accompanying help file.

head(sfbay)
##            date time stn depth chl dox spm ext   sal temp nox nhx
## 6835  1/23/1985 1120  21     1 5.6  NA  17 1.6 28.15   NA  NA  NA
## 6836  1/23/1985 1120  21     2 3.4  NA  17 1.6 28.58   NA  NA  NA
## 6837  1/23/1985 1120  21     6 3.1  NA  18 1.6 28.91   NA  NA  NA
## 6838  1/23/1985 1120  21    12 3.4  NA  21 1.9 29.36   NA  NA  NA
## 6841  1/23/1985 1222  24     1 6.2  NA  17 1.6 27.42   NA  NA  NA
## 6842  1/23/1985 1222  24     2 5.6  NA  18 1.6 27.42   NA  NA  NA

The next step is to add any necessary derived variables to the data frame. An initial data set will sometimes contain conductivity rather than salinity data, and we might want to use ec2pss to derive the latter. That’s not the case here, but let’s assume that we want dissolved oxygen as percent saturation rather than in concentration units. Using oxySol and the convention of expressing percent saturation with respect to surface pressure:

x <- sample(seq_len(nrow(sfbay)), 10)
sfbay[x, "dox"]
##  [1]  8.3  9.1   NA  9.2  6.7 11.8  7.1  9.5  8.1  7.4
sfbay1 <- transform(sfbay,
dox = round(100 * dox/oxySol(sal, temp), 1))
sfbay1[x, "dox"]
##  [1] 117.9 104.6    NA 103.4  80.7 130.0  99.5 120.5 110.2 106.8

The WqData class

We define a standardized format for water quality data by creating a formal (S4) class, the WqData class, that enforces the standards, and an accompanying generating function wqData (note lower-case w). This generating function constructs a WqData object from a data frame. The WqData object is just a restricted version of a data.frame that requires specific column names and classes.

We decided to accommodate two types of sampling time, namely, the date either with or without the time of day. The former are converted to the POSIXct class and the latter to the Date class. A special class DateTime is created, which is the union of these two time classes. Classes that combine date and time of day require an additional level of care with respect to time zone (Grothendieck and Petzoldt 2004).

Surface location is specified by a site code, as the intention is to handle discrete monitoring programs as opposed to continuous transects. Latitude-longitude and distances from a fixed point are implicit in the site code and can be recorded in a separate table (see sfbayVars). The depth is specified separately as a number. Other information that may not be depth-specific, such as the mean vertical extinction coefficient in the near-surface layer, can be coded by a negative depth number. The last two fields in the data portion of a WqData object are the variable code and the value. The variables are given as character strings and the values as numbers. As in the case of the sampling site, additional information related to the variable code can be maintained in a separate table (see sfbayVars).

Like all S4 classes, WqData has a generating function called new automatically created along with the class. This function, however, requires that its data frame argument already have a fairly restricted form of structure. In order to decrease the manipulation required of the imported data, a separate, less restrictive generating function called wqData is available. This function is more forgiving of field names and classes and does a few other cleanup tasks with the data before calling new. Perhaps most useful, it converts data from a wide format with one field per variable into the long format used by the WqData class. For example, sfbay can be converted to a WqData object with a single command:

sfb <- wqData(sfbay, c(1, 3:4), 5:12, site.order = TRUE,
type = "wide", time.format = "%m/%d/%Y")
head(sfb)
##         time site depth variable value
## 1 1985-01-23  s21     1      chl   5.6
## 2 1985-01-23  s21     2      chl   3.4
## 3 1985-01-23  s21     6      chl   3.1
## 4 1985-01-23  s21    12      chl   3.4
## 5 1985-01-23  s24     1      chl   6.2
## 6 1985-01-23  s24     2      chl   5.6

There is a summary method for this class that tabulates the number of observations by site and variable, as well as the mean and quartiles for individual variables:

summary(sfb)
##       time             site           depth           variable
##  Min.   :1985-01-23   s21:23933   Min.   : 0.500   sal    :23172
##  1st Qu.:1993-04-15   s24:15348   1st Qu.: 3.000   temp   :23156
##  Median :1996-06-12   s27:18122   Median : 6.000   chl    :22063
##  Mean   :1996-07-24   s30:20445   Mean   : 6.836   spm    :16463
##  3rd Qu.:2000-07-13   s32:16905   3rd Qu.:10.000   dox    :15505
##  Max.   :2004-12-14   s36: 7973   Max.   :20.000   nox    :  807
##                                                    (Other): 1560
##      value
##  Min.   :  0.01
##  1st Qu.:  7.50
##  Median : 13.90
##  Mean   : 17.78
##  3rd Qu.: 23.00
##  Max.   :983.00
## 

Plotting a WqData object produces a plot for each variable specified, each plot containing a boxplot of the values for each site. If no variables are specified, then the first 10 will be plotted.

plot(sfb, vars = c('dox', 'temp'), num.col = 2)

Apart from summary and plot, one can subset a WqData object with the [ operator. All other existing methods for data frames will produce an object of class data.frame rather than one of class WqData.

Generating time series

Historical water quality data are often suitable for analyzing as monthly time series, which permits the use of many existing time series functions. tsMake is a function for WqData objects that creates monthly time series for all variables at a single site or for a single variable at all sites, when the option type = "ts.mon". If the quantile probability qprob = NULL, all replicates are first averaged and then the mean is found for the depth layers of interest. Otherwise the respective quantile will be used both to aggregate depths for each day and to aggregate days for each month. If no layers are specified, all depths will be used. If layer = "max.depths", the time series will be values of the deepest sample for each time, site and variable. The layer argument allows for flexibility in specifying depths, including a list of layers and negative depths used as codes for, say, near botton or entire water column.

y <- tsMake(sfb, focus = "chl", layer = c(0, 5))
y[1:4, ]
##           s21       s24       s27       s30      s32    s36
## [1,] 4.500000  5.900000       NaN  1.300000  2.65000  6.250
## [2,]      NaN       NaN       NaN  1.600000  5.55000    NaN
## [3,] 5.858333 10.654167 12.291667 12.787500 11.86667 40.100
## [4,] 4.638889  5.916667  8.133333  8.388889 11.45556  4.525
tsp(y)
## [1] 1985.000 2004.917   12.000

The function plotTs is convenient for a quick look at the series. Lines join only adjacent data; otherwise, data are isolated dots.

plotTs(y[, 1:4], dot.size = 1.3, ylab = "Chlorophyll in San Francisco Bay",
strip.labels = paste("Station", 21:24), ncol = 1, scales = "free_y")

If the option type = "zoo", then tsMake produces an object of class zoo containing values by date of observation, rather than a monthly time series.

head(tsMake(sfb, focus = "chl", layer = c(0, 5), type = 'zoo'))
##               s21      s24       s27       s30       s32   s36
## 1985-01-23  4.500  5.90000       NaN  1.300000  2.650000  6.25
## 1985-02-27    NaN      NaN       NaN  1.600000  5.550000   NaN
## 1985-03-07  4.800  3.90000  5.200000  5.033333  5.166667   NaN
## 1985-03-13  2.600  9.35000  7.066667  5.066667  4.500000   NaN
## 1985-03-21    NaN  7.70000 13.300000 10.200000  4.700000   NaN
## 1985-03-29 10.175 21.66667 23.600000 30.850000 33.100000 40.10

Reshaping

There are several functions for further reshaping of time series, preparing them for use in specific analyses. ts2df converts a monthly time series vector to a year $$\times$$ month data frame. Leading and trailing empty rows are removed, additional rows with missing data are optionally removed, and the data frame can be reconfigured to represent a local water year:

chl27 <- sfbayChla[, 's27']
tsp(chl27)
## [1] 1978.000 2009.583   12.000
chl27 <- round(chl27, 1)
head(ts2df(chl27))
##      Jan Feb Mar  Apr  May Jun Jul Aug Sep Oct Nov Dec
## 1978 1.1 2.8 5.6  2.7  3.4 1.9 1.6  NA 1.7 2.1 2.2 1.7
## 1979 1.9 1.8 2.4  3.8  2.3 4.8 1.6 3.9 2.1 1.2 1.1  NA
## 1980 1.3 1.9 2.1 10.2  3.4 2.1 1.1 1.4 1.6 1.4 1.7 1.3
## 1981  NA 1.7 2.0  9.1   NA  NA  NA  NA  NA  NA  NA  NA
## 1982 2.8 4.5 6.5  9.3  8.2 3.4 1.4  NA 2.1 1.8 1.7 0.9
## 1983  NA 1.4 7.0 16.4 16.6 5.4 1.4 1.7 2.0 1.5 1.5 1.4

Another example of its use is shown in Empirical Orthogonal Functions below. A similar reshaping function is mts2ts, which converts a matrix time series to a vector time series for various analyses. It first aggregates the multivariate matrix time series by year, then converts it to a vector time series in which the seasons correspond to these annnualized values for the original variables. The seas parameter enables focusing the subsequent analysis on seasons of special interest, or to ignore seasons where there are too many missing data. The function can be used in conjunction with seaKen to conduct a Regional Kendall trend analysis, as described in Trends below:

y <- window(sfbayChla, start = 2005,
end = c(2009, 12))  # 5 years, 16 sites
round(mts2ts(y, seas = 2:4), 1)  # focus on Feb-Apr spring bloom
## Time Series:
## Start = c(2005, 1)
## End = c(2009, 16)
## Frequency = 16
##  [1]  5.8  4.7  6.0  4.6  5.5  5.6  5.9  6.3  6.5  7.6  7.5  7.8  8.5  8.8  8.0
## [16]  8.4 18.1  9.8 12.0 12.5 12.8 16.2 18.1 20.6 22.5 26.9 26.4 29.9 31.1 33.7
## [31] 32.1 33.2  7.9  6.6  7.8  7.9  7.9  9.2 10.1 10.2 10.5 11.9 12.0 12.1 13.2
## [46] 13.0 13.0 15.1 15.1 10.9 12.5 13.8 14.1 14.8 15.9 17.0 16.7 20.2 21.0 21.8
## [61] 22.3 23.5 23.4 24.0  4.7  4.5  4.6  4.7  4.7  4.4  4.6  5.2  5.4  6.0  6.8
## [76]  7.7  8.5  9.1  8.1  8.1

Some functions (e.g., eof) do not permit NAs and some kind of data imputation or omission will usually be required. The function interpTs is handy for interpolating small data gaps. It can also be used for filling in larger gaps with long-term or seasonal means or medians. Here, we use it to bridge gaps of up to three months.

chl27 <- sfbayChla[, "s27"]
chl27a <- interpTs(chl27, gap = 3)

The interpolated series is then plotted in red and the original series overplotted below.

plot(chl27a, col = "red", lwd = .5, xlab = "")
lines(chl27, col = "blue", lwd = 1.5)

Analyzing

Empirical Orthogonal Functions

Empirical Orthogonal Function (EOF) analysis is a term used primarily in the earth sciences for principal component analysis applied to simultaneous time series at different spatial locations. Hannachi, Jolliffe, and Stephenson (2007) provide a comprehensive summary. The function eof in this package, based on prcomp and varimax in the stats package, optionally scales the time series and applies a rotation to the EOFs.

eof requires an estimate of the number of EOFs to retain for rotation. eofNum provides a guide to this number by plotting the eigenvalues and their confidence intervals in a scree plot. Here, we apply eofNum to annualized San Francisco Bay chlorophyll data and retain the stations with no missing data, namely, the first 12 stations.

chla1 <- aggregate(sfbayChla, 1, mean, na.rm = TRUE)
chla1 <- chla1[, 1:12]
eofNum(chla1)

These stations have similar coefficients for the first EOF and appear to act as one with respect to chlorophyll variability on the annual scale. It suggests that further exploration of the interannual variability of these stations can be simplified by using a single time series, namely, the first EOF.

e1 <- eof(chla1, n = 1)
e1
## $REOF ## EOF1 ## s21 0.9152475 ## s22 0.8817009 ## s23 0.9426172 ## s24 0.9316475 ## s25 0.9240967 ## s26 0.8237361 ## s27 0.9556114 ## s28 0.8561061 ## s29 0.9329812 ## s30 0.8988690 ## s31 0.7818497 ## s32 0.7499585 ## ##$amplitude
##             EOF1
## 1978 -1.21246216
## 1979 -1.08159929
## 1980 -1.19668945
## 1981 -0.95979724
## 1982 -0.88995894
## 1983  0.01869466
## 1984 -0.65889638
## 1985 -0.61722327
## 1986 -0.09960840
## 1987 -1.36420948
## 1988 -0.77820092
## 1989 -0.35212181
## 1990 -0.29661253
## 1991 -0.99695028
## 1992 -0.88599877
## 1993 -0.21069317
## 1994 -0.70986756
## 1995  0.75970351
## 1996 -0.84507273
## 1997  0.28070836
## 1998  1.09741867
## 1999  0.88113847
## 2000  1.05562316
## 2001  0.90843729
## 2002  0.50056531
## 2003  1.76822671
## 2004  0.45840044
## 2005  0.19162750
## 2006  2.04777652
## 2007  1.28143762
## 2008  1.90620420
##
## $eigen.pct ## [1] 78.4 8.1 7.0 3.5 1.4 0.5 0.3 0.3 0.2 0.2 0.1 0.1 ## ##$variance
##  [1]  78.4  86.5  93.5  97.0  98.4  98.9  99.2  99.5  99.7  99.8  99.9 100.0

The function eofPlot produces a graph of either the EOFs or their accompanying time series. In this case, with n = 1, there is only one plot for each such graph.

eofPlot(e1, type = "amp")

Principal component analysis can also be useful in studying the way different seasonal modes of variability contribute to overall year-to-year variability of a single time series . The basic approach is to consider each month as determining a separate annual time series and then to calculate the eigenvalues for the resulting $$12 \times n$$ years time series matrix. The function ts2df is useful for expressing a monthly time series in the form needed by eof. For example, the following code converts the monthly chlorophyll time series for Station 27 in San Francisco Bay to the appropriate data frame with October, the first month of the local water year, in the first column, and years with missing data omitted:

chl27b <- interpTs(sfbayChla[, "s27"], gap = 3)
chl27b <- ts2df(chl27b, mon1 = 10, addYr = TRUE, omit = TRUE)
head(round(chl27b, 1))
##      Oct Nov Dec Jan Feb Mar  Apr  May Jun Jul Aug Sep
## 1979 2.1 2.2 1.7 1.9 1.8 2.4  3.8  2.3 4.8 1.6 3.9 2.1
## 1980 1.2 1.1 1.2 1.3 1.9 2.1 10.2  3.4 2.1 1.1 1.4 1.6
## 1983 1.8 1.7 0.9 1.2 1.4 7.0 16.4 16.6 5.4 1.4 1.7 2.0
## 1984 1.5 1.5 1.4 1.9 2.8 3.0  9.8  3.5 1.2 1.7 2.3 2.9
## 1986 1.5 1.1 1.2 1.2 1.2 4.0 25.5  4.0 1.5 1.5 1.4 1.4
## 1987 1.3 1.2 1.1 1.4 1.4 5.1  5.9  5.1 2.9 1.7 2.0 2.0

The following example plots the EOFs from an analysis of this month $$\times$$ year data frame for Station 27 chlorophyll after scaling the data. eofNum (not shown) suggested retaining up to two EOFs. The resulting rotated EOFs imply two separate modes of variability for further exploration, the first operating during May-Sep and the other during Nov-Jan:

e2 <- eof(chl27b, n = 2, scale. = TRUE)
eofPlot(e2, type = "coef")

Time series decomposition

An analysis of chlorophyll-a time series from many coastal and estuarine sites around the world demonstrates that the standard deviation of chlorophyll is approximately proportional to the mean, both among and within sites, as well as at different time scales (Cloern and Jassby 2010). One consequence is that these monthly time series are well described by a multiplicative seasonal model: $$c_{ij} = C y_i m_j \epsilon_{ij}$$, where $$c_{ij}$$ is chlorophyll concentration in year $$i$$ and month $$j$$; $$C$$ is the long-term mean; $$y_i$$ is the annual effect; $$m_j$$ is the mean seasonal (in this case monthly) effect; and $$\epsilon_{ij}$$ is the residual series, which we sometimes refer to as the events component. The annual effect is simply the annual mean divided by the long-term mean: $$y_{i} = Y_{i}/C$$, where $$Y_{i} = (1/12) \sum_{j=1}^{12}c_{ij}$$. The mean monthly effect is given by $$m_{j}=(1/N) \sum_{i=1}^{N} M_{ij}/(C y_{i})$$, where $$M_{ij}$$ is the value for month $$j$$ in year $$i$$, and $$N$$ is the total number of years. The events component is then obtained by $$\epsilon_{ij}=c_{ij}/C y_{i} m_{j}$$. This simple approach is motivated partly by the observation that many important events for estuaries (e.g., persistent dry periods, species invasions) start or stop suddenly. Smoothing to extract the annualized term, which can disguise the timing of these events and make analysis of them unnecessarily difficult, is not used.

The decompTs listed here accomplishes this multiplicative decomposition (an option allows additive decomposition as an alternative). The median rather than the mean can be used in the operations described above, and the median is, in fact, the default for the function. Large, isolated events are common in environmental time series, especially from the ocean or ocean-influenced habitats such as certain types of estuary. The median leads to a more informative decomposition in these cases. decompTs requires input of a time series matrix in which the columns are monthly time series. It allows missing data, but it is up to the user to decide how many data are sufficient and if the pattern of missing data will lead to bias in the results. If so, it would be advisable to eliminate problem years beforehand by setting all month values to NA for those years. There are two cases of interest here: one in which the seasonal effect is held constant from year to year, and another in which it is allowed to vary by not distinguishing a separate events component. The choice is made by setting event = TRUE or event = FALSE, respectively, in the input. The output of this function is a matrix time series containing the original time series and its multiplicative model components, except for the long-term median or mean.

The average seasonal pattern may not resemble observed seasonality in a given year. Patterns that are highly variable from year to year will result in an average seasonal pattern of relatively low amplitude (i.e., low range of monthly values) compared to the amplitudes in individual years. An average seasonal pattern with high amplitude therefore indicates both high amplitude and a recurring pattern for individual years. The default time series plot again provides a quick illustration of the result.

chl27 <- sfbayChla[, "s27"]
d1 <- decompTs(chl27)
plot(d1, nc = 1, main = "Station 27 Chl-a decomposition")

The average seasonal pattern does not provide any information about potential secular trends in the pattern. A solution is to apply the decomposition to a moving time window. The window should be big enough to yield a meaningful average of interannual variability but short enough to allow a trend to manifest. This may be different for different systems, but a decadal window can be used as a starting point. A more convenient way to examine changing seasonality is with the dedicated function plotSeason. It divides the time period into intervals and plots a composite of the seasonal pattern in each interval. The intervals can be specifed by a single number – the number of equal-length intervals – or by a vector listing the breaks between intervals. The function also warns of months that may not be represented by enough data by colouring them red. plotSeason is an easy way to decide on the value for the event option in decompTs.

plotSeason(chl27, num.era = 3, same.plot = FALSE, ylab = 'Stn 27 Chl-a')

The same boxplots can also be combined in one plot, with boxplots for the same month grouped together.

plotSeason(chl27, num.era = 3, same.plot = TRUE, ylab = 'Stn 27 Chl-a')

plotSeason also has an option to plot all individual months separately as standardized anomalies for the entire record.

plotSeason(chl27, "by.month", ylab = 'Stn 27 Chl-a')

With all types of seasonal plots, it is often helpful to adjust the device aspect ratio and size manually to get the clearest information.

Phenological parameters

phenoPhase and phenoAmp act on monthly time series or dated observations (zoo objects) and produce measures of the phase and amplitude, respectively, for each year. phenoPhase finds the month containing the maximum value, the fulcrum or center of gravity, and the weighted mean month. phenoAmp finds the range, the range divided by mean, and the coefficient of variation. Both functions can be confined to only part of the year, for example, the months containing the spring phytoplankton bloom. This feature can also be used to avoid months with chronic missing-data problems.

Illustrating once again with chlorophyll observations from Station 27 in San Francisco Bay:

chl27 <- sfbayChla[, 's27']
p1 <- phenoPhase(chl27)
head(p1)
##   year max.time fulcrum mean.wt
## 1 1978       NA      NA      NA
## 2 1979       NA      NA      NA
## 3 1980        4    4.52    5.54
## 4 1981       NA      NA      NA
## 5 1982       NA      NA      NA
## 6 1983       NA      NA      NA
p2 <- phenoPhase(chl27, c(1, 6))
head(p2)
##   year max.time fulcrum mean.wt
## 1 1978        3    3.37    3.58
## 2 1979        6    3.94    4.01
## 3 1980        4    3.99    3.90
## 4 1981       NA      NA      NA
## 5 1982        4    3.86    3.75
## 6 1983       NA      NA      NA
p3 <- phenoAmp(chl27, c(1, 6))
head(p3)
##         range       var      mad     mean   median
## [1,] 4.450000  2.312417 1.111950 2.908333 2.750000
## [2,] 3.033333  1.445630 0.766010 2.822222 2.350000
## [3,] 8.900000 11.274519 0.728945 3.505556 2.100000
## [4,]       NA        NA       NA       NA       NA
## [5,] 6.509444  7.006464 3.572860 5.798750 5.515972
## [6,]       NA        NA       NA       NA       NA

Using the actual dated observations:

zchl <- tsMake(sfb, focus = "chl", layer = c(0, 5), type = 'zoo')
head(zchl)
##               s21      s24       s27       s30       s32   s36
## 1985-01-23  4.500  5.90000       NaN  1.300000  2.650000  6.25
## 1985-02-27    NaN      NaN       NaN  1.600000  5.550000   NaN
## 1985-03-07  4.800  3.90000  5.200000  5.033333  5.166667   NaN
## 1985-03-13  2.600  9.35000  7.066667  5.066667  4.500000   NaN
## 1985-03-21    NaN  7.70000 13.300000 10.200000  4.700000   NaN
## 1985-03-29 10.175 21.66667 23.600000 30.850000 33.100000 40.10
zchl27 <- zchl[, 3]
head(phenoPhase(zchl27))
##   year   max.time    fulcrum    mean.wt  n
## 1 1985 1985-03-29 1985-03-31 1985-04-19 17
## 2 1986 1986-04-29 1986-04-25 1986-04-27 21
## 3 1987 1987-04-16 1987-05-13 1987-05-18 20
## 4 1988 1988-04-14 1988-04-27 1988-06-09 16
## 5 1989 1989-03-01 1989-04-12 1989-04-12 25
## 6 1990 1990-04-12 1990-04-30 1990-04-21 13
head(phenoPhase(zchl27, c(1, 6), out = 'doy'))
##   year max.time fulcrum mean.wt  n
## 1 1985       88      85      94 11
## 2 1986      119     111     109 15
## 3 1987      106     107     107 12
## 4 1988      105      84      98  7
## 5 1989       60      86      87 18
## 6 1990      102     106      98 10
head(phenoPhase(zchl27, c(1, 6), out = 'julian'))
##   year max.time fulcrum mean.wt  n
## 1 1985     5566    5563    5572 11
## 2 1986     5962    5954    5952 15
## 3 1987     6314    6315    6315 12
## 4 1988     6678    6657    6671  7
## 5 1989     6999    7025    7026 18
## 6 1990     7406    7410    7402 10

Miscellaneous plotting functions

plotTsAnom plots (unstandardized) departures of vector or matrix time series from their long-term mean and can be a useful way of examining trends in annualized data.

chl <- aggregate(sfbayChla[, 1:6], 1, meanSub, 2:4, na.rm = TRUE)
plotTsAnom(chl, ylab = 'Chlorophyll-a',
strip.labels = paste('Station', substring(colnames(chl), 2, 3)))

plotTsTile plots a monthly time series as a month $$\times$$ year grid of tiles, with color representing magnitude. The data can be binned in either of two ways. The first is simply by deciles. The second, which is intended for log-anomaly data, is by four categories: Positive numbers higher or lower than the mean positive value, and negative numbers higher or lower than the mean negative value. In this version of plotTsTile, the anomalies are calculated with respect to the overall mean month.

chl27 <- sfbayChla[, "s27"]
plotTsTile(chl27)

This plot shows clearly the change in chlorophyll magnitude after 1999.

References

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Cloern, James E, and Alan D Jassby. 2010. “Patterns and Scales of Phytoplankton Variability in Estuarine-Coastal Ecosystems.” Estuaries and Coasts 33: 230–41.
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Pettitt, A. N. 1979. “A Non-Parametric Approach to the Change-Point Problem.” Journal of the Royal Statistical Society. Series C (Applied Statistics) 28 (2): 126–35.
Schertz, Terry L., Richard B. Alexander, and Dane J. Ohe. 1991. The computer program EStimate TREND (ESTREND), a system for the detection of trends in water-quality data.” Water-Resources Investigations Report 91-4040. U.S. Geological Survey.