New 10Be exposure ages improve Holocene ice sheet thinning history near the grounding line of Pope Glacier, Antarctica

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Location: Deutsche Nationalbibliothek Frankfurt am Main

Extent: Online-Ressource

Language: Englisch

Bibliographic citation: New ¹⁰Be exposure ages improve Holocene ice sheet thinning history near the grounding line of Pope Glacier, Antarctica ; day:05 ; month:05 ; year:2022 ; pages:1-27 ; extent:27
The Cryosphere discussions ; (05.05.2022), 1-27 (gesamt 27)

Creator: Adams, Jonathan Richard
Johnson, Joanne S.
Roberts, Stephen J.
Mason, Philippa J.
Nichols, Keir A.
Venturelli, Ryan A.
Wilcken, Klaus
Balco, Greg
Goehring, Brent
Hall, Brenda
Woodward, John
Rood, Dylan H.

DOI: 10.5194/tc-2022-82

URN: urn:nbn:de:101:1-2022051205282363438321

Rights: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 15.08.2025, 7:34 AM CEST

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Associated

Adams, Jonathan Richard
Johnson, Joanne S.
Roberts, Stephen J.
Mason, Philippa J.
Nichols, Keir A.
Venturelli, Ryan A.
Wilcken, Klaus
Balco, Greg
Goehring, Brent
Hall, Brenda
Woodward, John
Rood, Dylan H.

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New 10Be exposure ages improve Holocene ice sheet thinning history near the grounding line of Pope Glacier, Antarctica

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HETerogeneous vectorized or Parallel (HETPv1.0): an updated inorganic heterogeneous chemistry solver for the metastable-state NH4+–Na+–Ca2+–K+–Mg2+–SO42−–NO3−–Cl−–H2O system based on ISORROPIA II

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New 10Be exposure ages improve Holocene ice sheet thinning history near the grounding line of Pope Glacier, Antarctica

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Holocene thinning of Darwin and Hatherton glaciers, Antarctica, and implications for grounding-line retreat in the Ross Sea

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Modelling oxygen (18O, 17O, 16O) and hydrogen (2H, 1H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

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Modelling oxygen (18O, 17O, 16O) and hydrogen (2H, 1H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

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New <sup>10</sup>Be exposure ages improve Holocene ice sheet thinning history near the grounding line of Pope Glacier, Antarctica

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Associated

Other Objects (12)

New <sup>10</sup>Be exposure ages improve Holocene ice sheet thinning history near the grounding line of Pope Glacier, Antarctica

Holocene thinning and grounding-line retreat of Darwin and Hatherton Glaciers, Antarctica

Holocene thinning of Darwin and Hatherton glaciers, Antarctica, and implications for grounding-line retreat in the Ross Sea

Mid-Holocene thinning of David Glacier, Antarctica: chronology and controls

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Relationship between meteoric <sup>10</sup>Be and NO<sub>3</sub><sup>−</sup> concentrations in soils along Shackleton Glacier, Antarctica

Basal channels, ice thinning and grounding zone retreat at Thwaites Glacier, West Antarctica

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

Modelling oxygen (<sup>18</sup>O, <sup>17</sup>O, <sup>16</sup>O) and hydrogen (<sup>2</sup>H, <sup>1</sup>H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Glacier response to Holocene warmth inferred from in situ <sup>10</sup>Be and <sup>14</sup>C bedrock analyses in Steingletscher’s forefield (central Swiss Alps)

New <sup>10</sup>Be exposure ages improve Holocene ice sheet thinning history near the grounding line of Pope Glacier, Antarctica

Holocene thinning and grounding-line retreat of Darwin and Hatherton Glaciers, Antarctica

Holocene thinning of Darwin and Hatherton glaciers, Antarctica, and implications for grounding-line retreat in the Ross Sea

Mid-Holocene thinning of David Glacier, Antarctica: chronology and controls

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Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

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Glacier response to Holocene warmth inferred from in situ <sup>10</sup>Be and <sup>14</sup>C bedrock analyses in Steingletscher’s forefield (central Swiss Alps)

New <sup>10</sup>Be exposure ages improve Holocene ice sheet thinning history near the grounding line of Pope Glacier, Antarctica

Holocene thinning and grounding-line retreat of Darwin and Hatherton Glaciers, Antarctica

Holocene thinning of Darwin and Hatherton glaciers, Antarctica, and implications for grounding-line retreat in the Ross Sea

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Relationship between meteoric <sup>10</sup>Be and NO<sub>3</sub><sup>−</sup> concentrations in soils along Shackleton Glacier, Antarctica

Basal channels, ice thinning and grounding zone retreat at Thwaites Glacier, West Antarctica

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

Modelling oxygen (<sup>18</sup>O, <sup>17</sup>O, <sup>16</sup>O) and hydrogen (<sup>2</sup>H, <sup>1</sup>H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Glacier response to Holocene warmth inferred from in situ <sup>10</sup>Be and <sup>14</sup>C bedrock analyses in Steingletscher’s forefield (central Swiss Alps)

New <sup>10</sup>Be exposure ages improve Holocene ice sheet thinning history near the grounding line of Pope Glacier, Antarctica

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Other Objects (12)

New <sup>10</sup>Be exposure ages improve Holocene ice sheet thinning history near the grounding line of Pope Glacier, Antarctica

Holocene thinning and grounding-line retreat of Darwin and Hatherton Glaciers, Antarctica

Holocene thinning of Darwin and Hatherton glaciers, Antarctica, and implications for grounding-line retreat in the Ross Sea

Mid-Holocene thinning of David Glacier, Antarctica: chronology and controls

Mid-Holocene thinning of David Glacier, Antarctica: Chronology and Controls

Relationship between meteoric <sup>10</sup>Be and NO<sub>3</sub><sup>−</sup> concentrations in soils along Shackleton Glacier, Antarctica

Basal channels, ice thinning and grounding zone retreat at Thwaites Glacier, West Antarctica

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

Modelling oxygen (<sup>18</sup>O, <sup>17</sup>O, <sup>16</sup>O) and hydrogen (<sup>2</sup>H, <sup>1</sup>H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Glacier response to Holocene warmth inferred from in situ <sup>10</sup>Be and <sup>14</sup>C bedrock analyses in Steingletscher&rsquo;s forefield (central Swiss Alps)

New <sup>10</sup>Be exposure ages improve Holocene ice sheet thinning history near the grounding line of Pope Glacier, Antarctica

Holocene thinning and grounding-line retreat of Darwin and Hatherton Glaciers, Antarctica

Holocene thinning of Darwin and Hatherton glaciers, Antarctica, and implications for grounding-line retreat in the Ross Sea

Mid-Holocene thinning of David Glacier, Antarctica: chronology and controls

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Relationship between meteoric <sup>10</sup>Be and NO<sub>3</sub><sup>−</sup> concentrations in soils along Shackleton Glacier, Antarctica

Basal channels, ice thinning and grounding zone retreat at Thwaites Glacier, West Antarctica

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

Modelling oxygen (<sup>18</sup>O, <sup>17</sup>O, <sup>16</sup>O) and hydrogen (<sup>2</sup>H, <sup>1</sup>H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Glacier response to Holocene warmth inferred from in situ <sup>10</sup>Be and <sup>14</sup>C bedrock analyses in Steingletscher&rsquo;s forefield (central Swiss Alps)

New <sup>10</sup>Be exposure ages improve Holocene ice sheet thinning history near the grounding line of Pope Glacier, Antarctica

Holocene thinning and grounding-line retreat of Darwin and Hatherton Glaciers, Antarctica

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Mid-Holocene thinning of David Glacier, Antarctica: chronology and controls

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Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

Modelling oxygen (<sup>18</sup>O, <sup>17</sup>O, <sup>16</sup>O) and hydrogen (<sup>2</sup>H, <sup>1</sup>H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Glacier response to Holocene warmth inferred from in situ <sup>10</sup>Be and <sup>14</sup>C bedrock analyses in Steingletscher&rsquo;s forefield (central Swiss Alps)

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Glacier response to Holocene warmth inferred from in situ <sup>10</sup>Be and <sup>14</sup>C bedrock analyses in Steingletscher’s forefield (central Swiss Alps)

Glacier response to Holocene warmth inferred from in situ <sup>10</sup>Be and <sup>14</sup>C bedrock analyses in Steingletscher’s forefield (central Swiss Alps)

Glacier response to Holocene warmth inferred from in situ <sup>10</sup>Be and <sup>14</sup>C bedrock analyses in Steingletscher’s forefield (central Swiss Alps)