threatened ice sheet integrity by: carl egede bøggild the university centre in svalbard, unis...

20
Threatened Ice sheet Integrity By: Carl Egede Bøggild The University Centre in Svalbard, UNIS Department of Arctic Geophysics

Post on 20-Jan-2016

214 views

Category:

Documents


0 download

TRANSCRIPT

Page 1: Threatened Ice sheet Integrity By: Carl Egede Bøggild The University Centre in Svalbard, UNIS Department of Arctic Geophysics

Threatened Ice sheet Integrity

By: Carl Egede BøggildThe University Centre in Svalbard, UNIS

Department of Arctic Geophysics

Page 2: Threatened Ice sheet Integrity By: Carl Egede Bøggild The University Centre in Svalbard, UNIS Department of Arctic Geophysics

Sea level and climate sensitivity

Page 3: Threatened Ice sheet Integrity By: Carl Egede Bøggild The University Centre in Svalbard, UNIS Department of Arctic Geophysics

Is the Greenland ice sheet threatened?

• yes/no/don’t know – is all true• New observational methods has

proven that past knowledge was not sufficient

• The mass balance becomes ever more negative

• No absolute method to assess the mass balance – and different methods deviate

Page 4: Threatened Ice sheet Integrity By: Carl Egede Bøggild The University Centre in Svalbard, UNIS Department of Arctic Geophysics

Greenland sea level and ocean circulation

Page 5: Threatened Ice sheet Integrity By: Carl Egede Bøggild The University Centre in Svalbard, UNIS Department of Arctic Geophysics

Ice sheet model predictions

An irreversible melt down may occur if around ¼ of the ice sheet mass is lost

Page 6: Threatened Ice sheet Integrity By: Carl Egede Bøggild The University Centre in Svalbard, UNIS Department of Arctic Geophysics

The principle of instability

Increase in ablation area

0

1

2

3

4

5

6

7

8

9

0 0.5 1 1.5 2 2.5

Dynamic effect

Page 7: Threatened Ice sheet Integrity By: Carl Egede Bøggild The University Centre in Svalbard, UNIS Department of Arctic Geophysics

An overview of results

• Climate models

• Gravity satellite

• Laser altimetry

• Radar altimetry

• SAR

Page 8: Threatened Ice sheet Integrity By: Carl Egede Bøggild The University Centre in Svalbard, UNIS Department of Arctic Geophysics

Why is it so difficult to measure changes?

Page 9: Threatened Ice sheet Integrity By: Carl Egede Bøggild The University Centre in Svalbard, UNIS Department of Arctic Geophysics

Melt water reaching the base

Page 10: Threatened Ice sheet Integrity By: Carl Egede Bøggild The University Centre in Svalbard, UNIS Department of Arctic Geophysics

Changes in calving fluxes

Is ice discharge climate or weather dependent?

Page 11: Threatened Ice sheet Integrity By: Carl Egede Bøggild The University Centre in Svalbard, UNIS Department of Arctic Geophysics

Ice sheet memory: response to the LIA

Page 12: Threatened Ice sheet Integrity By: Carl Egede Bøggild The University Centre in Svalbard, UNIS Department of Arctic Geophysics

Even different climate models produce different results

Page 13: Threatened Ice sheet Integrity By: Carl Egede Bøggild The University Centre in Svalbard, UNIS Department of Arctic Geophysics

Increased observed surface melt

Page 14: Threatened Ice sheet Integrity By: Carl Egede Bøggild The University Centre in Svalbard, UNIS Department of Arctic Geophysics

Is there a consensus?

IPCC: “loss of the Greenland ice sheet is likely not to occur in the 21st century”

Ice dynamics in the future:

-Assume that the flow accelerationwill persist unchanged-Scale up ice sheet discharge-Assume that the present imbalance is only transient

Page 15: Threatened Ice sheet Integrity By: Carl Egede Bøggild The University Centre in Svalbard, UNIS Department of Arctic Geophysics

How does all this relate to short lived pollutants?

Page 16: Threatened Ice sheet Integrity By: Carl Egede Bøggild The University Centre in Svalbard, UNIS Department of Arctic Geophysics

Carbon dates

y = -21.421x + 1335.5R2 = 0.7998

0

200

400

600

800

1000

1200

1400

0 10 20 30 40 50

Distance from margin (km)

year

bp

First results

-4000

-2000

0

2000

4000

6000

8000

10000

12000

0 20 40 60 80 100

Distance from margin (km)

year

s

regression line ofcarbon dates

carbon age after tuning8,5 times

carbon age withcorrection for modern+50% increase for 50years

D-J model h'=0 andc=400

- Aerosols and BC remains on the ice margin surface-15% albedo reduction => 1 meter of annual melt

Page 17: Threatened Ice sheet Integrity By: Carl Egede Bøggild The University Centre in Svalbard, UNIS Department of Arctic Geophysics

Results from NE-Greenland

Impurity: aerosols + micro organisms

Page 18: Threatened Ice sheet Integrity By: Carl Egede Bøggild The University Centre in Svalbard, UNIS Department of Arctic Geophysics

The effect of the “agricultural revolution”

Forest clearing in North-America can potentially have caused more BC

0

500

1000

1500

2000

2500

3000

3500

4000

0 20 40 60 80 100

Distance (km)

year

s b

p

BC ages

BC ages incl. AC contrib.

Model conditions: Excess BC 2 times, period 150-50 yr bp

Page 19: Threatened Ice sheet Integrity By: Carl Egede Bøggild The University Centre in Svalbard, UNIS Department of Arctic Geophysics

0

1

2

3

4

5

6

1875 1885 1895 1905 1915 1925 1935 1945 1955 1965 1975 1985 1995

10 yr. averages of industrial and charcoal soot(from Greenland ice core)

charcoal

industrial

McConnell et al. 2007. 20th-Century Industrial Black Carbon Emissions Altered Arctic Climate Forcing. Science Vol. 317. no. 5843, pp. 1381 - 1384

Modern industrial soot

Modelled BC ages

0

500

1000

1500

2000

2500

3000

3500

4000

0 20 40 60 80 100

Distance (km)

year

s b

p

Including modern soot

0

1000

2000

3000

4000

5000

6000

0 20 40 60 80 100

Distance (km)

year

s bp BC ages

BC ages w ith modern soot

Page 20: Threatened Ice sheet Integrity By: Carl Egede Bøggild The University Centre in Svalbard, UNIS Department of Arctic Geophysics

Modelled BC ages

0

500

1000

1500

2000

2500

3000

3500

4000

0 20 40 60 80 100

Distance (km)

year

s b

p

First guessStorage:500-2000 yrs

Short lived pollutants are not short lived in GreenlandResidence time to be estimated by modelling