Posts tagged Surf Holidays
No fear when the forecast says no surf!
0If you are here in the UK for August, and the surf is flat, here’s some ideas for enjoying the coastline in Cornwall. Bring your wetsuit, you’ll still need it!

Swim in a rock pool
There are some fantastic naturally occurring rockpools to be found along the British coast. In North Cornwall Treyarnon Cove is great for surfing, but also has a number of rock pools. The best being the larger one at the North end of the beach. At low tide this beautiful pool reveals itself. It looks just like a pool; rectangular shaped, and about 30 feet long, with a depth of around 8 feet in its centre.
After your dip in the sea you could warm yourself up with lunch and a hot coffee in one of the cafe’s facing the picturesque harbour in neaby Padstow. It’s about 10 minutes drive from Treyarnon.

Coasteer
Feed your need for adrenline by trying coasteering with Vertical Descents, a Newquay based adventure company. It’s a combination of rock climbing, canyoning and cliff jumping all rolled into one! You’ll be jumping from the cliffs, swimming through caves and scrambling along the coastline in a small group lead by one of the instructors. Contact Sam on 07891 264342 and see Vertical Descents for more details.
Eat Well
If the weather has taken a turn for the worse, which is highly likely given we are in the UK, hunker down for some great food at The Beach Hut, Watergate Bay. They prepare fresh, interesting food with good service too. The views across the Bay are great too. It’s half the price of Fifteen but just as tasty. I like their fab detox salads, the falafel and their amazing Extreme Hot Chocolate drinks with marshmellows on top! Great for warming you up after a brisk walk on the beach. Remember to go at low tide to get the long walk! Book a table on weekends as it can get quite busy 01637 860543.
Go au-naturel
If the weather suddenly takes a turn for the better and the sunshine is everywhere, take a chance and enjoy the beaches the way nature intended! Vault Beach is located in an area of National Trust-owned land at Dodman Point, Gorran Haven, south of St Austell on Cornwall’s South Coast. Nude use of the South end of this privately owned beach has continued for many years; which can take the unsuspecting surfer by surprise! For more info on where you can strip off in the South West see the Naturist UK wesbite.
Swell window and beach orientation
0
In the last article in our series about surfing and the weather we look at the location of your local coastline in relation to the position of active low pressure systems. We relate this to the direction and movement of the ‘low’, and how this affects waves in the ocean, and ultimately, swell at your fave spot.
Swell window
The swell window is the area of cosatline that is exposed to groundswell. The majority of swell in the North Atlantic travels from the North and East to the West and South. This means that the most consistent places in Europe exposed to the swell are Northern Spain and Western Ireland, as well as the West coasts of Portugal and Morocco. The Azores and the Canary Islands also get a fair amount of swell. The North coast of Cornwall and Devon have much smaller swell windows from this direction of swell, because Ireland’s land mass blocks most North West and Northerly groundswells.
Another factor that will determine your swell is your surf spot’s location in relation to the low, and the usual path of the low. For instance Western Ireland in the winter can get consistent large surf, but it is often blown out due the fact that the low is too near the coast; creating strong winds. Also there can be many lows, one after the other, and each one ‘blows out’ the other’s swell.
On the other hand, Morocco and the Canary Islands get lots of good winter groundswell with calm, warm weather conditions. This is because the lows pass far enough away not to affect the warm high pressure weather at the coast.
Beach orientation
The orientation of individual beaches is equally important in determining how big the swell will be when it arrives. For example, the North coast of Cornwall picks up most of its swell from a Westerly direction, so those beaches facing West get the full impact of the swell. Those facing North will get less of the impact of the swell, and have smaller waves as a result, as the swell has to wrap around a headland to reach the shore.
Conversely many of Cornwall’s South East coast beaches don’t receive much or any of the Westerly swells, and as a result are less consistent for surfing. They tend to have a lot of ‘flat’ days. This coast relies on the rarer South and South Westerly swells or really large Westerly swells we sometimes get in the winter. These can then wrap around the coast and hit the shore with some good surf.
To check your surf conditions we recommend you use windguru, and the BBC weather site to track pressure systems.
So next time you look at your weather chart and see a low pressure system coming in, it could be generating some great waves for you! Happy surfing!
What makes waves?
0In the first of our series of articles about how the weather affects surfing, we look at what causes our swell in the South West of Britain;
Low pressure systems

As you know the UK is situated on the Eastern side of the North Atlantic Ocean. Out at sea there is a lot of activity in the weather. Understanding how the weather works will help you see how waves are formed.
Our UK waves are formed by low pressure systems. To find out about low pressure systems and how they are created, we need to first consider what is happening to air pressure across the world.
No prizes for guessing that the equator is hotter than the rest of the planet, so we can also guess that over the equator the air is heated. This air rises, and is replaced by cooler air from the poles. These pockets of air are called ‘highs’ and ‘ lows’.
Low pressure areas suck in air from hotter areas. When a pocket of warm and cooler air meet the hot air passes over the top, which lowers the pressure, and makes the air spin. Low pressures spin anti-clockwise and highs clockwise. As you can imagine, in winter, when the difference in temperatures is greater, these low pressures are more dynamic and the air spins faster.
In the Atlantic the pattern we see is a low pressure system predominantly coming from the South West heading North East for our Western coastline. Why does it go this way? Well, its all down to the jet-stream. This is the name for the flow of air at high levels in the atmosphere. The jet stream travels faster than the air lower down in our atmosphere, where the highs and lows are moving. The jet stream moves West to East around the world. This movement is caused by the rotation of the Earth. It can be pushed North or South, and can be stronger or weaker, depending on the other weather systems it comes into contact with. Some scientists have said that with climate change these jet streams are being pushed further towards the polar regions.
These highs and lows are often depicted on TV weather charts called ‘synoptic charts’. (We’ll look at these in more detail later in our series.)
So next time you tune in see if you can spot one, and predict which way it is heading!
In our next article we will look at what these low pressure systems are doing to the surface of the ocean.
Gandering around in the sun
1

Its a lovely morning here on the farm. The sun is shining and the geese are enjoying strolling round the yard like the own the place!


