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des; 1 itu 0 H at m -l il e reaches -7 ° 0 FW um id m i h is is whe in re e. Th po e to f th Th tropo
er
ht
ig
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L here:
Fall to near ze ro W r e : e this h e gh tu ov i h b r a ce. A l and mag t, it net is a pa n tio ntains th i co a u r o e r
ayer:
What do w 8°F e
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er: y a
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om t
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tmosphe r A r e” te miles T e m 0 u p o 40,00 e same as outer to e h s is t h’s gra es e Eart vita h
sph exo ere re the r he
her wi get th to ight th (ab e H know?: Th o v e e at o we d m e e at ly th “atmosp os on h x e e r t d l s e o c fi agneto m m a e ap
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t
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ve
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(above ear th ht Equato ’s ig at r Te s es n o k w e ?: C w m o on d t at d almo s e an lif ropos t a p et
p
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m
yer a L
spher
miles T e
her re, make phe s u os h’s sur face ): p “ r m a r t ensity at 6 U d e , 000 c i r mi p e l ph s e e n h s t e n tha e” i tt er influence. Th e e e r , he w sp pea
30
sp
ermo Th
The Earth’s atmosphere is 78.08 percent nitrogen, 20 95 percent oxygen, 0 93 percent argon, and 0.03 percent carbon dioxide.
Exos :
):
r
mass of th ea
is the o
p atros here str
Atmospheric Zones
ure: erat De cre mp Te e to give “shooti as ng zo n es s i th s, and th a e y cle re rt i which ra off e co m tel
Height ( ab ov again at top W e g n i hat is r do re here, this laye p s rc o o rm os e ion phere h t t e nc o a ou ati o n
tains 24% of th on e
ce
ow
?: C
ar th’s s e e ur f
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ov
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b (a
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Meso : s u r f a c e ) : 50 ’s m th il r : Meteors burn u ea pi o w? n n k e w s many ionized ain pa nt is is the lay er th w radio llo s
miles ; 7 a t es m ol very 1,000 ft u p p; °F e m .6 of the atmos ph ass is found. d the lle
at ature: Drop s p 5% of the total s7 m ain f our weath ll o e is c a h er
er
tm
fa
sp
ur
Strato
5 mile s ce):
ase to -166 F at b °F, 20° be m ether with t fo h fro s;” tog et he r es a tively terme st llec d co signals b dio uni m c