WX0403 · Fronts, Storms & Hurricanes
25 questions · 22 multiple choice · 3 written · ASA 109 Marine Weather — Fronts, Storms & Hurricanes
Squalls in the NH move in a direction that is veered from the ambient surface winds in that they are driven by the higher winds which are veered. Something like 30° off will be about the range.
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80° F is the accepted value based on research cited in the course materials.
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We are talking here about the general behavior of a squall, not specifically what you might experience depending on your location relative to the squall.
Strong winds come with the rain.
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The statistic is usually recorded as thunderstorm days per year.
Florida wins by far, peaking out at over 100 squall days per year on both coasts.
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The answer is different on land.
At sea in warm waters, at night when the air cools, the warmer air near the surface of the water starts to rise, triggering squalls. On land, squalls are more common in the afternoon.
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Wind builds as the front approaches, then suddenly veers at the frontal surface, and then remains more or less steady as the warm sector passes.
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Clouds at fronts are covered in Graphic G207
Short heavy rain, cumulonimbus clouds, larger veer… in contrast the warm front would have long light rains, stratus clouds, and a relatively smaller veer.
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Think of modern usage of these terms more than just definitions that were used mostly in the past.
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There are of course many links to related topics but we are asking here for the one recommended throughout our course.
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The wind will sharply veer at the passage of any front.
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The same general name would apply if the cold front rode up and over the warm front it overtook.
“Secluded front” is a fake answer. An occluded front forms when a cold front overtakes a warm front. There are two kinds: warm and cold occlusions.
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Peak is August-September.
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It is fundamental to learn the natural signs of approaching bad weather.
Generally, in open water, there is “no calm before the storm.” The winds just gradually build. Long swells, cirrus clouds, and halos are all signs of an approaching tropical storm.
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If we have maps we often are told this. But sometimes it is missing from the surface maps.
It is the winds aloft that drag the surface systems around the globe, so the surface speed is related. 1/3 to 1/2 is the general guideline.
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These are valuable statistics to keep in mind when these notices first appear on your weather maps.
About 10%. Even in a very active year, there are only some 50 hurricanes in the NH.
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Right side means you are facing the same direction it is moving.
All of these factors contribute to making the right side more dangerous.
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There is certainly no fixed answer, but what would be a rough estimate for a hurricane of this size.
Hurricanes are typically not very big. In several examples, winds were down to 40 knots at just 80 miles out of the eye. Every mile we can put between us and the center is crucial.
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Each zone—warm front, warm sector, and cold front—have distinctly different weather.
The isobars in the warm sector are usually more or less straight and evenly spaced, which means steady wind.
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Draw a sketch of a Low with several isobars of circulating winds.
In the navigable semicircle. In the navigable side the wind backs; in the dangerous side it veers.
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See text section 1.2.
Force increases like the square of the wind speed. In this case a factor of (30/20)² = (3/2)² = 2.25 ≈ 2.3.
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What causes the wind in the first place?
Any circumstance where the gradient is increasing as the pressure rises will lead to this. The bent-back occlusion is a notable example. Sometimes called the sting in the scorpion’s tail.
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They often develop to be more intense than the primary Low that created them.
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See starpath.com/ASCAT for use of our new ASCAT index.
Two to four times a day depending on latitude.
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See www.starpath.com/ascat for much info on this topic
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Both the OSWT and the KNMI main sites have links to theoretical discussions of the data.
All of the listed limitations might apply. See text section 4.2 on satellite winds.