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View article: Safeguarding the polar regions from dangerous geoengineering: a critical assessment of proposed concepts and future prospects
Safeguarding the polar regions from dangerous geoengineering: a critical assessment of proposed concepts and future prospects Open
Fossil-fuel burning is heating the planet with catastrophic consequences for its habitability and for the natural world on which our existence depends. Halting global warming requires rapid and deep decarbonization to “net zero” carbon dio…
View article: Obliquity disruption and Antarctic ice sheet dynamics over a 2.4-Myr astronomical grand cycle
Obliquity disruption and Antarctic ice sheet dynamics over a 2.4-Myr astronomical grand cycle Open
Marine δ 18 O data reveal astronomical forcing of the climate and cryosphere during the Miocene, when atmospheric P co 2 was on par with emissions scenarios over the next century. This inspired hypotheses for how Milankovitch cycles, ice-o…
View article: Survival strategies of Antarctic vegetation during extensive glacial expansion across the Oligocene/Miocene Transition
Survival strategies of Antarctic vegetation during extensive glacial expansion across the Oligocene/Miocene Transition Open
Antarctica’s terrestrial ecosystems are at risk from a rapidly changing climate. Investigating how Antarctica’s vascular plants responded to major climatic variations in the geological past, especially under atmospheric CO2 values similar …
View article: A Sea Change is Needed For Adapting to Sea-Level Rise in Aotearoa New Zealand
A Sea Change is Needed For Adapting to Sea-Level Rise in Aotearoa New Zealand Open
Sea-level rise is accelerating globally and will continue for centuries under all shared socioeconomic pathways. Although sea-level rise is a global issue, its impacts manifest heterogeneously at the local scale, with some coastal communit…
View article: Spatially variable response of Antarctica's ice sheets to orbital forcing during the Pliocene
Spatially variable response of Antarctica's ice sheets to orbital forcing during the Pliocene Open
Variations in Earth’s orbit pace global ice-volume/sea-level changes, but the variability in the response for different sectors of the Antarctic Ice Sheet (AIS) to orbitally-forced climate change remains unclear. We present geological reco…
View article: Uncertain Pathways to a Future Safe Climate
Uncertain Pathways to a Future Safe Climate Open
Global climate change is often thought of as a steady and approximately predictable physical response to increasing forcings, which then requires commensurate adaptation. But adaptation has practical, cultural and biological limits, and cl…
View article: The Significance of Interseismic Vertical Land Movement at Convergent Plate Boundaries in Probabilistic Sea‐Level Projections for AR6 Scenarios: The New Zealand Case
The Significance of Interseismic Vertical Land Movement at Convergent Plate Boundaries in Probabilistic Sea‐Level Projections for AR6 Scenarios: The New Zealand Case Open
Anticipating and managing the impacts of sea‐level rise for nations astride active tectonic margins requires understanding of rates of sea surface elevation change in relation to coastal land elevation. Vertical land motion (VLM) can eithe…
View article: Plio-Pleistocene Southern Ocean Paleoceanography: Latitudinal drilling in the Southwestern Indian sector of the Southern Ocean
Plio-Pleistocene Southern Ocean Paleoceanography: Latitudinal drilling in the Southwestern Indian sector of the Southern Ocean Open
Proposal 918-pre in the Southern Ocean exists in the current science evaluation system of IODP. Site surveys were completed in 2019. We would like to develop an international research project based on this proposal by conducting new drilli…
View article: Uncertain Pathways to a Future Safe Climate
Uncertain Pathways to a Future Safe Climate Open
Global climate change is often thought of as a steady and approximately predictable physical response to increasing forcings, which then requires commensurate adaptation. But adaptation has practical, cultural and biological limits, and cl…
View article: A ∼200-year relative sea-level reconstruction from the Wellington region (New Zealand) reveals insights into vertical land movement trends
A ∼200-year relative sea-level reconstruction from the Wellington region (New Zealand) reveals insights into vertical land movement trends Open
View article: COP28: Earth’s frozen zones are in trouble – we’re already seeing the consequences
COP28: Earth’s frozen zones are in trouble – we’re already seeing the consequences Open
View article: Melting ice and rising seas – connecting projected change in Antarctica’s ice sheets to communities in Aotearoa New Zealand
Melting ice and rising seas – connecting projected change in Antarctica’s ice sheets to communities in Aotearoa New Zealand Open
Changes in global mean sea level are a clear indicator of a warming climate, but local factors including land subsidence or uplift, cause changes in relative sea level that drive shoreline shifts. These local changes and their impact on co…
View article: Antarctic tipping points: the irreversible changes to come if we fail to keep warming below 2°C
Antarctic tipping points: the irreversible changes to come if we fail to keep warming below 2°C Open
View article: Genomic evidence for West Antarctic Ice Sheet collapse during the Last Interglacial
Genomic evidence for West Antarctic Ice Sheet collapse during the Last Interglacial Open
The marine-based West Antarctic Ice Sheet (WAIS) is considered vulnerable to irreversible collapse under future climate trajectories and its tipping point may even lie within the mitigated warming scenarios of 1.5–2 °C of the United Nation…
View article: A ~200-year relative sea-level reconstruction from the Wellington region (New Zealand) reveals insights into vertical land movement trends
A ~200-year relative sea-level reconstruction from the Wellington region (New Zealand) reveals insights into vertical land movement trends Open
Dataset associated with the manuscript: A ~200-year relative sea-level reconstruction from the Wellington region (New Zealand) reveals insights into vertical land movement trends. Submitted to Marine Geology. pdf containing surface and do…
View article: Climatic and tectonic drivers of late Oligocene Antarctic ice volume
Climatic and tectonic drivers of late Oligocene Antarctic ice volume Open
View article: Early to middle Miocene ice sheet dynamics in the westernmost Ross Sea (Antarctica): Regional correlations
Early to middle Miocene ice sheet dynamics in the westernmost Ross Sea (Antarctica): Regional correlations Open
The present-day morpho-stratigraphy of the Ross Sea is the result of Cenozoic tectonic and cryospheric events, and constitutes a key record of Antarctica's cryospheric evolution. An enduring problem in interpreting this record in a broader…
View article: Sensitivity of the West Antarctic Ice Sheet to +2 °C (SWAIS 2C)
Sensitivity of the West Antarctic Ice Sheet to +2 °C (SWAIS 2C) Open
The West Antarctic Ice Sheet (WAIS) presently holds enough ice to raise global sea level by 4.3 m if completely melted. The unknown response of the WAIS to future warming remains a significant challenge for numerical models in quantifying …
View article: The Uncertain Future of Antarctica’s Melting Ice
The Uncertain Future of Antarctica’s Melting Ice Open
A new multidisciplinary, international research program aims to tackle one of the grand challenges in climate science: resolving the Antarctic Ice Sheet’s contribution to future sea level rise.
View article: Climate and Cryosphere (CliC) Strategy Plan 2022-2031
Climate and Cryosphere (CliC) Strategy Plan 2022-2031 Open
The CliC Strategic Plan 2022–2031 was prepared by the CliC Scientific Steering Group (2021), the CliC International Project Office (IPO), and the WCRP Secretariat.
View article: Meteoric Beryllium-10 in Miocene permafrost and the onset of persistent polar aridity in East Antarctica
Meteoric Beryllium-10 in Miocene permafrost and the onset of persistent polar aridity in East Antarctica Open
Continental scale ice sheets have occupied Antarctica since the major global cooling across the Eocene/Oligocene boundary (~33.9 Ma). However, the timing and nature of the transition to a relatively stable and persistent terrestrial East A…
View article: Retreat of the Antarctic Ice Sheet During the Last Interglaciation and Implications for Future Change
Retreat of the Antarctic Ice Sheet During the Last Interglaciation and Implications for Future Change Open
The Antarctic Ice Sheet (AIS) response to past warming consistent with the 1.5–2°C “safe limit” of the United Nations Paris Agreement is currently not well known. Empirical evidence from the most recent comparable period, the Last Intergla…
View article: Early and middle Miocene ice sheet dynamics in the Ross Sea: Results from integrated core-log-seismic interpretation
Early and middle Miocene ice sheet dynamics in the Ross Sea: Results from integrated core-log-seismic interpretation Open
Oscillations in ice sheet extent during early and middle Miocene are intermittently preserved in the sedimentary record from the Antarctic continental shelf, with widespread erosion occurring during major ice sheet advances, and open marin…
View article: Cryostratigraphy of mid-Miocene permafrost at Friis Hills, McMurdo Dry Valleys of Antarctica – ERRATUM
Cryostratigraphy of mid-Miocene permafrost at Friis Hills, McMurdo Dry Valleys of Antarctica – ERRATUM Open
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View article: The SWAIS 2C Project - sensitivity of the West Antarctic ice sheet in a warmer world
The SWAIS 2C Project - sensitivity of the West Antarctic ice sheet in a warmer world Open
9th SCAR Open Science Conference and XXXVI SCAR Meetings, Hobart, Tasmania, Australia, 31 July - 11 August 2020
View article: Bila pemanasan global melebihi 2°C, lelehan es Antarktika bisa menaikkan muka laut hingga 20 meter
Bila pemanasan global melebihi 2°C, lelehan es Antarktika bisa menaikkan muka laut hingga 20 meter Open
View article: If warming exceeds 2°C, Antarctica’s melting ice sheets could raise seas 20 metres in coming centuries
If warming exceeds 2°C, Antarctica’s melting ice sheets could raise seas 20 metres in coming centuries Open
View article: Antarctic ice-sheet sensitivity to obliquity forcing enhanced through ocean connections
Antarctic ice-sheet sensitivity to obliquity forcing enhanced through ocean connections Open
View article: A Pliocene relative sea level record from New Zealand calculated from grain size
A Pliocene relative sea level record from New Zealand calculated from grain size Open
Earth is heading towards a climate that was last experienced more than 3 Myr during the “mid-Pliocene warm period”1. Atmospheric carbon dioxide (pCO2) concentrations were ~400 ppm, global sea level oscillated in response to orbital forcing…
View article: Lipid biomarker distributions in Oligocene and Miocene sediments from the Ross Sea region, Antarctica: Implications for use of biomarker proxies in glacially-influenced settings
Lipid biomarker distributions in Oligocene and Miocene sediments from the Ross Sea region, Antarctica: Implications for use of biomarker proxies in glacially-influenced settings Open