By Dag Pike
This is a booklet approximately functional climate forecasting, and it starts off the place such a lot different books end. climate forecasts offer you loads of information regarding the elements to return yet they typically pass over many of the aspect, and the timing of alterations can be obscure. during this ebook, Dag Pike exhibits tips to translate the fundamentals into useful climate forecasts that you should determine what it is going to be like on your zone and alongside your proposed direction. Sailors can be in a position to make larger use of the to be had wind and keep away from tough parts, while powerboat drivers extra attracted to the ocean stipulations might be capable of finding the smoothest waters for a greater ride.
With assistance from this e-book, readers will decide up specialist suggestions such as
50 how you can increase Your climate Forecasting distils Dag Pike's...
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This can be a e-book approximately useful climate forecasting, and it starts off the place such a lot different books end. climate forecasts provide you with loads of information regarding the elements to return yet they typically omit many of the element, and the timing of alterations can be obscure. during this publication, Dag Pike exhibits tips on how to translate the fundamentals into sensible climate forecasts so you might figure out what will probably be like on your sector and alongside your proposed direction.
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Additional info for 50 Ways to Improve Your Weather Forecasting
This surge effect is likely to be felt in strong winds that have been blowing from the same direction for some time and, even if there are not strong winds in your area, winds within 160km (100 miles) or so could cause this surge effect. There can be lower than predicted tides when the wind is flowing against the tidal stream. The other cause for the tidal surge is that the stronger winds will often be associated with a depression or low-pressure area, giving the tides more freedom to rise higher because the atmospheric pressure is less.
The airflow will usually follow fairly closely the lines of the isobars, tending to flow more into the centre of a low pressure than along the direct line of the isobar. In assessing the weather, it is mainly the variations in the distance apart of the direction of the lines that are important. Closely packed lines will indicate strong winds, and when they are wide apart you can expect weaker winds. Variations in the direction of the isobars could indicate the location of a front, when you can expect a change in wind direction.
This is covered in more detail in the chapter Local weather conditions (see here) and will certainly give you a better idea of what is going on, particularly if there is a frontal system passing through. However, it isn’t likely to give you much idea about wind strengths and the timing of changes – you need to rely on the forecast for that. You should also consider the effect of tidal flow changes – while the main effect will be on the waves, strong tides can affect the wind strength as the water flow drags the surface wind along.
50 Ways to Improve Your Weather Forecasting by Dag Pike