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“Win
ter
is a
n et
chin
g,
sprin
g a
wat
erco
lor,
sum
mer
an
oil
pain
ting
and
autu
mn
a m
osai
c of
them
all”
-S
tanl
ey H
orow
itz
Wha
t We
Will
Lea
rn T
oday
•W
hat c
ause
s se
ason
s on
Ear
th?
•W
hy d
o w
e se
e ph
ases
of t
he M
oon?
The
Rea
son
for
Sea
sons
Why
is s
umm
er is
hot
ter
than
win
ter?
A.
The
Sun
bur
ns h
otte
r du
ring
sum
mer
B.
We
are
clos
er to
the
Sun
dur
ing
sum
mer
C.T
he E
arth
’s a
xis
is ti
lted
with
res
pect
to
the
eclip
ticD
.Ear
th r
otat
es s
low
er d
urin
g su
mm
er,
mak
ing
for
long
er d
ays
Clu
es R
egar
ding
Sea
sons
•D
ays
are
hotte
r in
the
sum
mer
•D
ays
are
long
er in
the
sum
mer
•S
easo
ns r
epea
t with
a p
erio
d of
one
ye
ar•
Sea
sons
are
mild
nea
r th
e E
quat
or
and
seve
re n
ear
the
pole
s•
Whe
n it
is s
umm
er h
ere,
it is
win
ter
in
Aus
tral
ia!
The
Rea
son
for
Sea
sons
Why
is s
umm
er is
hot
ter
than
win
ter?
A.
The
Sun
bur
ns h
otte
r du
ring
sum
mer
B.
We
are
clos
er to
the
Sun
dur
ing
su
mm
erC
.The
Ear
th’s
axi
s is
tilte
d w
ith r
espe
ct
to th
e ec
liptic
D.E
arth
rot
ates
slo
wer
dur
ing
sum
mer
, m
akin
g fo
r lo
nger
day
s
23.5
o
Nor
ther
n H
emis
pher
e S
umm
er
Sun
’s r
ays
The
Ecl
iptic
Sum
mer
Day
s A
re H
otte
r &
Lon
ger
Nor
ther
n H
emis
pher
e S
umm
er•
Vie
w fr
om th
e S
un–
Nor
ther
n H
emis
pher
e is
tilte
d to
war
ds th
e S
un–
Can
see
mor
e of
the
Nor
ther
n H
emis
pher
e–
Can
see
it fo
r lo
nger
as
Ear
th s
pins
(da
ys a
re
lo
nger
)–
Ray
s co
ncen
trat
ed in
NH
(d
ays
are
hotte
r)
The
Sea
sons
•N
ote:
The
sea
sons
are
nam
ed fr
om th
e no
rthe
rn
hem
isph
ere’
s pe
rspe
ctiv
e
Fig
2.1
5
Sun
’s P
ath
as S
een
Fro
m E
arth
+40o
0o
+90o
Dec
linat
ion
•V
iew
from
40o
N (
say
Col
umbu
s, O
H)
•S
un a
lway
s ris
es d
ue E
ast,
right
? N
o!–
NE
in s
umm
er, S
E in
win
ter,
E a
t equ
inox
es
Fig
S1.
17
Sun
’s P
ath
from
Pol
e &
Equ
ator
•S
un r
ises
& s
ets
ever
y da
y, r
ight
?–
Not
at t
he p
oles
!
Vie
w fr
om N
pol
eV
iew
from
Equ
ator
Fig
S1.
19F
ig S
1.20
Spe
cial
Lat
itude
s on
Ear
th
Bas
ed o
n S
un’s
pat
h in
the
sky F
ig S
1.18
The
Tro
pics
•B
etw
een
the
Tro
pics
of C
ance
r an
C
apric
orn
–S
un w
ill r
each
Zen
ith a
t noo
n on
two
days
of t
he y
ear
The
Arc
tic &
Ant
arct
ic C
ircle
s
•A
t the
se c
ircle
s, th
e S
un s
tays
abo
ve th
e ho
rizon
for
at le
ast o
ne d
ay p
er y
ear
–A
lso,
bel
ow th
e ho
rizon
!
•A
t the
pol
es, w
e ha
ve th
e ex
trem
es–
6 m
onth
s of
ligh
t and
6 m
onth
s of
dar
knes
s
Fig
2.1
8
Pha
ses
of th
e M
oon
•W
hat c
ause
s th
e ph
ases
of t
he
Moo
n?•
Wha
t are
the
phas
es?
•W
hen
does
the
Moo
n ris
e &
set
?
Moo
n’s
Mot
ion
in O
ur S
ky
•R
ises
Eas
t, S
ets
Wes
t–
Due
to E
arth
’s s
pin
•M
oves
Wes
t to
Eas
t–
Due
to M
oon’
s or
bit a
roun
d E
arth
•R
esul
t–
Moo
n ris
es 1
day
and
51 m
inut
es la
ter
each
day
(on
ave
rage
)
Moo
n P
hase
Dem
onst
ratio
n
Fig
2.2
2
Moo
n’s
Syn
chro
nous
Rot
atio
n
Fig
2.2
3
Mis
nom
er: D
ark
side
of t
he M
oon