2 Atmospheric Pressure Y

meteorolog 2 Atmospheric Pressure y 2.1 Definition and Pressure 2.1.2 The Mercury Barometer Measurement The Italian physicist Torricelli invented the Mercury barometer in the 17th century, 2.1.1 Definition see fig. ME 2.2. Pressure acts in all directions, up and sideways as well as down, but it is convenient in meteorology to regard atmospheric pressure as the weight of an air column acting on unit area, see fig. ME 2.1. Vacuum Pressure at this level = W Column of air A with weight (W) Atmospheric Atmospheric pressure pressure Surface area (A) Mercury column Fig. ME 2.1 Atmospheric pressure Fig. ME 2.2 Mercury barometer The units of pressure are Force divided Atmospheric pressure forces mercury to rise by Area (or Force per Unit Area N/m2 in an evacuated glass tube. or Pa (Pascal)). The unit of pressure in meteorology is the hecto Pascal (hPa) which The unit of pressure was then mm Hg (Hg replaces the millibar (mb) which was in use is the abbreviation for mercury). This unit in former times. However the units are of has been replaced by the SI-unit hecto identical magnitude, therefore: Pascal, hPa. 1 mb = 1 hPa The reading of a mercury barometer has to be manually corrected for the temperature of the mercury column and gravity at each site. Atmospheric Pressure 2-1 meteorolog 760 mm Hg = 1013 hPa variations. This is used to provide a meteorologist with the pressure tendency, or In the USA barometric pressure is still rise and fall of pressure over time and is an y measured in inches Hg: important forecasting tool, see fig. ME 2.4. 29.92 inches Hg = 1013 hPa. Amplifying Protective case Record paper 2.1.3 Aneroid Barometer levers on cylinder The aneroid barometer consists of a flexible metallic capsule which is partially evacuated. Noon 10 8 6 It compresses under small increases in air 1020 1015 pressure and the capsule compression/ 1010 expansion is converted by a lever system to 1005 1000 drive a pointer on an amplified scale. It is a 995 much more convenient and portable system than a mercury barometer, see fig. ME 2.3. Aneroid cell Ink trace Graduated scale Fig. ME 2.4 Barograph 2.2 Pressure Reduction to Mean Sea Level and Pressure Systems Lever 2.2.1 Pressure at the Surface system QFE The atmospheric pressure measured on a Aneroid capsule barometer at an airfield is known as the QFE or Aerodrome Pressure. Fig. ME 2.3 Aneroid barometer The QFE varies widely, both from day to day and place to place, due to variations in the 2.1.4 The Barograph weight of the air column above the surface The barograph is an aneroid barometer used in conjunction with a recording drum. 2.2.2 Pressure at Mean Sea Level Instead of a needle and graduated scale the QFF lever mechanism moves a pointer which Since QFE is measured at station level, it is leaves an ink trace on a scaled recording not immediately usable for meteorological paper wrapped around the drum. This purposes because of the differences in leaves a permanent record of the pressure altitude of the observing stations. In order to 2-2 Atmospheric Pressure be usable in meteorology all pressures need meteorolog to be measured at the same level. Therefore QFE values have to be adjusted to Mean C 952 894 A 979 Sea Level (MSL) and the adjusted pressure is Sea level Sea level y B D known as QFF. 600 m 1100 m 1000 300 m A In temperate latitudes QFF varies between +60 hPa +30 hPa +110 hPa +0 hPa 970 hPa and 1030 hPa, but occasionally N A B C D pressure falls as low as 900 hPa or rises as W E high as 1060 hPa. 1012 hPa 1009 hPa 1004 hPa 1000 hPa B S In different countries different methods 1012 1008 1004 1000 1015 1007 998 are used to calculate this QFF. Sometimes 1009 1004 the method is dependent on season. All 1012 1002 1000 1013 1006 1003 methods use the observed temperature at the station and some type of assumed C Isobars temperature profile down to or up to sea level. In meteorology this is called reduction. Fig. ME 2.5 Surface isobars Once reduction is done, all points with the same QFF can be joined up with lines of constant pressure referred to as isobars. Pressure Patterns Revealed by the Isobars are: 2.2.3 Pressure Systems Anticyclones or Highs In order to forecast weather it is important These are regions where the pressure at its to know the distribution of pressure at mean centre is highest relative to its surroundings. sea level. The circulation is clockwise in the northern hemisphere and anticlockwise in the Isobars are usually drawn at intervals 1, 2, 4, southern hemisphere. 5 or 10 hPa, the custom varies with latitude and country. Local barometric pressures at Ridge or Wedge observation stations (QFE) above sea level A region of isobars extending away from a are adjusted for the difference in height high centre. Pressure along the line of the to bring them all to a common datum, ridge is higher than its surroundings. normally Mean Sea Level (MSL) to enable a chart of pressure distribution to be drawn Depressions or Lows (or Cyclones) known as a synoptic chart. The adjusted These are regions where the pressure at its MSL pressures are known as the QFF, centre is lowest relative to its surroundings. see fig. ME 2.5. The circulation is anticlockwise in the Atmospheric Pressure 2-3 meteorolog northern hemisphere and clockwise in the atmosphere as the weight of the air column southern hemisphere. above reduces. How much it reduces depends upon the gravitational acceleration y Trough and density of the air column, see fig. ME 2.7. A trough is a region of isobars extending From fig. ME 2.7 it can be seen that the most away from a low centre and may have sharp curvature. Pressure along the line of the trough is lower than its surroundings. Above 99.9 % 50 1 hPa Col A col is a region of nearly uniform pressure 40 situated between a pair of highs and a pair 5 hPa Above 99 % of lows. 10 hPa 30 25 hPa Wind circulation around pressure systems is 50 hPa 20 usually along the isobars, see fig. ME 2.6. Above 90 % Altitude (km) 10 Above 50 % 1008 1011 Mt. Everest 1005 1014 0 1011 1002 1017 0 100 300 500 700 900 Pressure (hPa) H Fig. ME 2.7 Variation of pressure with height 1008 1017 Col L 1014 1002 rapid decrease in pressure with height is in 1005 1008 the troposphere up to about 500 hPa at which Ridge Trough point about 50% of the atmosphere is below this level. The rate of pressure decrease with Fig. ME 2.6 Wind circulation around pressure systems height begins to decrease significantly as one approaches the tropopause. The pressure will of course be determined by the density of the 2.3 Vertical Pressure Distribution air above. 2.3.1 Variation of Pressure with Height Table ME 2.1 shows the height change at various altitudes for a pressure change The pressure at any level in the atmosphere of 1 hPa. is equal to the weight of air column above a surface of 1m2. It follows therefore that pressure must reduce with height in the 2-4 Atmospheric Pressure meteorolog Height Height difference for same height and surface pressure. If one a change of 1 hPa column is cooled while the other is heated, MSL 27 ft the colder column will be more dense and 18 000 ft (500 hPa) 50 ft contain less air above the fixed datum of y 39 000 ft (200 hPa) 100 ft 10 000 ft. The warm column will expand, decreasing in density and pushing more air see fig. ME 2.8. Table ME 2.1 Height variation for 1 hPa pressure change at above the fixed datum, various heights The pressure at 10 000 ft in the cold column 2.4 Atmospheric Density will therefore be less than the pressure at 10 000 ft in the warm air column. This will 2.4.1 Density create pressure differences aloft and result in Density is defined as mass per unit volume, winds aloft. expressed in kg/m3. When air is heated it expands, and the same mass (or weight) The rate of decrease of pressure with height occupies a larger volume and so density is therefore greater in the cold air than in becomes less. As pressure decreases with the warm air, so at any height above the height the density of the air is decreasing surface the pressure aloft will be lower in as well. This will also be dependent on the the cold air than in the warm air. temperature of the air as warm air is less dense than cold air and warm columns of air will be taller than cold air columns. Assume two columns of air both have the 500 hPa 8 800 ft 8 000 ft 700 hPa 7 200 ft 10 000 ft 11 000 ft 10 000 ft 9 000 ft 1000 hPa Warm/low density Cold/high density Fig. ME 2.8 Density variations Atmospheric Pressure 2-5 meteorolog 2.4.2 Density of Dry and Moist Air change of 27 ft for 1 hPa pressure change, As stated earlier, dry air is made up of 78% and 50 ft at 500 hPa.

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