NOBODY likes to be ridiculed, but for some people it can become a matter of life and death. Take Robert FitzRoy, the founding father of the UK’s Meteorological Office and captain of the Beagle during Charles Darwin’s five-year voyage. A keen amateur forecaster, he enthusiastically applied the science of his day to weather prediction. Much good did it do him. Instead of hailing his tentative prognostications as a useful first step, politicians, newspapers and other scientists harangued and mocked FitzRoy whenever he got it wrong. Depression quickly set in, to fatal effect. One Sunday morning in 1865, FitzRoy cut his throat in despair.
These days, most meteorologists have got used to being the target of jokes. The criticisms are the same, though. People expect weather forecasts to be accurate. In this age of weather-forecasting supercomputers and 24-hour satellite surveillance, what’s more, those expectations of accuracy have risen to new heights. The forecasters, of course, say their predictions are more accurate than ever before. Can we tell if they’re right?
Though theories abound, no one – not even the meteorologists – can agree on the best way to measure a forecast’s accuracy. Forecasters produce a whole slew of predictions every day, and those predictions can be checked against hard drives full of weather data. The problem is how best to put the two side by side to see how good the forecasts are. “A lot of the standards we use were developed more than 100 years ago,” says Barbara Brown, an expert on forecast verification based at the US National Center for Atmospheric Research in Boulder, Colorado. “It’s really sad.” It’s time, she says, for meteorologists to put their house in order – something she hopes to work towards this month when meteorologists from around the world will gather in Reading, UK, to talk about methods of forecast verification. At the moment, odd as it may seem, the best way forward may be to go back to the “warts and all” way forecasts were presented 100 years ago.
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“The best way forward may be to go back to the 100-year-old ‘warts and all’ approach”
Forecasting the weather is a huge undertaking. The computer programs that provide the raw materials for modern weather forecasts employ complex arrays of equations that take a set of initial conditions – variables such as air pressure, temperature, ocean current speeds, humidity and so on – and use theories such as fluid dynamics and thermodynamics to work out what sort of weather those initial conditions will evolve into after a given time. To make accurate predictions the information has to be gathered from as many points on, above and below the surface of the Earth as possible.
However many weather stations you have they will never be enough. The famous butterfly effect of chaos theory, which can turn a tiny air movement in one part of the globe into a storm thousands of miles away, is all too real: minuscule errors or omissions in the initial conditions can blow up into hugely erroneous forecasts. That chaotic behaviour is why two and three-day forecasts are so much more reliable than five-day forecasts: those extra few days are enough for the weather at a given location to develop in a completely different way.
If two or three days doesn’t sound like much, consider that in FitzRoy’s day, when little more than personal experience was available to turn weather data into forecasts, a one-day forecast pushed the limits of what was possible; it was an attempt at a two-day forecast that was FitzRoy’s undoing.
Forecasting has moved on a very long way since then. Ever more powerful supercomputers are ingesting ever more detailed data from satellites and weather stations as the initial conditions for their calculations. Over time, our understanding of the processes behind the weather – the way oceans and the atmosphere interact, for example – has improved, making computerised climate models more realistic. FitzRoy’s brainchild, now called the Met Office, claims its three-day forecasts are now as accurate as its one-day forecasts were 20 years ago. That doesn’t mean, however, that all the forecasters’ predictions are useful.
Indeed, when it comes to longer-range predictions looking months ahead, some experts doubt there is any value to them at all. In December, Pascal Mailier, a meteorologist at the University of Reading, told an audience of European energy-industry executives that when they buy certain long-range predictions to assess future energy demand, they might be wasting their money. The Met Office, for instance, sells long-range forecasts as well as providing public information. Last July it issued its early predictions for the British winter, based on temperature measurements in the North Atlantic Ocean. This “NAO signal” is supposed to give an indication of whether the winter will be wet and mild, or dry and cold. Mailier’s analysis says those who bought this information might have been better off saving their cash and just casting their minds back a few months: it is just as instructive to assume that this winter will be the same as last year’s, Mailier says.
Keith Fenwick, a forecaster at the Met Office, disputes Mailier’s analysis. The NAO signal is more complex than Mailier makes out, he says, and provides more information than a simple persistence forecast can. It can, for instance, make good predictions of year-to-year changes in winter surface temperatures.
Not all assessments of forecasting skill are so contentious, but they are still largely subjective, as forecasters assess themselves using whatever criteria they choose. The Met Office, for example, uses something called a numerical weather prediction (NWP) index. This starts off with a set of “skill scores”, which gauge how well a forecast compares with weather-station measurements of rainfall, surface temperature, visibility, total cloud cover and wind. The assessors then combine the skill scores for each of these parameters into one result for each month’s forecasts for the climate model they are using.
The monthly score does not provide a good measure of success by itself. Local effects at the weather stations create huge variations, says the Met Office’s Simon Fuller. That’s because, in order to get forecasts out in a reasonable time, the weather computers operate on a limited resolution: they give single predictions for the rainfall, wind speed, temperature and air pressure for a region of, say, 4 square kilometres, because it would take too long to calculate more detailed forecasts. The forecasters know that the weather will vary in microclimates across that area: a farm in the shelter of a hill, for instance, might get less rain than is forecast for the whole region on a particular day. Only by averaging out the observations over a long period can you get a true reflection of the accuracy of the predictions, and if you smooth the anomalies out across 36 months, Fuller says, you can see that the overall forecast skill is improving steadily (see Graph).
Not all meteorologists are convinced that the NWP index is a good measure of short-range forecasting skill. Though it gives some indication of how things are going, the NWP index is “a bit simplistic”, says Beth Ebert of the Bureau of Meteorology Research Centre in Brisbane, Australia. She thinks measuring the accuracy of a forecast requires taking its end users into account: airports need accurate fog measures, for example, rather than accurate measures of sunshine; hurricane forecasters need to know wind speeds and the location and timing of landfall, rather than cloud height.
The truth is, she says, there isn’t a straightforward way to assess how forecasters are doing – but try telling that to a forecaster’s boss. “People prefer a short answer,” Ebert says, “even when the short answer is clearly inadequate.” It can be worse than inadequate, too – the pressure to meet an oversimplified “accuracy” target can change the way forecasters interpret their data, altering the prediction. “It can warp the forecasting process,” says meteorologist David Stephenson at the University of Reading. That’s because forecasters can improve their numbers by “hedging”, he says: not making forecasts based on what their models actually predict, but arbitrarily reining in any perceived extremes, blurring the location of a weather front, or reducing the probability of rain from 50 per cent to 20 per cent. All these moves can improve a forecast’s verification scores – and, at the Met Office, a forecaster’s annual bonus – but they will also make it less useful.
Head in the sand
There’s another, less cynical reason why forecasters sometimes don’t pass on what the computer says: because we don’t want to hear it. Television forecasts, for example, rely on phrases such as “scattered showers in the west” and “windy in the north-west later”. But think about it: what do these phrases mean? “Windy in the north-west later” might be a simplification of the computer’s prediction that “at some time in a 12-hour period mean wind speed at station A in the north-west will exceed a specified threshold”; “frost is likely” may mean “the probability of frost exceeds 70 per cent”. The trouble is, no one wants to digest those details over breakfast, so they are boiled down to a set of vague predictions. Unfortunately, the media-issued forecasts most of us run our lives by are so vague they are “impossible to verify with objectivity”, according to a report published last year by the UK’s Royal Meteorological Society. “Any claim for skill of descriptive forecasts should be treated with scepticism,” the authors say.
“The media-issued forecasts most of us run our lives by are so vague they are impossible to verify with any objectivity”
To make that scepticism melt away, TV forecasters could start by doing a very simple thing: embrace uncertainty and start giving us a precise indication of their confidence. “Uncertainty is… a fundamental characteristic of weather,” says a report issued by the US National Research Council late last year. “No forecast is complete without a description of its uncertainty.”
The report recognises that things have got worse, not better, in this respect. In FitzRoy’s time, some forecasts were called “probabilities”, and included specific information on uncertainty. Not any more. “Decisions by users at all levels, but perhaps most critically those associated directly with protection of life and property, are being made without the benefit of knowing the uncertainties of the forecasts upon which they rely,” the report says. The US National Weather Service now recognises that being clear about uncertainty has to become a fundamental part of its forecasts again.
The point, after all, is to give forecast information that helps people make decisions. It’s not that TV forecasts are useless; for most people they are a valuable guide to the next day’s weather. However, that value would increase dramatically if the forecasters were willing to add an indication of probability alongside a prediction. Should you take your umbrella out with you in the morning? You get a much better idea of the answer from “there is a 70 per cent chance of rain” than “there is a chance of some rain”.
Forecasters have been reluctant to go down the probabilistic route, though. Ten years ago, a study led by J. Frank Yates of the University of Michigan, Ann Arbor, showed that the general public viewed people giving a probabilistic forecast as incompetent, ignorant or even lazy (International Journal of Forecasting, vol 12, p 41). A 50 per cent chance of rain, for instance, gets misinterpreted as “I don’t know what the hell is going to happen tomorrow.”
“There is a misconception that a 50:50 probability is complete ignorance,” says Met Office meteorologist Mark Roulston. That’s only true if you know the event you’re talking about occurs exactly half the time, but if it normally occurs less frequently, then being told there’s a 50:50 chance is telling you there’s been an increased likelihood. So, a 50 per cent chance of rain is worse than, say, a 10 per cent chance; without this information, making a decision based on the chance of rain is like placing a bet at the bookies without knowing the odds.
The National Research Council report makes a similar point, but says that forecasters will just have to live with any accusations of ignorance: they have been getting away with an unjustifiable air of certainty for too long, anyway.
Roulston is now working with psychologists at the University of Exeter, UK, to establish how uncertainty information might best be presented. He has been watching people play games in which they pretend to run a road-gritting company. The grit costs money but the local authority will fine the company if it fails to grit when the temperature falls below freezing; the company profits depend on good weather forecasting. Roulston’s results show that being equipped with a temperature forecast plus its margins of error puts the user at a great advantage. Adding in the probability that the temperature will fall below freezing makes little difference: the margins of error are enough, it seems (Weather and Forecasting, vol 21, p 116).
Unscrupulous forecasters
Of course, providing explicit information about the uncertainty of a forecast is a dangerous thing in an unregulated market: what if the utilities company or supermarket is approached by a forecasting service that offers a lower error level or – something that no one can do honestly with any accuracy – predictions out to 10 days? Might unscrupulous companies be tempted to claim a higher-than-realistic accuracy? The answer, from current experience, is yes. “There are companies here in the US that offer 10-day forecasts, updated hourly,” Brown says. “It’s nuts – but people do buy them.”
Perhaps that’s why some forecast providers are averse to a big, open discussion of forecast verification and quality issues. In the course of their research Stephenson, Mailier and two of their Reading colleagues issued questionnaires to organisations providing forecasts, and asked them to forward the questionnaires to the people who used their forecasts. Many simply refused to take part. “Forecast providers and their users have rather intimate, special relationships,” Stephenson says. “I am not sure all the providers want their users to know that there are better providers or how to judge and criticise the forecasts.”
Whatever the truth, all kinds of prediction may be about to get even more difficult, thanks to climate change. Though no one is sure exactly what the effects will be, it seems that extreme weather events such as storms and hurricanes are likely to become more common, in many parts of the world (èƵ, 20 January, p6). Such events have far-reaching effects on distant weather systems, making general forecasting much harder. Though our models are getting better and satellite data is more comprehensive and accurate, we may soon be like the Red Queen in Alice through the Looking Glass, running to stand still. For forecasters, the only answer will be to go back to the way forecasting was done in FitzRoy’s day: with doubts and disclaimers. All the weather satellites in space, it seems, can’t compensate for some good old-fashioned honesty.
