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[PDF] Top 20 On the gas-ice depth difference ( depth) along the EPICA Dome C ice core

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On the gas-ice depth difference ( depth) along the EPICA Dome C ice core

On the gas-ice depth difference ( depth) along the EPICA Dome C ice core

... of ice thickness H (t ) are obtained from a 1-D model (Parrenin et ...Antarctic ice sheet (Ritz et ...reduced ice thickness) at Dome C during glacial ...an ice sheet in the Ross ... See full document

17

Spatial pattern of accumulation at Taylor Dome during Marine Isotope Stage 4: stratigraphic constraints from Taylor Glacier

Spatial pattern of accumulation at Taylor Dome during Marine Isotope Stage 4: stratigraphic constraints from Taylor Glacier

... thus ice core air is younger than the ice matrix that encloses it (Schwander and Stauffer, ...the difference between ice age and gas age (1age) depends primarily on temperature ... See full document

20

Towards orbital dating of the EPICA Dome C ice core using O2 /N 2

Towards orbital dating of the EPICA Dome C ice core using O2 /N 2

... each depth, two adjacent ice samples covering the same depth interval were cut from the ice ...outer ice was shaved off each face to yield two 10 g ice ...the ice sam- ... See full document

13

Spiky fluctuations and scaling in high-resolution EPICA ice core dust fluxes

Spiky fluctuations and scaling in high-resolution EPICA ice core dust fluxes

... Beyond confirming the results of the spectral analysis and allowing for direct interpretations of the fluctuation values in terms of typical fluxes, Haar analysis also quantifies the in- termittency from the convergence ... See full document

19

Volcanic synchronisation between the EPICA Dome C and Vostok ice cores (Antarctica) 0–145 kyr BP

Volcanic synchronisation between the EPICA Dome C and Vostok ice cores (Antarctica) 0–145 kyr BP

... the EPICA Dome C (EDC) and Vostok ice cores in the time interval 0–145 kyr BP by using the volcanic ...the ice core chronologies (Udisti et ...Antarctic Ice Core ... See full document

15

Anomalous flow below 2700 m in the EPICA Dome C ice core detected using 18 O of atmospheric oxygen measurements

Anomalous flow below 2700 m in the EPICA Dome C ice core detected using 18 O of atmospheric oxygen measurements

... of C(z) −1 greater than 1 contract the original expected agescale (equivalent to an in- creased accumulation rate or stretched ice ...2 depth-δD depth (circles shaded according to confidence, ... See full document

13

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

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

... mechanical ice-flow model, Parrenin et ...the ice core chronology only if they are compensated by a propor- tional decrease in the thinning ...of depth (∼50 kyr BP) and it is considered very ... See full document

14

A sequential Bayesian approach for the estimation of the age–depth relationship of the Dome Fuji ice core

A sequential Bayesian approach for the estimation of the age–depth relationship of the Dome Fuji ice core

... the difference between each tie point and the median of the ...the difference between the esti- mate by Parrenin et ...the difference between the two results is about 3000 years at the ... See full document

14

Retrieving the paleoclimatic signal from the deeper part of the EPICA Dome C ice core

Retrieving the paleoclimatic signal from the deeper part of the EPICA Dome C ice core

... then ice under increasing metamorphism, these impurities could therefore be found either within the ice crystals themselves, or within the unfrozen liquid that separates the grain bound- aries as a result ... See full document

16

The EDC3 chronology for the EPICA Dome C ice core

The EDC3 chronology for the EPICA Dome C ice core

... 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 ...markers ... See full document

13

1-D-ice flow modelling at EPICA Dome C and Dome Fuji, East Antarctica

1-D-ice flow modelling at EPICA Dome C and Dome Fuji, East Antarctica

... at Dome C, there has been an excess of accumulation during the early Holocene that is not simply related to the isotopic content of the ice during this ...simplified ice sheet model, we ... See full document

17

Direct north-south synchronization of abrupt climate change record in ice cores using Beryllium 10

Direct north-south synchronization of abrupt climate change record in ice cores using Beryllium 10

... NorthGRIP ice core (Huber et ...at Dome C inferred from the δD signal (Stenni et ...from EPICA Dome C. For AIM 9–11, the time difference between the predicted and ... See full document

7

Change in ice rheology during climate variations – implications for ice flow modelling and dating of the EPICA Dome C core

Change in ice rheology during climate variations – implications for ice flow modelling and dating of the EPICA Dome C core

... the difference in the trend of the curves obtained at the divide (dotted lines) and 30 km downstream for the stationary run (thin solid ...by ice, fabric at 30 km of the dome clusters more rapidly ... See full document

13

Uncertainties in Arctic sea ice thickness and volume: new estimates and implications for trends

Uncertainties in Arctic sea ice thickness and volume: new estimates and implications for trends

... snow depth retrievals remains an issue, and explains why we have used the climatological values from W99 for this ice type in all our ...snow depth algorithm for thick ice has been developed ... See full document

16

The relation between sea ice thickness and freeboard in the Arctic

The relation between sea ice thickness and freeboard in the Arctic

... sea ice thickness from CryoSat-2 radar altimeter freeboard data requires observa- tional data to verify the relation between these two ...in-situ ice and snow data from 689 observation sites, obtained ... See full document

8

Dating a tropical ice core by time–frequency analysis of ion concentration depth profiles

Dating a tropical ice core by time–frequency analysis of ion concentration depth profiles

... Andean ice records started in the mid-1980s with paleo-climate reconstructions based on the comparison of water stable isotope profiles with Antarctic or Greenland data (Thompson et ...polar ice cores. ... See full document

14

CSIB v1 (Canadian Sea-ice Biogeochemistry): a sea-ice biogeochemical model for the NEMO community ocean modelling framework

CSIB v1 (Canadian Sea-ice Biogeochemistry): a sea-ice biogeochemical model for the NEMO community ocean modelling framework

... (1979). Ice (snow) volume was defined as the sum of the product of grid-cell-mean ice thickness (snow depth) and the grid-cell ...area. Ice extent was defined as the areal sum of all grid ... See full document

26

The influence of a model subglacial lake on ice dynamics and internal layering

The influence of a model subglacial lake on ice dynamics and internal layering

... an ice stream (Leysinger Vieli et ...and ice thickness are compared (n = 3). Isochrones relative to the ice base are shown in ...smaller ice flux at depth outside the lake compared to ... See full document

10

High-resolution mineral dust and sea ice proxy records from the Talos Dome ice core

High-resolution mineral dust and sea ice proxy records from the Talos Dome ice core

... Antarctic ice core records in the following, all covering at least the last 150 ka (a map of Antarctica with all investi- gated ice core sites is shown in ...deep ice cores drilled ... See full document

19

Centennial mineral dust variability in high-resolution ice core data from Dome C, Antarctica

Centennial mineral dust variability in high-resolution ice core data from Dome C, Antarctica

... Figure 3 (bottom panel) shows EDC insoluble dust mass concentrations during the past 800 kyr, with Ca 2+ and nssCa 2+ to insoluble dust ratios in black and grey, respec- tively (top panel). The Ca 2+ and nssCa 2+ to ... See full document

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