However, during an El Niño, these trade winds weaken, so the warm waters slide back towards the central and eastern Pacific, in what is known as an equatorial Kelvin Wave, so the central and eastern tropical Pacific waters get warmer, a hallmark of an El Niño. These warm waters have a positive feedback in weakening the trade winds further, and even reversing the winds, so strengthening El Niño.
Record Strong ‘Monster’ El Nino in 2015
Several indicators suggest that the current El Nino event underway is already one of the strongest observed, if not the strongest, ever recorded. One of the strong scientific indicators are Oceanic Kelvin waves, as they help carry the warm West Pacific waters eastward across the Pacific. One record Kelvin Wave raged eastward across the equatorial Pacific in spring 2014, which seemed to kick start the warming last year towards El Nino conditions. Further impressive Kelvin waves in the Pacific Ocean this year continue to result in upward spikes of the ENSO 3.4 Index, a standard index to monitor the magnitude of El Nino conditions in the ocean via sea-surface temperature anomalies. The ENSO regions of the equatorial Pacific are shown below:
A look at the great red scar spanning more than half of the Equatorial Pacific Ocean on the upper Climate map (below) indicates it’s a Monster El Nino year. This zone is now showing an amazing +1.26 C sea surface temperature anomaly above the already hotter than normal 1979-to-2000 average. As a result, the Equatorial atmosphere continues to contribute to global temperatures that for 2015 will be the hottest ever recorded over the past 135 years.
No two El Ninos are exactly alike as they can vary in intensity and distribution of warmest temperatures in the ENSO regions, as indicated in the map above. Furthermore, El Nino/ENSO is not the sole driver of our weather, but works in tandem with other drivers such as solar activity, winds in the tropical stratosphere (measured by the Quasi Biennial Oscillation), heat fluxes from snow cover, global sea surface temperatures, day-to-day blocking patters, etc. Changes in the behaviour or the dominance of any of the other drivers of our weather, then different weather may be experienced between winters where a strong El Nino is present.
Below lists the seven strongest El Nino events since 1950, using the Multivariante ENSO index (MEI). Alternatively, the Oceanic Nino Index (ONI) shows strongest/weakest El Nino/La Nina years.
Cold & snowy UK winters with El Nino
2009/10 is listed as having a moderate El Nino (1.0-1.4C SST anomaly) on the ONI index, above, though doesn’t appear in the MEI top 7. The winter of 09/10 was then the coldest winter since 1978-79, with a mean temperature of 1.5 °C (34.7 °F). However, unlike this autumn and coming winter, solar activity had reached a minimum during that winter which probably contributed. Also, the Quasi Biennial Oscillation was in an easterly phase. An easterly phase of the QBO often coincide with more sudden stratospheric warmings, a weaker Atlantic jet stream and cold winters in Northern Europe and eastern USA.
1986/87 is listed as having a moderate El Nino on the ONI index, though on the MEI is one of the top 7 strongest El Ninos since 1950. January 1987 was an exceptionally cold month with much snow in places, as was March that year. Again, like winter 09/10, solar sunspot activity was at a minimum and an easterly QBO was present. (See graphs below for historic solar activity and QBO phase)
1965/66 is listed as having a strong El Nino on the ONI index and in the top 7 on the MEI. Winter 65/66 saw colder than average December and January, with quite a bit of snow in the east between the 14th and 22nd January, though February was mild. Again, the winter was during a minimum in solar activity and also the QBO was in an easterly phase.
Mild UK winters with El Nino
1997/98 is listed as very strong on the ONI index and is the strongest on record, along with 1982/83, on the MEI. The winter of 97/98 was rather mild, expectionally so in February, the warmest February of the century. A new record Feb temperature of 19.7C was recorded at Greenwich on the 13th. That winter was just coming out of a solar minimum and the QBO was neutral to slightly easterly.
1972/73 is listed as having a strong El Nino on the ONI index and is in the top 7 on the MEI. The winter was mild overall, though there were a few cold snaps. Sunspot activity was on a downward trend from its peak in 1970, though the minimum that decade wasn’t until 1976. The QBO was easterly during much of 1972 though to turn westerly in the New Year.
1987/88 El Nino listed as moderate on the ONI, but doesn’t appear in the MEI top 7. The winter was mild overall and quite wet and stormy. The winter was just coming out of a solar minimum with the QBO turning westerly into the New Year.
Quasi Biennial Oscillation Index (grey/shaded areas are westerly phase)
Correlation between El Nino and UK winters.
Above is just a snapshot of cold and mild winters during El Nino episodes, but it is apparent that a moderate or strong El Nino can still bring a cold winter if given solar activity is low and the QBO is solidly in an easterly phase.
Of course there are other drivers too that maybe at play. The Snow Cover Extent (SCE) is a fairly new index used to quantify the amount of snow cover present across the continent of Eurasia during the month of October. The logic behind this tool is that during high snow cover years in Eurasia, the Siberian snow cover expands during October – inducing surface cooling and strengthening the Siberian high. As result, the tropospheric jet amplifies, enhancing poleward heat flux or vertical wave propagation. This, in turn, weakens (warms) the Stratospheric Polar Vortex as we head into winter. So by January, typically stratospheric warming then propagates into the troposphers, creating a negative Arctic Oscillation (AO) and thus increasing the risk of cold and snowy weather across the UK, as the jet stream is forced much further south with the UK on the cold side of the jet stream
Prospects for winter UK winter 2015/16
Put all the above together, I can perhaps give some hints or pointers to what the coming winter may hold.
El Nino this year is forecast to peak in the next few months, before declining in magnitude as we head into the New Year. Whether this decline will be enough to change the strength and configuration of the currently strong and flat jet stream in the northern hemisphere, remains to be seen. This year’s El Nino is shaping up to be the strongest since the last very strong El Nino in 1997/98 – which was itself the strongest since accurate records begun. However, we are perhaps in uncharted territory with regards to this year’s 'super El Nino' – as not only is it equatorial basin wide, also the north and northeast Pacific is anomolously warm too, which differs from the SST make-up during the last super El Nino of 97/98.
Historically, El Nino peaking late in the year tends to correlate with milder and wetter than average conditions overall across the UK during the first half of winter, with a corresponding increased risk of Atlantic storms, as we’ve seen illustrated on Friday 13th November by Storm Abigail. The classic signature of a strong El Nino is a strong Alaska low, troughing across western N America, ridging across SE Canada and a broad trough dominating the North Atlantic to the west of the UK, while pressure is high over mainland Europe.
Of course, as I have mentioned earlier, El Nino is not the sole driver. So we need to look at how other drivers may behave this year too.
Quasi-Biennial Oscillation - the current westerly phase of the QBO is helping to strengthen the stratospheric polar vortex as we head into winter, which will eventually propagate towards the surface as low heights/pressure thus more likely keeping cold air locked up over polar regions – certainly during the first half of this winter. Though, for now, there are no signs of a tropospheric vortex setting up across Greenland for now, its traditional home during winters where we see weeks and weeks of westerly winds with gales and high rainfall.
Eurasian Snow Cover Extent (SCE) this October is looking high enough to be favourable for increased wave activity transferred to the stratosphere, which may disturb the stratospheric polar vortex and perhaps trigger a Sudden Stratospheric Warming (SSW) which eventually propagates to the troposphere, forcing cold air in the arctic equatorward, leading to a greater risk of cold weather for the UK.
Solar Activity – currently sun spot activity is in decline from its peak in 2014, though someway to go until the next solar cycle minimum in 2017, so this decline may have a negligible effect on the stratosphere.
Pacific and Atlantic Sea Surface Temperatures – anomalously warm SSTs across the NE and N Pacific this year may aid in planetary wave amplification over this sector, these waves perhaps strong enough to transfer towards the poles and perhaps help destabilise the stratospheric and tropospheric polar vortex and increase the chance of cold conditions pushing south to our latitudes. The anomalous cold pool over the N Atlantic off Greenland will probably not have a great effect on weather patterns this winter though.
Arctic sea ice levels - Arctic sea ice extent for October 2015 averaged the sixth lowest October in the satellite record. Below average ice extent tends to mean anomalously warm SSTs and air temperatures within the arctic circle, which can promote higher pressure/heights and thus an increased possibility of a negative AO.
There are other factors that may affect weather patterns this winter too. But these are the main winter drivers I feel. The wQBO and the strong El Nino are currently working against sustained cold and snowy spells this winter by creating the +AO/+NAO pattern that favours predominantly mild and stormy conditions for the UK. Though a decline in magnitude of El Nino in the New Year, anomalously warm north Pacific SSTs and good Eurasian SCE increasing wave flux activity may perhaps allow an increased chance for a more convoluted flow pattern later in the winter and a disrupted polar vortex.
Of course, there are unforeseen factors that may come into play that could disrupt the pattern, this maybe more short-term changes in the flow pattern, such as waves amplifying in the upper flow developing blocking highs which could position favourably for cold and snowy spells. These are more difficult to predict and may still happen even when the weather is seemingly stuck in rut of strong flat westerlies.
Indeed, despite the background signal of a strong and flat Atlantic jet stream heading towards the UK, recent NWP model runs and their ensembles having being hinting at a stationary wave in the weaker northern arm of the jet over N. America developing and setting up a blocking high over eastern Canada and eventually Greenland next week and weekend, which may allow a cold northerly to develop across the UK. So, that’s why it is difficult to give any detail with regards to how the weather will behave in 10 days, let alone 3 winter months!