Graphics Reference
In-Depth Information
Proof.
See [Hirs76]. Hirsch also explains why one needs the strange constraint
on r.
[Hirs76] gives a number of applications of this theorem and Theorem 8.11.3. For
example, one can use it to give a fairly simple proof of the fact that there is no dif-
ferentiable retraction f :
M
Æ∂
M
(see Exercise 8.11.1 and compare this result with
Theorem 7.5.1.4) and the Brouwer fixed-point theorem that every differentiable map
f:
D
n
Æ
D
n
has a fixed point. The standard proofs of the continuous versions of these
theorems involve algebraic topology. We shall sketch two applications of Theorem
8.11.3 and the Morse-Sard Theorem. The first results in an alternate definition of the
degree of a map and the second deals with intersection numbers, vector fields, and
the Euler characteristic. The transversality approach to these results will give us addi-
tional insights into the underlying geometry.
Let (
M
n
,s) and (
N
n
,m) be closed compact connected oriented differentiable man-
ifolds and assume that
n
n
f
:
MN
Æ
is a differentiable map. By the Morse-Sard theorem, f has regular values. Let
q
Œ
N
be one such regular value for f. By Theorem 8.11.3 and the compactness of
M
, f
-1
(
q
)
consists of a finite number of isolated points. Let
p
Œ f
-1
(
q
).
Definition.
The
degree of f at
p
, deg
p
f, is defined by
deg
p
f = +1,
if Df(
p
) maps T
p
(
M
) in an orientation preserving way to T
q
(
N
)
= -1,
if Df(
p
) maps T
p
(
M
) in an orientation reversing way to T
q
(
N
).
Define the
degree of f over
q
, deg(f,
q
), by
Â
1
()
=
-
1
()
π
deg
f
,
q
deg
f
,
if f
q
f
,
p
-
pq
Œ
f
(
)
=
0
,
otherwise
.
Note that since the set f
-1
(
q
) is finite, the sum in the definition of deg(f,
q
) is finite.
Figure 8.35 attempts to show what we are doing in the case of a map f :
S
1
Æ
S
1
. The
map f indicated in the figure has f
-1
(
q
) = {
p
1
,
p
2
,
p
3
}, so that, with the orientations as
shown,
(
)
=-+=
deg f,
q
111 1
.
Observe also that if we assume that f(
S
1
) is a rubber band and pull it tight, then the
two point
p
2
and
p
3
in the pre-image of
q
disappear but the degree over
q
of the new
map is still 1. This “pulling tight” corresponds to changing the map f by a homotopy
and should suggest that homotopies do not change the degree.
8.11.7. Example.
Define f :
S
1
Æ
S
1
by f(
z
) =
z
n
,
z
Œ
C
. Then deg(f,1) = n
because the n nth roots of unity map to 1 in an orientation-preserving way (Exercise
8.11.2).