AOSS 605 (004)
Climate and Gla
Define ice sheet bed:
Define balance rate: The e
Steady-state mass balance dictates:
aciers Revisited
equilibrium line elevation
AOSS 605 (004)
Climate and Gla
Define ice sheet bed:
Define balance rate: The e
Steady-state mass balance dictates:
aciers Revisited
equilibrium line elevation
AOSS 605 (004)
Climate and Gla
Define ice sheet bed:
Define balance rate: The e
Steady-state mass balance dictates:
aciers Revisited
equilibrium line elevation
AOSS 605 (004)
Climate and Gla
aciers Revisited
AOSS 605 (004)
Climate and Gla
aciers Revisited
AOSS 605 (004)
Climate and Gla
aciers Revisited
AOSS 605 (004)
Climate and Gla
aciers Revisited
AOSS 605 (004)
Climate and Gla
aciers Revisited
AOSS 605 (004)
Climate and Gla
Assume plastic in a global sense:
aciers Revisited
AOSS 605 (004)
Climate and Gla
Assume plastic in a global sense:
aciers Revisited
Steady-state length (km)AOSS 605 (004)
Climate and Gla
120
τ0 = 100 kPa
z0 - E = 500 m
60
0
0
Sl
aciers Revisited
a
m
0.1 0.2
lope
Steady-state length (km)AOSS 605 (004)
Climate and Gla
120
τ0 = 100 kPa
z0 - E = 500 m
60
0
0
Sl
aciers Revisited
Small slopes - large glacier?
a
m
0.1 0.2
lope
AOSS 605 (004)
Climate and Gla
Small slope means glacier has to g
drop beneath the equilibrium line
Equilibrium line
aciers Revisited
Small slopes - large glacier?
grow large to
AOSS 605 (004)
Climate and Gla
Large slope means that as th
moves beneath the equilibrium
Equilibrium line
aciers Revisited
Small slopes - large glacier?
he glacier grows it
m line quickly
AOSS 605 (004)
A first look at cl
limate sensitivity
AOSS 605 (004)
A first look at cl
limate sensitivity
AOSS 605 (004)
A first look at cl
Glaciers on a be
sensitive than gl
slope
limate sensitivity
ed with a small slope are more
laciers on a bed with a large
AOSS 605 (004)
A first look at cl
Glaciers on a be
sensitive than gl
slope
Fractional change in length:
limate sensitivity
ed with a small slope are more
laciers on a bed with a large
AOSS 605 (004)
Climate sensitivit
Recall: E = elevati
ty and lapse rate
ion of equilibrium line
AOSS 605 (004)
Climate sensitivit
Recall: E = elevati
Lapse rate
ty and lapse rate
ion of equilibrium line (z)
AOSS 605 (004)
Climate sensitivit
Recall: E = elevati
Lapse rate
Change in equilibri
ty and lapse rate
ion of equilibrium line (z)
ium line with temp.
AOSS 605 (004)
Climate sensitivit
Recall: E = elevati
Lapse rate
Change in equilibri
ty and lapse rate
ion of equilibrium line (z)
ium line with temp.
dL/dTa (km/K)AOSS 605 (004)
Climate sensitivit
0
γ = -4 K/km
γ = -6 K/km
γ = -10 K/km
-5
-100 Slope
ty and lapse rate
e 0.2