Barometers
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references. There are many more links, too.
Barometer
Your barometer was
designed to give the user accurate air pressure readings from sea level to an
altitude of 7000 feet. Before leaving the factory your barometer was
calibrated to standard air pressure at sea level. For your barometer to
give you optimum results, you will have to recalibrate it to your local
barometric pressure before use.
Locate your barometer in an area where it
will remain undisturbed. Do not position it in direct sunlight, as this
could cause inaccurate readings.
You need to calibrate your barometer to
your location. This can be done by getting the pressure from a local
radio or television station. Use a small slotted screwdriver to turn the
small screw on the back of the barometer case to adjust your barometer until
the black pressure indicator hand points to a reading that corresponds to your
known local barometric pressure. Your barometer has now been
calibrated. For daily operation of your barometer, place the gold pointer
attached to the lens directly over the black pressure indicator hand.
This will allow you to measure any change
in pressure that may have taken place. It is the amount of change in
pressure and the rate of that change that will be an indicator of the weather.
The following basic rules apply in
using the barometer to predict weather conditions:
·
A fast rise in barometric pressure means good weather of short duration.
·
A rapid drop in barometric pressure means disturbances nearby - showers of
short duration.
·
Regular elevation of barometric pressure usually will indicate clear, dry
weather conditions (cold and dry in the winter)
·
A drop of 2-3 tenths of an inch per 24 hours indicates a depression some
distance away.
·
Drops of 1-2 tenths per hour means disturbances near by, of short duration
·
Steep drops of 6-10 tenths within a 4-5 hour period indicates coming rain and a
storm with strong winds.
How do I adjust my barometer? (FAQ - Pressure)
The answer to this question depends on the type of barometer in question,
particularly whether its pressure sensing mechanism is influenced by gravity or
not, and what you are trying to get it to measure - the air pressure
immediately surrounding the barometer or the pressure at another height, such
as mean sea level.
Altitude effects
All barometers, whether they are mercury-filled, aneroid or
other designs, are affected by altitude because atmospheric pressure reduces
with vertical distance from the Earth. If a barometer is moved upwards from
nominal sea level its readings should reduce roughly by 1 hPa (1 mbar) for
every 10 metres increase in altitude but note that the rate-of-change of
pressure with altitude itself reduces significantly and non-linearly with
altitude.
Mercury barometers are doubly affected by altitude because
their readings (ie the length of their mercury columns) are also dependent on the local value of gravitational
acceleration - which itself reduces with altitude - to which they are
subjected. A gravity correction
is undertaken separately from and in addition to altitude-induced direct
pressure effects and is described below.
All barometers measure the pressure at the level of their
internal sensor - the surface of the cistern mercury in the case of a mercury
barometer. They do not measure the pressure at sea level, as is sometimes
implied, unless they happen to be at sea level. For weather forecasting purposes,
however, and to enable pressure values at different locations to be compared,
pressure values issued by weather forecasters are usually mathematically
corrected to an arbitrarily agreed datum height - mean sea level. In other
words, the pressure values published or broadcast are not those directly
measured by barometers - which are rarely sited at sea level - but rather the
pressure values that those barometers would have measured had they been sited
at (ie mostly lowered to) sea level.
So if your barometer is not sited at sea level and you wish
to compare its readings with weather forecast values you will first need to
calculate and apply an altitude correction. This is in addition to the gravity-related height issue applicable to
mercury barometers mentioned above and it is a bigger and more significant
correction too.
With rare exception, mercury barometers cannot be adjusted
for altitude - their scales are fixed and the correction has to be applied by
calculation. (The exception was a 1940s instrument which incorporated a
mechanical computer with a latitude adjustment that automatically calculated
the corresponding value of g
and varied the barometer's pressure readings accordingly. Even this instrument,
however, did not compute pressure values corrected to sea level.)
Some domestic aneroid barometers have a scale or pointer
whose position and hence reading can be adjusted. This is a fairly crude
method, adequate for relatively inaccurate domestic purposes, that allows an
instrument's readings to be 'offset' to bring them in line with those of a
pressure value from a trusted source. If that value is itself corrected to sea
level then the subsequent readings of the barometer similarly will be those
that it would have indicated had it been at sea level. It should be stressed,
though, that this adjustment procedure cannot ensure that the barometer will
change its readings in line with changes in atmospheric pressure; indeed it
cannot show whether the pressure-sensing element or other parts of the
mechanism are broken or not. Proper calibration of barometers can only be accomplished
by direct pneumatic connection to an appropriate pressure standard and
adherence to well defined procedures that include pressure-cycling.
If your barometer's pressure sensing mechanism is one that
is not significantly influenced by changes in the value of gravitational
acceleration (ie most non-mercury barometers), it is functioning properly and
you are interested in the pressure at the location of the barometer (rather
that at sea level) there should be no need to make any adjustments when you move
it to a different height.
Temperature effects - non-mercury barometers
Temperature affects all instruments to some degree but most
non-mercury barometers are designed to be compensated, to a reasonable degree,
for variations in temperature - provided that ambient temperature does not go
outside prescribed limits or change too quickly.
Temperature and gravity corrections - Fortin
and Kew Pattern mercury barometers
Each reading of a Fortin and Kew Pattern mercury barometer
has to be corrected for the local value of gravitational acceleration, g, and the temperature of the
instrument at the time of the measurement. Changes in the value of g cause a directly proportional
change to the barometer's readings. Temperature variations affect mercury
barometer readings because the materials from which they are made - generally
steel, brass, mercury and glass - have very different coefficients of thermal
expansion and there are no built-in compensating elements. (See How do I use a Fortin or Kew Pattern
barometer?)
Standard conditions
Since 1955 mercury barometers made in the UK have been
designed to measure pressures directly in their respective units when subjected
to standard conditions, viz 0
°C and gravity 9.806 65 m s-2. The size of the corrections needed to
take into account the actual temperature of the instrument and the acceleration
due to gravity at the place of observation are not small and may amount to 0.5%
of the reading (5 hPa) - see BS 2520 :
1983, Barometer conventions and tables, their application and use. This
error is in addition to other effects caused by non-perfect operation of a
barometer. Proper pressure readings depend on barometers being in good
condition, properly mounted in a thermally stable environment and provided with
adequate temperature measuring facilities. (See How do I use a Fortin or Kew Pattern
barometer?)
Summary
The best and certainly the most accurate way to use a
barometer is to set it up so that it measures its 'local' pressure - that is at
its sensing level - properly; a pressure altitude correction should then be
applied ONLY if a pressure value corresponding to one at mean sea level is
required.
The full procedure would be to:
- read
the barometer (after setting its fiducial point in the case of a Fortin
barometer)
- add
any correction that has been determined from a prior calibration of the
barometer
- apply
temperature and gravity corrections (mercury barometers only)
- IF
REQUIRED, add an altitude correction to give a value of pressure
equivalent to that at mean sea level
If you have a normal domestic aneroid barometer, its
inherent potential accuracy will probably be quite low and the procedural
detail for applying corrections might not make much difference in reality - it
might be more convenient simply to off-set its readings by the magnitude of
your local height correction - but don't say I said that.
How do I set my
barometer?
Air pressure decreases with altitude, so if you
live in an elevated location you will have a lower pressure than places at sea
level. The correct local pressure is called Station Level Pressure. It can?t,
however, be compared with Mean Sea Level Pressure. The pressures you see on
Weatherzone have all been corrected to MSLP. It is therefore most useful if you
set your barometer to MSLP. You will then be able to compare your pressure with
the weather charts and observations on the website.
To do this, find your current pressure on Your
Local Weather Page. If there is no observation for the town in which you live,
use the observation for the nearest available station. Set your barometer to
the pressure given. You will be able to move the pointer with a screw in the
back of the barometer. It is not the pointer at the front that you want to
move.
Check your barometer 24 hours later against the
observations to ensure that it has remained calibrated. It should only need to
be adjusted by a small amount, if at all. Regularly check your barometer
against the official readings provided on the website. You should generally do
this during periods of stable weather when the pressure is not changing
rapidly.
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