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63 Cards in this Set

  • Front
  • Back

clouds

an area of the atmosphere that saturated or supr saturated

Types of clouds :

warm clouds (T>-10) - consist exclusively of water droplets




cold clouds (T<-10) - tiny ice cristals. snow forms in here

Clouds attributes (names)on basis of altitude:

cirro : high level (always cold)




alto: mid level

clouds attributes (names) on basis of pattern

cumulo : vertically developed (cold)




strato: stratified, confined to a single level , layered (warm)


clouds attributes (names) based on ability to produce precipitation

nimbo: precipitation bearing (cold and warm)

Cloud types :

high clouds :


-cirrus


-cirrocumulos


-cirrostratus


-contrails



mid-clouds:


-altocummulus


-altostratus



low clouds:


-stratus


-nimbostratus


-stratocumulus


-cumulus


-cumulunimbus



High clouds:

always cold


altitude 20,000 +

cirrus:

High


cold


wispy


streched out


very thin


allow sun to shine throught

Cirrocumulos

*high


*fine grained appereance


*bubble like clouds


*interwoven with blue sky


*a little vertical development (rising motions with cloud elements, sinking motions surronding cloud elements )


*variation in vertical and horizontal air motions --> bumpy plane ride

cummulostratus

*high


*very thin


*cover the whole sky in a layered fashion given


- a ring-like appereance around the sun


- mini-rainbow; diffraction of light (sun dogs)

contrails:

-high


-trail of loud consisting of liquid water



1. condensation and largely deposition


2. water-vapor comes out of plane engines and instantaneously turns to ice crystals


3. the relative humidity is close to 100%


middle clouds:

8000- 20,000

altocumulus:

middle clouds


warm


similar to cirrocumulus just lower in the column

altostratus:

*middle clouds


*warm


*thicker


*lower in the atmosphere so block out sunlight more than cirrostratus


*ring around the sun

low clouds :

500 to 8,000 high

stratus

*low level


*stratified


*effectively block out the sun


(can produce drizzle, but not measurable

Nimbostratus

*low thicker


*darker


*producing recipitation


*streaked appereance



rather featureless as falling precipitation obscures cloud edges

stratocumulus

*low


*stratified


*not thick


*connected with a stable atmosphere


(air doesn't want to move vertically )



note that the dark clouds are associated with a low sun angle

clouds associated with vertical development

cumulus


cumulunimbus



cumulus:

*low level


*unstable atmosphere(Air is lifting )


*daytime heating when the relative humidity is high


*vertical development


*late morning hours in carolina summer



*common with daytime heating when the relative hummidity is relatively high


*show some vertical development (deeper instability )


cumulonimbus

*largest clouds


*dark bottom


*thunderstorm

precipitation

requires the development of droplet/ snowflakes that are 100 times bigger than cloud water droplets/ice crystals



most clouds don't have precipitation

two processes for growing hydrometeors

a. bergeon



b. collision-coallecence

hydometeors:

refers to any type of precipitation

Bergeron process definition :

grows ice crystal through multiple processes involving all 3 stages of water



requires a cold cloud where ice crystals, water vapor, and supercooled water coexist.

bergeron processes:

deposition of vapor --> ice crystals growth. '



removal of water around ice crystals so relative humidity drops



rising air motions keep growing snowflakes aloft until it becomes too heavy

what is the dominant process in bergeon

deposition is the dominant process

is it possible for the bergeron process to occur in lower altitudes creating snow?

yes, on winter when the surface temperature is cold enough

what appereance the bergeron process gives to clouds?

porvides a distinct glazed and/or streaked appereance

bergeron porcess OFTEN produces ice cristals taht acts like seeds for growing hydrometers bellow in the lower portion of the clouds ?

true

what types of clouds does bergeron process occur normally?

high cold clouds

cirrus (image)

cirrucumulus (image)

cirrostratus (image)

contrails (image)

altocumulus(image)

altostratus (image)

stratus(image)

startus 2 (image)

nimbostratus(image)

stratocumulus (image)

cumulus (image)

cumulunimbus (image)

Bergeron proceess (image)starting

bergeron process (image ) cold situation

why do bereron process louds have that aspect ?

when it produces snowflake steh refelcton of light make them look like tehy are falling or rotating

collision coalescence

hydrometers growth as it collides with smaller dropplets through the sky

collision coallescenece characteristics

only preciotation formation that pperates in warm clouds



can supplement bergeon process in cold clouds



large cloud droplets falls through smaller cloud droplets accumulating them along the way

seeder-feeder process

combination of bergeron and collision coalescence (warmer droplets are feeding teh seeds)

seeder feeder scenario 1:

rain dropletsfrom melted snowflakes are feed by the warm cloud water droplets

seeder feeder scenario 2:

cloud water droplets freeze on falling snowflakes, ina a process called riming teh snowflakes growth in size as it falls though the warmer parts of the cloud

is it possible to determine the degree at which a snowflake has being rimed ?

yes it si

precipitation rate:

amount of precipitation per a given amound of time

controls on precipitation rate:

1. amount of water vapor condensed / deposited out





2. rate of lifting

amount of WV condensed/deposited depends on :

- air temperature



-proximity to warm body of water

rate of lifting:

how quickly the air is being lifted up

rate of lifting depends on:

convective lift an order of magnitude



(stronger teh lift the moretiem teh bergeron process has to make snowflakes


how faster is the convective lift from the frontal lifts ?

convective lift 10-50 times faster

Two precipitation types:

stratiform



convective

startiform


*sudden changes in temperature, humidity and pressure of air



*warm mets the cold ar and warm is forced to rise



*less intense with over a longer perod time than convective

convective

*precipitation falls as a showers with rapidly changing intensify over a certain areas for a relative short time



*mainly in a conditionally unstable or moist atmosphere

what type of clouds produce startiform precipitation?

nimbostratus

what type of cloud produces convective precipitaton?

cumulonimbus