chap5 Flashcards

1
Q

a rising parcel of air

A

expands and cools

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2
Q

a sinking parcel

A

compresses and warms

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2
Q

If a parcel of air expands and cools, or compresses and
warms, with no interchange of heat with its outside
surroundings, this situation is called

A

adiabatic process

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3
Q

the rate of adiabatic cooling or warming remains constant and
is about

A

10°C for every 1000 meters

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4
Q

As the rising air cools, its relative humidity

A

increases as the air temperature approaches the
dew-point temperature.

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5
Q

If the rising air cools to
its dew-point temperature

A

the relative humidity becomes 100 percent.

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6
Q

Further lifting results in condensation, a cloud forms, and ________ is released into the rising air.

A

latent heat

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7
Q

Unlike the dry adiabatic rate, the moist adiabatic rate is not
constant, but varies greatly with ___________ and __________

A

temperature and moisture content

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8
Q

TRUE OR FALSE: warm saturated air produces more liquid water than cold saturated air

A

TRUE

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9
Q

the moist adiabatic rate is equal to?

A

an average of 6°C per 1000 m.

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10
Q

if the air in a stable atmosphere strongly resists
upward vertical motion, and is forced to rise,
it tends to

A

spread out horizontally

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10
Q

Expected clouds to see in a stable atmosphere

A

cirrostratus, altostratus, nimbostratus, or
stratus

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11
Q

The cooling of the surface air may be due to:

A
  1. nighttime radiational cooling of the surface
  2. an influx of cold surface air brought in by the wind
  3. air moving over a cold surface
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12
Q

If the surface air becomes saturated in a stable
atmosphere, a __________ may
form

A

a persistent layer of haze or fog

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13
Q

The atmosphere is unstable when the
air temperature __________ as we
move up into the atmosphere.

A

decreases rapidly

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14
Q

The warming of the surface air may be due to:

A
  1. daytime solar heating of the surface
  2. influx of warm surface air brought in by the wind
  3. air moving over a warm surface
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15
Q

Instability brought on by the lifting of air is often associated with
the development of

A

severe weather, such as thunderstorms and
tornadoes

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16
Q

The following mechanisms are responsible for the development of the majority of clouds we observe:

A
  1. surface heating and free convection
  2. uplift along topography
  3. widespread ascent due to the flowing together
    (convergence) of surface air
  4. uplift along weather fronts
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17
Q

Forced lifting along a topographic barrier is called

A

orographic uplift

18
Q

The most important factor in the production of raindrops is
the

A

cloud’s liquid water content

19
Q

In a cloud with sufficient water, other significant factors are:

A
  1. The range of droplet sizes
  2. the cloud thickness
  3. the updrafts of the cloud
  4. the electric charge of the droplets and the electric field in
    the cloud
20
Q

Water droplets existing at temperatures below
freezing are referred to as

A

supercooled droplets

21
Q

Examples of excellent ice nuclei’s

A

clay minerals, bacteria in decaying plant leaf
material, and ice crystals

22
Q

The primary goal in cloud seeding is to

A

inject (or seed) a cloud with small particles that will act as nuclei

23
The most common chemicals used for cloud seeding include
salt, silver iodide, potassium iodide and dry ice (solid carbon dioxide).
24
Aims at speeding up droplet coalescence in liquid clouds, leading to production of large droplets that start to precipitate.
HYGROSCOPIC CLOUD SEEDING
25
Cloud seeding material consists usually of large salt particles dispersed by some means to the cloud base.
HYGROSCOPIC CLOUD SEEDING
26
Aims to trigger ice production in supercooled clouds, leading to precipitation.
GLACIOGENIC CLOUD SEEDING
27
For it to be considered as rain, the water droplet must have a diameter equal to, or greater than
RAIN
28
Fine uniform drops of water whose diameters are smaller than 0.5 mm is called
Drizzle
29
Evaporating streaks of precipitation are called
VIRGA
29
Drizzle is mostly from
stratus clouds
30
If the updraft weakens or changes direction and becomes a downdraft , the suspended drops will fall to the ground as a sudden rain
shower
31
The showers falling from cumuliform clouds are usually brief and sporadic, as the cloud moves overhead and then drifts on by. If the shower is excessively heavy, it is termed a
cloudburst
32
When ice crystals and snowflakes fall from high cirrus clouds they are called
fallstreaks
33
Snow falling from developing cumulus clouds is often in the form of
flurries
34
These are usually light showers that fall intermittently for short durations and produce only light accumulations.
flurries
35
A more intense snow shower is called a
snow squall
36
A weather condition characterized by low temperatures and strong winds (greater than 30 knots) bearing large amounts of fine, dry, powdery particles of snow, which can reduce visibility to only a few meters
Blizzard
37
partially melted snowflake or cold raindrop turns back into ice, not as a snowflake, but as a tiny transparent (or translucent) ice pellet
Sleet
38
The cold surface layer beneath a cloud may be too shallow to freeze raindrops as they fall. In this case, they reach the surface as supercooled liquid drops. This is called
FREEZING RAIN OR GLAZE
39
snow grains came from ____ clouds
stratus
40
snow pellets came from _____ clouds
Cumulus congestus
41
Pieces of ice either transparent or partially opaque, ranging in size from that of small peas to that of golf balls or larger Some are round, and others take on irregular shapes.
Hail
42
Hail is produced in a ______ cloud
cumulonimbus
43
For a hailstone to grow to golf ball-size, it must remain in the cloud between
5 to 10 minutes