Set: Weather & Climate III

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All 85 terms

TermDefinition
Standard Rain Gaugeconsists of a funnel attached to a graduated cylinder that fits into a larger container. If the water overflows from the graduated cylinder the outside container will catch it.
Tipping Bucket Rain GaugeConsists of a large copper cylinder set into the ground. At top of the cylinder is a funnel that collects and channels the precipitation. The precipitation falls onto one of two small buckets or levers which are balanced in same manner as a scale (or child's seesaw).
Weighing Type Rain GaugeConsists of a storage bin, which is weighed to record the mass. Certain models measure the mass using a pen on a rotating drum, or by using a vibrating wire attached to a data logger. The advantages of this type of gauge are that it does not underestimate intense rain, and it can measure other forms of precipitation, including rain, hail and snow.
Water Equivalent of Snowfall Coverage1" of liquid rainfall equals 10" of snowfall
Wet snow may yield...1" of liquid rainfall to 5" of snowfall
Dry powdery snow may yield...1" of liquid rainfall to 15" of snowfall
What is Air pressure?it is the weight of air above a given surface
Air pressure ALWAYS...decreases with height
As one climbs in elevation...there are fewer air molecules
In a column with fixed width... if we move air INTO the column with NO temperature change...Surface pressure would INCREASE
In a column with fixed width... if we move air OUT OF the column with NO temperature changeSurface pressure would DECREASE
In a WARM column with fixed width and same air pressure...the molecules move faster and spread farther apart, the air becomes less dense and the column expands in height
In a COLD column with fixed width and same air pressure...the molecules move more slowly and crowd closer together, the air becomes more dense and the column shrinks in height
** It takes a shorter column of cold, dense air to...exert the same surface pressure as a taller column of warm, less dense air
**Atmospheric pressure decreases more RAPIDLY with...elevation in a COLD column in a cold column of air
elevation in a WARM column of airelevation in a WARM column of air
Warmer air aloft is normally associated with...HIGHER ATMOSPHERIC PRESSURE aloft (resulting in a more stable atmosphere) (in texas with no rain)
**COLDER AIR ALOFT is normally associated with...LOWER ATMOSPHERIC PRESSURE aloft (resulting in a more unstable atmosphere)
Horizontal temperature differences results in a...hoorizontal difference in pressure
*** Unequal heating of the earth's surface...causes wind to blow
two types of Barometers are...-Mercurial and -Aneroid (without fluid)
BarometerAn instrument that measures air pressure
When measuring air pressure with a barometer, corrections must be made for...-Temperature ;-Instrument / -Gravity ;-Sea Level
Atmospheric pressure decreases on average...1" of mercury for each 1000 feet RISE in altitude
***Standard Surface Atmospheric Pressure*** in Mercury:29.92"/mercury
***Standard Surface Atmospheric Pressure*** in millibars:1013.2 millibars
***Standard Surface Atmospheric Pressure*** in pounds:14.7 lbs/in 2 (squared)
An altimeter is...an instrument used to measure the altitude of an object above a fixed level... it is mainly used in airplanes to measure air pressure
Always correct air pressure to...sea level so as to compare pressure to other cities
Does cold air weigh more?YES, because it is more dense
Example of place with high pressureSiberia
Example of low pressuretropical cyclones and tornados (10% less than 29.92"/mercury => around 26%)
Characteristics of High PressureAir blows around a high in a clockwise manner in the northern hemisphere and counterclockwise in the southern hemisphere. In a cross-section, there is surface divergence and upper air conversion
Characteristics of Low PressureAir blows around a low in a counterclockwise in the northern hemisphere and clockwise in the in the southern hemisphere.In a cross-section, there is surface convergence and upper air divergence
surface pressureis the atmospheric pressure at a point of Earth's surface. It is directly proportional to the mass of air over that point. With corrections made to surface pressure readings, surface pressure charts use ISOBARS to depict lines of equal surface pressure
newton's first law of of motionDone in millibars - 1013.2 millibars => standard atmospheric pressure **(not the same as upper air charts)**
Upper Air (Constant Height) Charts are constructed to show...height variations along a constant pressure height surface
Higher heights equals...higher pressure
Lower Heights equals...lower pressure
On upper air charts, what kind of lines depict pressure?Height contour lines
Where is the ideal location of the upper air chart?500 millibars because it's at the halfway point
at which level are high or low pressure driven at?500 millibar level
Newton's First Law of MotionAn object at rest will remain at rest and an object in motion will remain in motion (and will travel at a contant velocity along a straight line) as long as no force is excerted on the object
Newton's Second Law of MotionThe force exerted on an object equals its mass times the acceleration produced (F=ma)
Newton's Third Law of MotionFor every action, there is an opposite and equal reaction
How much coriolis is there around the equator?ZERO!!
How much coriolis is there around the poles?A LOT?!!
Coriolis Force...(Deflection caused by a rotating object) Coriolis Force ONLY effects wind direction!!!!! (not speed)
The amount of Coriolis deflection depends on...-Rotation of the Earth -The latitude -The objects speed
What kind of coriolis deflection is there in the Northern hemisphere?Rightward deflection!
What kind of coriolis deflection is there in the Southern hemisphere?Leftward Deflection!
Fricton...wiond blowing across the Earth's surface and against other air molecules
***The stronger the winds are......the greater the deflection will be
*** The Coriolis affects...large scale circulation
Which direction do hurricanes rotate in?counterclockwise
A theoretical horizontal wind blowing in a straight path, parallel to the the isobars/constant contour lines, at a constant speedA theoretical horizontal wind blowing in a straight path, parallel to the the isobars/constant contour lines, at a constant speed
What are Geostropic Wind caused by?an exact balance of pressure gradient force and the coriolis force
Where are Geostropic Winds found?they are found in upper level wind flow (parallel)
Hydrostatic Balanceoccurs in the vertical when an EXACT BALANCE between vertical pressure gradient force and gravity (the earth's atmosphere remain in place)
What causes the earth's atmosphere to be imbalanced?Thunderstorms
WInd is characterized by...-Direction -Speed -Gustiness -Wind Roses
Scales of Atmospheric Motion: Microscale...example... around a building
Scales of Atmospheric Motion: Mesoscale***Example... in a county, state => This one is used for forcasting!!
Scales of Atmospheric Motion: Macroscaleexample... synoptic (weather map) scale-surface map of USA (at 500 millibar level) and -Global scale
-wind vane -Anemometer -Aerovane -Wind Sock -Rawinsonde -Doppler Radar -Atmosperic profilers-wind vane -Anemometer -Aerovane -Wind Sock -Rawinsonde -Doppler Radar -Atmosperic profilers
*****With (doppler) radar...there is range and height!!!!
Intertropical Convergence ZoneAn area of low pressure near or on the equator where the northeast trades and the southeast trades converge
DoldrumsRegion of ocean near the equator, characterized by calm, light winds (constant low pressure)
Horse LatitudeEither of two belts or regions near 30 degrees north or 30 degrees south; characterized by calms and light-baffling winds
Single Cell Atmospheric CirculationWith higher air pressure at the poles, sinking cold air flowed southward from the polar regions, once it got to the equator, after warmer air was lifted... it's one big circulation cell with various cells of lows & highs at different latitudes
Hadley CellThree-dimensional atmospheric circulation cell located at roughly 0 to 30° North and South of the equator. The Hadley cell consists of rising air (intertropical convergence zone) at the equator and descending air (subtropical highs) at 30° North and South
The Intertropical Convergence Zone stays at north of the Equator because of...Continentality
Average Global Surface PressureDuring winter, "highs" hoover over land, during warm seasons, "Highs" hoover over water
Jet Streamsnarrow belts of high speed winds that blow in the (upper level) upper troposphere and lower stratosphere
Polar Jet StreamsWhere cold air from the North pole moves southward and converges with warmer air... found best at 300 mb height/130,000 ASL
Subtropical Jet StreamsWhere warm air and moisture move away from equator toward the north... found best at 200 mb height/38,500' ASL
Low Level Jet StreamsFound best at 850 mb to 700mb height/4000' to 9800' ASL... forms in plains states and *provides moisture for thunderstorms**
What sustains thunderstorms??Updrafts because air has to rise
Upwellingan upward flow of cold water from the ocean depths (brings nutrient rich waters to the surface)
Surface water of oceans tend to move with ...the surface winds
La ninaAn ocean and weather pattern that causes the eastern Pacific Ocean to be colder than normal (air moves from High to Low)... -west of south America
El Ninoan event that occurs every two to seven years in the pacific ocean, during which winds shift and push warm surface water toward the coast of south America; it can cause dramatic climate change
A change in water temperature...changes wind patterns
prevailing winda wind that consistently blows from one direction more than from any other
doppler Radara type of radar that calculates distance and shows direction of movement

Set Information

Terms 85
Creator makazine
Created August 3, 2009
Groups None
Subjects geography, weather, climate, air pressure, precipitation
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