Hostname: page-component-586b7cd67f-dlnhk Total loading time: 0 Render date: 2024-11-23T04:16:06.575Z Has data issue: false hasContentIssue false
  • English
  • Français

An investigation of the possibility of non-Laurentide ice stream contributions to Heinrich event 3

Published online by Cambridge University Press:  24 November 2020

Jesse Velay-Vitow Open the ORCID record for Jesse Velay-Vitow [Opens in a new window] ,
W. Richard Peltier  and
Gordan R. Stuhne
Jesse Velay-Vitow*
Affiliation:
Department of Physics, University of Toronto, 60 St. George St, Toronto, Ontario, M5S 1A7
W. Richard Peltier
Affiliation:
Department of Physics, University of Toronto, 60 St. George St, Toronto, Ontario, M5S 1A7
Gordan R. Stuhne
Affiliation:
Department of Physics, University of Toronto, 60 St. George St, Toronto, Ontario, M5S 1A7
*
*Corresponding author e-mail address: [email protected] (J. Velay-Vitow).
Get access Rights & Permissions [Opens in a new window]

Abstract

The ocean floor sedimentological signature of Heinrich event 3 (H3) is markedly different from that of other Heinrich events that are known to have originated in Hudson Strait. It has therefore been suggested that the H3 contribution to iceberg flux may have been delivered by ice streams located in the eastern sector of the North Atlantic, from the Fennoscandian or British Isles ice sheets. To investigate this possibility and whether the instability involved may have been tidally induced, as seems to have been the case for H1, we consider several eastern Atlantic sector possibilities: a hypothetical Barents Sea ice stream, the Norwegian ice stream, and the Irish Sea ice stream. We find that the extremely high amplitude of the M2 tidal constituent in the western North Atlantic that appears to have forced H1 did not exist in the northeastern Atlantic. This suggests that, with one possible exception, if destabilized ice streams in this region did contribute to H3, tidal forcing was most probably not the cause. The single exception to this general conclusion may be the Irish Sea ice stream, and we comment on the probability of a contribution to H3 from this source.

Keywords

Heinrich eventsHeinrich event 3Marine Isotope Stage 3Sea level historyIce-Earth-Ocean Interaction
Type
Thematic Set: Heinrich Events
Information
Quaternary Research , Volume 101 , May 2021 , pp. 13 - 25
Check for updates
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2020

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

Accad, Y., Pekeris, C.L., 1978. Solution of the tidal equations for the M2 and S2 tides in the world oceans from a knowledge of the tidal potential alone. Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences 290:235–266.Google Scholar
Adkins, J.F., McIntyre, K., Schrag, D.P., 2002. The salinity, temperature, and δ18O of the glacial deep ocean. Science 298:1769–1773.CrossRefGoogle ScholarPubMed
Adkins, J., Schrag, D., 2001. Pore fluid constraints on deep ocean temperature and salinity during the last glacial maximum. Geophysical Research Letters 28:771–774.CrossRefGoogle Scholar
Álvarez-Solas, J., Montoya, M., Ritz, C., Ramstein, G., Charbit, S., Dumas, C., Nisanciogl, K., Dokken, T., Ganopolski, A., 2011. Heinrich event 1: an example of dynamical ice-sheet reaction to oceanic changes. Climate of the Past 7:1297–1306.CrossRefGoogle Scholar
Andersen, K.K., Azuma, N., Barnola, J.-M., Bigler, M., Biscaye, P., Caillon, N., Chappellaz, J., et al. , 2004. High-resolution record of the Northern Hemisphere climate extending into the last interglacial period. Nature 431:147–151.Google ScholarPubMed
Andrews, J., Jennings, A.E., Kerwin, M., Kirby, M., Manley, W., Miller, G., Bond, G., MacLean, B., 1995. A Heinrich-like event, H-0 (DC-0): Source (s) for detrital carbonate in the North Atlantic during the Younger Dryas chronozone. Paleoceanography 10:943–952.CrossRefGoogle Scholar
Andrews, J.T., Voelker, A.H., 2018. Heinrich events (& sediments): A history of terminology and recommendations for future usage. Quaternary Science Reviews 187:31–40.CrossRefGoogle Scholar
Arbic, B., Garner, S., Hallberg, R., Simmons, H., 2004. The accuracy of surface elevations in forward global barotropic and baroclinic tide models. Deep-Sea Research Part II-Topical Studies in Oceanography 51:3069–3101.CrossRefGoogle Scholar
Bak, P., Tang, C., 1989. Earthquakes as a self-organized critical phenomenon. Journal of Geophysical Research: Solid Earth 94(B11):15635–15637.CrossRefGoogle Scholar
Bond, G., Heinrich, H., Broecker, W., Labeyrie, L., McManus, J., Andrews, J., Huon, S., et al. 1992., Evidence for massive discharges of icebergs into the North Atlantic ocean during the last glacial period. Nature 360:245–249.CrossRefGoogle Scholar
Bond, G., Lotti, R., 1995. Iceberg discharges into the North Atlantic on millennial time scales during the last glaciation. Science 267:1005–1010.CrossRefGoogle ScholarPubMed
Boyle, E.A., Keigwin, L., 1987. North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperature. Nature 330:35–40.CrossRefGoogle Scholar
Broecker, W.S., Kennett, J.P., Flower, B.P., Teller, J.T., Trumbore, S., Bonani, G., Wolfli, W., 1989. Routing of meltwater from the Laurentide Ice Sheet during the Younger Dryas cold episode. Nature 341:318.CrossRefGoogle Scholar
Butler, S., Peltier, W., 1997. Internal thermal boundary layer stability in phase transition modulated convection. Journal of Geophysical Research: Solid Earth 102(B2):2731–2749.CrossRefGoogle Scholar
Dowdeswell, J., Maslin, M., Andrews, J., McCave, I., 1995. Iceberg production, debris rafting, and the extent and thickness of Heinrich layers (H-1, H-2) in North Atlantic sediments. Geology 23:301–304.2.3.CO;2>CrossRefGoogle Scholar
Egbert, G.D., Ray, R.D., Bills, B.G., 2004. Numerical modeling of the global semidiurnal tide in the present day and in the last glacial maximum. Journal of Geophysical Research: Oceans 109(C3).CrossRefGoogle Scholar
Farrell, W., 1972. Deformation of the Earth by surface loads. Reviews of Geophysics 10:761–797.CrossRefGoogle Scholar
Galewsky, J., Scott, R.K., Polvani, L.M., 2004. An initial-value problem for testing numerical models of the global shallow-water equations. Tellus A: Dynamic Meteorology and Oceanography 56:429–440.CrossRefGoogle Scholar
Griffiths, S.D., Grimshaw, R.H., 2007. Internal tide generation at the continental shelf modeled using a modal decomposition: Two-dimensional results. Journal of Physical Oceanography 37:428–451.CrossRefGoogle Scholar
Griffiths, S.D., Peltier, W.R., 2008. Megatides in the Arctic Ocean under glacial conditions. Geophysical Research Letters 35.CrossRefGoogle Scholar
Griffiths, S.D., Peltier, W.R., 2009. Modeling of polar ocean tides at the Last Glacial Maximum: Amplification, sensitivity, and climatological implications. Journal of Climate 22:2905–2924.CrossRefGoogle Scholar
Grousset, F.E., Cortijo, E., Huon, S., Hervé, L., Richter, T., Burdloff, D., Duprat, J., Weber, O., 2001. Zooming in on Heinrich layers. Paleoceanography 16:240–259.CrossRefGoogle Scholar
Gwiazda, R., Hemming, S., Broecker, W., 1996a. Provenance of icebergs during Heinrich event 3 and the contrast to their sources during other Heinrich episodes. Paleoceanography 11:371–378.CrossRefGoogle Scholar
Gwiazda, R.H., Hemming, S.R., Broecker, W.S., Onsttot, T., Mueller, C., 1996b. Evidence from 40 Ar/39 Ar ages for a Churchill Province source of ice-rafted amphiboles in Heinrich layer 2. Journal of Glaciology 42:440–446.CrossRefGoogle Scholar
Heinrich, H., 1988. Origin and consequences of cyclic ice rafting in the northeast Atlantic Ocean during the past 130,000 years. Quaternary Research 29:142–152.CrossRefGoogle Scholar
Hemming, S.R., 2004. Heinrich events: Massive late Pleistocene detritus layers of the North Atlantic and their global climate imprint. Reviews of Geophysics 42.CrossRefGoogle Scholar
Keigwin, L.D., Klotsko, S., Zhao, N., Reilly, B., Giosan, L., Driscoll, N.W., 2018. Deglacial floods in the Beaufort Sea preceded Younger Dryas cooling. Nature Geoscience 11:599.CrossRefGoogle Scholar
MacAyeal, D.R., 1993. Binge/Purge oscillations of the Laurentide Ice Sheet as a cause of the North Atlantic’s Heinrich Events. Paleoceanography and Paleoclimatology 8:775–784.CrossRefGoogle Scholar
Margold, Martin, Stokes, Chris R., and Clark, Chris D., 2015. Ice streams in the Laurentide Ice Sheet: Identification, characteristics and comparison to modern ice sheets. Earth-Science Reviews 143: 117–146.CrossRefGoogle Scholar
Murton, J.B., Bateman, M.D., Dallimore, S.R., Teller, J.T., Yang, Z., 2010. Identification of Younger Dryas outburst flood path from Lake Agassiz to the Arctic Ocean. Nature 464:740.CrossRefGoogle ScholarPubMed
Peltier, W., Argus, D., Drummond, R., 2015. Space geodesy constrains ice age terminal deglaciation: The global ICE-6G C (VM5a) model. Journal of Geophysical Research: Solid Earth 120:450–487.Google Scholar
Peltier, W.R., Ma, Y., Chandan, D., 2020. The KPP Trigger of Rapid AMOC Intensification in the Nonlinear Dansgaard-Oeschger Relaxation Oscillation. Journal of Geophysical Research: Oceans 125:e2019JC015557.Google Scholar
Peltier, W.R., Vettoretti, G., 2014. Dansgaard-Oeschger oscillations predicted in a comprehensive model of glacial climate: A “kicked” salt oscillator in the Atlantic. Geophysical Research Letters 41:7306–7313.CrossRefGoogle Scholar
Peltier, W.R., Vettoretti, G., Stastna, M., 2006. Atlantic meridional overturning and climate response to Arctic Ocean freshening. Geophysical Research Letters 33:L06713.CrossRefGoogle Scholar
Rashid, H., Hesse, R., Piper, D.J., 2003a. Distribution, thickness and origin of Heinrich layer 3 in the Labrador Sea. Earth and Planetary Science Letters 205:281–293.CrossRefGoogle Scholar
Rashid, H., Hesse, R., Piper, D.J., 2003b. Evidence for an additional Heinrich event between H5 and H6 in the Labrador Sea. Paleoceanography 18.CrossRefGoogle Scholar
Rashid, H., Piper, D.J., Flower, B.P., 2011. The role of Hudson Strait outlet in Younger Dryas sedimentation in the Labrador Sea. Geophysical Monograph Series, 193:93–110.Google Scholar
Rohling, E.J., Marsh, R., Wells, N.C., Siddall, M. and Edwards, N.R., 2004. Similar meltwater contributions to glacial sea level changed from Antarctic and northern ice sheets. Nature 430:1016–1021.CrossRefGoogle Scholar
Roy, K., Peltier, W., 2018. Relative sea level in the Western Mediterranean basin: a regional test of the ICE-7G NA (VM7) model and a constraint on late Holocene Antarctic deglaciation. Quaternary Science Reviews 183:76–87.CrossRefGoogle Scholar
Roy, K., Peltier, W.R., 2017. Space-geodetic and water level gauge constraints on continental uplift and tilting over North America: Regional convergence of the ICE-6G C (VM5a/VM6) models. Geophysical Journal International 210:1115–1142.CrossRefGoogle Scholar
Ruddiman, W.F., McIntyre, A., 1981. The North Atlantic Ocean during the last deglaciation. Palaeogeography, Palaeoclimatology, Palaeoecology 35:145–214.CrossRefGoogle Scholar
Salehipour, H., Peltier, W.R., Caulfield, C.P., 2018. Self-organized criticality of turbulence in strongly stratified mixing layers. Journal of Fluid Mechanics 856:228–256.CrossRefGoogle Scholar
Salehipour, H., Stuhne, G.R., Peltier, W.R., 2013. A higher order discontinuous Galerkin, global shallow water model: Global ocean tides and aquaplanet benchmarks. Ocean Modelling 69:93–107.CrossRefGoogle Scholar
Schoof, C., 2007. Ice sheet grounding line dynamics: Steady states, stability, and hysteresis. Journal of Geophysical Research: Earth Surface 112(F3).CrossRefGoogle Scholar
Schoof, C., 2012. Marine ice sheet stability. Journal of Fluid Mechanics 698:62–72.CrossRefGoogle Scholar
Scourse, J.D., Hall, I.R., McCave, I.N., Young, J.R., Sugdon, C., 2000. The origin of Heinrich layers: evidence from H2 for European precursor events. Earth and Planetary Science Letters 182:187–195.CrossRefGoogle Scholar
Stoner, J.S., Channell, J.E.T., Hillaire-Marcel, C., 1998. A 200 ka geomagnetic chronostratigraphy for the Labrador Sea: Indirect correlation of the sediment record to SPECMAP. Earth and Planetary Science Letters 159(3–4):165–181.CrossRefGoogle Scholar
Tarasov, L., Peltier, W., 2005. Arctic freshwater forcing of the Younger Dryas cold reversal. Nature 435:662.CrossRefGoogle ScholarPubMed
Taylor, G.I., 1919. Tidal friction in the Irish Sea. Proceedings of the Royal Society of London A: Mathematical, Physical and Engineering Sciences 96:330–330.Google Scholar
Velay-Vitow, J., Peltier, W.R., Stuhne, G.R., 2020. The Tides of the Glacial Ocean and Their Possible Connection to Heinrich Event Instabilities of the Laurentide Ice Sheet. Journal of Geophysical Research: Oceans 125:e2019JC015444.Google Scholar
Vettoretti, G., Peltier, W.R., 2013. Last Glacial Maximum ice sheet impacts on North Atlantic climate variability: The importance of the sea ice lid. Geophysical Research Letters 40:6378–6383.CrossRefGoogle Scholar
Waelbroeck, C., Labeyrie, L., Michel, E., Duplessy, J.C., McManus, J., Lambeck, K., Balbon, E., Labracherie, M., 2002. Sea-level and deep water temperature changes derived from benthic foraminifera isotopic records. Quaternary Science Reviews 21:295–305.CrossRefGoogle Scholar
Williamson, D., Drake, J., Hack, J., Jakob, R., Swarztrauber, P., 1992. A standard test set for numerical approximations to the shallow-water equations in spherical geometry. Computational Physics 102:211–224.CrossRefGoogle Scholar