ns2 3.2 clouds and fog

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CHAPTER 2 CLOUDS AND FOG

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Page 1: NS2 3.2 Clouds and Fog

CHAPTER 2

CLOUDS AND FOG

Page 2: NS2 3.2 Clouds and Fog

Tiny particles of dust, pollen from plants,

factory smoke, and salt particles from

oceans are always present in the air. These

fragments are called hygroscopic nuclei.

Page 3: NS2 3.2 Clouds and Fog

Tiny particles that absorb or attract

moisture from the air

Hygroscopic Nuclei

Page 4: NS2 3.2 Clouds and Fog

A mass of hygroscopic nuclei that

have soaked up moisture from the

water vapor in the air.

Cloud

Page 5: NS2 3.2 Clouds and Fog

Clouds form when:

• Water vapor rises

• Vapor condenses

• Droplets cling to hydroscopic nuclei

• Nuclei bunch together and form clouds

or fog

Page 6: NS2 3.2 Clouds and Fog

Three things may happen to the water

droplets:

• Reevaporate and rise

• Rise and freeze into ice crystals

• Collide with other nuclei and form

larger drops

Page 7: NS2 3.2 Clouds and Fog

Cloud formations give clues concerning

the forces at work in our atmosphere.

Page 8: NS2 3.2 Clouds and Fog

Fragments of matter that are always in

the air are called _________ nuclei.

a. hydroscopic

b. hygroscopic

c. psychroscopic

d. psychrodropic

Page 9: NS2 3.2 Clouds and Fog

Fragments of matter that are always in

the air are called _________ nuclei.

a. hydroscopic

b. hygroscopic

c. psychroscopic

d. psychrodropic

Page 10: NS2 3.2 Clouds and Fog

Cirrus Stratus

Cumulus

There are three

basic cloud types.

Page 11: NS2 3.2 Clouds and Fog

A cloud of a class characterized by

thin white filaments or narrow bands

and a composition of ice crystals: of

high altitude, about 20,000 - 40,000

feet

Cirrus

Page 12: NS2 3.2 Clouds and Fog

A cloud of a class characterized by

dense individual elements in the form

of puffs, mounds, or towers, with flat

bases and tops that often resemble

cauliflower

Cumulus

Page 13: NS2 3.2 Clouds and Fog

A cloud of a class characterized by a

gray, horizontal layer with a uniform

base, found at a lower altitude than

altostratus, usually below 8,000 feet

Stratus

Page 14: NS2 3.2 Clouds and Fog

There are also other types of clouds

having names with combinations of

the following:

• Nimbus - rain

• Alto - high

• Fracto - fragmented or windblown

Page 15: NS2 3.2 Clouds and Fog

Clouds are sometimes classified by

altitudes at which they most frequently

occur:

• Low - surface - 7,000 feet

• Middle - 7,000 - 20,000 feet

• High - above 20,000 feet

• Towering - exceptionally high cloud

with its base in low-altitude

Page 16: NS2 3.2 Clouds and Fog

Middle clouds seldom attain heights

greater than 13,000 feet in polar regions

but may reach 23,000 - 45,000 feet in

temperate and tropical zones.

Page 17: NS2 3.2 Clouds and Fog

There are ten general types of clouds

grouped into low, middle, and high

categories.

Page 18: NS2 3.2 Clouds and Fog

Low Clouds

Stratus

Nimbostratus

Stratocumulus

Cumulus

Cumulonimbus

Page 19: NS2 3.2 Clouds and Fog

• Lowest cloud type

• Gray layer with uniform base

• May cause drizzle, but never rain

• Fog becomes stratus when it lifts

Stratus

Page 20: NS2 3.2 Clouds and Fog

• Dark, shapeless, rain-laden

• Often have streaks of rain extending

to ground

• Often seen in summer at base of

thunderheads

• Brings steady, heavy snow in winter

Nimbostratus

Page 21: NS2 3.2 Clouds and Fog

A cloud of a class characterized

by a formless layer that is almost

uniformly dark gray, a rain cloud

of the larger type, of low altitude,

usually below 8,000 feet

Nimbostratus

Page 22: NS2 3.2 Clouds and Fog

The upper portion of a cumulus

cloud characterized by dense,

sharply defined cauliflower-like

upper parts and sometimes of

great verticality

Thunderhead

Page 23: NS2 3.2 Clouds and Fog

Stratocumulus

• Irregular, rounded masses spread out

in puffy or rolling layers

• Usually gray with darker spots

• Do not produce rain

• Usually precede bad weather

Page 24: NS2 3.2 Clouds and Fog

A cloud of a class characterized

by large dark, rounded masses,

usually in groups, lines, or

waves, the individual elements

being larger than those in

altocumulus and the whole being

at a lower altitude, usually below

8,000 feet

Stratocumulus

Page 25: NS2 3.2 Clouds and Fog

Cumulus

• Dense, puffy clouds with a beautiful,

cauliflower-like appearance

• They rise by day and disappear at night

• Fleecy cumulus clouds usually mean

fair weather ahead

Page 26: NS2 3.2 Clouds and Fog

Consisting of, or resembling a

fleece (soft, fluffy)

Fleecy

Page 27: NS2 3.2 Clouds and Fog

• Dense clouds of the towering variety

• The base is a dark nimbus rain cloud

• May produce severe thunderstorms

and tornadoes

Cumulonimbus

(Thunderheads)

Page 28: NS2 3.2 Clouds and Fog

A cloud of a class indicative of

thunderstorm conditions,

characterized by large, dense

towers that may reach altitudes

of 75,000 feet, uniform except

for the tops, which appear

fibrous because of the

presence of ice crystals

Cumulonimbus

Page 29: NS2 3.2 Clouds and Fog

Middle Clouds

Altocumulus

Altostratus

Page 30: NS2 3.2 Clouds and Fog

Altocumulus

• Gray or whitish layers, puffy, fleecy

• Made up of water droplets

• Sometimes produce a pale blue or

yellow corona

• Presence means rain is probable

within 24 hours

Page 31: NS2 3.2 Clouds and Fog

A cloud of a class characterized by

globular masses or rolls in layers or

patches, the individual elements

being larger and darker than those of

cirrocumulus and smaller than those

of stratocumulus: of medium

altitude, about 8,000 - 20,000 feet

Altocumulus

Page 32: NS2 3.2 Clouds and Fog

Altostratus

• Dense sheets of gray or blue

• Sun or Moon will show through but

without corona

• Light rain is likely within 24 hours

Page 33: NS2 3.2 Clouds and Fog

A cloud of a class characterized

by a generally uniform gray sheet

or layer, lighter in color than

nimbostratus and darker than

cirrostratus: of medium altitude,

about 8,000 - 20,000 feet

Altostratus

Page 34: NS2 3.2 Clouds and Fog

High Clouds

Cirrus

Cirrostratus

Cirrocumulus

Page 35: NS2 3.2 Clouds and Fog

Cirrus

• Thin, wispy, made up of ice crystals

• Called “mare’s tails”

• If scattered, indicate clear, cold

weather

• If in parallel lines, indicate violent

change in weather within 36 hours

Page 36: NS2 3.2 Clouds and Fog

Cirrostratus

• May nearly cover the sky with a filmy

cloud

• Curly appearance at their edges

• Form large halos around the Sun and

Moon

• Indicate clear and cold weather

Page 37: NS2 3.2 Clouds and Fog

A cloud of a class characterized

by a composition of ice crystals

and often by the production of

halo phenomena and appearing as

a whitish and usually somewhat

fibrous veil, often covering the

whole sky and sometimes so thin

as to be hardly discernible: of high

altitude, 20,000 - 40,000 feet

Cirrostratus

Page 38: NS2 3.2 Clouds and Fog

Cirrocumulus

• Thin, patchy clouds that sometimes

form in wavelike patterns

• Do not leave shadows

• Precipitation usually follows within

24 hours

Page 39: NS2 3.2 Clouds and Fog

A cloud of a class characterized

by thin, white patches, each of

which is composed of very small

granules or ripples: of high

altitude, 20,000 - 40,000 feet

Cirrocumulus

Page 40: NS2 3.2 Clouds and Fog

Thunderheads start at almost any

altitude and sometimes extend to

heights of as much as 75,000 feet. The

name given to these clouds is

__________.

a. nimbostratus

b. stratocumulus

c. cumulus

d. cumulonimbus

Page 41: NS2 3.2 Clouds and Fog

Thunderheads start at almost any

altitude and sometimes extend to

heights of as much as 75,000 feet. The

name given to these clouds is

__________.

a. nimbostratus

b. stratocumulus

c. cumulus

d. cumulonimbus

Page 42: NS2 3.2 Clouds and Fog

Clouds have been leading lost seamen,

navigators, and explorers to land since

the days of the earliest hardy sea

voyagers.

Page 43: NS2 3.2 Clouds and Fog

Stationary clouds on the horizon usually

indicate an island is close by.

Page 44: NS2 3.2 Clouds and Fog

In the tropics, clouds often reflect the

colors of the sandy beaches or coral

reefs below.

Page 45: NS2 3.2 Clouds and Fog

Precipitation (rain, snow, sleet, and hail)

cannot occur without clouds.

Page 46: NS2 3.2 Clouds and Fog

Temperature and presence of

hygroscopic nuclei or ice crystals

determine if there will be precipitation

and in what form it will take.

Page 47: NS2 3.2 Clouds and Fog

Raindrops form when moist air is

cooled to the point where the moisture

condenses into heavy drops.

Page 48: NS2 3.2 Clouds and Fog

Cloud moisture

droplets are

1/2,500 of an inch in

diameter. If the

droplet grows to

1/125 of an inch, it

will fall from the

cloud. The

combining of

moisture droplets is

called coalescence.

Large Raindrop

Small Raindrop

Not to Scale

Page 49: NS2 3.2 Clouds and Fog

To grow together into one body

Coalescence

Page 50: NS2 3.2 Clouds and Fog

Coalescence occurs in two known ways:

• Bigger droplets move about slowly,

bump into other droplets and combine

with them (low clouds).

Page 51: NS2 3.2 Clouds and Fog

Coalescence occurs in two known ways:

• Ice crystals and water droplets form

near each other, the droplets evaporate

and resulting vapor collides with ice

crystals and condenses into snow or

ice pellets. They melt into rain as they

pass through warmer air at lower

altitudes.

Page 52: NS2 3.2 Clouds and Fog

_________and the presence of

hygroscopic nuclei will determine

whether or not there will be precipitation

and what form it will take.

a. Humidity

b. Temperature

c. Altitude

d. Pressure

Page 53: NS2 3.2 Clouds and Fog

_________and the presence of

hygroscopic nuclei will determine

whether or not there will be precipitation

and what form it will take.

a. Humidity

b. Temperature

c. Altitude

d. Pressure

Page 54: NS2 3.2 Clouds and Fog

Rainmaking has been a concern of

humans since the most ancient times.

Page 55: NS2 3.2 Clouds and Fog

Rain dances, sacrifices, drums, cannons,

and smoke have all been used in an attempt

to make rain, especially during a drought.

Page 56: NS2 3.2 Clouds and Fog

A long period of dry weather that

is injurious to crops, animals, and

humans

Drought

Page 57: NS2 3.2 Clouds and Fog

Seeding a large cumulus cloud with one

pound of artificial nuclei made of dry-ice

or silver-iodide crystals can start a

shower.

Page 58: NS2 3.2 Clouds and Fog

Sowing or scattering clouds with

crystals or particles of silver iodide

or solid carbon dioxide to induce

precipitation

Seeding

Page 59: NS2 3.2 Clouds and Fog

A pale yellow, water-insoluble solid,

which darkens on exposure to light:

used chiefly in medicine, photography,

and artificial rain making

Silver-Iodide Crystals

Page 60: NS2 3.2 Clouds and Fog

Seeding can cause:

• Rain to fall sooner

• More rain to fall

• Rain to fall from a cloud that normally

would not produce rain

Page 61: NS2 3.2 Clouds and Fog

Seeding cannot cause:

• Rain to fall from fair skies or

fair-weather cumulus clouds

• Rain to fall over a large area

Page 62: NS2 3.2 Clouds and Fog

Sleet occurs when rain formed in relatively

warm air falls through a layer of freezing air.

Page 63: NS2 3.2 Clouds and Fog

Precipitation in the form of ice

pellets created by the freezing of

rain as it falls

Sleet

Page 64: NS2 3.2 Clouds and Fog

Hail usually occurs in the summertime. It

begins as raindrops, that updrafts take to

greater heights. They are coated with water

from lower clouds, lifted again and again until

too heavy to be lifted.

Page 65: NS2 3.2 Clouds and Fog

Showery precipitation in the form of

irregular pellets or balls of ice more

than 1/5 inch in diameter

Hail

Page 66: NS2 3.2 Clouds and Fog

Most hailstones are smaller than

marbles. Hailstones as large as

baseballs have killed people and

animals.

Page 67: NS2 3.2 Clouds and Fog

In wintertime, when the upper air is very

cold, water vapor will condense into ice

crystals. Snow is the result.

Page 68: NS2 3.2 Clouds and Fog

Dew is water vapor that condenses on

objects that have cooled below the

condensation point of the air around them.

Page 69: NS2 3.2 Clouds and Fog

Moisture condensed from the

atmosphere and deposited in

the form of small drops upon

any cool surface

Dew

Page 70: NS2 3.2 Clouds and Fog

Frost is similar to dew, but it forms

at temperatures below freezing.

Page 71: NS2 3.2 Clouds and Fog

A covering of minute ice needles,

formed from the atmosphere at

night upon the ground and other

exposed objects when they have

cooled by radiation below the

dew point, and when the dew

point is below the freezing point

Frost

Page 72: NS2 3.2 Clouds and Fog

Water vapor that has condensed on

objects that have cooled below the

freezing point is called ___________.

a. sleet

b. dew

c. hail

d. frost

Page 73: NS2 3.2 Clouds and Fog

Water vapor that has condensed on

objects that have cooled below the

freezing point is called ___________.

a. sleet

b. dew

c. hail

d. frost

Page 74: NS2 3.2 Clouds and Fog

Fog is really a low-lying cloud that is near

or touching the surface of the Earth.

Page 75: NS2 3.2 Clouds and Fog

A cloudlike mass or layer of minute

water droplets or ice crystals near

the surface of the Earth, appreciably

reducing visibility

Fog

Page 76: NS2 3.2 Clouds and Fog

Fog formation requires the presence of

moisture, a gentle breeze, and a combination

of warm and cold temperatures.

Page 77: NS2 3.2 Clouds and Fog

Fog is hazardous to aviation because

it limits both ceiling and visibility.

Page 78: NS2 3.2 Clouds and Fog

The height above ground level of

the lowest layer of clouds that cover

more than one half the sky

Ceiling

Page 79: NS2 3.2 Clouds and Fog

The distance at which a given standard

object can be seen and identified with

the unaided eye

Visibility

Page 80: NS2 3.2 Clouds and Fog

Fog at sea is a continual hazard

to safe navigation.

Page 81: NS2 3.2 Clouds and Fog

Fog at Sea

Page 82: NS2 3.2 Clouds and Fog

The nautical "Rules of the Road" require

that extra lookouts be stationed aboard

ship in foggy conditions.

Page 83: NS2 3.2 Clouds and Fog

Any of the regulations concerning

the safe handling of vessels with

respect to one another, imposed by

a government on ships in its own

waters or upon its own ships on the

high seas

Rules of the Road

Page 84: NS2 3.2 Clouds and Fog

Fog at sea is frequently formed through a

process known as advection. Fog is likely

to develop when warm air that has passed

over warm water moves to an area of colder

water.

Page 85: NS2 3.2 Clouds and Fog

The horizontal transport of atmospheric

properties

The horizontal flow of air, water, etc.

Advection

Page 86: NS2 3.2 Clouds and Fog

When warm moist air comes in contact

with colder water, advection fog forms.

Page 87: NS2 3.2 Clouds and Fog

Advection fog is the name given to

air-mass fog produced by air in motion,

or to fog formed in one place and

transported by wind to another. It will

usually dissipate when the Sun rises.

Page 88: NS2 3.2 Clouds and Fog

To scatter in various directions;

disperse; dispel

Dissipate

Page 89: NS2 3.2 Clouds and Fog

Every Sailor is aware of the fogs that

blanket the harbors and coastlines

near these areas.

Puget Sound

San Francisco

Los Angeles

San Diego

Newport

New York

Norfolk

Page 90: NS2 3.2 Clouds and Fog

Steam fog is a type of advection fog

formed by air saturation.

Page 91: NS2 3.2 Clouds and Fog

A condition in the atmosphere

corresponding to 100 percent

relative humidity

Saturation

Page 92: NS2 3.2 Clouds and Fog

In the far north, "sea smoke" can be seen

in the late fall or winter when a river or

pond "steams" as frigid air cools the water

until it begins to form ice.

Page 93: NS2 3.2 Clouds and Fog

Fog caused by cold air flowing over

a body of comparatively warm water,

the vapor condensing in small

convective columns near the water

surface and giving the appearance of

smoke or steam

Sea Smoke

Page 94: NS2 3.2 Clouds and Fog

The heat that the Earth radiates causes

radiation fog. It forms only at night,

over a land surface. The Sun usually

burns the fog away.

Page 95: NS2 3.2 Clouds and Fog

Fog produced by the nocturnal

cooling of the surface boundary

layer to a temperature at which

its content of water vapor

condenses

Radiation Fog

Page 96: NS2 3.2 Clouds and Fog

The movement of cold air masses

causes frontal fog. It is common in

the upper Midwest.

Page 97: NS2 3.2 Clouds and Fog

A fog caused by the movement of two

dissimilar air masses

Frontal Fog

Page 98: NS2 3.2 Clouds and Fog

A type of fog formed by air saturation is

called ______ fog.

a. steam

b. frontal

c. radiation

d. advection

Page 99: NS2 3.2 Clouds and Fog

A type of fog formed by air saturation is

called ______ fog.

a. steam

b. frontal

c. radiation

d. advection

Page 100: NS2 3.2 Clouds and Fog

Q.1. What does the term

hygroscopic nuclei mean?

Page 101: NS2 3.2 Clouds and Fog

Q.1. What does the term

hygroscopic nuclei mean?

A.1. Particles that readily absorb

moisture

Page 102: NS2 3.2 Clouds and Fog

Q.2. What are examples of

hygroscopic nuclei?

Page 103: NS2 3.2 Clouds and Fog

A.2. Particles that are present in the

air, such as dust, smoke, and

pollen

Q.2. What are examples of

hygroscopic nuclei?

Page 104: NS2 3.2 Clouds and Fog

Q.3. How are raindrops formed?

Page 105: NS2 3.2 Clouds and Fog

A.3. Raindrops are formed when

moist air is cooled to the point

where the moisture condenses

into heavy drops.

Q.3. How are raindrops formed?

Page 106: NS2 3.2 Clouds and Fog

Q.4. What are the three basic types

of clouds?

Page 107: NS2 3.2 Clouds and Fog

A.4. Cirrus, cumulus, and stratus

Q.4. What are the three basic types

of clouds?

Page 108: NS2 3.2 Clouds and Fog

Q.5. What does the prefix “fracto”

mean?

Page 109: NS2 3.2 Clouds and Fog

A.5. Fragmented or wind-blown

Q.5. What does the prefix “fracto”

mean?

Page 110: NS2 3.2 Clouds and Fog

Q.6. What clouds are made of water

droplets, sometimes laid out in

parallel bands?

Page 111: NS2 3.2 Clouds and Fog

A.6. Altocumulus clouds

Q.6. What clouds are made of water

droplets, sometimes laid out in

parallel bands?

Page 112: NS2 3.2 Clouds and Fog

Q.7. What accounts for the different

shapes and altitudes of clouds?

Page 113: NS2 3.2 Clouds and Fog

A.7. Changes in the atmospheric

conditions

Q.7. What accounts for the different

shapes and altitudes of clouds?

Page 114: NS2 3.2 Clouds and Fog

Q.8. What clouds are often called

“mares’ tails?”

Page 115: NS2 3.2 Clouds and Fog

A.8. Cirrus clouds

Q.8. What clouds are often called

“mares’ tails?”

Page 116: NS2 3.2 Clouds and Fog

Q.9. What altitudes are associated

with high, middle, and low

clouds?

Page 117: NS2 3.2 Clouds and Fog

A.9. High: above 20,000 ft.

Middle: 7,000 to 20,000 ft.

Low: surface to 7,000 ft.

Q.9. What altitudes are associated

with high, middle, and low

clouds?

Page 118: NS2 3.2 Clouds and Fog

Q.10. How are clouds generally

named?

Page 119: NS2 3.2 Clouds and Fog

A.10. According to their appearance

and altitude

Q.10. How are clouds generally

named?

Page 120: NS2 3.2 Clouds and Fog

Q.11. What are the main types of

low clouds?

Page 121: NS2 3.2 Clouds and Fog

A.11. Stratus, nimbostratus, and

stratocumulus

Q.11. What are the main types of

low clouds?

Page 122: NS2 3.2 Clouds and Fog

Q.12. What are the main types of

middle clouds?

Page 123: NS2 3.2 Clouds and Fog

A.12. Altocumulus and altostratus

Q.12. What are the main types of

middle clouds?

Page 124: NS2 3.2 Clouds and Fog

Q.13. What are the main types of

high clouds?

Page 125: NS2 3.2 Clouds and Fog

A.13. Cirrus, cirrostratus, and

cirrocumulus

Q.13. What are the main types of

high clouds?

Page 126: NS2 3.2 Clouds and Fog

Q.14. What type of weather is

associated with

cumulonimbus clouds?

Page 127: NS2 3.2 Clouds and Fog

A.14. Thunderstorms and

tornadoes

Q.14. What type of weather is

associated with

cumulonimbus clouds?

Page 128: NS2 3.2 Clouds and Fog

Q.15. What weather condition

follows cirrocumulus

clouds?

Page 129: NS2 3.2 Clouds and Fog

Q.15. What weather condition

follows cirrocumulus

clouds?

A.15. Precipitation