We have circulated two documents, one on the rainfall of November 2009 and the other on the cold spell of January 2010. I will give a brief overview and make some comments on these, as there is significant detail in the documents. The documents provide more information than I can provide in my brief summary.
I will begin with the rainfall of November 2009 and will deal with it in both a broad and specific context. The information I have provided in the documents is a draft of a report which was in preparation and which will, eventually, be published by Met Éireann, although perhaps in a slightly different format. The figures are sound, but I may just rephrase some of the facts. I ask members to please bear this in mind if they see a different version in the future. I also ask members to bear in mind that I will be speaking about rainfall. Sometimes in the media there is confusion when people talk about return periods and how rare events are, whether talking about a flooding event, a river flow event or a rainfall event. I would like to make it very clear that I will deal specifically with rainfall events.
To set the scene, let us look back about three years. It will not be news to anybody present that we have suffered three very wet years and particularly wet summers. To take 2009 itself, we had just come through a very wet summer. At Valentia Observatory near Cahirciveen, County Kerry, which is one of our top quality, long-standing stations with over 150 years of records, the summer rainfall record was not just broken but shattered, with close to 600 mm of rain in the summer compared with approximately 400 mm in the previous wettest summer. That is the broad context of the lead-up to the weather of November 2009.
Following that, there was a brief dry spell but coming into the middle of October it became wet again and that wet spell lasted into November 2009. The only word that can describe the rainfall of November in Ireland is "extraordinary", both in terms of the amount of rainfall and of the spatial extent — the area of the country — that was covered by very heavy or extreme rainfall events. It is often the case that these are of short duration and only cover a small area, perhaps a few square kilometres. However, for November 2009, we are talking about a rainfall event which lasted over most of the month and which had extensive geographic coverage, as I will show on the maps I have provided, particularly in the western part of the country, an area broadly delineated by the River Shannon, which was badly affected. This rainfall was extraordinary in many respects. While I will not read the document in detail, I would like to quote one figure, namely, that 79% of our rainfall stations recorded their highest ever November rainfall in 2009. This begins to give a flavour of the issue — records were being set and the effect was widespread.
Page 6 of the document contains two maps which give the broad picture of the November rainfall, with the one on the left giving the amount of rainfall in millimetres, ranging from 300 mm to 600 mm, which are large amounts of rainfall. The map gives an idea of where the heaviest rain fell. It is not unusual in a map that presents rainfall amounts that one can pick out the higher mountains — it is a fact of life that there is heavier rainfall high up in the mountains — and this is the case with this map, where such mountain areas can be identified in Kerry, Wicklow, west Galway, Mayo and Donegal.
The map on the right is a slightly more informative map, which gives the percentage of normal rainfall for November 2009. It shows many areas which received 250% more than normal and some nearly reached 400% more. Again, I would use the word "extraordinary" to describe it; this is an awful lot of rainfall, no matter how it is assessed.
To put rainfall of this nature in context, we often use the term "return period" and, as it is often misunderstood, I will take a moment to explain the term. It is a useful concept in expressing how rare or unusual an event is. If I say the rainfall return period for a particular event is, say, 100 years, I mean there is a probability of one in 100 of that happening in any given year. It does not mean that if it happened last year, one has 99 years in the clear; it is simply a probability. If the rainfall return period is 200 years, there is a probability in any given year of one in 200 of that happening.
The more important context begins on page 8 of the document, which deals with the duration of the rainfall from one to 25 days, spread over the entire country. Each grid square on each map contains information on the probability or return period, which tells us how rare or unusual the events are. The one-day duration is not particularly spectacular but, as we move to two-day duration, we begin to see the colours coming out and the more extreme events begin to happen. A map location on the Wexford border gives a good indication that even within a very large-scale event, there are still small-scale variations. The event in Wexford is for real, although it is quite localised. I simply point out it is not a mistake in the map — it is for real.
The next page deals with the four-day and eight-day durations. One begins to see widespread areas of the map shaded in colour, particularly in the west and broadly along the Shannon. This tells us that in some areas which experienced eight-day durations the event is rare beyond one in 100 years or even beyond one in 200 years. The next page deals with 16-day and 25-day durations. Talking on a broad scale, covering the whole country, the 25-day duration is where the event is peaking and where the worst picture is drawn. One can see swathes of the country affected by the 25-day duration.
One of the extraordinary points about the November rainfall was how much of the map of the country is covered by colours which represent a return period of 500 years plus — we do not go beyond 500 years to, say, a 739-year return period because accuracy is not possible. These are very rare, unusual and extreme events, covering a very large swathe of the country. Having seen the news reports, nobody will be surprised to see where the colours are located on the map and where the 500-year plus return periods occurred.
One event seemed to carry particular significance, namely, the event in Cork on 18-19 November, which has been mentioned at today's meeting. We have tried to shed some light on that event. Moving into a brief discussion of the Cork situation, members should keep in mind the context in which this is happening. It is not just two days; it is two days on top of all the other events which have already happened and all the rainfall that has already fallen. However, to take the two days in isolation, we have taken the opportunity to provide two charts, one giving the amount of rainfall in the millimetre amounts we believe fell in the various areas over those two days. We have tried to pin this down to the wettest 24-hour period. We have done the same exercise with the return periods to try to express how rare or extreme an event this was.
Members will see that the rain in the area was certainly heavy — we are not just talking about Cork city but about the catchment of the River Lee to the west and up into the mountains, which is the important area. However, taken in the context of what had been happening overall, particularly in November 2009, one could not say it was extraordinary — we are talking about return periods measured in decades, perhaps several decades and up to 50 years, but not hundreds of years in this case. Therefore, the way the events in the Cork area on 18-19 November must be understood is as a very wet couple of days by any standards, but against the background of the extraordinary amounts of rainfall which had been happening overall. The document shows there are some areas in the same catchment area in the mountains in the west of Cork, heading towards the Kerry border where, again, the return periods are measured in hundreds of years, although these are not as widespread or large scale as those further north. So, the story of 18-19 November is that while there was heavy rainfall, it is set against a backdrop of what had already happened leading up to that point.
At the back of this document, which I am not going to read out, members of the committee will find a table containing a selection of information for various specific point rainfall stations where we have actual measurements that we can contribute. They are grouped by county and show how much the maximum rainfall was over one, two, four, five, 16 and 25 days, along with the return period. That return period is a probability. Members should think of one over that number as being the probability of having that much rain over that number of days in any given year.
That is all I have to say in my initial introduction about the rainfall of November 2009. More information is contained in the document I referred to. If anybody has any questions I will be happy to try to answer them. Will I move on to the next item, Chairman?