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Tim Helweg-Larsen & Richard Hawkins

Tim Helweg-Larsen & Richard Hawkins. The Arctic

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Page 1: Tim Helweg-Larsen & Richard Hawkins. The Arctic

Tim Helweg-Larsen & Richard Hawkins

Page 2: Tim Helweg-Larsen & Richard Hawkins. The Arctic
Page 3: Tim Helweg-Larsen & Richard Hawkins. The Arctic

The Arctic

Page 4: Tim Helweg-Larsen & Richard Hawkins. The Arctic

1989

Page 5: Tim Helweg-Larsen & Richard Hawkins. The Arctic

2007

Page 6: Tim Helweg-Larsen & Richard Hawkins. The Arctic

1989 2007

Page 7: Tim Helweg-Larsen & Richard Hawkins. The Arctic

Arctic Sea Ice ExtentArea of ocean with at least 15% sea ice

Page 8: Tim Helweg-Larsen & Richard Hawkins. The Arctic

1989

Page 9: Tim Helweg-Larsen & Richard Hawkins. The Arctic

2007

Page 10: Tim Helweg-Larsen & Richard Hawkins. The Arctic

1989 / 2007

+ 5 years − 5 years Ocean

Age of Arctic Sea Ice

Page 11: Tim Helweg-Larsen & Richard Hawkins. The Arctic

IPCC, WG I (2007)

… late summer sea-ice is projected to

disappear almost completely towards the end of the 21st century

Page 12: Tim Helweg-Larsen & Richard Hawkins. The Arctic
Page 13: Tim Helweg-Larsen & Richard Hawkins. The Arctic

“The Arctic Ocean could be nearly ice-free at the end of summer by 2012”

Dr Jay Zwally, NASA

“Our projection of 2013 is alreadytoo conservative.”

Dr Wieslaw Maslowski, US Navy

“Worst-case scenarios about sea-ice loss are coming true: the Arctic Ocean could be ice-

free in summertime as soon as 2010”

Louis Fortier, Université Laval

Page 14: Tim Helweg-Larsen & Richard Hawkins. The Arctic
Page 15: Tim Helweg-Larsen & Richard Hawkins. The Arctic

Mark Serreze, NSIDC

No matter where we stand at the end of the

melt season, it’s just reinforcing this notion that the Arctic ice is in

its death spiral.

Page 16: Tim Helweg-Larsen & Richard Hawkins. The Arctic

So what?

Page 17: Tim Helweg-Larsen & Richard Hawkins. The Arctic

Over and above existing model projections

Page 18: Tim Helweg-Larsen & Richard Hawkins. The Arctic
Page 19: Tim Helweg-Larsen & Richard Hawkins. The Arctic

1989 2012?

Page 20: Tim Helweg-Larsen & Richard Hawkins. The Arctic

Albedo%

of

rad

iati

on

refl

ecte

d

Hugo Ahlenius,UNEP/GRID-Arendal

0.3°C

Page 21: Tim Helweg-Larsen & Richard Hawkins. The Arctic
Page 22: Tim Helweg-Larsen & Richard Hawkins. The Arctic
Page 23: Tim Helweg-Larsen & Richard Hawkins. The Arctic
Page 24: Tim Helweg-Larsen & Richard Hawkins. The Arctic

Permafrost extent in the Northern Hemisphere, http://maps.grida.no/go/graphic/permafrost-extent-in-the-northern-hemisphere

Page 25: Tim Helweg-Larsen & Richard Hawkins. The Arctic
Page 26: Tim Helweg-Larsen & Richard Hawkins. The Arctic

1672billion

tonnes

Page 27: Tim Helweg-Larsen & Richard Hawkins. The Arctic
Page 28: Tim Helweg-Larsen & Richard Hawkins. The Arctic

0.1% melt = 1600mtc

80% global cut

=1600mtc

Page 29: Tim Helweg-Larsen & Richard Hawkins. The Arctic

Existing coupled climate models lack a

robust treatment of soil carbon dynamics.

Page 30: Tim Helweg-Larsen & Richard Hawkins. The Arctic
Page 31: Tim Helweg-Larsen & Richard Hawkins. The Arctic
Page 32: Tim Helweg-Larsen & Richard Hawkins. The Arctic

The [IPCC] range does not include

… contributions from rapid dynamic processes in the

Greenland and West Antarctic ice sheets which… could

eventually raise sea level by many meters. Lacking such

processes… projections based on such models may seriously

understate potential future increases.

Oppenheimer et al.

Page 33: Tim Helweg-Larsen & Richard Hawkins. The Arctic

IPCC, Synthesis (2007)

“Because understanding of some important effects driving

sea-level rise is too limited, this report does not assess the

likelihood, nor provide a best estimate or an upper bound for

sea-level rise… therefore the upper values of the ranges are

not to be considered upper bounds for sea-level rise.”

Page 34: Tim Helweg-Larsen & Richard Hawkins. The Arctic
Page 35: Tim Helweg-Larsen & Richard Hawkins. The Arctic
Page 36: Tim Helweg-Larsen & Richard Hawkins. The Arctic

Over and above existing model projections

Additional

Page 37: Tim Helweg-Larsen & Richard Hawkins. The Arctic

endthe

Page 38: Tim Helweg-Larsen & Richard Hawkins. The Arctic

Tim Helweg-Larsen & Richard Hawkins