Term
| How many degrees centigrade does the temperature decrease per 1,000 meters of altitude in the troposphere? |
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Definition
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Term
| The stratosphere is characterized by |
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Definition
| a temperature that remains isothermal to about 100,000 feet, the strongest concentration of ozone, and excellent flying conditions. |
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Term
| Above 13 miles, the radiation from the sun breaks down the oxygen in the atmosphere into |
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Definition
|
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Term
| Which is true of water vapor in the atmosphere? |
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Definition
| The more water capor, the lighter the air will be. |
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Term
| The earth's atmosphere receives the most heating through what process? |
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Definition
| Reradiated energy from the earth's surface. |
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Term
| The two atmospheric gases most responsible for the absorption of incoming solar radiation are: |
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Definition
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Term
| Explain why the sky is blue. |
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Definition
| Short-wave radiation is reflected by the atmospheric particles smaller than .5 microns. |
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Term
| The driving mechanism that is mainly responsible for the earth's large-scale atmostpheric circulations is the: |
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Definition
| Unequal heating of the earth |
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Term
| The three circulation cells in the three-cell theory are: |
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Definition
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Term
| Which force is the "equal and opposite reaction" to the center seeking force? |
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Definition
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Term
| Centrifugal force will increase when there is a decrease in: |
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Definition
|
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Term
| Coriolis force is created by: |
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Definition
| the cyclonic rotation of the earth. |
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Term
| If you throw a ball toward a stationary target from the window of a speeding vehicle, coriolis force will cause the ball to miss the target: |
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Definition
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Term
| The force that is responsible for starting the horizontal movement of air over earth's surface is: |
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Definition
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Term
| To achieve geostrophic windflow, there must be a balance between: |
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Definition
| pressure gradient force and coriolis force |
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Term
| The balance of forces needed for gradient anticyclonic circulation are pressure gradient: |
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Definition
| and centrifugal balances against coriolis force. |
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Term
| The balance of forces needed to gradient cyclonic circulation is pressure gradient: |
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Definition
| balanced against coriolis and centrifugal forces. |
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Term
| The areas of low pressure that correspond to the belt of low pressure at 60 N created by the 3-cell circulation are the: |
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Definition
| Icelandic and Aleutian lows |
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Term
| In relation to the jet core, the greatest vertical wind shear is usually located: |
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Definition
|
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Term
| In relation to the jet core, the greatest horizontal wind shear is usually located: |
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Definition
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Term
| The simplest method for locating the 500 millibar frontal zone is to: |
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Definition
| locate the position of the -17 Centigrade isotherm. |
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Term
| The width of the jet stream core is approximately equal to the: |
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Definition
| width of the 500 millibar isotherm ribbon. |
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Term
| What causes the subtropical jet to recurve? |
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Definition
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Term
| The jet core that is located between the midlatitude and the tropical tropopause's is called the: |
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Definition
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Term
| These suggest that the jet stream is beginning to dissipate. |
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Definition
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Term
| Converging contours downstream of the jet stream will cause the jet to: |
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Definition
| Deflect toward lower heights |
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Term
| Using average surface frontal slopes, how far behind the surface cold front is the jet stream located? |
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Definition
|
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Term
| Using average surface frontal slopes, how far ahead the surface warm front is the jet stream located? |
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Definition
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Term
| What will the jet stream usually do when a cold, moving, polar high stagnates and begins to warm? |
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Definition
| Dissipate and a new jet forms to the north. |
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Term
| This law states that the wavelength at which maximum energy is emitted is inversly proportional to the object's temperature. |
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Definition
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Term
| Which heat transfer process involves the transfer of energy by molecular motion from hot to cold objects. |
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Definition
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Term
| Which heat transfer process vertically transports the atmospheric properties of heat and moisture and is more efficient method of heat transfer than by molecular motion? |
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Definition
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Term
| Advection transfers temperature: |
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Definition
| horizontally by the wind. |
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Term
| What factors must a region possess in order to facilitate air mass formation? |
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Definition
| Uniform surface, stagnant air, and large scale difluent flow. |
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Term
| Which process is most responsible for the slow formation of air masses in the polar region? |
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Definition
| Loss of heat by radiation. |
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Term
| Air mass stability characteristics often depend on the temperature differences between the: |
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Definition
| air mass and the surface over which it is traveling. |
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Term
| A stable air mass that formed over land in the Arctic has now moved over the ocean's warmer surface. You would classify this air mass as: |
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Definition
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Term
| What air mass classification signifies an unstable, maritime tropical air mass that is colder than the surface it is moving over? |
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Definition
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Term
| What air mass classification signifies a stable, continental polar air mass that is warmer than the surface it is moving over. |
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Definition
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Term
| What air mass forms over land only during the summer? |
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Definition
|
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Term
| What factors act as air mass modifiers? |
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Definition
| Radiation loss, thermodynamics, advection, and mechanical mixing. |
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Term
| It is winter. A cPk air mass is moving over the Great Lakes. In this situation, the southern shores of the Great Lakes will experience: |
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Definition
|
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Term
| Which air mass involves most of the windertime storms for the North American Pacific coast? |
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Definition
|
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Term
| In the summer, the continental highs: |
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Definition
| Dissipate over the heated land and the cP source regions move farther north. |
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Term
| Continental tropical air masses are usually assocaited with: |
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Definition
|
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Term
| The rate that an air mass modifies depends on the: |
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Definition
| temperature differences between the new surface and the air mass, the nature of the surface over which it moves, and the speed with which the air mass travels. |
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Term
| The weather characteristics of a particular month in a given locality are governed by: |
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Definition
| effects of local topography and proximity to a zone of convergence. |
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Term
| Surface pressure changes largely controlled by: |
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Definition
| mass changes in the upper troposphere |
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Term
| Horizontal divergence within an air mass will: |
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Definition
| vertically contract the original column of air and then expand it horizontally. |
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Term
| As air converges at the surface and toward the center of a layer, there will be horizontal: |
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Definition
| contraction and vertical expansion. |
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Term
| An increase of mass in a column of air will cause the surface pressure to: |
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Definition
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Term
| A decrease of mass in a column of air will cause the surface pressure to: |
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Definition
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Term
| The primary cause of surface pressure changes for a dynamic low is net: |
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Definition
|
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Term
| The damper effect is comprised of upper-level: |
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Definition
| convergence and surface high pressure |
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Term
| You are evaluating a jet maximum in straight line flow. To do this properly, you would locate the maximum area of convergence at the: |
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Definition
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Term
| A low-pressure system undergoing cyclogenesis is said to be: |
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Definition
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Term
| When the central pressure of an anticyclone is rising, you can infer the anticyclone is: |
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Definition
|
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Term
| A high-pressure system undergoes anticyclolysis when the clockwise circulation area: |
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Definition
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Term
| A cyclone that develops on a polar front, does not intensify significantly, and never occludes is called: |
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Definition
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Term
| After warm air with an unstable wave is pushed aloft and cuts off from a cyclone the cyclone will become: |
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Definition
| barotropic and begin to fill. |
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Term
| Unstable waves are classified as: |
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Definition
|
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Term
| In the barolcinic instability process: |
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Definition
| potential energy is transferred to the major short wave by thermal advection |
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Term
| Aloft, during the baroclinic instability process, the thermal wave and contour wave are: |
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Definition
| out of phase and cold air advection occurs into the contour trough. |
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Term
| An intense cyclogenesis normally occurs in troughs with a: |
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Definition
| negative tilt that is oriented northwest/southeast |
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Term
| When using Pettersen's rule, the factors needed for cyclogenesis are upper-level: |
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Definition
| divergence and a frontal zone where thermal advection is weak. |
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Term
| What causes the surface low to deepen during the self-development process? |
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Definition
|
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Term
| A low dissipates after proceeding through its entire life cycle which ranges from the: |
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Definition
| bottom up as boundary layer convergence adds mass to the column of air. |
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Term
| How many stages are there in the life cycle of a low |
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Definition
|
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Term
| In the life cycle of a low, the wave will reach its maximum intensity in the: |
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Definition
|
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Term
| Anticyclongenesis typically occurs at, and just downstream from, long-wave |
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Definition
| ridges under confluent flow aloft |
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Term
| What causes a surface high to build during the self-development process? |
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Definition
|
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Term
| Which is primarly responsible for low-level divergence acting as a braking mechanism for a high? |
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Definition
|
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Term
|
Definition
| has great vertical extent and its axis tilts with height. |
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Term
| The best sources for identifying a frontal inversion are the: |
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Definition
| temperature and dew point curves and the vertical wind distribution |
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Term
| With the passage of a cold front in the Northern Hemisphere, the horizontal wind direction will: |
|
Definition
| shift in a clockwise direction |
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Term
| The cold conveyor belt originates in the low levels that are located: |
|
Definition
| east of a low center and flow westward. |
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Term
| The average slope of a cold front is: |
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Definition
|
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Term
| A warm frontal occlusion occurs when the cool air |
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Definition
| behind the cold front overrides the colder air ahead of the warm front. |
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Term
| With an active cold front, the net flow is: |
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Definition
|
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Term
| An inactive cold front is characterized by a relatively: |
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Definition
| steeper slope, a narrow weather pattern, and is called katafront. |
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Term
| When an inactive front passes your station, the dew points will |
|
Definition
| decreases sharply with the passage. |
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Term
| When only high and middle clouds are associated with a warm front, the: |
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Definition
| overrunning warm air is dry |
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Term
| Which region of the United States facors the development of frontal occlusions? |
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Definition
|
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Term
| In a cold occlusion, the coldest air is found: |
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Definition
|
|
Term
| In a warm frontal occlusion, the coldest air is found: |
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Definition
|
|
Term
| The frontolytic processess are most effective: |
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Definition
| in the lower layers of the atmosphere |
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Term
| Frontogenesis requires two adjacent air masses with: |
|
Definition
| different densities and a wind flow to bring the air masses together. |
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Term
| The atmospheric properties that can be a measure of the strength of a frontal system are thickness gradient, |
|
Definition
| temperature gradient, lapse rate, turbulence and wind shear. |
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Term
| Low cloud bases range from: |
|
Definition
| near the surface to 6,500 feet above ground level. |
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Term
| Which low cloud type and classifiction is identified by the presence of a cirriform anvil? |
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Definition
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Term
| The best way to distinguish stratocumulus from altocumulus clouds is to use: |
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Definition
| the size of the elements. |
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Term
| The primary difference between stratus and altostratus clouds is: |
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Definition
| the composition of the clouds. |
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Term
| How would you classify middle clouds that can lower to within several hundred feet of the surface? |
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Definition
|
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Term
| A corona is often present at night with: |
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Definition
|
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Term
| Cirrus clouds in the form of an anvil are classified as: |
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Definition
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Term
| Which high cloud can occasionally be so transparent that the only indication of its presence is a halo phenomenon? |
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Definition
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Term
| Which high cloud classifiction is also referred to as a mackerel sky? |
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Definition
|
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Term
| Which orographic cloud resembles an almond or a fish? |
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Definition
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Term
| "Clouds or obscuring phenomena that have bases at the same approximate level" is the definition of: |
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Definition
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|
Term
| Pilot reported ceiling heights must be converted from height above: |
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Definition
| mean sea level to height above ground level. |
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Term
| What color balloon would you use to determine the ceiling heights of thin cloud? |
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Definition
|
|
Term
| You are preparing to use a convective cloud height table to determine the heights of clouds. To do this properly, you must first determine the: |
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Definition
| dew point temperature and free air temperature. |
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Term
| The most desirable night-visibility markers are: |
|
Definition
|
|
Term
| How do you report prevailing visibility at CONUS stations and overseas stations? |
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Definition
| Statute miles for CONUS and meters for overseas stations. |
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Term
| You are reporting the visibility for more than one sector. To do this properly, you would list the sectors in a: |
|
Definition
| Clockwise direction starting from the northernmost sector. |
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Term
| The designated runway visual range (RVR) runway is: |
|
Definition
| any runway that has been instrumented with a transmissometer. |
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Term
| For a runway visual range (RVR) report of R15/1600, what is the visual range that a pilot can expect to see down the runway? |
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Definition
|
|
Term
| The three main forms of precipitation are liquid, |
|
Definition
|
|
Term
| What type of precipitation might you observe with clear skies? |
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Definition
|
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Term
| You would classify precipitation as intermittent if it: |
|
Definition
| stopped and started at least once within the preceding hour |
|
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Term
| What is the intensity of snow which restricts visibility to less than 1/4 mile? |
|
Definition
|
|
Term
| Precipitation is reported to the nearest: |
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Definition
|
|
Term
| The distinguishing feature of any tornadic activity is: |
|
Definition
| the funnel-shaped appendage that hangs from the base of the clouds. |
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Term
| A thunderstorm is present and occurring at your station. In addition, the local noice level is preventing you from hearing the thunderstorm. For observation purposes you would say: |
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Definition
|
|
Term
| A thunderstorm offically ends: |
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Definition
| fifteen minutes after the last occurence of thunder, hail, or lightning. |
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Term
| For observing purposes, four hydrometers are considered to be obstructions to vision. They include fog, blowing snow,: |
|
Definition
| freezing fog and blowing spray. |
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Term
| Blowing spray is reported only at sea stations near large bodies of water and when visibility at eye level is rescricted to: |
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Definition
|
|
Term
| Which type of obstruction to vision is classified as a lithometer? |
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Definition
|
|
Term
| What pressure value is the basis for determinig all other pressure values? |
|
Definition
|
|
Term
| What is the reference level for all pressure values? |
|
Definition
|
|
Term
| Which is the calculated sea-level pressure in inches of mercury? |
|
Definition
|
|
Term
| The temperature an air parcel would have if it were cooled adiabatically to saturation at constant pressure by evaporation of water into it is called: |
|
Definition
|
|
Term
| Wind observing equipment is oriented to: |
|
Definition
|
|
Term
| A sudden increase of wind speed of at least 16 knots and a sustained average of 22 knots (or more) that is maintained for at least 1 minute before the speed diminishes is called a: |
|
Definition
|
|