Yachting Monthly

THE WEATHER

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Understand­ing the weather is an essential thing to grasp when you’re planning a stint of out-of-season sailing.

There are four challenges to contend with as sailors: frontal depression­s, cold polar air, low sea temperatur­es and fog. Depending on whether you’re in the autumn, winter or spring their frequency will vary, but you need to be prepared for them at any point.

The seasons are created by the sun’s annual migration from 23° south in mid-winter, to 23° north in mid-summer.

It’s an extraordin­ary journey covering almost 3,000 miles in six months. The sun drags the weather systems with it and the patterns we experience shift dramatical­ly, giving us our seasons.

If we’re lucky, during the summer months the British Isles lie under the protective embrace of the Azores High, which is pushed north towards us. It creates stable, dry weather which can be rather windless unless a sea breeze kicks in.

FRONTAL DEPRESSION­S

As the sun slips back across the equator at the time of the autumnal equinox we must fend for ourselves against the trademark weather feature of the North Atlantic: frontal depression­s. These systems are generated on the boundary between two different types of air mass: cold, dry polar air and warm, wet maritime air. The boundary forms two distinct fronts. The warm front is the leading edge of the low and brings a grizzly, grey day of drizzle and rain. It precedes the warm sector, which is a wedge of maritime air that has infiltrate­d the surroundin­g polar air mass. Behind the warm sector is the mighty cold front. Though more compact in stature than its sprawling warmer brother, it packs quite a punch. Towering cumulonimb­us clouds bring heavy, often thundery, downpours and gusty conditions. Although it heralds the beginning of the end of the low pressure system this is often where the strongest winds are found. This, combined with a marked veer in direction, makes for tricky conditions on the water. Often a secondary low is spawned on the trailing edge of a cold front, perpetuati­ng a cycle of unsettled conditions.

Although these systems are generally well forecast these days, it pays to take heed of synoptic charts. Simon Rowell, meteorolog­ist for the British Olympic Sailing team, explained that ‘the autumn is particular­ly unstable as it’s the time of year when sea temperatur­es are at their highest and it’s peak hurricane season in the Caribbean. Some of them will come our way as deep lows.’

SEA TEMPERATUR­E

One of the most under-appreciate­d changes through the winter is sea temperatur­e, both on a local and global scale. ‘The temperatur­e difference between the poles and the equator increases dramatical­ly through the winter months,’ explains Rowell. ‘This imbalance is a key driver and one of the reasons behind stronger trade winds and more extreme weather in the winter.’

On a more local scale, the temperatur­e differenti­al between the land and sea which creates summer sea breezes, weakens. A windless day in the summer can become a Force 4 by early afternoon thanks to the convection created by rising temperatur­es on shore, but that won’t be a feature in the winter months. A windless day will most likely remain a windless day.

One of the biggest difference­s between spring and autumn sailing is the sea temperatur­e. It’s still relatively high in October, but hits rock bottom around the end of February just as bright spring days and longer hours of daylight lure us out on our boats. What may seem pleasant weather on land is very different offshore, and the invisible chill of the water should not be underestim­ated.

COLD POLAR AIR

In my early twenties I worked on the Fasttrack Yachtmaste­r Programme at UKSA which ran all year round. One of the most senior skippers gave me a stark warning at the beginning of winter: ‘Beware the easterlies,’ he said with dread in his voice. He was right of course. At least with a chain of depression­s you get a let up at some point. But if high pressure establishe­s itself over Scandinavi­a then expect relentless, bitter winds of Force 6 and above. It’s what caused the Beast from the East in 2018 and it’s a time for armchair sailing only.

FOG

Fog is an often-overlooked feature of winter sailing. Technicall­y it’s visibility of less than 1,000m, although anything less than 2 miles probably requires a change in the way you’re operating on board. As a rule of thumb if you can’t see the horizon from the cockpit of a small yacht, the visibility is 2 miles or less.

It’s easy to fall into the habit of just checking the wind forecast on an app and forgetting visibility. In the summer months fog is less likely, but out of season the risk increases. It’s an integral part of the Shipping forecast though, so pay attention to it.

There are two types of fog: advection, or ‘sea’ fog, and radiation or ‘land’ fog. The ‘land’ and ‘sea’ refer to the cold surface on which the fog forms when warm, damp air drifts over it. Although they look the same from the inside, it’s important to differenti­ate them as their impact on sailing differs.

Land fog is a local phenomenon which tends to occur in the autumn when warm land radiates heat and moisture to the air above overnight. This causes the morning mists which gather in estuaries, rivers and other low-lying areas. It’s a purely coastal phenomenon which usually burns off by late morning or by heading a mile or so offshore. You shouldn’t need to cancel a whole day of sailing for land fog, but you might want to hit the snooze button a few times.

Sea fog is much more widespread, usually in spring when sea temperatur­es are at their lowest. Large areas of relatively warm, damp air drift in from the Atlantic and condense when they reach cold water. The resulting fog is pernicious – it doesn’t disperse even with strong winds and requires a whole new air mass to arrive before clearing up.

AIR DENSITY

When I’ve sailed in the high latitudes I’m always amazed by how forceful the wind is. Cold air seems to hit the sails much harder. There isn’t a definitive explanatio­n for this, with theories ranging from the increased density of the air to more complex hypotheses. Whatever the cause, you’ll need to be more conservati­ve about the sail plan.

 ?? ?? There’s more to late season than a warm coat, but the extra effort is often worth it
There’s more to late season than a warm coat, but the extra effort is often worth it
 ?? ?? A warm front will signal high pressure giving way to a depression
A warm front will signal high pressure giving way to a depression
 ?? ?? Land fog becomes more prevalent but should disperse quickly
Land fog becomes more prevalent but should disperse quickly
 ?? ?? A cold front will bring rain and strong squalls
A cold front will bring rain and strong squalls
 ?? ?? Prolonged easterlies mean plummeting temperatur­es, as was the case during the ‘Beast from the East’ in 2018
Prolonged easterlies mean plummeting temperatur­es, as was the case during the ‘Beast from the East’ in 2018

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