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Stable isotope records for the past 1000 years from 5 ice cores in central Dronning Maud Land (DML)

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Stable isotope records for the past 1000 years from 5 ice

cores in central

Dronning Maud Land (DML)

Hans Oerter, Sepp Kipfstuhl, Frank Wilhelms

Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany

European Science Foundation -

EuroPOLAR

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EPICA - European Project for Ice Core drilling in Antarctica

Interglacial

5.5 7.5

9.3 11.3

13.3 17.3

19.3 15.5 1

MIS 5.5 MIS 1

AIM corresp. D/O events

?

-8 -4 0 4

Temperature difference (°C)

150 140 130 120 110 100 90 80 70 60 50 40 30 20 10 0 Time EDML1 (kilo years BP)

-8 -4 0 4

800 750 700 650 600 550 500 450 400 350 300 250 200 150 100 50 Time EDC3 (kilo years BP) 0

Mean 1000-2000 A.D.

1950 A.D.

1950 A.D.

Jouzel et al., Orbital and Millennial Antarctic Climate Variability over the Past 100,000 Years. Science 317, 793-796 (2007)

EPICA Dome C

(EDC)

EPICA community members, One-to-one coupling of glacial climate variability in Greenland and Antarctica. Nature 444, 195-198 (2006)

EPICA

DML

(EDML)

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EDML - Kohnen station B32

B33 B34 B37

Satellite Image Map Dronning Maud Land 1:2000000, Draft Vers.4.2, BKG, Frankfurt am Main, Nov.1998 (detail)

75°S 0°4‘E, 2782 m a.s.l., acc. rate 65 mm w.e./a; -44.6 °C

75°S 0°0.4‘E, 2782 m asl,

75°10‘S 6°30‘E, 3160 m a.s.l.

47 mm w.e./a; -46.2°C

75°S 0°E, 2782 m asl,

75°S 0°E, 2782 m asl,

(2001-2006)

(1997/98)

(1997/98) (2004/05)

(2005/06)

Neumayer

B32, B34, B37 EDML/Kohnen

B33

5°W 0° 5°E

76°S 76°S

75°S 74°S

73°S 70°S

75°S

10°W 10°E

EDML - Kohnen station B32

B33 B34 B37

Satellite Image Map Dronning Maud Land 1:2000000, Draft Vers.4.2, BKG, Frankfurt am Main, Nov.1998 (detail)

75°S 0°4‘E, 2782 m a.s.l., acc. rate 65 mm w.e./a; -44.6 °C

75°S 0°0.4‘E, 2782 m asl,

75°10‘S 6°30‘E, 3160 m a.s.l.

75°S 0°E, 2782 m asl,

75°S 0°E, 2782 m asl,

(2001-2006)

(1997/98)

(1997/98) (2004/05)

(2005/06)

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Example for lab measurements: δ 18 O and DEP at core B37

Depth (m w.e.)

Depth (m)

Delta 18-O (‰-SMOW) Electrical conductivity (µS/m)

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Synchronizing the cores

0: snow surface Jan. 2000

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Synchronizing the cores grey: original

red: adjusted to EDML 1259 A.D.

1816

B32, B33: Oerter et al.: Annals Glac. (1999); www.pangaea.de 0: snow surface Jan. 2000

1452

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Deviation δ 18 O from average 1816 A.D. (Tambora) through 1259 A.D. (Unknown)

-46.99‰

-44.98‰

-45.07‰

-44.81‰

-45.19‰

Depth for each core on own scale Common period 1816-1259 A.D.

Mean

1816-1259 A.D.

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Adjusting the depth of the cores to the EDML depth scale

depth on own scale depth on EDML scale

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Common depth (m w.e.) & sample interval (65mm w.e.)

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Correlation B32, B33, B34 , B37 with EDML

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The stacked record of 5 cores

isotope-temperatur e gradient: 0.69 ±0.04 δ 18 O-‰ / °C

sample length 65 mm w.e.

moving average 11 samples

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Oerter et al.: Accumulation rates in Dronning Maud Land, Antarctica, as revealed by dielectric-profiling measurements of shallow firn cores. Annals of Glaciology 30, 27-34 (2000)

Stack of annual means

Deviation

from average 1801-1997

1801-1905:

δ 18 O: -0.010 ‰/a

Acc.: -0.120 kg m -2 a -1 /a Tambora 1815

20 10 0 -10

-2 -1 Accum. (kg m a ) -20

2000 1950

1900 1850

1800 Years A.D.

2 1 0 -1

18 δ O (‰-SMOW) -2

10 firn cores

13 firn cores

Krakatau 1883

1905-1997:

δ 18 O: +0.009 ‰/a

Acc.: +0.068 kg m -2 a -1 /a

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b

1816 1884 1964

ca. 26m ca. 18m ca. 8m

long term snow accumulation ca. 65 kg m -2 a -1

DML stack + EDML core + B34 core + B35 core

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Thank you for your attention !

foto: hans oerter, 2006

European Science Foundation - EuroPOLAR

Acknowledgement:

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