Simon Noone , Conor Murphy and Csaba Horvath
Irish Climate Analysis and Research units (ICARUS), Maynooth
University, Maynooth , Ireland.
Introduction
These are exceptional times. While the fine weather has
served to make Covid-19 lockdown more bearable for many, the dry conditions
themselves have been exceptional, especially in the east and in the Dublin
region in particular. With 2 days left until the official end of spring, no
rain is forecast so this is unlikely to change. Here we analyse precipitation
records for the Phoenix Park station dating back to 1837, one of the longest
continuous records in Ireland. We show that 2020 has returned the lowest spring
[March, April and May (MAM)] rainfall total since at least 1837 and resulted in
the development of drought conditions more extreme (and earlier in the year)
than in summer 2018. The month of May, with a total rainfall of 8.3 mm
(reported on Met Éireann’s website) ranks in the top 1% of driest months in the
entire Phoenix Park record. However, truly remarkable is the fact that combined
rainfall totals for April and May 2020 rank as the driest consecutive two months
ever recorded at Phoenix Park, the longest running continuous series in the
Republic. These are remarkable statistics on their own, however, long range
forecasts and seasonal outlooks show little sign of significant rain at this
stage.
The Phoenix Park Rainfall Record
Figure 1. Phoenix
Park site photo sourced from Met Éireann. 53°21‘50” N, 06°20’00’’ W, 48 m above
mean sea level.
Figure 2 plots the
annual rainfall totals for Phoenix Park over the full period of record for
complete years (1837-2019). To check the quality of the data we applied the
Pettit test and Standard Normal Homogeneity Test (SHNT) to the annual series.
Both tests identify a statistically significant (p < 0.05) break point in
1913. However, we find no evidence from available metadata for any significant
changes in the gauge, measurement practice or site at this time. Notes on the
ten-year books highlight a change from an 8-inch gauge to a 5 inch gauge for some
months in 1913, but reverts back to an 8 inch gauge before the end of the year.
We note that Noone et al. (2016) also highlight a break point around this time
at a number of other long-term gauges in Ireland. Given that we know of no
systematic changes in measurement practice that would affect multiple series
simultaneously at this time, it may be that this break point is due to a natural
cause. Therefore we do not make any adjustments to the series here. We also
emphasise that the identified break suggests that the pre-1913 series may be
artificially low. As we are assessing low precipitation totals and droughts, we
note that if adjustments were to lift the early series, it would make the
spring 2020 totals even more remarkable in the long-term context.
Figure 2 Annual precipitation totals for
Phoenix Park 1837-2019. The black line represents low frequency variability in
the series using a lowess smoothing function. The vertical black lines
represents the timing of the possible breakpoint identified using both the
Pettit test and the SNHT.
Record Rainfall
We extracted precipitation totals for spring [MAM] and all
spring months from 1837 to 2020. These are plotted in Figure 3. Evident is the very
low total for Spring 2020 (52.6 mm), by far and away the lowest spring total in
the entire record. Totals for each month have been low, especially in April and
May, but not record breakers on their own. Figure 4 shows just how extreme the
spring 2020 totals have been, far lower than any other total recorded in the
entire series. While March totals (30.7 mm) were below average, both April
(13.6 mm) and especially May (just 8.3 mm) have been extremely low. These
numbers are not just remarkable for Spring. The combined April and May total is
the driest consecutive two-month total ever recorded (at any time of the year)
at Phoenix Park. The total for May 2020 lies in the top 1% of driest months
ever recorded at the station back to 1837. The total for the three months of
March, April and May mark the 5th driest three-month period ever
recorded across the record.
Figure 3 Precipitation totals for
Spring [MAM] (top) and for each spring month (bottom) recorded at Phoenix Park,
Dublin 1837-2020. Red line is a lowess smoothing function.
Drought Conditions
To examine drought
conditions at Phoenix Park we use the Standardised Precipitation Index (SPI) (McKee
et al. 1993). SPI is one of the most widely used drought indices and can be
used to examine drought of various accumulations. Here we derived SPI-3 to examine
how deficits accrued during spring 2020 compare to other droughts in the
record. SPI-3 is widely used to measure agricultural drought and soil moisture
deficits. SPI values between 0.99 and −0.99 are generally considered to be near
normal, −1.00 to −1.49 is moderate drought, −1.50 to −1.99 is severe drought
and less than −2.00 is defined as an extreme drought (Noone et al., 2017).
Figure 5 shows the SPI-3 index applied to all months since
1837. Evident is the extreme nature of the drought in which we currently find
ourselves. In terms of three month accumulated deficits, the current drought
has already surpassed the minimum SPI-3 values for the summer 2018 drought at
Phoenix Park. It has done so more than a month earlier also. Across the entire
record May 2020 and April 1854 are ranked joint fourth most extreme (SPI-3 =
-3.24) drought events. March 1891 is ranked second (SPI-3 = -3.53) and April
1938 ranked as the most extreme (SPI-3 = -3.76). It is worth noting that the
current drought event is ongoing and with no end in sight. It is already in the
top 5 most extreme droughts in the series.
Figure 5 SPI-3 series for Phoenix Park 1837-2020. Blue shows wetter
than average periods, red drier than average. The grey dashed horizontal line
shows the threshold for severe drought, the black dashed line is the threshold
for extreme drought.
Figure 6 shows just the Spring SPI-3 series (SPI-3 extract
for month of May) from 1837 to present. May 2020 is by far the most extreme Spring
drought (SPI-3= -3.24) experienced at Phoenix Park in more than 180 years. No
other event comes close. This is despite the fact that over the long-term there
is a statistically significant trend towards less extreme Spring droughts. This
should highlight the danger of planning based on the extrapolation of trends. Table
1 shows the top ten ranked spring droughts in the Phoenix Park record, with
spring 2020 head and shoulders above the rest.
Figure 6 SPI-3 series for spring (May SPI-3) for Phoenix Park
1837-2020. The series shows a statistically significant trend (p=0.02) towards increased
SPI-3 values over the long term (i.e. less extreme droughts). Despite this the
May 2020 SPI-3 value is by far the most extreme on record.
Rank |
year |
Month |
Phoenix Park SPI-3 |
1st |
2020 |
5 |
-3.24 |
2nd |
1929 |
5 |
-2.16 |
3rd |
1944 |
5 |
-2.08 |
4th |
1875 |
5 |
-2.02 |
5th |
1990 |
5 |
-1.90 |
6th |
2007 |
5 |
-1.90 |
7th |
1893 |
5 |
-1.88 |
8th |
1938 |
5 |
-1.84 |
9th |
1855 |
5 |
-1.73 |
10th |
2011 |
5 |
-1.73 |
Table 1.
Top ten ranked SPE-3 Spring (MAM) at Phoenix park 1837-2020
Outlook from here
It is important to note that this drought is ongoing. The
passing of a season causes excitement for us to tally numbers, but the drought
continues. The numbers are exceptional to date but large soil moisture deficits
exist. It will take a considerable amount of rain to bring this drought event
to an end. Continued dry conditions will make the 2020 drought an even more
remarkable event. While forecasts for the coming weeks show some chance of
rain, the totals for now look to be small. The longer-term seasonal forecasts
for summer, while uncertain, suggest a drier and hotter summer than average
over western Europe. The impacts of the 2018 drought live large in the memory.
While the drought of 2020 is more limited in spatial scale thus far, affecting
the east most intensely, the unfolding situation needs to be carefully
monitored. Unlike 2018 we now find ourselves in the midst of a global pandemic
where water has taken on a new public health importance and created new
vulnerabilities.
References
McKee TB, Doesken NJ, Kleist J. 1993. The relationship of drought
frequency and duration of time scales. In Eighth Conference on Applied
Climatology. Am. Meteorol. Soc. January 17–23, 1993, Anaheim CA, 179–186.
Noone, S., Murphy, C., Coll, J.,
Matthews, T., Mullan, D., Wilby, R.L. and Walsh, S., 2016. Homogenization and
analysis of an expanded long‐term monthly rainfall network for the Island of
Ireland (1850–2010). International Journal of Climatology, 36(8),
pp.2837-2853.
Noone, S., Broderick, C., Duffy,
C., Matthews, T., Wilby, R.L. and Murphy, C., 2017. A 250‐year drought
catalogue for the island of Ireland (1765–2015). International Journal
of Climatology, 37, pp.239-254.
Supporting
Information
Screenshot of monthly
rainfall totals for Phoenix Park, accessed 30/5/2020
Seasonal
Forecast-ECMWF shows the likely predominance of high pressure over western
Europe for summer 2020.
2 comments:
Is there a correlation between lower rainfall in Leinster and lower that normal Atlantic sea temperatures off the coast of Ireland?
Thanks for your comment,this is something that we have not investigated. But there have been some previous research that has looked at the relationship with the AMO and changes in the European climate. Here are a few links to papers that might be of interest: http://centaur.reading.ac.uk/30109/1/NG_paper.pdf https://rmets.onlinelibrary.wiley.com/doi/full/10.1002/wea.2543
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