Yachting Monthly

PRECISION WEATHER FORECASTIN­G

Building your own bespoke forecast is the best way to get reliable weather updates with which to make sound decisions at sea. Toby Heppell finds out how the experts do it

- Toby Heppell is the Sailing Editor for Yachting Monthly. He has beeen sailing all his life and has been writing about the subject for more than 15 years.

If you want precise weather forecasts where you are, here’s how to build your own from scratch

Forecasts are flawed. Weather forecasts online, on an app or from the Met Office via VHF radio, are all subjective. Inshore waters or shipping forecasts are limited by brevity, large areas and a high degree of caution – they often forecast stronger winds than you may experience. Mobile apps lean towards forecasts for specific locations and so don't give you the big picture. Some are created for specific purposes such as surfing or farming and have a level of interpreta­tion; without access to the algorithms behind them, however, it's almost impossible to work out what the built-in bias may be.

Often these forecasts are accurate, but sometimes they will be wrong. If you’re using someone else's forecast, you won’t know the reasons why it was inaccurate. Expert navigators and meteorolog­ists build their own forecasts so they are in control of the subjective elements or variables. Learning to do this means you can judge if a forecast is accurate or reliable, and make your own informed forecasts for the precise route and time you plan to sail. If you get it wrong, you can learn from your mistakes and make better informed decisions about when to put to sea and what conditions to expect.

To do this, you'll need to be able to access and read GRIB files (Gridded Informatio­n in Binary), which have been around for years, but are always getting more accurate, read them, and get an idea of the broad weather picture. You will need to interrogat­e highresolu­tion GRIB files for problem spots using your understand­ing of local weather effects, and compare this overall picture to other sources of forecast to judge your assessment.

This is a skill that takes time to hone, but develop your skills over time and you will be able to make expert-level judgments about the weather, and know how to judge which forecasts you can trust or not.

ABOUT GRIBS

GRIB files are output direct from Numerical Weather Prediction programmes and can provide a very useful and cost effective tool for personal weather forecastin­g. Most of us use GRIB data to some degree, as it is from these computer-generated models most forecasts make their prediction­s to a greater or lesser degree.

It is worth noting at the outset that GRIB data is purely objective as the informatio­n arrives to you without any human assessment, quality control nor guarantee that it is even correct – computer and communicat­ions systems can and do fail from time to time.

For short-term use it is essential to view them in the context of GMDSS forecasts that benefit from expert assessment of the computer prediction­s. You can easily argue that a GRIB file does not provide a forecast, as there is no interpolat­ion of the data provided. A wise sailor will always take in as much informatio­n as possible before choosing to put to sea, but by getting into the habit of downloadin­g and reading GRIB files you can be better equipped to understand the stability of a forecast and how conditions are likely to change.

‘I think the main benefit to me of GRIB data is the ability to plan ahead,’ says Frank Singleton, forecaster and author of the Reeds Weather Handbook. ‘That is best done by looking at the overall pattern being shown by the files, rather than the wind at points. Looking at that overall pattern via GRIB files is the best way you can understand how the weather might change over fairly small distances – and by that I mean 30-40km rather than 4-5km. I take one model, usually GFS, and look for consistenc­y from one day to the next. To my mind, that is the most useful way for a sailor to decide whether you can plan ahead or not.’

This is a point echoed, to some extent by author of the Mariner’s Weather Handbook, Steve Daschew. ‘It is absolutely a useful thing to be looking at weather a long way out and see what it is doing. Today we are lucky that we can sit at home with our computers and look at systems as they roll across the world. It’s worth noting that this is all quite fun to do, too. It’s good for your forecastin­g to get into the habit of watching the GRIB files as they change to give you an

idea of what the wind is doing on a large scale. It is worth stating, though, that what you see on your barometer and out of your window are the key things when it comes down to weather on a boat.’

‘GRIB files essentiall­y offer the same informatio­n as the synoptic charts, so in many ways when you are using low resolution GRIB file, you use it in the same way that you are using a synoptic chart,’ adds weather guru, Chris Tibbs.

‘The GRIB files are rather easier to look at than synoptic charts, I am adamant that people should be using GRIB files. We have moved on from the days of measuring isobar distance and then guessing at what the winds would be, simply because GRIBS do that for us and it is so much easier to see it and understand it in GRIB format.’

MODELS

There are many weather prediction programmes running across the globe, to which most sailors can get varying degrees of access. The best know is the American NOAAA Global Forecast System (GFS). Alternativ­es are the CMC GEM (Canadian Global Environmen­tal Model), the US Navy NAVGEM, the French ARPEGE and the German (DWD) ICON. There are many others, of course, but these are generally either unable to be accessed easily or are not provided for free.

These various programmes all provide slightly different forecast models, and big forecastin­g bodies like the UK’S Met Office may use an amalgam of any number of these models to create their forecast. However, for most, choosing one model and sticking to it offers the easiest solution over trying to make comparison­s. ‘Typically the models tend to converge in terms of prediction at something like 3-4 days out,’ says Singleton ‘but even in the short term where they might diverge there is not that much to be gained from comparing them. For a sailor looking at a GRIB file, you are trying to determine the reliabilit­y of the weather to come, not the reliabilit­y of the prediction model being used. I am always looking for consistenc­y of the prediction from one day to the next to decide how accurate and so believable it is.’

Of course if you are going to be downloadin­g GRIB files then you are naturally going to be faced with a choice over which model to select, so is there any significan­t difference between one another?

‘As far as I am concerned there is very little difference between them,’ says Singleton. ‘I tend to use GFS as it is the easiest one to find.’

The American GFS model has been upgraded in recent months, to bring it slightly more up to date, where some considered it a little behind some of the European models. In reality, however, these modelling updates are occurring pretty continuous­ly on all the systems and will have very little discernibl­e affect on the output for the casual user, as Singleton explains: ‘If you were doing some very sophistica­ted modelling then you might see a difference when models are updated but day-to-day weather is so unpredicta­ble, for a wind forecast you are not going to see any difference.’

Where there is a slight difference between models is in the time of their release, however. Almost all of the models provide a new file every six hours. ‘The German model runs every three hours, so in theory that will often be the most recent forecast but in terms of weather I am not sure that higher frequency makes any significan­t difference,’ Singleton concludes.

LIMITATION­S

The principal drawback with a GRIB file is that the global files only provide data on a grid of roughly 10km. As such, they are not all that useful in terms of specificit­y. You can, however, download high-resolution files (often for a subscripti­on fee) that reduce the grid to 1.4km, which are better for providing more accurate informatio­n for a specific area. The downside to this, of course, is the significan­tly larger number of files you will need to download for any given passage.

The distances involved in the global scale data also lead to a common misconcept­ion surroundin­g the GRIB forecastin­g, that they have a tendency to under-read the wind, but this is not the case. ‘With global models and with a grid length of 10km, if you are calculatin­g on a grid of that size then the

calculatio­n on that grid is smoothed somewhat,’ explains Singleton.

‘Although the forecasts are probably pretty good at predicting the mean or average windspeed they do not do well on the extremes. So if I am crossing the channel and the model says a Force 4-5 then I am pretty sure that at some point on that passage I’ll probably get a wind speed of Force 6 and/ or 3. So there will always be quite large variation in that – as we know the weather varies tremendous­ly.’

Similarly, because of this smoothing effect GRIBS do not do well with local weather effects. A global GRIB file may well tell you that the wind will be a Force 4-5 across the Channel, but in a southweste­rly, you would expect that windspeed to increase as it accelerate­s through the Dover straight but be more accurate in the West Country. As such, a Force 4-5 might well mean Force 6-7 for a Dover crossing, where Force 3-6 is the more likely when going from Dartmouth to the Channel Islands.

In addition to this struggle with landbased effects they are not all that good at reacting to specific weather anomalies: ‘Tropical storms are not very well modelled by GRIB weather files,’ say Daschew. ‘You can often see them start to form in terms of the overall wind picture and direction as it begins to build but as they are pretty quick to form, a very stable picture can become unstable much more quickly than the six-hour GRIB models can cope with very well.’

THE HUMAN FACTOR

Whilst a lack of interpreta­tion is one of the drawbacks to using GRIB files for forecastin­g, it can also be seen as one of its positives. ‘Forecasts are inherently political,’ says Daschew. ‘They are the result of people perhaps getting it wrong at some point so some pressures to interpret them in a different or more conservati­ve way very often. These pressures change all the time so they are often subject to outside factors.’

Singleton says he understand­s how pressures on forecaster­s can lead to this opinion being formed. ‘In my days at the Met Office when the Shipping Forecast used to work under me, they always said they try to tell it like it is and they do not try to make it sound worse.’

‘A forecaster in the UK must issue a gale warning if the wind might reach Force 8 for that area, anywhere in the sea area. That might only be a part of the sea area, but on the shipping forecast, there is not the time (and in the inshore waters forecast the space) to define that level of specificit­y, so they might say ‘round headlands’ or give as much detail as they can that way, but it will still be a little unclear. That can provide an impression of over-forecastin­g. Also, the forecaster can only cancel a gale warning if they are sure there is no chance of there being one in that sea area. So if you put that together this naturally leads to an appearance of over-forecastin­g.’

Though it might still be broad-stroke, a personal interpreta­tion of the GRIB data allows you to see if this gale is likely to be making its way in one direction or another.

The difference­s in forecast and GRIBS are not only political, as Singleton touches on. Many forecasts are designed for specific purpose. The Shipping Forecast, as noted above, necessaril­y needs to be both brief and geared towards safety in terms of topend reading. As such, it is prone to predicting the possibilit­y of a gale where there might, in fact, be none as a result of erring on the side of caution and not having the time or space to provide a truly in-depth picture. Elsewhere other forecast tools take in GRIB informatio­n and run it through a

proprietar­y model to achieve a goal. Singleton points to some forecasts which are often used, which make very coastal specific forecasts. These can be very accurate for picking up sea breeze and other factors as they are variables added on top of the GRIB informatio­n received. This is useful close to shore but if you are making a long passage and are 10 miles offshore, their prediction will be taking into account effects that will have little bearing on your forecastin­g.

Without knowledge of how different forecastin­g models prioritise certain factors, it can be hard to know whether the informatio­n provided is going to be accurate for you. GRIB files simply lay out the prediction with nothing added and nothing taken away, which allows you to be in control of what factors you should consider on top of this standard informatio­n. As they are essentiall­y apolitical then GRIB files, driven purely by data, can allow for some decent analysis to allow you to form an opinion.

‘One thing that is really good about GFS is that you can now access informatio­n on the accuracy of the data as compared with the real-world informatio­n,’ says Daschew. ‘So you are able to look at the historical GRIB informatio­n for an area and match that up with how accurate the forecast was.’ Again, this purely data-driven approach that all the models take, without any human interactio­n makes for a much more transparen­t forecastin­g tool.

‘Let’s say I’m planning a Channel crossing from Dartmouth, then I would start to look at GRIBS from around five days out,’ says Chris Tibbs. ‘At that stage, as I am at my computer at home with broadband – so no issues with bandwidth – I will take a look at a file of the whole Atlantic. Broadly what I am looking at is the way that systems are forming and direction of travel out in the mid-altantic.

‘One thing that lots of readers will do – I tend to use Predict Wind’s Offshore App – is to animate files and I think that is a really useful tool so you can see how the fronts and systems are shaping up and how they are developing over time.

‘Once I have a good idea of what broadly is coming my way, I would be looking to get some high-resolution files for specific sections.

‘It’s a three-step approach, effectivel­y. You have the coastal waters on the English side first. So I would look at things like Start Point in high resolution and be looking at what sort of accelerati­on you will be getting there and considerin­g the tide and whether that will add to any wind accelerati­on. It might be worth looking at something like Wind Guru or some other coast-specific forecast to see if that is predicting any sort of thermal enhancemen­t.

‘Then the further offshore you get, the more GRIB files’ accuracy increases as they are not dealing with the land effects, so I’d be focusing on them and what I expect to come in based on what has been developing in the Atlantic. Finally for the other side of the Channel I would once again be looking at high-resolution files again comparing them with a coastal waters forecast or similar for that side to see if they are matching what the GRIBSS suggest and what I expect.’

 ??  ??
 ??  ?? Localised storms and squalls are not served well by GRIB files, which look at the conditions as a whole, so will need local interpreta­tion
Localised storms and squalls are not served well by GRIB files, which look at the conditions as a whole, so will need local interpreta­tion
 ??  ?? This squall is visible from a distance, but as it is localised it may not show on a forecast. It’s always worth having a ‘head out the boat’ attitude to weather
This squall is visible from a distance, but as it is localised it may not show on a forecast. It’s always worth having a ‘head out the boat’ attitude to weather
 ??  ?? The Straight of Dover is a well-known wind accelerati­on zone
The Straight of Dover is a well-known wind accelerati­on zone

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