Reconstructing and Modelling the Last Glacial Maximum
713
Prunet P, Minster J, Ruiz-Pino D (1996a) Assimilation of
surface data in a one-dimensional physicalbiogeochemical model of the surface ocean. 1.
Method and preliminary results. Global Biogeochem
Cycles 10: 111-138
Prunet P, Minster J, Echevin V, Dadou 1 (1996b) Assimilation of surface data in a one-dimensional physical-biogeochemical model of the surface ocean. 2.
Adjusting a simple trophic model to chlorophyll,
temperature, nitrate, and pC0 2 data. Global
Biogeochem Cycles 10: 139-158
Rind D, Peteet D (1985) Terrestrial conditions at the last
glacial maximum and CLIMAP sea-surface temperature estimates: Are they consistent? Quat Res 24:
1-22
Roeckner E, Arpe K, Bengtsson L, Christoph M,
Claussen M, Diimenil L, Esch M, Giorgetta M,
Schlese U, Schulzweida U (1996) The atmospheric
general circulation model ECHAM 4: Model description and simulation of present-day climate. Report
No. 218, Max-Planck-Institut fiir Meteorologie,
Hamburg
Sarnthein M, Winn K, Zahn R (1987) Paleoproductivity
of oceanic upwelling and the effect on atmospheric
CO 2 and climatic change during deglaciation times.
In: Berger WH, Labeyrie LD (eds) Abrupt Climatic
Change. NATO ASI Series C 216, Springer, Berlin
Heidelberg New York, pp311-337
Samthein M, Winn K, Duplessy JC, Fontugne MR(1988)
Global variations of surface ocean productivity in
low and mid latitudes. Paleoceanography 3: 361-399
Sarnthein M, Jansen E, Arnold M, Duplessy JC,
Erlenkeuser H, Flatoy A, Veum T, Vogelsang E,
Weinelt MS (1992) A time-slice reconstruction of
meltwater anomalies at termination I in the North
Atlantic between 50 and 80 0 N. In: Bard E, Broecker
W (eds) The Last Deglaciation: Absolute and Radiocarbon Chronologies. NATO AS! Series, Vol 12,
Springer, Berlin Heidelberg New York,
pp433-458
Sarnthein M, Winn K, Jung SJA, Duplessy JC, Labeyrie
L, Erlenkeuser H, Ganssen G (1994) Changes in east
Atlantic deepwater circulation over the last 30,000
years: Eight time slice reconstructions.
Paleoceanography 9: 209-267
Sarnthein M, Jansen E, Weinelt M, Arnold M, Duplessy
JC, Erlenkeuser H, Flatoy A, Johannessen G,
Johannessen T, Jung S, Koc N, Labeyrie L, Maslin
M, Ptlaumann U, Schulz H (1995) Variations
in Atlantic surface ocean paleoceanography,
50 0 N - 80 0 N: A time-slice record of the last
30,000 years. Paleoceanography 10: 1063-1094
Sausen R, Barthel K, Hasselmann K (1988) Coupled
ocean-atmosphere models with flux correction. Clim
Dyn2: 145-163
Sausen R, Lunkeit F (1990) Some remarks on the cause
of the climate drift of coupled ocean-atmosphere
models. Beitr Phys Atmosph 63: 141-146
Sausen R, Voss R (1996) Techniques for asynchronous
and periodically synchronous coupling of atmosphere and ocean models. Part I: General strategy and
application to cyclo-stationary case. Clim Dyn 12:
313-323
Schafer-Neth C (1998) Changes in the seawater-oxygen
isotope relation between last glacial and present:
Sediment core data and OGCM modelling. Paleoclimates 2 (2-3): 101-131
Schlesinger ME (1979) Discussion of"A global oceanatmosphere model with seasonal variation for future
studies of climate sensitivity". Dynam Atmos Oceans
3:427-432
Schlitzer R (1993a) An adjoint model for the determination of the mean oceanic circulation, air-sea fluxes
and mixing coefficients. Habilitation thesis, Univ
Bremen, pp 1-88
Schlitzer R (1993b) Determining the mean, large-scale circulation of the Atlantic with the adjoint method.
J Phys Oceanogr 23: 1935-1952
Seidov D, Prien R (1996) A coarse resolution North
Atlantic Ocean circulation model: An intercomparison study with a paleoceanographic example. Annals Geophys 14: 246-257
Seidov D, Sarnthein M, Stattegger K, Prien R, Weinelt
M (1996) North Atlantic ocean circulation during the
last glacial maximum and a subsequent meltwater
event: A numerical model. J Geophys Res 101:
16,305-16,332
Stiissel A, Oberhuber JM, Maier-Reimer E (1996) On the
representation of sea ice in global ocean general circulationmodels.JGeophysRes 101: 18,193-18,212
Thompson SL, Pollard D (1997) Ice-sheet mass balance
at the last glacial maximum from the GENESIS Version 2 Global Climate Model. Ann Glaciol, in press
Turchin VF, Kozlov VP, Malkevich MS (1971) The use
of mathematical-statistics methods in the solution
of incorrectly posed problems. Soviet Physics
Uspekhi 13: 681
Tushingham HM, Peltier WR (1991) A global model of
late pleistocene deglaciation based upon geophysical predictions of post-glacial relative sea level
change. J Geophys Res 96: 4497-4523
713
Prunet P, Minster J, Ruiz-Pino D (1996a) Assimilation of
surface data in a one-dimensional physicalbiogeochemical model of the surface ocean. 1.
Method and preliminary results. Global Biogeochem
Cycles 10: 111-138
Prunet P, Minster J, Echevin V, Dadou 1 (1996b) Assimilation of surface data in a one-dimensional physical-biogeochemical model of the surface ocean. 2.
Adjusting a simple trophic model to chlorophyll,
temperature, nitrate, and pC0 2 data. Global
Biogeochem Cycles 10: 139-158
Rind D, Peteet D (1985) Terrestrial conditions at the last
glacial maximum and CLIMAP sea-surface temperature estimates: Are they consistent? Quat Res 24:
1-22
Roeckner E, Arpe K, Bengtsson L, Christoph M,
Claussen M, Diimenil L, Esch M, Giorgetta M,
Schlese U, Schulzweida U (1996) The atmospheric
general circulation model ECHAM 4: Model description and simulation of present-day climate. Report
No. 218, Max-Planck-Institut fiir Meteorologie,
Hamburg
Sarnthein M, Winn K, Zahn R (1987) Paleoproductivity
of oceanic upwelling and the effect on atmospheric
CO 2 and climatic change during deglaciation times.
In: Berger WH, Labeyrie LD (eds) Abrupt Climatic
Change. NATO ASI Series C 216, Springer, Berlin
Heidelberg New York, pp311-337
Samthein M, Winn K, Duplessy JC, Fontugne MR(1988)
Global variations of surface ocean productivity in
low and mid latitudes. Paleoceanography 3: 361-399
Sarnthein M, Jansen E, Arnold M, Duplessy JC,
Erlenkeuser H, Flatoy A, Veum T, Vogelsang E,
Weinelt MS (1992) A time-slice reconstruction of
meltwater anomalies at termination I in the North
Atlantic between 50 and 80 0 N. In: Bard E, Broecker
W (eds) The Last Deglaciation: Absolute and Radiocarbon Chronologies. NATO AS! Series, Vol 12,
Springer, Berlin Heidelberg New York,
pp433-458
Sarnthein M, Winn K, Jung SJA, Duplessy JC, Labeyrie
L, Erlenkeuser H, Ganssen G (1994) Changes in east
Atlantic deepwater circulation over the last 30,000
years: Eight time slice reconstructions.
Paleoceanography 9: 209-267
Sarnthein M, Jansen E, Weinelt M, Arnold M, Duplessy
JC, Erlenkeuser H, Flatoy A, Johannessen G,
Johannessen T, Jung S, Koc N, Labeyrie L, Maslin
M, Ptlaumann U, Schulz H (1995) Variations
in Atlantic surface ocean paleoceanography,
50 0 N - 80 0 N: A time-slice record of the last
30,000 years. Paleoceanography 10: 1063-1094
Sausen R, Barthel K, Hasselmann K (1988) Coupled
ocean-atmosphere models with flux correction. Clim
Dyn2: 145-163
Sausen R, Lunkeit F (1990) Some remarks on the cause
of the climate drift of coupled ocean-atmosphere
models. Beitr Phys Atmosph 63: 141-146
Sausen R, Voss R (1996) Techniques for asynchronous
and periodically synchronous coupling of atmosphere and ocean models. Part I: General strategy and
application to cyclo-stationary case. Clim Dyn 12:
313-323
Schafer-Neth C (1998) Changes in the seawater-oxygen
isotope relation between last glacial and present:
Sediment core data and OGCM modelling. Paleoclimates 2 (2-3): 101-131
Schlesinger ME (1979) Discussion of"A global oceanatmosphere model with seasonal variation for future
studies of climate sensitivity". Dynam Atmos Oceans
3:427-432
Schlitzer R (1993a) An adjoint model for the determination of the mean oceanic circulation, air-sea fluxes
and mixing coefficients. Habilitation thesis, Univ
Bremen, pp 1-88
Schlitzer R (1993b) Determining the mean, large-scale circulation of the Atlantic with the adjoint method.
J Phys Oceanogr 23: 1935-1952
Seidov D, Prien R (1996) A coarse resolution North
Atlantic Ocean circulation model: An intercomparison study with a paleoceanographic example. Annals Geophys 14: 246-257
Seidov D, Sarnthein M, Stattegger K, Prien R, Weinelt
M (1996) North Atlantic ocean circulation during the
last glacial maximum and a subsequent meltwater
event: A numerical model. J Geophys Res 101:
16,305-16,332
Stiissel A, Oberhuber JM, Maier-Reimer E (1996) On the
representation of sea ice in global ocean general circulationmodels.JGeophysRes 101: 18,193-18,212
Thompson SL, Pollard D (1997) Ice-sheet mass balance
at the last glacial maximum from the GENESIS Version 2 Global Climate Model. Ann Glaciol, in press
Turchin VF, Kozlov VP, Malkevich MS (1971) The use
of mathematical-statistics methods in the solution
of incorrectly posed problems. Soviet Physics
Uspekhi 13: 681
Tushingham HM, Peltier WR (1991) A global model of
late pleistocene deglaciation based upon geophysical predictions of post-glacial relative sea level
change. J Geophys Res 96: 4497-4523