So, how can we tell a bad meteorologist from a good meteorologist? I can’t imagine how a weatherman asks his boss for a raise: “Weeeeell, the accuracy of my weather forecasts is now solid 40% compared to miserable 32% when I was a rookie five years ago - so I really deserve that raise”
Is the person reading out the weather on the news actually a meterologist? I always thought they got their data from some centralised source and just parroted out the results. In fact, come to think of it, it would be a perfect job to outsource.
Sometimes it is, and sometimes it isn’t. I remember the weather guy on the news my parents watched when I was a kid was a real meteorologist since it turned out he knew a friend of my parents who was a professor of meteorology.
Well, not all the mathematicans are sitting on their sliderules.
Again, this is really marginal improvement. You simply can’t get any better in air pressure than an error of about 100,000 times your measurement error within two weeks time, and that’s about the best-behaved weather equation there is.
Sorry for bumping a month-old thread, but I don’t visit here too often, but when I do it’s in spurts. Anyway, I wanted to add some additional thoughts as a resident meteorologist. Some very good points were raised and cited.
The main reason that medium range forecasts (past a couple of days) is not as accurate as one may hope is due to relative lack of data, and the relative primitiveness (is that a word?) of the numerical models we use. Yes, some of the models we now use are very high resolution (with grid points less than 10 km on many of them), but that doesn’t necessarily help at some point. Our upper-air observing stations are on average about 300 miles apart. These are the stations that launch balloons twice a day for a full cross-sectional sampling of the atmosphere. Other forms of data are helping out, which include satellite-based samplings (huge positive effect of being able to sample tons of different points).
Anyway, even if the data problem is solved, even with a fine-scale model, lets assume say 10km. The model will not be able to capture any feature that is less than 20km in diameter. Local effects such as rain bands, individual thunderstorms, lake, can’t be modelled at this point in time. Granted, through parameterization (which I’m not sure of the details of, but can find out if anyone is really interested), we can make the model output better, but the model still can’t do everything.
Finally, as has been mentioned, the chaos of the atmosphere is the last reason. There are so many things happening on the order of tens of meters (from local fluxes, turbulence, gravity waves, etc. that are extremely difficult to model, and must be parameterized to try and capture them). Take these out 3-4 days, and it’s no wonder that local effects can seem way off.
All that said, our experience with large-scale weather patterns is very good. We have the same accuracy now at 6-7 days that we did maybe 15 years ago at 2-3 days (I’m sure these numbers aren’t exact, I’m a bit rushed for time, but I can find something if needed). We are now forecasting hurricanes with the same accuracy at 4-5 days that we did at 2-3 days 10 years ago. As computer power continues to progress exponentially, we will continue to see better forecasts, and as data retrieval techniques combined with higher resolution modelling get better, we will see much better forecasting of smaller-scale effects.
Just a comment on chaos, for those with only a pop-culture knowledge. This is true no matter how fine the scale is.
If the current technology has a resolution of 10km, then smaller features than that can’t be seen. If you make an assumption (and you have to) about how it behaves in there, your error will be smaller than 10km. This will blow up relatively quickly and completely throw off your calculations no matter how accurate your model is.
Now, it’s easy to see how being off in a 10km sample outside New York City will make it difficult to see what’s going to happen next week in Boston, but when you really realize that being off in a single 10km sample in Hollywood throws off all the calculations for the entire United States within a relatively short period of time you really get an idea what “chaos” means.