Articles | Volume 15, issue 9
https://doi.org/10.5194/tc-15-4357-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-15-4357-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Holocene sea-ice dynamics in Petermann Fjord in relation to ice tongue stability and Nares Strait ice arch formation
Henrieka Detlef
CORRESPONDING AUTHOR
Department of Geoscience, Aarhus University, Høegh-Guldbergs Gade
2, 8000 Aarhus C, Denmark
Arctic Research Centre, Aarhus University, Ny Munkegade 114, 8000
Aarhus C, Denmark
Brendan Reilly
Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA 92037, USA
Anne Jennings
Institute of Arctic and Alpine Research, University of Colorado,
Boulder, CO 80309-0450, USA
Mads Mørk Jensen
Department of Chemistry, Aarhus University, Langelandsgade 140, 8000
Aarhus C, Denmark
Matt O'Regan
Department of Geological Sciences, Stockholm University, 10691
Stockholm, Sweden
Marianne Glasius
Department of Chemistry, Aarhus University, Langelandsgade 140, 8000
Aarhus C, Denmark
Jesper Olsen
Arctic Research Centre, Aarhus University, Ny Munkegade 114, 8000
Aarhus C, Denmark
Department of Physics and Astronomy, Aarhus University, Ny Munkegade
120, 8000 Aarhus C, Denmark
School of Culture and Society – Centre for Urban Network Evolutions,
Moesgård Alle 20, 8270 Højbjerg, Denmark
Martin Jakobsson
Department of Geological Sciences, Stockholm University, 10691
Stockholm, Sweden
Christof Pearce
Department of Geoscience, Aarhus University, Høegh-Guldbergs Gade
2, 8000 Aarhus C, Denmark
Arctic Research Centre, Aarhus University, Ny Munkegade 114, 8000
Aarhus C, Denmark
Related authors
Joanna Davies, Kirsten Fahl, Matthias Moros, Alice Carter-Champion, Henrieka Detlef, Ruediger Stein, Christof Pearce, and Marit-Solveig Seidenkrantz
The Cryosphere, 18, 3415–3431, https://doi.org/10.5194/tc-18-3415-2024, https://doi.org/10.5194/tc-18-3415-2024, 2024
Short summary
Short summary
Here, we evaluate the use of biomarkers for reconstructing sea ice between 1880 and 2017 from three sediment cores located in a transect across the Northeast Greenland continental shelf. We find that key changes, specifically the decline in sea-ice cover identified in observational records between 1971 and 1984, align with our biomarker reconstructions. This outcome supports the use of biomarkers for longer reconstructions of sea-ice cover in this region.
Christof Pearce, Karen Søby Özdemir, Ronja Forchhammer Mathiasen, Henrieka Detlef, and Jesper Olsen
Geochronology, 5, 451–465, https://doi.org/10.5194/gchron-5-451-2023, https://doi.org/10.5194/gchron-5-451-2023, 2023
Short summary
Short summary
Reliable chronologies lie at the base of paleoclimatological reconstructions. When working with marine sediment cores, the most common dating tool for recent sediments is radiocarbon, but this requires calibration to convert it to calendar ages. This calibration requires knowledge of the marine radiocarbon reservoir age, and this is known to vary in space and time. In this study we provide 92 new radiocarbon measurements to improve our knowledge of the reservoir age around Greenland.
Teodora Pados-Dibattista, Christof Pearce, Henrieka Detlef, Jørgen Bendtsen, and Marit-Solveig Seidenkrantz
Clim. Past, 18, 103–127, https://doi.org/10.5194/cp-18-103-2022, https://doi.org/10.5194/cp-18-103-2022, 2022
Short summary
Short summary
We carried out foraminiferal, stable isotope, and sedimentological analyses of a marine sediment core retrieved from the Northeast Greenland shelf. This region is highly sensitive to climate variability because it is swept by the East Greenland Current, which is the main pathway for sea ice and cold waters that exit the Arctic Ocean. The palaeoceanographic reconstruction reveals significant variations in the water masses and in the strength of the East Greenland Current over the last 9400 years.
Matt O'Regan, Thomas M. Cronin, Brendan Reilly, Aage Kristian Olsen Alstrup, Laura Gemery, Anna Golub, Larry A. Mayer, Mathieu Morlighem, Matthias Moros, Ole L. Munk, Johan Nilsson, Christof Pearce, Henrieka Detlef, Christian Stranne, Flor Vermassen, Gabriel West, and Martin Jakobsson
The Cryosphere, 15, 4073–4097, https://doi.org/10.5194/tc-15-4073-2021, https://doi.org/10.5194/tc-15-4073-2021, 2021
Short summary
Short summary
Ryder Glacier is a marine-terminating glacier in north Greenland discharging ice into the Lincoln Sea. Here we use marine sediment cores to reconstruct its retreat and advance behavior through the Holocene. We show that while Sherard Osborn Fjord has a physiography conducive to glacier and ice tongue stability, Ryder still retreated more than 40 km inland from its current position by the Middle Holocene. This highlights the sensitivity of north Greenland's marine glaciers to climate change.
Madeleine Santos, Lisa Bröder, Matt O'Regan, Iván Hernández-Almeida, Tommaso Tesi, Lukas Bigler, Negar Haghipour, Daniel B. Nelson, Michael Fritz, and Julie Lattaud
EGUsphere, https://doi.org/10.5194/egusphere-2025-3953, https://doi.org/10.5194/egusphere-2025-3953, 2025
This preprint is open for discussion and under review for Climate of the Past (CP).
Short summary
Short summary
Our study examined how sea ice in the Beaufort Sea has changed over the past 13,000 years to better understand today’s rapid losses. By analyzing chemical tracers preserved in seafloor sediments, we found that the Early Holocene was largely ice-free, with warmer waters and lower salinity. Seasonal ice began forming about 7,000 years ago and expanded as the climate cooled. These long-term patterns show that continued warming could return the region to mostly ice-free conditions.
Felicity A. Holmes, Jamie Barnett, Henning Åkesson, Mathieu Morlighem, Johan Nilsson, Nina Kirchner, and Martin Jakobsson
The Cryosphere, 19, 2695–2714, https://doi.org/10.5194/tc-19-2695-2025, https://doi.org/10.5194/tc-19-2695-2025, 2025
Short summary
Short summary
Northern Greenland contains some of the ice sheet's last remaining glaciers with floating ice tongues. One of these is Ryder Glacier, which has been relatively stable in recent decades, in contrast to nearby glaciers. Here, we use a computer model to simulate Ryder Glacier until 2300 under both a low- and a high-emissions scenario. Very high levels of surface melt under a high-emissions future lead to a sea level rise contribution that is an order of magnitude higher than under a low-emissions future.
Jamie Barnett, Felicity Alice Holmes, Joshua Cuzzone, Henning Åkesson, Mathieu Morlighem, Matt O'Regan, Johan Nilsson, Nina Kirchner, and Martin Jakobsson
EGUsphere, https://doi.org/10.5194/egusphere-2025-653, https://doi.org/10.5194/egusphere-2025-653, 2025
Short summary
Short summary
Understanding how ice sheets have changed in the past can allow us to make better predictions for the future. By running a state-of-the-art model of Ryder Glacier, North Greenland, over the past 12,000 years we find that both a warming atmosphere and ocean play a key role in the evolution of the Glacier. Our conclusions stress that accurately quantifying the ice sheet’s interactions with the ocean are required to predict future changes and reliable sea level rise estimates.
Lasse Z. Jensen, Julie K. Simonsen, Ada Pastor, Christof Pearce, Per Nørnberg, Lars Chresten Lund-Hansen, Kai Finster, and Tina Šantl-Temkiv
Aerosol Research, 3, 81–100, https://doi.org/10.5194/ar-3-81-2025, https://doi.org/10.5194/ar-3-81-2025, 2025
Short summary
Short summary
Our study explores particles in Arctic soils and streams that influence ice formation in clouds. By analyzing these environments, we identified specific microorganisms producing these particles. This research, which measured these particles in Arctic streams for the first time, provides new insights into their ecological role and transfer from soil to water. Our findings help us understand their production, sources, and potential impact on climate.
Yuanyuan Luo, Ditte Thomsen, Emil Mark Iversen, Pontus Roldin, Jane Tygesen Skønager, Linjie Li, Michael Priestley, Henrik B. Pedersen, Mattias Hallquist, Merete Bilde, Marianne Glasius, and Mikael Ehn
Atmos. Chem. Phys., 24, 9459–9473, https://doi.org/10.5194/acp-24-9459-2024, https://doi.org/10.5194/acp-24-9459-2024, 2024
Short summary
Short summary
∆3-carene is abundantly emitted from vegetation, but its atmospheric oxidation chemistry has received limited attention. We explored highly oxygenated organic molecule (HOM) formation from ∆3-carene ozonolysis in chambers and investigated the impact of temperature and relative humidity on HOM formation. Our findings provide new insights into ∆3-carene oxidation pathways and their potential to impact atmospheric aerosols.
Joanna Davies, Kirsten Fahl, Matthias Moros, Alice Carter-Champion, Henrieka Detlef, Ruediger Stein, Christof Pearce, and Marit-Solveig Seidenkrantz
The Cryosphere, 18, 3415–3431, https://doi.org/10.5194/tc-18-3415-2024, https://doi.org/10.5194/tc-18-3415-2024, 2024
Short summary
Short summary
Here, we evaluate the use of biomarkers for reconstructing sea ice between 1880 and 2017 from three sediment cores located in a transect across the Northeast Greenland continental shelf. We find that key changes, specifically the decline in sea-ice cover identified in observational records between 1971 and 1984, align with our biomarker reconstructions. This outcome supports the use of biomarkers for longer reconstructions of sea-ice cover in this region.
Allison P. Lepp, Lauren E. Miller, John B. Anderson, Matt O'Regan, Monica C. M. Winsborrow, James A. Smith, Claus-Dieter Hillenbrand, Julia S. Wellner, Lindsay O. Prothro, and Evgeny A. Podolskiy
The Cryosphere, 18, 2297–2319, https://doi.org/10.5194/tc-18-2297-2024, https://doi.org/10.5194/tc-18-2297-2024, 2024
Short summary
Short summary
Shape and surface texture of silt-sized grains are measured to connect marine sediment records with subglacial water flow. We find that grain shape alteration is greatest in glaciers where high-energy drainage events and abundant melting of surface ice are inferred and that the surfaces of silt-sized sediments preserve evidence of glacial transport. Our results suggest grain shape and texture may reveal whether glaciers previously experienced temperate conditions with more abundant meltwater.
Lara F. Pérez, Paul C. Knutz, John R. Hopper, Marit-Solveig Seidenkrantz, Matt O'Regan, and Stephen Jones
Sci. Dril., 33, 33–46, https://doi.org/10.5194/sd-33-33-2024, https://doi.org/10.5194/sd-33-33-2024, 2024
Short summary
Short summary
The Greenland ice sheet is highly sensitive to global warming and a major contributor to sea level rise. In Northeast Greenland, ice–ocean–tectonic interactions are readily observable today, but geological records that illuminate long-term trends are lacking. NorthGreen aims to promote scientific drilling proposals to resolve key scientific questions on past changes in the Northeast Greenland margin that further affected the broader Earth system.
Julia Muchowski, Martin Jakobsson, Lars Umlauf, Lars Arneborg, Bo Gustafsson, Peter Holtermann, Christoph Humborg, and Christian Stranne
Ocean Sci., 19, 1809–1825, https://doi.org/10.5194/os-19-1809-2023, https://doi.org/10.5194/os-19-1809-2023, 2023
Short summary
Short summary
We show observational data of highly increased mixing and vertical salt flux rates in a sparsely sampled region of the northern Baltic Sea. Co-located acoustic observations complement our in situ measurements and visualize turbulent mixing with high spatial resolution. The observed mixing is generally not resolved in numerical models of the area but likely impacts the exchange of water between the adjacent basins as well as nutrient and oxygen conditions in the Bothnian Sea.
Christof Pearce, Karen Søby Özdemir, Ronja Forchhammer Mathiasen, Henrieka Detlef, and Jesper Olsen
Geochronology, 5, 451–465, https://doi.org/10.5194/gchron-5-451-2023, https://doi.org/10.5194/gchron-5-451-2023, 2023
Short summary
Short summary
Reliable chronologies lie at the base of paleoclimatological reconstructions. When working with marine sediment cores, the most common dating tool for recent sediments is radiocarbon, but this requires calibration to convert it to calendar ages. This calibration requires knowledge of the marine radiocarbon reservoir age, and this is known to vary in space and time. In this study we provide 92 new radiocarbon measurements to improve our knowledge of the reservoir age around Greenland.
Johan Nilsson, Eef van Dongen, Martin Jakobsson, Matt O'Regan, and Christian Stranne
The Cryosphere, 17, 2455–2476, https://doi.org/10.5194/tc-17-2455-2023, https://doi.org/10.5194/tc-17-2455-2023, 2023
Short summary
Short summary
We investigate how topographical sills suppress basal glacier melt in Greenlandic fjords. The basal melt drives an exchange flow over the sill, but there is an upper flow limit set by the Atlantic Water features outside the fjord. If this limit is reached, the flow enters a new regime where the melt is suppressed and its sensitivity to the Atlantic Water temperature is reduced.
Gabriel West, Darrell S. Kaufman, Martin Jakobsson, and Matt O'Regan
Geochronology, 5, 285–299, https://doi.org/10.5194/gchron-5-285-2023, https://doi.org/10.5194/gchron-5-285-2023, 2023
Short summary
Short summary
We report aspartic and glutamic acid racemization analyses on Neogloboquadrina pachyderma and Cibicidoides wuellerstorfi from the Arctic Ocean (AO). The rates of racemization in the species are compared. Calibrating the rate of racemization in C. wuellerstorfi for the past 400 ka allows the estimation of sample ages from the central AO. Estimated ages are older than existing age assignments (as previously observed for N. pachyderma), confirming that differences are not due to taxonomic effects.
Alistair J. Monteath, Matthew S. M. Bolton, Jordan Harvey, Marit-Solveig Seidenkrantz, Christof Pearce, and Britta Jensen
Geochronology, 5, 229–240, https://doi.org/10.5194/gchron-5-229-2023, https://doi.org/10.5194/gchron-5-229-2023, 2023
Short summary
Short summary
Accurately dating ocean cores is challenging because the radiocarbon age of water masses varies substantially. We identify ash fragments from eruptions more than 4000 km from their source and use these time markers to develop a new age–depth model for an ocean core in Placentia Bay, North Atlantic. Our results show that the radiocarbon age of waters masses in the bay varied considerably during the last 10 000 years and highlight the potential of using ultra-distal ash deposits in this region.
Jesse R. Farmer, Katherine J. Keller, Robert K. Poirier, Gary S. Dwyer, Morgan F. Schaller, Helen K. Coxall, Matt O'Regan, and Thomas M. Cronin
Clim. Past, 19, 555–578, https://doi.org/10.5194/cp-19-555-2023, https://doi.org/10.5194/cp-19-555-2023, 2023
Short summary
Short summary
Oxygen isotopes are used to date marine sediments via similar large-scale ocean patterns over glacial cycles. However, the Arctic Ocean exhibits a different isotope pattern, creating uncertainty in the timing of past Arctic climate change. We find that the Arctic Ocean experienced large local oxygen isotope changes over glacial cycles. We attribute this to a breakdown of stratification during ice ages that allowed for a unique low isotope value to characterize the ice age Arctic Ocean.
David J. Harning, Brooke Holman, Lineke Woelders, Anne E. Jennings, and Julio Sepúlveda
Biogeosciences, 20, 229–249, https://doi.org/10.5194/bg-20-229-2023, https://doi.org/10.5194/bg-20-229-2023, 2023
Short summary
Short summary
In order to better reconstruct the geologic history of the North Water Polynya, we provide modern validations and calibrations of lipid biomarker proxies in Baffin Bay. We find that sterols, rather than HBIs, most accurately capture the current extent of the North Water Polynya and will be a valuable tool to reconstruct its past presence or absence. Our local temperature calibrations for GDGTs and OH-GDGTs reduce the uncertainty present in global temperature calibrations.
Bernadette Rosati, Sini Isokääntä, Sigurd Christiansen, Mads Mørk Jensen, Shamjad P. Moosakutty, Robin Wollesen de Jonge, Andreas Massling, Marianne Glasius, Jonas Elm, Annele Virtanen, and Merete Bilde
Atmos. Chem. Phys., 22, 13449–13466, https://doi.org/10.5194/acp-22-13449-2022, https://doi.org/10.5194/acp-22-13449-2022, 2022
Short summary
Short summary
Sulfate aerosols have a strong influence on climate. Due to the reduction in sulfur-based fossil fuels, natural sulfur emissions play an increasingly important role. Studies investigating the climate relevance of natural sulfur aerosols are scarce. We study the water uptake of such particles in the laboratory, demonstrating a high potential to take up water and form cloud droplets. During atmospheric transit, chemical processing affects the particles’ composition and thus their water uptake.
Raisa Alatarvas, Matt O'Regan, and Kari Strand
Clim. Past, 18, 1867–1881, https://doi.org/10.5194/cp-18-1867-2022, https://doi.org/10.5194/cp-18-1867-2022, 2022
Short summary
Short summary
This research contributes to efforts solving research questions related to the history of ice sheet decay in the Northern Hemisphere. The East Siberian continental margin sediments provide ideal material for identifying the mineralogical signature of ice sheet derived material. Heavy mineral analysis from marine glacial sediments from the De Long Trough and Lomonosov Ridge was used in interpreting the activity of the East Siberian Ice Sheet in the Arctic region.
Teodora Pados-Dibattista, Christof Pearce, Henrieka Detlef, Jørgen Bendtsen, and Marit-Solveig Seidenkrantz
Clim. Past, 18, 103–127, https://doi.org/10.5194/cp-18-103-2022, https://doi.org/10.5194/cp-18-103-2022, 2022
Short summary
Short summary
We carried out foraminiferal, stable isotope, and sedimentological analyses of a marine sediment core retrieved from the Northeast Greenland shelf. This region is highly sensitive to climate variability because it is swept by the East Greenland Current, which is the main pathway for sea ice and cold waters that exit the Arctic Ocean. The palaeoceanographic reconstruction reveals significant variations in the water masses and in the strength of the East Greenland Current over the last 9400 years.
Jaclyn Clement Kinney, Karen M. Assmann, Wieslaw Maslowski, Göran Björk, Martin Jakobsson, Sara Jutterström, Younjoo J. Lee, Robert Osinski, Igor Semiletov, Adam Ulfsbo, Irene Wåhlström, and Leif G. Anderson
Ocean Sci., 18, 29–49, https://doi.org/10.5194/os-18-29-2022, https://doi.org/10.5194/os-18-29-2022, 2022
Short summary
Short summary
We use data crossing Herald Canyon in the Chukchi Sea collected in 2008 and 2014 together with numerical modelling to investigate the circulation in the western Chukchi Sea. A large fraction of water from the Chukchi Sea enters the East Siberian Sea south of Wrangel Island and circulates in an anticyclonic direction around the island. To assess the differences between years, we use numerical modelling results, which show that high-frequency variability dominates the flow in Herald Canyon.
Matt O'Regan, Thomas M. Cronin, Brendan Reilly, Aage Kristian Olsen Alstrup, Laura Gemery, Anna Golub, Larry A. Mayer, Mathieu Morlighem, Matthias Moros, Ole L. Munk, Johan Nilsson, Christof Pearce, Henrieka Detlef, Christian Stranne, Flor Vermassen, Gabriel West, and Martin Jakobsson
The Cryosphere, 15, 4073–4097, https://doi.org/10.5194/tc-15-4073-2021, https://doi.org/10.5194/tc-15-4073-2021, 2021
Short summary
Short summary
Ryder Glacier is a marine-terminating glacier in north Greenland discharging ice into the Lincoln Sea. Here we use marine sediment cores to reconstruct its retreat and advance behavior through the Holocene. We show that while Sherard Osborn Fjord has a physiography conducive to glacier and ice tongue stability, Ryder still retreated more than 40 km inland from its current position by the Middle Holocene. This highlights the sensitivity of north Greenland's marine glaciers to climate change.
Louise N. Jensen, Manjula R. Canagaratna, Kasper Kristensen, Lauriane L. J. Quéléver, Bernadette Rosati, Ricky Teiwes, Marianne Glasius, Henrik B. Pedersen, Mikael Ehn, and Merete Bilde
Atmos. Chem. Phys., 21, 11545–11562, https://doi.org/10.5194/acp-21-11545-2021, https://doi.org/10.5194/acp-21-11545-2021, 2021
Short summary
Short summary
This work targets the chemical composition of α-pinene-derived secondary organic aerosol (SOA) formed in the temperature range from -15 to 20°C. Experiments were conducted in an atmospheric simulation chamber. Positive matrix factorization analysis of data obtained by a high-resolution time-of-flight aerosol mass spectrometer shows that the elemental aerosol composition is controlled by the initial α-pinene concentration and temperature during SOA formation.
David J. Harning, Brooke Holman, Lineke Woelders, Anne E. Jennings, and Julio Sepúlveda
Biogeosciences Discuss., https://doi.org/10.5194/bg-2021-177, https://doi.org/10.5194/bg-2021-177, 2021
Manuscript not accepted for further review
Short summary
Short summary
In order to better reconstruct the geologic history of the North Water Polynya, we provide modern validations and calibrations of lipid biomarker proxies in Baffin Bay. We find that sterols, rather than HBIs, most accurately capture the current extent of the North Water Polynya and will be a valuable tool to reconstruct its past presence/absence. Our local temperature calibrations for alkenones, GDGTs and OH-GDGTs reduce the uncertainty present in global temperature calibrations.
Kai Wang, Ru-Jin Huang, Martin Brüggemann, Yun Zhang, Lu Yang, Haiyan Ni, Jie Guo, Meng Wang, Jiajun Han, Merete Bilde, Marianne Glasius, and Thorsten Hoffmann
Atmos. Chem. Phys., 21, 9089–9104, https://doi.org/10.5194/acp-21-9089-2021, https://doi.org/10.5194/acp-21-9089-2021, 2021
Short summary
Short summary
Here we present the detailed molecular composition of the organic aerosol collected in three eastern Chinese cities from north to south, Changchun, Shanghai and Guangzhou, by applying LC–Orbitrap analysis. Accordingly, the aromaticity degree of chemical compounds decreases from north to south, while the oxidation degree increases from north to south, which can be explained by the different anthropogenic emissions and photochemical oxidation processes.
Alix G. Cage, Anna J. Pieńkowski, Anne Jennings, Karen Luise Knudsen, and Marit-Solveig Seidenkrantz
J. Micropalaeontol., 40, 37–60, https://doi.org/10.5194/jm-40-37-2021, https://doi.org/10.5194/jm-40-37-2021, 2021
Short summary
Short summary
Morphologically similar benthic foraminifera taxa are difficult to separate, resulting in incorrect identifications, complications understanding species-specific ecological preferences, and flawed reconstructions of past environments. Here we provide descriptions and illustrated guidelines on how to separate some key Arctic–North Atlantic species to circumvent taxonomic confusion, improve understanding of ecological affinities, and work towards more accurate palaeoenvironmental reconstructions.
Svend Funder, Anita H. L. Sørensen, Nicolaj K. Larsen, Anders A. Bjørk, Jason P. Briner, Jesper Olsen, Anders Schomacker, Laura B. Levy, and Kurt H. Kjær
Clim. Past, 17, 587–601, https://doi.org/10.5194/cp-17-587-2021, https://doi.org/10.5194/cp-17-587-2021, 2021
Short summary
Short summary
Cosmogenic 10Be exposure dates from outlying islets along 300 km of the SW Greenland coast indicate that, although affected by inherited 10Be, the ice margin here was retreating during the Younger Dryas. These results seem to be corroborated by recent studies elsewhere in Greenland. The apparent mismatch between temperatures and ice margin behaviour may be explained by the advection of warm water to the ice margin on the shelf and by increased seasonality, both caused by a weakened AMOC.
David J. Harning, Anne E. Jennings, Denizcan Köseoğlu, Simon T. Belt, Áslaug Geirsdóttir, and Julio Sepúlveda
Clim. Past, 17, 379–396, https://doi.org/10.5194/cp-17-379-2021, https://doi.org/10.5194/cp-17-379-2021, 2021
Short summary
Short summary
Today, the waters north of Iceland are characterized by high productivity that supports a diverse food web. However, it is not known how this may change and impact Iceland's economy with future climate change. Therefore, we explored how the local productivity has changed in the past 8000 years through fossil and biogeochemical indicators preserved in Icelandic marine mud. We show that this productivity relies on the mixing of Atlantic and Arctic waters, which migrate north under warming.
Kasper Kristensen, Louise N. Jensen, Lauriane L. J. Quéléver, Sigurd Christiansen, Bernadette Rosati, Jonas Elm, Ricky Teiwes, Henrik B. Pedersen, Marianne Glasius, Mikael Ehn, and Merete Bilde
Atmos. Chem. Phys., 20, 12549–12567, https://doi.org/10.5194/acp-20-12549-2020, https://doi.org/10.5194/acp-20-12549-2020, 2020
Short summary
Short summary
Atmospheric particles are important in relation to human health and the global climate. As the global temperature changes, so may the atmospheric chemistry controlling the formation of particles from reactions of naturally emitted volatile organic compounds (VOCs). In the current work, we show how temperatures influence the formation and chemical composition of atmospheric particles from α-pinene: a biogenic VOC largely emitted in high-latitude environments such as the boreal forests.
Anne Sofie Søndergaard, Nicolaj Krog Larsen, Olivia Steinemann, Jesper Olsen, Svend Funder, David Lundbek Egholm, and Kurt Henrik Kjær
Clim. Past, 16, 1999–2015, https://doi.org/10.5194/cp-16-1999-2020, https://doi.org/10.5194/cp-16-1999-2020, 2020
Short summary
Short summary
We present new results that show how the north Greenland Ice Sheet responded to climate changes over the last 11 700 years. We find that the ice sheet was very sensitive to past climate changes. Combining our findings with recently published studies reveals distinct differences in sensitivity to past climate changes between northwest and north Greenland. This highlights the sensitivity to past and possible future climate changes of two of the most vulnerable areas of the Greenland Ice Sheet.
Colin Ware, Larry Mayer, Paul Johnson, Martin Jakobsson, and Vicki Ferrini
Geosci. Instrum. Method. Data Syst., 9, 375–384, https://doi.org/10.5194/gi-9-375-2020, https://doi.org/10.5194/gi-9-375-2020, 2020
Short summary
Short summary
Geographic coordinates (latitude and longitude) are widely used in geospatial applications, and terrains are often defined by regular grids in geographic coordinates. However, because of convergence of lines of longitude near the poles there is oversampling in the latitude (zonal) direction. Also, there is no standard way of defining a hierarchy of grids to consistently deal with data having different spatial resolutions. The proposed global geographic grid system solves both problems.
Cited articles
Amundson, J. M., Fahnestock, M., Truffer, M., Brown, J., Lüthi, M. P.,
and Motyka, R. J.: Ice mélange dynamics and implications for terminus
stability, Jakobshavn Isbræ, Greenland, J. Geophys. Res., 115,
F01005, https://doi.org/10.1029/2009JF001405, 2010.
Ardyna, M. and Arrigo, K. R.: Phytoplankton dynamics in a changing Arctic
Ocean, Nat. Clim. Change, 10, 892–903, https://doi.org/10.1038/s41558-020-0905-y,
2020.
Axford, Y., Lasher, G. E., Kelly, M. A., Osterberg, E. C., Landis, J.,
Schellinger, G. C., Pfeiffer, A., Thompson, E., and Francis, D. R.: Holocene
temperature history of northwest Greenland – With new ice cap constraints
and chironomid assemblages from Deltasø, Quaternary Sci. Rev., 215, 160–172,
https://doi.org/10.1016/j.quascirev.2019.05.011, 2019.
Barber, D. G., Hanesiak, J. M., Chan, W., and Piwowar, J.: Sea-ice and
meteorological conditions in Northern Baffin Bay and the North Water polynya
between 1979 and 1996, Atmos.-Ocean, 39, 343–359,
https://doi.org/10.1080/07055900.2001.9649685, 2001.
Belicka, L. L., Macdonald, R. W., Yunker, M. B., and Harvey, H. R.: The role
of depositional regime on carbon transport and preservation in Arctic Ocean
sediments, Mar. Chem., 86, 65–88, https://doi.org/10.1016/j.marchem.2003.12.006,
2004.
Belt, S. T.: Source-specific biomarkers as proxies for Arctic and Antarctic
sea ice, Org. Geochem., 125, 277–298, https://doi.org/10.1016/J.ORGGEOCHEM.2018.10.002,
2018.
Belt, S. T. and Müller, J.: The Arctic sea ice biomarker IP25: a
review of current understanding, recommendations for future research and
applications in palaeo sea ice reconstructions, Quaternary Sci. Rev., 79, 9–25,
https://doi.org/10.1016/j.quascirev.2012.12.001, 2013.
Belt, S. T., Massé, G., Rowland, S. J., Poulin, M., Michel, C., and
LeBlanc, B.: A novel chemical fossil of palaeo sea ice: IP25, Org.
Geochem., 38, 16–27, https://doi.org/10.1016/J.ORGGEOCHEM.2006.09.013, 2007.
Belt, S. T., Vare, L. L., Massé, G., Manners, H. R., Price, J. C.,
MacLachlan, S. E., Andrews, J. T., and Schmidt, S.: Striking similarities in
temporal changes to spring sea ice occurrence across the central Canadian
Arctic Archipelago over the last 7000 years, Quaternary Sci. Rev., 29,
3489–3504, https://doi.org/10.1016/j.quascirev.2010.06.041, 2010.
Belt, S. T., Brown, T. A., Rodriguez, A. N., Sanz, P. C., Tonkin, A., and
Ingle, R.: A reproducible method for the extraction, identification and
quantification of the Arctic sea ice proxy IP25 from marine sediments,
Anal. Methods, 4, 705, https://doi.org/10.1039/c2ay05728j, 2012.
Belt, S. T., Cabedo-Sanz, P., Smik, L., Navarro-Rodriguez, A., Berben, S. M.
P., Knies, J., and Husum, K.: Identification of paleo Arctic winter sea ice
limits and the marginal ice zone: Optimised biomarker-based reconstructions
of late Quaternary Arctic sea ice, Earth Planet. Sc. Lett., 431, 127–139,
https://doi.org/10.1016/J.EPSL.2015.09.020, 2015.
Belt, S. T., Brown, T. A., Smik, L., Tatarek, A., Wiktor, J., Stowasser, G.,
Assmy, P., Allen, C. S., and Husum, K.: Identification of C25 highly
branched isoprenoid (HBI) alkenes in diatoms of the genus Rhizosolenia in
polar and sub-polar marine phytoplankton, Org. Geochem., 110, 65–72,
https://doi.org/10.1016/J.ORGGEOCHEM.2017.05.007, 2017.
Bennike, O.: Late Quaternary history of Washington Land, North Greenland,
Boreas, 31, 260–272, https://doi.org/10.1111/j.1502-3885.2002.tb01072.x, 2002.
Briner, J. P., McKay, N. P., Axford, Y., Bennike, O., Bradley, R. S., de
Vernal, A., Fisher, D., Francus, P., Fréchette, B., Gajewski, K.,
Jennings, A., Kaufman, D. S., Miller, G., Rouston, C., and Wagner, B.:
Holocene climate change in Arctic Canada and Greenland, Quaternary Sci. Rev.,
147, 340–364, https://doi.org/10.1016/j.quascirev.2016.02.010, 2016.
Brown, T. A., Belt, S. T., Tatarek, A., and Mundy, C. J.: Source
identification of the Arctic sea ice proxy IP25, Nat. Commun., 5,
4197, https://doi.org/10.1038/ncomms5197, 2014.
Cabedo-Sanz, P., Belt, S. T., Knies, J., and Husum, K.: Identification of
contrasting seasonal sea ice conditions during the Younger Dryas, Quaternary Sci.
Rev., 79, 74–86, https://doi.org/10.1016/j.quascirev.2012.10.028, 2013.
Cai, C., Rignot, E., Menemenlis, D., and Nakayama, Y.: Observations and
modeling of ocean-induced melt beneath Petermann Glacier Ice Shelf in
northwestern Greenland, Geophys. Res. Lett., 44, 8396–8403,
https://doi.org/10.1002/2017GL073711, 2017.
Carr, J. R., Vieli, A., Stokes, C. R., Jamieson, S. S. R., Palmer, S. J.,
Christoffersen, P., Dowdeswell, J. A., Nick, F. M., Blankenship, D. D., and
Young, D. A.: Basal topographic controls on rapid retreat of Humboldt
Glacier, northern Greenland, J. Glaciol., 61, 137–150,
https://doi.org/10.3189/2015JoG14J128, 2015.
Carstens, J., Hebbeln, D., and Wefer, G.: Distribution of planktic foraminifera at the ice margin in the Arctic (Fram Strait), Mar. Micropaleontol., 29, 257–269, https://doi.org/10.1016/S0377-8398(96)00014-X, 1997.
Ceperley, E. G., Marcott, S. A., Reusche, M. M., Barth, A. M., Mix, A. C.,
Brook, E. J., and Caffee, M.: Widespread early Holocene deglaciation,
Washington Land, northwest Greenland, Quaternary Sci. Rev., 231, 106181,
https://doi.org/10.1016/j.quascirev.2020.106181, 2020.
Darby, D. A., Ortiz, J. D., Grosch, C. E., and Lund, S. P.: 1,500-year cycle
in the Arctic Oscillation identified in Holocene Arctic sea-ice drift, Nat.
Geosci., 5, 897–900, https://doi.org/10.1038/ngeo1629, 2012.
Davidson, T. A., Wetterich, S., Johansen, K. L., Grønnow, B., Windirsch,
T., Jeppesen, E., Syväranta, J., Olsen, J., González-Bergonzoni, I.,
Strunk, A., Larsen, N. K., Meyer, H., Søndergaard, J., Dietz, R.,
Eulears, I., and Mosbech, A.: The history of seabird colonies and the North
Water ecosystem: Contributions from palaeoecological and archaeological
evidence, Ambio, 47, 175–192, https://doi.org/10.1007/s13280-018-1031-1, 2018.
Dawes, P., Frisch, T., Garde, A., Iannelli, T., Ineson JR, Monrad Jensen,
S., Pirajno, F., Stemmerik, L., Stouge, S., and Thomassen, B.: Kane Basin
1999: mapping, stratigraphic studies and economic assessment of Precambrian
and Lower Palaeozoic provinces in north-western Greenland, Geol. Greenl.
Surv. Bull., 186, 11–28, https://doi.org/0.34194/GGUB.V186.5211,
2000.
Dunbar, M.: The Geographical Position of the North Water on JSTOR, Arctic,
22, 438–441, https://doi.org/10.14430/ARCTIC3235,
1969.
England, J. H., Lakeman, T. R., Lemmen, D. S., Bednarski, J. M., Stewart, T.
G., and Evans, D. J. A.: A millennial-scale record of Arctic Ocean sea ice
variability and the demise of the Ellesmere Island ice shelves, Geophys.
Res. Lett., 35, L19502, https://doi.org/10.1029/2008GL034470, 2008.
Fetterer, F., Knowles, K., Meier, W. N., Savoie, M., and Windnagel, A. K.:
Sea Ice Index, Version 3.0,
National Snow & Ice Data Center (NSIDC) [data set], https://doi.org/10.7265/N5K072F8, 2017 (updated daily).
Fischer, N. and Jungclaus, J. H.: Evolution of the seasonal temperature cycle in a transient Holocene simulation: orbital forcing and sea-ice, Clim. Past, 7, 1139–1148, https://doi.org/10.5194/cp-7-1139-2011, 2011.
Funder, S., Goosse, H., Jepsen, H., Kaas, E., Kjær, K. H., Korsgaard, N.
J., Larsen, N. K., Linderson, H., Lyså, A., Möller, P., Olsen, J.,
and Willerslev, E.: A 10,000-year record of Arctic Ocean Sea-ice variability
– View from the beach, Science, 333, 747–750,
https://doi.org/10.1126/science.1202760, 2011.
Fürst, J. J., Goelzer, H., and Huybrechts, P.: Ice-dynamic projections of the Greenland ice sheet in response to atmospheric and oceanic warming, The Cryosphere, 9, 1039–1062, https://doi.org/10.5194/tc-9-1039-2015, 2015.
Gajewski, K.: Impact of Holocene climate variability on Arctic vegetation,
Global Planet. Change, 133, 272–287, https://doi.org/10.1016/j.gloplacha.2015.09.006,
2015.
Georgiadis, E., Giraudeau, J., Jennings, A., Limoges, A., Jackson, R.,
Ribeiro, S., and Massé, G.: Local and regional controls on Holocene sea
ice dynamics and oceanography in Nares Strait, Northwest Greenland, Mar.
Geol., 422, 106115, https://doi.org/10.1016/j.margeo.2020.106115, 2020.
Hansen, K. E., Giraudeau, J., Wacker, L., Pearce, C., and Seidenkrantz, M.-S.: Reconstruction of Holocene oceanographic conditions in eastern Baffin Bay, Clim. Past, 16, 1075–1095, https://doi.org/10.5194/cp-16-1075-2020, 2020.
Harrison, J. C., St-Onge, M. R., Petrov, O. V, Strelnikov, S. I., Lopatin, B. G., Wilson, F. H., Tella, S., Paul, D., Lynds, T., Shokalsky, S. P., Hults, C. K., Bergman, S., Jepsen, H. F., and Solli, A.: Geological map of the Arctic, Geol. Surv. Canada Open File 5816, 11, 743, https://doi.org/10.4095/287868, 2011.
Detlef, H., Reilly, B. T., Jennings, A. E., Mørk Jensen,
M., O’Regan, M., Glasius, M., Olsen, J., Jakobsson, M.,
and Pearce, C.: Sea-ice biomarkers, benthic and planktonic
foraminiferal abundance, and total organic carbon in
Holocene sediments from outer Petermann Fjord, PANGAEA [data set], https://doi.org/10.1594/PANGAEA.929918, 2021.
Heuzé, C., Wåhlin, A., Johnson, H. L., and Münchow, A.: Pathways
of Meltwater Export from Petermann Glacier, Greenland, J. Phys. Oceanogr.,
47, 405–418, https://doi.org/10.1175/jpo-d-16-0161.1, 2017.
Hill, E. A., Carr, J. R., and Stokes, C. R.: A Review of Recent Changes in
Major Marine-Terminating Outlet Glaciers in Northern Greenland, Front. Earth
Sci., 4, 111, https://doi.org/10.3389/feart.2016.00111, 2017.
Hörner, T., Stein, R., Fahl, K., and Birgel, D.: Post-glacial variability
of sea ice cover, river run-off and biological production in the western
Laptev Sea (Arctic Ocean) – A high-resolution biomarker study, Quaternary Sci.
Rev., 143, 133–149, https://doi.org/10.1016/J.QUASCIREV.2016.04.011, 2016.
Jackson, R., Kvorning, A. B., Limoges, A., Georgiadis, E., Olsen, S. M.,
Tallberg, P., Andersen, T. J., Mikkelsen, N., Giraudeau, J., Massé, G.,
Wacker, L., and Ribeiro, S.: Holocene polynya dynamics and their interaction
with oceanic heat transport in northernmost Baffin Bay, Sci. Rep.-UK, 11,
10095, https://doi.org/10.1038/s41598-021-88517-9, 2021.
Jakobsson, M., Hogan, K. A., Mayer, L. A., Mix, A., Jennings, A., Stoner,
J., Eriksson, B., Jerram, K., Mohammad, R., Pearce, C., Reilly, B., and
Stranne, C.: The Holocene retreat dynamics and stability of Petermann
Glacier in northwest Greenland, Nat. Commun., 9, 2104,
https://doi.org/10.1038/s41467-018-04573-2, 2018.
Jennings, A., Andrews, J., and Wilson, L.: Holocene environmental evolution
of the SE Greenland Shelf North and South of the Denmark Strait: Irminger
and East Greenland current interactions, Quaternary Sci. Rev., 30,
980–998, https://doi.org/10.1016/j.quascirev.2011.01.016, 2011a.
Jennings, A., Sheldon, C., Cronin, T., Francus, P., Stoner, J., and Andrews,
J.: The Holocene History of Nares Strait: Transition from Glacial Bay to
Arctic-Atlantic Throughflow, Oceanography, 24, 26–41,
https://doi.org/10.5670/oceanog.2011.52, 2011b.
Jennings, A., Andrews, J., Reilly, B., Walczak, M., Jakobsson, M., Mix, A.,
Stoner, J., Nicholls, K. W., and Cheseby, M.: Modern foraminiferal
assemblages in northern Nares Strait, Petermann Fjord, and beneath Petermann
ice tongue, NW Greenland, Arctic, Antarct. Alp. Res., 52, 491–511,
https://doi.org/10.1080/15230430.2020.1806986, 2020.
Johannessen, O. M., Babiker, M., and Miles, M. W.: Unprecedented Retreat in a
50-Year Observational Record for Petermann Glacier, North Greenland, Atmos.
Ocean. Sci. Lett., 6, 259–265, https://doi.org/10.3878/j.issn.1674-2834.13.0021,
2013.
Johnson, H. L., Münchow, A., Falkner, K. K., and Melling, H.: Ocean
circulation and properties in Petermann Fjord, Greenland, J. Geophys. Res.,
116, C01003, https://doi.org/10.1029/2010JC006519, 2011.
Jones, P. E. and Eert, J. A.: Waters of Nares Strait in 2001,
Polarforschung, 74, 185–189,
2004.
Kaufman, D., Ager, T., Anderson, N., Anderson, P., Andrews, J.,
Bartlein, P., Brubaker, L., Coats, L., Cwynar, L., Duvall, M.,
Dyke, A., Edwards, M., Eisner, W., Gajewski, K., Geirsdóttir, A.,
Hu, F., Jennings, A., Kaplan, M., Kerwin, M., Lozhkin, A.,
MacDonald, G., Miller, G., Mock, C., Oswald, W., Otto-Bliesner, B., Porinchu, D., Rühland, K., Smol, J., Steig, E., and Wolfe, B.:
Holocene thermal maximum in the western Arctic (0–180∘ W), Quaternary
Sci. Rev., 23, 529–560, https://doi.org/10.1016/J.QUASCIREV.2003.09.007, 2004.
Knudsen, K. L., Stabell, B., Seidenkrantz, M.-S., Eiriksson, J., and Blake,
W.: Deglacial and Holocene conditions in northernmost Baffin Bay: sediments,
foraminifera, diatoms and stable isotopes, Boreas, 37, 346–376,
https://doi.org/10.1111/j.1502-3885.2008.00035.x, 2008.
Kwok, R.: Variability of Nares Strait ice flux, Geophys. Res. Lett., 32,
L24502, https://doi.org/10.1029/2005GL024768, 2005.
Kwok, R., Toudal Pedersen, L., Gudmandsen, P., and Pang, S. S.: Large sea ice
outflow into the Nares Strait in 2007, Geophys. Res. Lett., 37, L03502,
https://doi.org/10.1029/2009GL041872, 2010.
Lasher, G. E., Axford, Y., McFarlin, J. M., Kelly, M. A., Osterberg, E. C.,
and Berkelhammer, M. B.: Holocene temperatures and isotopes of precipitation
in Northwest Greenland recorded in lacustrine organic materials, Quaternary Sci. Rev., 170, 45–55, https://doi.org/10.1016/j.quascirev.2017.06.016, 2017.
Lecavalier, B. S., Fisher, D. A., Milne, G. A., Vinther, B. M., Tarasov, L.,
Huybrechts, P., Lacelle, D., Main, B., Zheng, J., Bourgeois, J., and Dyke, A.
S.: High Arctic Holocene temperature record from the Agassiz ice cap and
Greenland ice sheet evolution, P. Natl. Acad. Sci. USA, 114,
5952–5957, https://doi.org/10.1073/pnas.1616287114, 2017.
Ledu, D., Rochon, A., de Vernal, A., and St-Onge, G.: Holocene
paleoceanography of the northwest passage, Canadian Arctic Archipelago,
Quaternary Sci. Rev., 29, 3468–3488,
https://doi.org/10.1016/J.QUASCIREV.2010.06.018, 2010.
Leu, E., Mundy, C. J., Assmy, P., Campbell, K., Gabrielsen, T. M., Gosselin,
M., Juul-Pedersen, T., and Gradinger, R.: Arctic spring awakening – Steering
principles behind the phenology of vernal ice algal blooms, Prog. Oceanogr.,
139, 151–170, https://doi.org/10.1016/j.pocean.2015.07.012, 2015.
Limoges, A., Weckström, K., Ribeiro, S., Georgiadis, E., Hansen, K. E.,
Martinez, P., Seidenkrantz, M., Giraudeau, J., Crosta, X., and Massé, G.:
Learning from the past: impact of the Arctic Oscillation on sea ice and
marine productivity off northwest Greenland over the last 9000 years, Glob.
Change Biol., 26, 6767–6786, https://doi.org/10.1111/gcb.15334, 2020.
Lougheed, B. C. and Obrochta, S. P.: MatCal: Open Source Bayesian 14C Age
Calibration in Matlab, J. Open Res. Softw., 4, p.e42, https://doi.org/10.5334/jors.130,
2016.
Marcott, S. A., Shakun, J. D., Clark, P. U., and Mix, A. C.: A reconstruction
of regional and global temperature for the past 11,300 years, Science, 339, 1198–1201, https://doi.org/10.1126/science.1228026, 2013.
Matsuo, A. and Sato, A.: Sterols of mosses, Phytochemistry, 30,
2305–2306, https://doi.org/10.1016/0031-9422(91)83635-X, 1991.
Mayot, N., Matrai, P. A., Arjona, A., Bélanger, S., Marchese, C.,
Jaegler, T., Ardyna, M., and Steele, M.: Springtime Export of Arctic Sea Ice
Influences Phytoplankton Production in the Greenland Sea, J. Geophys. Res.-Ocean., 125, e2019JC015799, https://doi.org/10.1029/2019JC015799, 2020.
Melling, H., Gratton, Y., and Ingram, G.: Ocean circulation within the North
Water polynya of Baffin Bay, Atmos.-Ocean, 39, 301–325,
https://doi.org/10.1080/07055900.2001.9649683, 2001.
Meyers, P. A. and Ishiwatari, R.: Lacustrine organic geochemistry-an
overview of indicators of organic matter sources and diagenesis in lake
sediments, Org. Geochem., 20, 867–900, https://doi.org/10.1016/0146-6380(93)90100-P,
1993.
Mode, W. N.: The Terrestrial Record of Postglacial Vegetation and Climate
from the Arctic/Subarctic of Eastern Canada and West Greenland, Geosci.
Canada, 23, 213–216, 1996.
Möller, P., Larsen, N. K., Kjær, K. H., Funder, S., Schomacker, A.,
Linge, H., and Fabel, D.: Early to middle Holocene valley glaciations on
northernmost Greenland, Quaternary Sci. Rev., 29, 3379–3398,
https://doi.org/10.1016/j.quascirev.2010.06.044, 2010.
Moore, G. W. K., Howell, S. E. L., Brady, M., Xu, X., and McNeil, K.:
Anomalous collapses of Nares Strait ice arches leads to enhanced export of
Arctic sea ice, Nat. Commun., 12, 1–8, https://doi.org/10.1038/s41467-020-20314-w,
2021.
Münchow, A.: Volume and Freshwater Flux Observations from Nares Strait
to the West of Greenland at Daily Time Scales from 2003 to 2009, J. Phys.
Oceanogr., 46, 141–157, https://doi.org/10.1175/JPO-D-15-0093.1, 2016.
Münchow, A. and Melling, H.: Ocean current observations from Nares
Strait to the west of Greenland: Interannual to tidal variability and
forcing, J. Mar. Res., 66, 801–833, https://doi.org/10.1357/002224008788064612,
2008.
Münchow, A., Falkner, K. K., and Melling, H.: Spatial continuity of
measured seawater and tracer fluxes through Nares Strait, a dynamically wide
channel bordering the Canadian Archipelago, J. Mar. Res., 65, 759–788,
https://doi.org/10.1357/002224007784219048, 2007.
Münchow, A., Falkner, K., Melling, H., Rabe, B., and Johnson, H.: Ocean Warming of Nares Strait Bottom Waters off Northwest Greenland, 2003–2009, Oceanography, 24, 114–123, https://doi.org/10.5670/oceanog.2011.62, 2011.
Münchow, A., Padman, L., and Fricker, H. A.: Interannual changes of the
floating ice shelf of Petermann Gletscher, North Greenland, from 2000 to
2012, J. Glaciol., 60, 489–499, https://doi.org/10.3189/2014JoG13J135, 2014.
Nagler, T., Rott, H., Hetzenecker, M., Wuite, J., and Potin, P.: The
Sentinel-1 Mission: New Opportunities for Ice Sheet Observations, Remote
Sens., 7, 9371–9389, https://doi.org/10.3390/rs70709371, 2015.
Navarro-Rodriguez, A., Belt, S. T., Knies, J., and Brown, T. A.: Mapping
recent sea ice conditions in the Barents Sea using the proxy biomarker IP25:
implications for palaeo sea ice reconstructions, Quaternary Sci. Rev., 79,
26–39, https://doi.org/10.1016/J.QUASCIREV.2012.11.025, 2013.
Pados, T. and Spielhagen, R. F.: Species distribution and depth habitat of
recent planktic foraminifera in Fram Strait, Arctic Ocean, Polar Res., 33, 22483, https://doi.org/10.3402/polar.v33.22483, 2014.
Parnell, J., Bowden, S., Andrews, J. T., and Taylor, C.: Biomarker
determination as a provenance tool for detrital carbonate events (Heinrich
events?): Fingerprinting Quaternary glacial sources into Baffin Bay, Earth
Planet. Sc. Lett., 257, 71–82, https://doi.org/10.1016/j.epsl.2007.02.021, 2007.
Rabe, B., Münchow, A., Johnson, H. L., and Melling, H.: Nares Strait
hydrography and salinity field from a 3-year moored array, J. Geophys. Res.,
115, C07010, https://doi.org/10.1029/2009JC005966, 2010.
Rabe, B., Johnson, H. L., Münchow, A., and Melling, H.: Geostrophic ocean
currents and freshwater fluxes across the Canadian polar shelf via Nares
Strait, J. Mar. Res., 70, 603–640, https://doi.org/10.1357/002224012805262725, 2012.
Rasmussen, T. A. S., Kliem, N., and Kaas, E.: Modelling the sea ice in the
Nares Strait, Ocean Model., 35, 161–172,
https://doi.org/10.1016/j.ocemod.2010.07.003, 2010.
Reilly, B. T., Stoner, J. S., Mix, A. C., Walczak, M. H., Jennings, A.,
Jakobsson, M., Dyke, L., Glueder, A., Nicholls, K., Hogan, K. A., Mayer, L.
A., Hatfield, R. G., Albert, S., Marcott, S., Fallon, S., and Cheseby, M.:
Holocene break-up and reestablishment of the Petermann Ice Tongue, Northwest
Greenland, Quaternary Sci. Rev., 218, 322–342,
https://doi.org/10.1016/j.quascirev.2019.06.023, 2019.
Reimer, P. J., Bard, E., Bayliss, A., Beck, J. W., Blackwell, P. G., Ramsey,
C. B., Buck, C. E., Cheng, H., Edwards, R. L., Friedrich, M., Grootes, P.
M., Guilderson, T. P., Haflidason, H., Hajdas, I., Hatté, C., Heaton, T.
J., Hoffmann, D. L., Hogg, A. G., Hughen, K. A., Kaiser, K. F., Kromer, B.,
Manning, S. W., Niu, M., Reimer, R. W., Richards, D. A., Scott, E. M.,
Southon, J. R., Staff, R. A., Turney, C. S. M., and van der Plicht, J.:
IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0–50,000 Years cal
BP, Radiocarbon, 55, 1869–1887, https://doi.org/10.2458/azu_js_rc.55.16947, 2013.
Ribeiro, S., Sejr, M. K., Limoges, A., Heikkilä, M., Andersen, T. J.,
Tallberg, P., Weckström, K., Husum, K., Forwick, M., Dalsgaard, T.,
Massé, G., Seidenkrantz, M.-S., and Rysgaard, S.: Sea ice and primary
production proxies in surface sediments from a High Arctic Greenland fjord:
Spatial distribution and implications for palaeoenvironmental studies,
Ambio, 46, 106–118, https://doi.org/10.1007/s13280-016-0894-2, 2017.
Ribeiro, S., Limoges, A., Massé, G., Johansen, K. L., Colgan, W.,
Weckström, K., Jackson, R., Georgiadis, E., Mikkelsen, N., Kuijpers, A.,
Olsen, J., Olsen, S. M., Nissen, M., Andersen, T. J., Strunk, A., Wetterich,
S., Syväranta, J., Henderson, A. C. G., Mackay, H., Taipale, S.,
Jeppesen, E., Larsen, N. K., Crosta, X., Giraudeau, J., Wengrat, S.,
Nuttall, M., Grønnow, B., Mosbech, A., and Davidson, T. A.: Vulnerability
of the North Water ecosystem to climate change, Nat. Commun.,
12, 4475, https://doi.org/10.1038/s41467-021-24742-0, 2021.
Rignot, E. and Kanagaratnam, P.: Changes in the Velocity Structure of the
Greenland Ice Sheet, Science, 311, 986–990,
https://doi.org/10.1126/science.1121381, 2006.
Rignot, E. and Steffen, K.: Channelized bottom melting and stability of
floating ice shelves, Geophys. Res. Lett., 35, L02503,
https://doi.org/10.1029/2007GL031765, 2008.
Robel, A. A.: Thinning sea ice weakens buttressing force of iceberg
mélange and promotes calving, Nat. Commun., 8, 14596,
https://doi.org/10.1038/ncomms14596, 2017.
Rontani, J. F., Charrière, B., Sempéré, R., Doxaran, D.,
Vaultier, F., Vonk, J. E., and Volkman, J. K.: Degradation of sterols and
terrigenous organic matter in waters of the Mackenzie Shelf, Canadian
Arctic, Org. Geochem., 75, 61–73, https://doi.org/10.1016/j.orggeochem.2014.06.002,
2014.
Rückamp, M., Neckel, N., Berger, S., Humbert, A., and Helm, V.: Calving
Induced Speedup of Petermann Glacier, J. Geophys. Res.-Earth, 124,
216–228, https://doi.org/10.1029/2018JF004775, 2019.
Ruttenberg, K. C. and Goñi, M. A.: Phosphorus distribution, C:N:P
ratios, and δ13C(OC) in arctic, temperate, and tropical coastal
sediments: Tools for characterizing bulk sedimentary organic matter, Mar.
Geol., 139, 123–145, https://doi.org/10.1016/S0025-3227(96)00107-7, 1997.
Ryan, P. A. and Münchow, A.: Sea ice draft observations in Nares Strait
from 2003 to 2012, J. Geophys. Res.-Ocean., 122, 3057–3080,
https://doi.org/10.1002/2016JC011966, 2017.
Safe, S., Safe, L. M., and Maass, W. S. G.: Sterols of three lichen species:
Lobaria pulmonaria, Lobaria Scrobiculata and Usnea Longissima,
Phytochemistry, 14, 1821–1823, https://doi.org/10.1016/0031-9422(75)85302-7, 1975.
Samelson, R. M., Agnew, T., Melling, H., and Münchow, A.: Evidence for
atmospheric control of sea-ice motion through Nares Strait, Geophys. Res.
Lett., 33, L02506, https://doi.org/10.1029/2005GL025016, 2006.
Seidenkrantz, M. S.: Benthic foraminifera as palaeo sea-ice indicators in
the subarctic realm – examples from the Labrador Sea-Baffin Bay region,
Quaternary Sci. Rev., 79, 135–144, https://doi.org/10.1016/j.quascirev.2013.03.014, 2013.
Shepherd, A., Ivins, E. R., Geruo, A., Barletta, V. R., Bentley, M. J.,
Bettadpur, S., Briggs, K. H., Bromwich, D. H., Forsberg, R., Galin, N.,
Horwath, M., Jacobs, S., Joughin, I., King, M. A., Lenaerts, J. T. M., Li,
J., Ligtenberg, S. R. M., Luckman, A., Luthcke, S. B., McMillan, M.,
Meister, R., Milne, G., Mouginot, J., Muir, A., Nicolas, J. P., Paden, J.,
Payne, A. J., Pritchard, H., Rignot, E., Rott, H., Sørensen, L. S.,
Scambos, T. A., Scheuchl, B., Schrama, E. J. O., Smith, B., Sundal, A. V.,
Van Angelen, J. H., Van De Berg, W. J., Van Den Broeke, M. R., Vaughan, D.
G., Velicogna, I., Wahr, J., Whitehouse, P. L., Wingham, D. J., Yi, D.,
Young, D., and Zwally, H. J.: A reconciled estimate of ice-sheet mass
balance, Science, 338, 1183–1189,
https://doi.org/10.1126/science.1228102, 2012.
Shroyer, E. L., Samelson, R. M., Padman, L., and Münchow, A.: Modeled
ocean circulation in Nares Strait and its dependence on landfast-ice cover,
J. Geophys. Res.-Ocean., 120, 7934–7959, https://doi.org/10.1002/2015JC011091,
2015.
Shroyer, E. L., Padman, L., Samelson, R. M., Münchow, A., and Stearns, L.
A.: Seasonal control of Petermann Gletscher ice-shelf melt by the ocean's
response to sea-ice cover in Nares Strait, J. Glaciol., 63, 324–330,
https://doi.org/10.1017/jog.2016.140, 2017.
Smik, L., Cabedo-Sanz, P., and Belt, S. T.: Semi-quantitative estimates of
paleo Arctic sea ice concentration based on source-specific highly branched
isoprenoid alkenes: A further development of the PIP25 index, Org. Geochem.,
92, 63–69, https://doi.org/10.1016/J.ORGGEOCHEM.2015.12.007, 2016.
Stein, R., Fahl, K., Schade, I., Manerung, A., Wassmuth, S., Niessen, F., and
Nam, S.-I.: Holocene variability in sea ice cover, primary production, and
Pacific-Water inflow and climate change in the Chukchi and East Siberian
Seas (Arctic Ocean), J. Quaternary Sci., 32, 362–379, https://doi.org/10.1002/jqs.2929,
2017.
Stocker, T. F., Qin, D., Plattner, G.-K., Tignor, M. M. B., Allen, S. K.,
Boschung, J., Nauels, A., Xia, Y., Bex, V., and Midgley, P. M.: Climate
Change 2013 The Physical Science Basis Working Group I Contribution to the
Fifth Assessment Report of the Intergovernmental Panel on Climate Change,
available at: https://www.cambridge.org/ (last access: 1 May 2020),
2013.
Tinto, K. J., Bell, R. E., Cochran, J. R., and Münchow, A.: Bathymetry in Petermann fjord from Operation IceBridge aerogravity, Earth Planet. Sc. Lett., 422, 58–66, https://doi.org/10.1016/j.epsl.2015.04.009, 2015.
Todd, J. and Christoffersen, P.: Are seasonal calving dynamics forced by buttressing from ice mélange or undercutting by melting? Outcomes from full-Stokes simulations of Store Glacier, West Greenland, The Cryosphere, 8, 2353–2365, https://doi.org/10.5194/tc-8-2353-2014, 2014.
Vare, L. L., Massé, G., Gregory, T. R., Smart, C. W., and Belt, S. T.:
Sea ice variations in the central Canadian Arctic Archipelago during the
Holocene, Quaternary Sci. Rev., 28, 1354–1366,
https://doi.org/10.1016/j.quascirev.2009.01.013, 2009.
Vincent, R. F.: A Study of the North Water Polynya Ice Arch using Four
Decades of Satellite Data, Sci. Rep.-UK, 9, 1–12,
https://doi.org/10.1038/s41598-019-56780-6, 2019.
Volkman, J. K.: A review of sterol markers for marine and terrigenous
organic matter, Org. Geochem., 9, 83–99,
https://doi.org/10.1016/0146-6380(86)90089-6, 1986.
Volkman, J. K.: Sterols in microorganisms, Appl. Microbiol Biot., 60,
495–506, https://doi.org/10.1007/s00253-002-1172-8, 2003.
Volkman, J. K., Barrett, S. M., Dunstan, G. A., and Jeffrey, S. W.:
Geochemical significance of the occurrence of dinosterol and other 4-methyl
sterols in a marine diatom, Org. Geochem., 20, 7–15,
https://doi.org/10.1016/0146-6380(93)90076-N, 1993.
Volkman, J. K., Rohjans, D., Rullkötter, J., Scholz-Böttcher, B. M.,
and Liebezeit, G.: Sources and diagenesis of organic matter in tidal flat
sediments from the German Wadden Sea, Cont. Shelf Res., 20,
1139–1158, https://doi.org/10.1016/S0278-4343(00)00016-9, 2000.
Washam, P., Münchow, A., and Nicholls, K. W.: A Decade of Ocean Changes
Impacting the Ice Shelf of Petermann Gletscher, Greenland, J. Phys.
Oceanogr., 48, 2477–2493, https://doi.org/10.1175/JPO-D-17-0181.1, 2018.
Washam, P., Nicholls, K. W., Münchow, A., and Padman, L.: Summer surface
melt thins Petermann Gletscher Ice Shelf by enhancing channelized basal
melt, J. Glaciol., 65, 662–674, https://doi.org/10.1017/jog.2019.43, 2019.
Wassmann, P. and Reigstad, M.: Future Arctic Ocean seasonal ice zones and
implications for pelagic-benthic coupling, Oceanography, 24, 220–231,
https://doi.org/10.5670/oceanog.2011.74, 2011.
Xiao, X., Fahl, K., and Stein, R.: Biomarker distributions in surface
sediments from the Kara and Laptev seas (Arctic Ocean): indicators for
organic-carbon sources and sea-ice coverage, Quaternary Sci. Rev., 79, 40–52,
https://doi.org/10.1016/J.QUASCIREV.2012.11.028, 2013.
Xiao, X., Fahl, K., Müller, J., and Stein, R.: Sea-ice distribution in
the modern Arctic Ocean: Biomarker records from trans-Arctic Ocean surface
sediments, Geochim. Cosmochim. Ac., 155, 16–29,
https://doi.org/10.1016/J.GCA.2015.01.029, 2015.
Yunker, M. B., Macdonald, R. W., Veltkamp, D. J., and Cretney, W. J.:
Terrestrial and marine biomarkers in a seasonally ice-covered Arctic estuary
– integration of multivariate and biomarker approaches, Mar. Chem., 49,
1–50, https://doi.org/10.1016/0304-4203(94)00057-K, 1995.
Short summary
Here we examine the Nares Strait sea ice dynamics over the last 7000 years and their implications for the late Holocene readvance of the floating part of Petermann Glacier. We propose that the historically observed sea ice dynamics are a relatively recent feature, while most of the mid-Holocene was marked by variable sea ice conditions in Nares Strait. Nonetheless, major advances of the Petermann ice tongue were preceded by a shift towards harsher sea ice conditions in Nares Strait.
Here we examine the Nares Strait sea ice dynamics over the last 7000 years and their...