Atmospheric Pressure Flashcards
What are the equivalents of 29.92
29.92 =
- 1 Atmosphere
- 101.325 kpa (kilopascals)
- 1013.25 mb
What is Station Pressure?
The actual weight of the column of air extending upwards from the station to the outer limit of the atmosphere of the observing station
It is what you read without any corrections.
Why can’t meteorologists use station pressures when drawing out maps for areas and high and low pressure?
Because as the elevation of the terrain rises from sea level, the pressure changes. So a station at sea level could be in a high pressure area while a station at 2000 ft, in the same high pressure area, would be under half as much pressure.
It would make it kind of impossible to have defined borders around areas of pressure because of all the fluctuations in elevation changing that pressure.
So meteorologists correct for elevation, to bring all areas to Mean Sea Level/Sea Level (MSL)
How do meteorologists correct for elevation in pressure altitudes/systems?
Remember that:
- One inch of mercury is lost for every 1000ft of altitude gained
- Air density/pressure is affected by temperature. An imaginary column of warm air between SL and the station will exert less pressure than one of cold air
They take the station pressure and add one inch of mercury x the elevation of the station from sea level. For the temperature correction, they use the average surface temperature over the last 12 hours to create this imaginaaaary column of air
If a station is located at 5000ft elevation with a pressure of 25.00 inches, what would it’s MSL be?
30.00”
What are Isobars?
If we were to take a plotted chart of sea level pressures, we could then connect the areas of equal pressure
Iso = the same
bar = connecting line
Isobars are usually spaced 4 millibars apart
In the picture below, in the high pressure system, the pressure is indicated as 1013mb, which is quite close to the standard (1013.25mb). Why is it marked as high pressure if its almost at standard?
Because on weather maps the pressure regions are relative to one another.
In the picture, the low pressure area is 1001mb, which compared to 1013, is quite a bit lower. This makes the other one higher in comparrison
High and Low pressure systems are not compared against ISA, they are based off of each other
What way do the winds move around high and low pressure areas?
Low: Counter-clockwise
High: Clockwise
Winds also move from high pressure to low pressure to tryto equalize. From the top down view this kind of looks like turning gears
What are Pressure Gradients on a weather map and why are some closer together or farther apart?
Pressure gradient is how the pressure changes between pressure systems.
When isobars are closer together (strong pressure gradient): the pressure is changing faster, which means the air is moving faster/its more windy
When isobars are farther apart (weak pressure gradient): the pressure is changing less quickly and the winds are less strong
Pressure Gradients can be thought of like topographical maps.
Why does pressure change horizontally?
High pressure areas are heavy, they sink and spread out along the ground and shove in to lower pressure areas, pushing them up. Which is why low pressure areas ‘rise’.
Conversely, warm are that is rising will tend to create areas of low pressure, while areas of cooler and denser air will sink and compact, creating areas of higher pressure.
What is the air doing in and around an area of high pressure?
- Air is sinking in high pressure areas.
- Air is rotating clockwise and flowing outward from the center (only in the norther hemisphere, in the soutern it would be the opposite)
** Areas of High Pressure are also sometimes called anticyclones
Some more info about Highs
- High pressure areas can be caused by a drop in temperature. As temp drops, the air density increases and will tend to sink.
- This will tend to push clouds and weather and shit out of the way. So areas of high pressures are associated wit clearer weather/skies
- High pressure systems tend to stick around for several days
**Rememeber that a high pressure system has descending air flowing in a clockwise direction
Some more info about Lows
- Lows are areas of rising air that is flowing counter-clockwise and inward towards the center.
- Also called cyclones
- Tend to bring crappy weather, as the air is rising and cooling, creating all kinds of bullshit
- Lows are also assimilating air from the highs, producing stronger winds
- Unlike Highs, Lows tend to move on/blow by after a day or two. Faster in the summer than the winter.
What is a trough?
- An elongated area of low pressure
- Indicated by a purple line on a weather map, usually sitting in the V of isobars (see picture below)
- Troughs are likely to bring about a wind shift at the surface as well as clouds and weather, particularly following the passage of the trough
- Fronts always lie in troughs