Fisher–KPP equation with free boundaries and time-periodic advections
We consider a reaction–diffusion–advection equation of the form: u t = u x x - β ( t ) u x + f ( t , u ) for x ∈ ( g ( t ) , h ( t ) ) , where β ( t ) is a T -periodic function representing the intensity of the advection, f ( t , u ) is a Fisher–KPP type of nonlinearity, T -periodic in t , g ( t )...
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Veröffentlicht in: | Calculus of variations and partial differential equations 2017-06, Vol.56 (3), p.1-36, Article 61 |
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Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
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Zusammenfassung: | We consider a reaction–diffusion–advection equation of the form:
u
t
=
u
x
x
-
β
(
t
)
u
x
+
f
(
t
,
u
)
for
x
∈
(
g
(
t
)
,
h
(
t
)
)
, where
β
(
t
)
is a
T
-periodic function representing the intensity of the advection,
f
(
t
,
u
) is a Fisher–KPP type of nonlinearity,
T
-periodic in
t
,
g
(
t
) and
h
(
t
) are two free boundaries satisfying Stefan conditions. This equation can be used to describe the population dynamics in time-periodic environment with advection. Its homogeneous version (that is, both
β
and
f
are independent of
t
) was recently studied by Gu et al. (J Funct Anal 269:1714–1768,
2015
). In this paper we consider the time-periodic case and study the long time behavior of the solutions. We show that a vanishing–spreading dichotomy result holds when
β
is small; a vanishing–transition–virtual spreading trichotomy result holds when
β
is a medium-sized function; all solutions vanish when
β
is large. Here the partition of
β
(
t
)
depends not only on the “size”
β
¯
:
=
1
T
∫
0
T
β
(
t
)
d
t
of
β
(
t
)
but also on its “shape”
β
~
(
t
)
:
=
β
(
t
)
-
β
¯
. |
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ISSN: | 0944-2669 1432-0835 |
DOI: | 10.1007/s00526-017-1165-1 |