T. Blunier

Publication List Details

Period

1999 - 2007

Number

38

Co-Authors

Climatic Changes (2007)

S. Valututti, S. Müller, M. Cella, E. Padovan, A. Lanzavecchia, H. M. Mcconnell, ...

40. The density and number of accumulated molecules in different regions of the contact area were calculated as the accumulated density (molecules/ �m 2) � {[intensity in masked area...

New constraints on the gas age-ice age difference along the EPICA ice cores, 0-50 kyr (2007)

Loulergue, L., Parrenin, F., Blunier, T., Spahni, R., Schilt, A., ...

Gas is trapped in polar ice sheets at 50–120m below the surface and is therefore younger than the surrounding ice. Firn densification models are used to evaluate this ice age-gas age difference...

The EDC3 chronology for the EPICA Dome C ice core (2007)

Parrenin, F., Beer, J., Blunier, T., Castellano, E., Chappellaz, J., ...

The EPICA (European Project for Ice Coring in Antarctica) Dome C drilling in East Antarctica has now been completed to a depth of 3260 m, at only a few meters above bedrock. Here we present the new...

New constraints on the gas age-ice age difference along the EPICA ice cores, 0-50 kyr (2007)

Loulergue, L., Parrenin, F., Blunier, T., Spahni, R., Schilt, A., ...

Gas is trapped in polar ice sheets at 50–120m below the surface and is therefore younger than the surrounding ice. Firn densification models are used to evaluate this ice age-gas age difference...

The EDC3 chronology for the EPICA Dome C ice core (2007)

Parrenin, F., Beer, J., Blunier, T., Castellano, E., Chappellaz, J., ...

The EPICA (European Project for Ice Coring in Antarctica) Dome C drilling in East Antarctica has now been completed to a depth of 3260 m, at only a few meters above bedrock. Here we present the new...

New constraints on the gas age-ice age difference along the EPICA ice cores, 0–50 kyr (2007)

Loulergue, L., Parrenin, F., Blunier, T., Spahni, R., Schilt, A., ...

Gas is trapped in polar ice sheets at ~50–120 m below the surface and is therefore younger than the surrounding ice. Firn densification models are used to evaluate this ice age-gas age difference...

The EDC3 chronology for the EPICA Dome C ice core (2007)

Parrenin, F., Beer, J., Blunier, T., Castellano, E., Chappellaz, J., ...

The EPICA (European Project for Ice Coring in Antarctica) Dome C drilling in East Antarctica has now been completed to a depth of 3260 m, at only a few meters above bedrock. Here we present the new...

"EDML1": a chronology for the EPICA deep ice core from Dronning Maud Land, Antarctica, over the last 150 000 years (2007)

Ruth, U., Beer, J., Bigler, M., Blunier, T., Castellano, E., ...

A chronology called EDML1 has been developed for the EPICA ice core from Dronning Maud Land (EDML). EDML1 is closely interlinked with EDC3, the new chronology for the EPICA ice core from Dome-C (EDC)...

Synchronization of ice core records via atmospheric gases (2007)

Blunier, T., Spahni, R., Chappellaz, J., Loulergue, L., Schwander, J.

To interpret new high resolution climate records it becomes more and more important to know about the succession of climate events. Such knowledge is hard to get especially when dealing with...

The EDC3 chronology for the EPICA Dome C ice core (2007)

Parrenin, F., Beer, J., Blunier, T., Castellano, E., Chappellaz, J., ...

The EPICA (European Project for Ice Coring in Antarctica) Dome C drilling in East Antarctica has now been completed to a depth of 3260 m, at only a few meters above bedrock. Here we present the new...

"EDML1": a chronology for the EPICA deep ice core from Dronning Maud Land, Antarctica, over the last 150 000 years (2007)

Ruth, U., Beer, J., Bigler, M., Blunier, T., Castellano, E., ...

A chronology called EDML1 has been developed for the EPICA ice core from Dronning Maud Land (EDML). EDML1 is closely interlinked with EDC3, the new chronology for the EPICA ice core from Dome-C (EDC)...

New constraints on the gas age-ice age difference along the EPICA ice cores, 0–50 kyr (2007)

Loulergue, L., Parrenin, F., Blunier, T., Spahni, R., Schilt, A., ...

Gas is trapped in polar ice sheets at ~50–120 m below the surface and is therefore younger than the surrounding ice. Firn densification models are used to evaluate this ice age-gas age difference...

Synchronization of ice core records via atmospheric gases (2007)

Blunier, T., Spahni, R., Chappellaz, J., Loulergue, L., Schwander, J.

To interpret new high resolution climate records it becomes more and more important to know about the succession of climate events. Such knowledge is hard to get especially when dealing with...

New constraints on the gas age-ice age difference along the EPICA ice cores, 0–50 kyr (2007)

Loulergue, L., Parrenin, F., Blunier, T., Spahni, R., Schilt, A., ...

Gas is trapped in polar ice sheets at ~50–120 m below the surface and is therefore younger than the surrounding ice. Firn densification models are used to evaluate this ice age-gas age difference...

The EDC3 chronology for the EPICA Dome C ice core (2007)

Parrenin, F., Beer, J., Blunier, T., Castellano, E., Chappellaz, J., ...

The EPICA (European Project for Ice Coring in Antarctica) Dome C drilling in East Antarctica has now been completed to a depth of 3260 m, at only a few meters above bedrock. Here we present the new...

"EDML1": a chronology for the EPICA deep ice core from Dronning Maud Land, Antarctica, over the last 150 000 years (2007)

Ruth, U., Beer, J., Bigler, M., Blunier, T., Castellano, E., ...

A chronology called EDML1 has been developed for the EPICA ice core from Dronning Maud Land (EDML). EDML1 is closely interlinked with EDC3, the new chronology for the EPICA ice core from Dome-C (EDC)...

Synchronization of ice core records via atmospheric gases (2007)

Blunier, T., Spahni, R., Chappellaz, J., Loulergue, L., Schwander, J.

To interpret new high resolution climate records it becomes more and more important to know about the succession of climate events. Such knowledge is hard to get especially when dealing with...

The EDC3 chronology for the EPICA Dome C ice core (2007)

Parrenin, F., Beer, J., Blunier, T., Castellano, E., Chappellaz, J., ...

The EPICA (European Project for Ice Coring in Antarctica) Dome C drilling in East Antarctica has now been completed to a depth of 3260 m, at only a few meters above bedrock. Here we present the new...

"EDML1": a chronology for the EPICA deep ice core from Dronning Maud Land, Antarctica, over the last 150 000 years (2007)

Ruth, U., Beer, J., Bigler, M., Blunier, T., Castellano, E., ...

A chronology called EDML1 has been developed for the EPICA ice core from Dronning Maud Land (EDML). EDML1 is closely interlinked with EDC3, the new chronology for the EPICA ice core from Dome-C (EDC)...

New constraints on the gas age-ice age difference along the EPICA ice cores, 0–50 kyr (2007)

Loulergue, L., Parrenin, F., Blunier, T., Spahni, R., Schilt, A., ...

Gas is trapped in polar ice sheets at ~50–120 m below the surface and is therefore younger than the surrounding ice. Firn densification models are used to evaluate this ice age-gas age difference...

Synchronization of ice core records via atmospheric gases (2007)

Blunier, T., Spahni, R., Chappellaz, J., Loulergue, L., Schwander, J.

To interpret new high resolution climate records it becomes more and more important to know about the succession of climate events. Such knowledge is hard to get especially when dealing with...

New constraints on the gas age-ice age difference along the EPICA ice cores, 0–50 kyr (2007)

Loulergue, L., Parrenin, F., Blunier, T., Spahni, R., Schilt, A., ...

Gas is trapped in polar ice sheets at ~50–120 m below the surface and is therefore younger than the surrounding ice. Firn densification models are used to evaluate this ice age-gas age difference...

The EDC3 chronology for the EPICA Dome C ice core (2007)

Parrenin, F., Beer, J., Blunier, T., Castellano, E., Chappellaz, J., ...

The EPICA (European Project for Ice Coring in Antarctica) Dome C drilling in East Antarctica has now been completed to a depth of 3260 m, at only a few meters above bedrock. Here we present the new...

The EDC3 chronology for the EPICA Dome C ice core (2007)

Parrenin, F., Beer, J., Blunier, T., Castellano, E., Chappellaz, J., ...

The EPICA (European Project for Ice Coring in Antarctica) Dome C drilling in East Antarctica has now been completed to a depth of 3260 m, at only a few meters above bedrock. Here we present the new...

New constraints on the gas age-ice age difference along the EPICA ice cores, 0–50 kyr (2007)

Loulergue, L., Parrenin, F., Blunier, T., Spahni, R., Schilt, A., ...

Gas is trapped in polar ice sheets at ~50–120 m below the surface and is therefore younger than the surrounding ice. Firn densification models are used to evaluate this ice age-gas age difference...

Synchronization of ice core records via atmospheric gases (2007)

T. Blunier, R. Spahni, J. Chappellaz, L. Loulergue, J. Schwander

To interpret new high resolution climate records it becomes more and more important to know about the succession of climate events. Such knowledge is hard to get especially when dealing with...

"EDML1": a chronology for the EPICA deep ice core from Dronning Maud Land, Antarctica, over the last 150 000 years (2007)

U. Ruth, J. Beer, M. Bigler, T. Blunier, E. Castellano, ...

A chronology called EDML1 has been developed for the EPICA ice core from Dronning Maud Land (EDML). EDML1 is closely interlinked with EDC3, the new chronology for the EPICA ice core from Dome-C (EDC)...

The EDC3 chronology for the EPICA Dome C ice core (2007)

F. Parrenin, J. Beer, T. Blunier, E. Castellano, J. Chappellaz, ...

The EPICA (European Project for Ice Coring in Antarctica) Dome C drilling in East Antarctica has now been completed to a depth of 3260 m, at only a few meters above bedrock. Here we present the new...

New constraints on the gas age-ice age difference along the EPICA ice cores, 0–50 kyr (2007)

L. Loulergue, F. Parrenin, T. Blunier, R. Spahni, A. Schilt, ...

Gas is trapped in polar ice sheets at ~50–120 m below the surface and is therefore younger than the surrounding ice. Firn densification models are used to evaluate this ice age-gas age...

Synchronization of ice core records via atmospheric gases (2007)

T. Blunier, R. Spahni, J. Chappellaz, L. Loulergue, J. Schwander

To interpret new high resolution climate records it becomes more and more important to know about the succession of climate events. Such knowledge is hard to get especially when dealing with...

New constraints on the gas age-ice age difference along the EPICA ice cores, 0–50 kyr (2007)

L. Loulergue, F. Parrenin, T. Blunier, R. Spahni, A. Schilt, ...

Gas is trapped in polar ice sheets at ~50–120 m below the surface and is therefore younger than the surrounding ice. Firn densification models are used to evaluate this ice age-gas age...

"EDML1": a chronology for the EPICA deep ice core from Dronning Maud Land, Antarctica, over the last 150 000 years (2007)

U. Ruth, J. Beer, M. Bigler, T. Blunier, E. Castellano, ...

A chronology called <I>EDML1</I> has been developed for the EPICA ice core from Dronning Maud Land (EDML). <I>EDML1</I> is closely interlinked with <I>EDC3</I>,...

The EDC3 chronology for the EPICA Dome C ice core (2007)

F. Parrenin, J. Beer, T. Blunier, E. Castellano, J. Chappellaz, ...

The EPICA (European Project for Ice Coring in Antarctica) Dome C drilling in East Antarctica has now been completed to a depth of 3260 m, at only a few meters above bedrock. Here we present the new...

Constraints on N2O budget changes since pre-industrial time from new firn air and ice core isotope measurements (2006)

Bernard, S., Röckmann, T., Kaiser, J., Fischer, H., Blunier, T., ...

A historical record of changes in the N2O isotope composition is important for a better understanding of the global N2O atmospheric budget. Here we have combined measurements of trapped gases in the...

Constraints on N2O budget changes since pre-industrial time from new firn air and ice core isotope measurements (2006)

Bernard, S., Röckmann, T., Kaiser, J., Fischer, H., Blunier, T., ...

A historical record of changes in the N2O isotope composition is important for a better understanding of the global N2O atmospheric budget. Here we have combined measurements of trapped gases in the...

Constraints on N2O budget changes since pre-industrial time from new firn air and ice core isotope measurements (2005)

Bernard, S., Röckmann, T., Kaiser, J., Fischer, H., Blunier, T., ...

A historical record of changes in the N2O isotope composition is important for a better understanding of the global N2O atmospheric budget. Here we have combined measurements of trapped gases in the...

Constraints on N2O budget changes since pre-industrial time from new firn air and ice core isotope measurements (2005)

Bernard, S., Röckmann, T., Kaiser, J., Fischer, H., Blunier, T., ...

A historical record of changes in the N2O isotope composition is important for a better understanding of the global N2O atmospheric budget. Here we have combined measurements of trapped gases in the...

Modelling the concentration of atmospheric CO 2 during the Younger Dryas climate event (1999)

O. Marchal, T.F. Stocker, F. Joos, A. Indermühle, Modelling Co, Younger Dryas, ...

The Younger Dryas (YD, dated between 12.7}11.6 ky BP in the GRIP ice core, Central Greenland) is a distinct cold period in the North Atlantic region during the last deglaciation. A popular, but...