Bipolar seesaw in the northeastern tropical Atlantic during Heinrich stadials

Two SST records based on Mg/Ca of G. ruber (pink) from the continental slope off West Africa at 15°N and 12°N shed new light on the thermal bipolar seesaw pattern in the northeastern tropical Atlantic during periods of reduced Atlantic Meridional Overturning Circulation (AMOC) associated with Heinrich stadials H1 to H6. The two records indicate that the latitudinal position of the bipolar seesaw's zero-anomaly line, between cooling in the North and warming in the South, gradually shifted southward from H6 to H1. A conceptual model is presented that aims to provide a physically consistent mechanism for the southward migration of the seesaw's fulcrum. The conceptual model suggests latitudinal movements of the Intertropical Convergence Zone, driven by a combination of orbital-forced changes in the meridional temperature gradient within the realm of the Hadley cell and the expansion of the Northern Hemisphere cryosphere, as a major factor.

[1]  Michael Schulz,et al.  Sahel megadroughts triggered by glacial slowdowns of Atlantic meridional overturning , 2008 .

[2]  J. Tison,et al.  One-to-one coupling of glacial climate variability in Greenland and Antarctica. , 2006 .

[3]  T. Guilderson,et al.  Radiocarbon calibration curve spanning 0 to 50,000 years BP based on paired 230 Th/ 234 U/ 238 U and 14 C dates on pristine corals , 2005 .

[4]  H. Elderfield,et al.  A study of cleaning procedures used for foraminiferal Mg/Ca paleothermometry , 2003 .

[5]  A. Mix,et al.  Late Quaternary paleoceanography of the tropical Atlantic, 2: The seasonal cycle of sea surface temperatures, 0–20,000 years B.P. , 1986 .

[6]  W. Cheng,et al.  Fast teleconnections to the tropical Atlantic sector from Atlantic thermohaline adjustment , 2008 .

[7]  Eric Guilyardi,et al.  The influence of a weakening of the atlantic meridional overturning circulation on ENSO , 2006 .

[8]  Norbert R Nowaczyk,et al.  Dominant Northern Hemisphere climate control over millennial-scale glacial sea-level variability , 2007 .

[9]  X. Querol,et al.  Geochemical variations in aeolian mineral particles from the Sahara-Sahel Dust Corridor. , 2006, Chemosphere.

[10]  Peter U. Clark,et al.  The role of the thermohaline circulation in abrupt climate change , 2002, Nature.

[11]  A. Timmermann,et al.  Effects of Salt Compensation on the Climate Model Response in Simulations of Large Changes of the Atlantic Meridional Overturning Circulation , 2007 .

[12]  N. Shackleton,et al.  Absolute calibration of the Greenland time scale: implications for Antarctic time scales and for Δ14C , 2004 .

[13]  T. Stocker The Seesaw Effect , 1998, Science.

[14]  A minimum thermodynamic model for the bipolar seesaw , 2003 .

[15]  Andreas Mackensen,et al.  The tropical rainbelt and productivity changes off northwest Africa: A 31,000-year high-resolution record , 2010 .

[16]  M. Vautravers,et al.  The relationship between shell size and Mg/Ca, Sr/Ca, δ18O, and δ13C of species of planktonic foraminifera , 2002 .

[17]  M. Prange The low-resolution CCSM2 revisited: new adjustments and a present-day control run , 2006 .

[18]  Andrei P. Sokolov,et al.  Investigating the Causes of the Response of the Thermohaline Circulation to Past and Future Climate Changes , 2006 .

[19]  R. Reynolds,et al.  The NCEP/NCAR 40-Year Reanalysis Project , 1996, Renewable Energy.

[20]  R. Tiedemann,et al.  Calibrating Mg/Ca ratios of multiple planktonic foraminiferal species with δ 18 O-calcification temperatures: Paleothermometry for the upper water column , 2009 .

[21]  Nicholas J Shackleton,et al.  Millennial-scale oceanic climate variability off the Western Iberian margin during the last two glacial periods , 2003 .

[22]  R. Schneider,et al.  Provenance of present‐day eolian dust collected off NW Africa , 2005 .

[23]  S. Rahmstorf Ocean circulation and climate during the past 120,000 years , 2002, Nature.

[24]  C. Bitz,et al.  Influence of high latitude ice cover on the marine Intertropical Convergence Zone , 2005 .

[25]  T. Crowley North Atlantic Deep Water cools the southern hemisphere , 1992 .

[26]  J. Tison,et al.  One-to-one coupling of glacial climate variability in Greenland during Ice Sheet Invasion , 2006 .

[27]  Rong‐Hua Zhang Anticorrelated multidecadal variations between surface and subsurface tropical North Atlantic , 2007 .

[28]  N. Shackleton,et al.  Rapid Communication Absolute calibration of the Greenland time scale: implications for Antarctic time scales and for D 14 C , 2004 .

[29]  J. Melack,et al.  Transport of carbon, nitrogen, phosphorus, and major solutes in the Gambia River, West Africa' , 1984 .

[30]  W. Broecker,et al.  Interhemispheric Atlantic seesaw response during the last deglaciation , 2009, Nature.

[31]  P. Grootes,et al.  The Leibniz-Labor AMS facility at the Christian-Albrechts University, Kiel, Germany , 1997 .

[32]  B. Otto‐Bliesner,et al.  The sensitivity of the climate response to the magnitude and location of freshwater forcing: last glacial maximum experiments , 2010 .

[33]  J Schwander,et al.  High-resolution record of Northern Hemisphere climate extending into the last interglacial period , 2004, Nature.

[34]  H. Flohn A hemispheric circulation asymmetry during Late Tertiar , 1981 .