WX0203 · Pressure & Wind
29 questions · 23 multiple choice · 6 written · ASA 109 Marine Weather — Pressure & Wind
📈 Figure WX0203-1 — surface analysis map
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Isobars are lines of constant surface pressure, shown at equal intervals, usually 4-mb apart.
Higher gradient means isobars are closer together.
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Isobars are drawn at constant pressure intervals across the map.
Widely spaced isobars means the pressure drops slowly, so the wind will be weak.
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Isobars. Generally anything with “iso” in it refers to something that is constant.
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All are equivalent expressions of standard atmospheric pressure.
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This is an official definition used consistently.
Pressure tendency is always given over the past 3 hours.
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Aneroid barometer is the typical kind used at sea.
Aneroid barometers have only the elevation correction. Quality aneroids are constructed to compensate for temperature. B and C apply to mercury barometers.
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The doldrums. The variation is a tidal action of the atmosphere, most prominent in the tropics.
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With your back to the wind, put your left arm out and slightly forward — it points to the low.
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Draw a person standing in the circulation of wind around a low.
Buys Ballot’s law: facing the wind, low pressure is to your right, slightly behind.
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Standard atmospheric pressure: 14.696 psi, 760 mm, 29.922 in, 1013.25 mb.
Millibars (hecto Pascals) are the conventional unit for marine use. Marine weather reports and fax maps use these units.
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Every vessel at sea has one, but are they really used.
It is a crucial instrument. Even an uncalibrated instrument is still of value in detecting pressure changes.
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Question is about “typical,” not records.
The Pacific and Atlantic Highs firm up at about 1025 to 1030 mb.
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Climatic weather data is in the Coast Pilot.
Can’t say. There is no “standard” atmospheric pressure in a practical sense. It varies by location and season.
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Consider the vertical motion of air.
Highs are characterized by light air and clear skies. Air is descending, which evaporates clouds.
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30.05 inches of mercury. On the millibar scale it would read 1017.6. There is no way to tell from a single reading if it is going up or down.
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A consistent pressure drop is a clear warning.
All given answers can contribute. In practice, the Low moving across you is most likely the biggest contributor.
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The pressure difference determines the pressure gradient.
The pressure gradient increases the wind speed, and force of the wind is proportional to the square of the wind speed.
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Use official sources. Any of the other methods could be right but we have no way to know that.
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Assume the barometer itself was all you had to go by.
It is the actual rate and the duration of the change that matters most in forecasting.
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Low pressure brings bad weather. Changing pressure can be good or bad depending on direction.
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This must be solved by plotting or a calculator.
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This must be solved by plotting or a calculator.
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Sketch a high or low and draw in the winds.
15° to 30° across the isobars, into the low out of the high pressures.
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If needed, draw in a new isobar at the location of interest. We are looking for ±2 kts and ±10°.
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The new text encourages getting involved with model forecasts via GRIB files as soon as possible.
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An X marks the location of a Low 24h later. Peak and minimum forecasted values are shown underlined.
The projected 24-later pressure is 996, shown by underlined 96 at the X of its 24hr later position. It started at 998.
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All steps are required for typical aneroids. Tapping reveals friction, parallax avoidance ensures accurate reading, and calibration correction ensures the value is correct.