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8/16/2019 Report Atmosphere

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JOHN PHILIP CHANREPORTER


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Atmosphere

“How do I livewithout you?”

Without the atmosphere, livingorganisms would not be able to

live.


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5/33“o !rote"tion”

With o AtmosphereWith Atmosphere

Example:


6/33Earth

Atmosphere

Example:


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Cmp!e!"s:

Air

#$one

Water %apor

&ust !arti"les


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A"msp#ere#ne ma'or reason why life is possible

Earth.#ther planet have also atmosphere but di(erent in"omposition.

)upiter

*ethane

Helium

%enus

*er"ury

%E+,%E+ -HI

A-*#!HE+E


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Cmpsi"i! $ Air

/0.10 22

31.40 2#2

1.45 2Ar

1.15 26#2

1.1170 2e

1.1118 2He 1.1178 26H4

1.1179 2:r 1.11118 2H2


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%a"er &apr

-he sour"e of all

6louds !re"ipitation


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WA-

E+

6 6;

E

traofo

anhe

abrel


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provide the nu"lei on whi"h moistur

"an "olle"t to form fogs, "louds andpre"ipitation.

'us" Par"i(les

Prism E$$e("opti"al phenomena ofhaving varied hues of redand orange during to thepresen"e of the dustparti"les.


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O)!e La*er*ole"ules that "ontains 5 atoms of

o


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A li=uid or solid that is >nely

dispersed in air and is in a stablestate.

Aersl

uspended variable in the atmosphere.

6louds mog


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A clear cloudless day-time s+* is

lue because molecules in the airscatter lue light from the sun more than

they scatter red light. When we look

towards the sun at sunset, we see red and

orange colors because the lue light hasbeen scattered out and away from the line

of sight.

%#* "#e s+* is lue-


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!roviding appropriate amount of

gases needed for photosynthesisand respiration

u!("i!s $ A"msp#ere

!hotosynthesis +espiration


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*oderator of temperature

u!("i!s $ A"msp#ere

Heat 6old


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!rote"tion from meteor parti"les

u!("i!s $ A"msp#ere

*eteor


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@ormation of "louds that brings

u!("i!s $ A"msp#ere

Weather 6limate


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;owest region of the earthBs

atmosphere, where masses of airare very well mi


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A thin layer forming the boundary

between the troposphere andstratosphere.

Trppause

- + # ! # ! A E


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-emperature in"reases as the

altitude in"rease and where o$onelayer is lo"ated.

/"ra"sp#ere


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Air masses are relatively mi


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;ayer of the atmosphere that is >rst

erst heated by the sun.

T#ermsp#ere


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+egion of the earthBs atmosphere

that is >lled with "harged parti"les.

I!sp#ere


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-he true upper limit of the earthBs

atmosphere.

Exsp#ere


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La*ers *

ele("ri(al prper"ies

eutral Atmosphere;ies below 91 miles

Ionosphere+egion of the earthBs atmosphere that is >lled with "

parti"les.*agnetosphere

*agneti" envelope shelters the earth from ioni$ed blthe solar wind.

Rei!s $ I!sp#ere


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Rei!s $ I!sp#ere& +egion

E


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La*ers *

i"s (mpsi"i!

Homosphere-urbulen"e "auses a "ontinuous mi

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