Will UK winter storms get worse?
The storms which have battered the UK over recent years, for example Storm Dennis and Ciara that occurred in February 2020, can be traced back to a strong front (a boundary separating air masses of different characteristics) of contrasting temperature between cold air over the north Atlantic and warmer air further south.
This strong temperature contrast across the Atlantic causes storms to form around the front, as hot and cold air circulates and mixes and tried to find a balance.
It is similar to when we add cold water into a hot bath – the cold water will form a boundary (a front) with the hot water, which must be mixed more evenly to make a comfortable balance of temperatures.
We have experienced a succession of deep Atlantic low pressure systems caused by a strong high level jet stream in the upper atmosphere. Add wind into the mix, which is also driven by strong contrasting temperatures, and this is why very wet and windy weather has been brought to parts of the UK during recent winters.
Storms in the UK are not necessarily going to get more energetic – they may or they may not, depending on where you are in the country. However, storm tracks are going to shift, but it is unclear whether this will be to the north or the south of the UK – climate models are not certain yet.
The key point is that wave climate will change and this will have an impact. Some areas will get stormier, others less so. Wave directions may also change, modifying longshore sediment transport, and this will also impact our coast.
What can be done to reduce the damage caused by storms?
England has experienced a major flood almost every year since 2007, leaving about 100,000 properties damaged, according to scientists in the Climate Coalition.
There is a need to increase the creation of more natural drainage systems if the government wants to avoid having to raise the level of sea and river defences every few years to counter the growing threat of flooding and storm surges.
Problems are often worsened by the erosion and concreting over of natural buffers, such as soil and green spaces. Ways to increase infiltration and places to slow and store water need to increase in order to add resilience to floodwalls.