WX0303 · Global Weather Patterns
22 questions · 22 multiple choice · 0 written · ASA 109 Marine Weather — Global Weather Patterns
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This is almost a tricky question if you know too much.
The horse latitudes is sometimes used to describe the Sarogassa Sea. Horse latitudes is also used generically to describe the subtropical highs, characterized by light airs and calms.
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If we were right at the pole, could we rule out any answers with a simple philosophical argument.
Polar easterlies. Right at the pole, there is no north and all directions are south, so north or south could not be the answer.
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The equatorial currents are primarily wind driven currents responding to the trade winds.
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The wind directions referred to are NE and SW.
See monsoon. The Indian monsoon is in effect a giant seasonal sea breeze.
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Horse latitudes are Highs, doldrums are Lows.
Trade winds blow from the subtropical highs toward the equatorial low.
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Trade-wind cumulus are low small puffy white clouds often seen at night as well as day.
All signs are needed: steady eastern-quadrant wind, big organized waves, and trade-wind cumulus.
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Both of these properties can have direct affect on what we experience on the surface.
The temperature drops at about 4°F per 1000 ft and the wind veers. Over the first 2,000 feet or so, the total veer is some 10 to 40°.
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Trade winds. They are primarily NE, not easterly, although they can at times be easterly.
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Stratiform clouds indicate stable air.
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The Coriolis effect is fundamental to understanding wind and ocean circulation.
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When air temp drops to dew point, water vapor condenses to clouds. If this happens at the surface the stratus clouds we get are called fog.
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Clearly we need to know what the letters stand for in these air mass symbols.
cP = continental (made over land and thus dry) and polar meaning cold.
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They could be formed in other situations, but which is most likely?
Large stable highs are often the source of air mass formation.
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Temperature is the most dependable indicator of the Gulf Stream.
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For Atlantic sailing this is one of the fundamental currents to know about.
2 to 4 kts flowing north.
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We are asking here for the first indications of the stream, not the axis or center.
About 2 nmi. The Gulf Stream is only about 2 miles offshore in this region. The center of the current is about 13 nmi offshore.
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Rossby waves were first identified in the atmosphere in 1939 by Carl-Gustaf Arvid Rossby.
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5 to 10 days. The Rossby waves slip around the globe with a period of about one week.
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dry lapse rate - dew point lapse rate = 5.5-1 = 4.5
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All factors contribute: night vs day, summer vs winter, land heats more and faster than water.
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The implication is that moving weather is moving air masses.
Heated air rises at the equator and is forced poleward. The Coriolis force bends the wind to the right setting up winds aloft running eastward, which move surface patterns to the east.
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Air masses are named after their properties which reflect their origins.
Warm moist air is called maritime tropic (mT).