Marine Weather forecasts need to be interpreted to make informed, localized decisions on the day.
Most of us nowadays, depend for our forecasts on National Meteorological services.
However, these services can rarely predict local conditions exactly.
And much of the weather that affects leisure sailors tends to be rather small scale.
We should also re-learn how to read the physical weather signs which our modem life has left us out of touch with.
putting out to
sea, especially in small
boats needs to understand how best to use and understand marine weather
Getting the forecasts is
not a problem, the
mainstream media issue general predictions, marine forecasts, including
marine weather warnings, are broadcast on radio by coastguard and other
agencies. Marine Weather
However, none of them
And large bodies of
water and indented
coastal areas can be susceptible to highly variable local weather
In order to interpret forecasts and adapt them to local conditions you will need to recognize the limitations of the various types of forecast and have a basic grasp of meteorological knowledge.
The first job is to know
what marine weather
forecasts are available and appropriate for your area.
The mainstream media
forecasts are very
general and cover large areas and are more concerned with the
land, however they can be used to get a feel for general weather
Local marine forecasts
are updated several
times a day, but even Inshore Waters Forecasts are predicted in general
rather than in detail.
There are different ways
in which forecasters
interpret the data.
Short term forecast,
such as those for the
next 24 hours, are normally the result of a human forecaster using his
experience to interpret the output from computers.
Longer term forecasts
tend to come straight
from computer modeling.
And how the initial data
is processed and
modeled can differ between the various centers.
So while some boaters
have their favorite
source of forecast information it does pay to look at several forecasts
arrive at a consensus view.
Then, adding your own
personal experience and
knowledge of local conditions you will be able to make more useful, if
necessarily accurate, short term decisions.
Weather forecasts can be received at sea using RTTY, Navtex and Radiofax.affiliate links
know the basic
used you will be able to interpret the broadcast information in a more
Since the establishment
in 1853 of the
International Meteorological Organization, now known as World
Organization the units used for wind
speed, pressure and wind direction
Synoptic pressure charts
are also a
standardized method of showing large scale atmospheric pressure
Being able to use and interpret synoptic charts is another invaluable way to get a feel for the way the weather is developing.
Barometer is one of those instruments, which like the magnetic compass
little or no maintenance, no external power and yet can be of immense
those on board.
Barometric pressure and
its tendency to
change is the basic information that forecasts are based upon.
Barometric data collated
from a network of
weather stations are used by forecasters to create synoptic weather
By drawing Isobar lines
between points of
equal pressure on a map or chart a contour map showing variations in
When this is combined with wind and other observations and the changes over time are observed, reasonably accurate forecasts can be made.
The aneroid type of barometer which is most commonly found on small boats provides a valuable indication pressure tendency, forecasting short term changes in the weather.
Generally high pressure
is an indicator of
fair weather while low pressure means that storms are more
it is the
movement, the rising and falling and the rate of change which is more
to the seafarer and is why barometer reading are normally recorded in
large change in pressure
will not only herald a large change in weather it will also mean an
the wind strength.
A drop in pressure is a
sign of a low
pressure system approaching bringing with it a good chance of
On the other hand a rise in pressure will generally accompany clearing skies and an improvement.affiliate links
were to combine
all the information
from the latest computer forecasting output with our own observations
today’s marine weather we should be able to accurately predict the
conditions for the following few hours.
Many of these smaller
localized features are
too small to be resolved by the computer models.
So for the small boater
there is considerable
benefit in being aware of how just observing sky conditions can be used
Unfortunately our modern
reduced our awareness of and feel for the natural signs and indicators
change in the atmosphere.
centuries folk have
been using the
simplest of methods for forecasting tomorrow conditions upon their
of today’s conditions.
Many of the sayings
lore that they used while being based on simple observation
do have a basis
in scientific fact.
And quite often the folk
who relied on them
were seafarers whose very lives depended on them.
So, rather than
dismissed these old sayings
as meaningless perhaps it is time to reassess them and use them as a
our own observations.
I'm sure everyone is
familiar with the saying
"red sky at night, sailor's delight, red sky in the morning a sailors
warning” but there are a host of others which are worth
For the coastal sailor
the effect on the
prevailing marine weather caused by the local topography can be
Wind speed, for example, can dramatically increase and be deflected
prevailing direction as it is funneled through narrow channels.
Even along open stretches of coastline the wind direction can be
Cliffs can produce localized turbulence, and the gust form an
direction can be caused by valleys or clefts in the cliff face.
Any coast fringed by high ground will be subject to localized phenomena
Wind over tide can cause short steep waves.
And sea breezes will modify the prevailing conditions depending on the
A good sense of observation will help you keep track of weather shifts
But predicting the affects of local conditions on Marine Weather requires an understanding of how and why these variations are produced.