Background Image
Table of Contents Table of Contents
Previous Page  66 / 78 Next Page
Information
Show Menu
Previous Page 66 / 78 Next Page
Page Background

FROZEN HEAT

66

In the East Siberian Arctic Shelf (ESAS, Fig. TB-3.2.1), methane

concentrations in the surface waters exceed typical seawater

values and far exceed the atmosphere’s equilibrium methane

concentrations (Shakhova

et al.

2010a). Shakhova

et al.

(2010b)

suggest methane is released into the atmosphere at an annual

rate of about 8 Tg of carbon (.008 GtC) for the ESAS alone,

Box 3.2

Methane release along the East Siberian Arctic Shelf

comparable to the rate expected for the rest of Earth’s oceans

combined. The present-day ESAS methane release rate is nearly 2

per cent of the nearly 450 Tg of methane carbon (.45 GtC) annually

released to the atmosphere from all sources globally (IPCC, 2007). A

current research challenge is to predict whether methane release rates

will increase significantly in response to ongoing climate change.

v

o

s

e

g

d

i

R

l

e

k

k

a

G

e

g

d

i

R

e

g

d

i

R

v

e

e

l

e

d

n

e

M

.

P

k

a

m

r

e

Y

.

R

Barents Sea

Kara Sea

Chukchi

Sea

0

100

1000

2000

3000

5000

Depth, metres

Source: adapted from NOAA

Arctic Ocean

East Siberian

Sea

NORTH POLE

East Siberian Arctic Shelf

EAST SIBERIAN

ARCTIC SHELF

Figure TB-3.2.1:

East Siberian Arctic Shelf (ESAS). The ESAS makes up a quarter of the Arctic shelf area (Shakhova

et al.

2010a), with an

average depth of only 58 metres (Jakobsson 2002) and significant riverine input.

East Siberian Arctic Shelf