2001 - 2003 <strong>The</strong> TEMPUS project on intercalibration and application of alkenones forpaleotemperature reconstructions in the surface ocean – EU 5 th FrameworkProgramme – (A. Rosell-Melé, Barcelona (coordinator))2002 - 2004 Coordinated European Surface <strong>Ocean</strong> Palaeo-estimation Collaboration, (CESOP)–- (E. Jansen, Bergen (coordinator))2002 - 2004 European Co-ordination on Mediterranean and Black Sea Prodeltas,(EURODELTA) – EU 5 th Framework Programme – (F. Trincardi, Bologna(coordinator))2002 - 2006 PROfiles across Mediterranean Sedimentary Systems. Part 1 (PROMESS 1) – EU5 th Framework Programme – (S. Berné, Brest (coordinator))2003 - 2006 Models and observations to test climate feedbacks (MOTIF) – EU 5 th FrameworkProgramme – (P. Branconot, Paris (coordinator))2003 - 2006 Sedimentation Processes on the Portuguese Margin (SEDPORT): <strong>The</strong> Role ofContinental Climate, <strong>Ocean</strong> Circulation, Sea Level, and Neotectonics – EuropeanScience Foundation, Eurocores Euromargin Programme – (coordinator)Main PublicationsLorenz S, Kim J-H, Rimbu N, Schneider RR, Lohmann G (2006) Contrary Holocene sea-surfacetemperature trends between the tropics and the extra-tropics. Paleoceanography, 21, PA1002,doi 10.1029/2005PA001152.Weldeab S, Schneider RR, Kölling M (2006) Deglacial sea surface temperature and salinityincrease in the western tropical Atlantic in synchrony with high latitude climate instabilities. EarthPlanetary Science Letters 241, 699 -706Schefuß E, Schouten S, Schneider RR (2005) Climatic controls on central African hydrologyduring the last 20,000 years. Nature doi 10.1038/03945.Rimbu N, Lohmann G, Lorenz S, Kim JH, Schneider RR (2004) Holocene climate variability asderived from alkenone sea surface temperature and coupled ocean-atmosphere modelexperiments. Climate Dynamics 23, 215–227.Kim JH, Rimbu N, Lorenz SJ, Lohmann G, Nam S-Il, Schouten S, Rühlemann C, Schneider RR(2004) North Pacific and North Atlantic sea-surface temperature variability during the Holocene.Quaternary Science Reviews 23, 2141–2154.Peeters FJC, Acheson R, Brummer G-J, deRuijter WPM, Schneider RR, Ganssen GM, Ufkes E,Kroon, D. (2004) Vigorous exchange between Indian and Atlantic ocean at the end of the pastfive glacial periods. Nature 430, 661-665.Kim J-H, Schneider RR (2003) Low-latitude control of interhemispheric sea-surface temperaturecontrast in the tropical Atlantic over the past 22 kyr: <strong>The</strong> role of SE trade winds. ClimateDynamics 21, 337-347.Kim J-H, Schneider RR, Mulitza S, Müller PJ (2003) Reconstruction of SE trade wind intensitybased on sea-surface temperature gradients in the SE Atlantic over the last 25 kyr. GeophysicalResearch Lett 30 (22), 2144, doi:10.1029/2003GL017557.Schneider RR (2001) Alkenone temperature and carbon isotope records: Temporal resolution,offsets, and regionality. Geochemistry, Geophysics, Geosystems 2, doi 2000GC000060.Schneider RR, Müller PJ, Ruhland G (1995) Late Quaternary surface circulation in the eastequatorialSouth Atlantic: Evidence from alkenone sea-surface temperatures. Paleoceanography10(2), 197-219.A59
Curriculum of ResearchPersonal DataNameSchneider, Reinhold, Prof. Dr.born at 20.03.1957 in BerndrothAffiliationInstitutionChristian-Albrechts-University in Kiel, (CAU)Institute/Department Department of Computer Science and Applied MathematicsAddress Christian-Albrechts-Platz 4City, ZIP CodeD-24118 KielPhone +49-431-880-7470Fax +49-431-880-4464e-mailrs@numerik.uni-kiel.deEducation1975 University Entrance Qualification1982 Masters (Mathematics)1989 PhD1995 HabilitationResearch Experience1994 - 1996 Member of SFB 298 Research Group “Deformation und Versagen beimetallischen und granularen Werkstoffen”1995 - 1996 Representation of C3-professorships , Univ. Essen and RWTH Aachen1996 C4-professorship, Techn. Univ. Chemnitz1997 - 2002 Member of EU-TMR-Network “Wavelets and multiscale methodsin numerical simulation”1997 - 2003 Member of SFB 393 Research Group “Numerische Simulation auf massivparallelen Rechnern”: Biorthogonale Waveletbasen zur parallelen Behandlung fürRandintegralgleichungen2002 - 2005 Member of EU-Project IHP Network H.HPRN-CT-2002-00286 “Nonlinearapproximation and adaptivity: breaking complexity in numerical modelling anddata representation”2003 - C4-professorship, CAU Kiel2004 - 2006 Member of SPP 1145 “Moderne und universelle first-principles Methoden fürMehrelektronensysteme in Chemie und Physik”2005 - 2007 Member of EU-Project BIGDFT: “Density functional calculations for systems ofunprecedented size on parallel computers”Main PublicationsDahmen W, Harbrecht H, Schneider R (2006) Compression Techniques for Boundary IntegralEquations - Optimal Complexity Estimates, SIAM J. Numer. Anal. 43 (6), 2251-2271.Flad H-J, Hackbusch W, Schneider R (2006) Best N-term approximation in electronic structurecalculations I. One-electron reduced density matrix. M2AN 40, 49-61.Harbrecht H, Schneider R (2006) Wavelet Galerkin Schemes for Boundary Integral Equations -Implementation and Quadrature, SIAM J. Sci. Comput. 27 (4), 1347-1370.Beuchler S, Schneider R, Schwab C (2004) Multiresolution weighted norm equivalences andapplications. Numer. Math. 98 (1), 67--97.Gatica G N, Harbrecht H, Schneider R (2003) Least squares methods for the coupling of FEMand BEM, SIAM J. Numer. Anal. 41 (5), 1974-1995.Harbrecht H, Pereverzev S, Schneider R (2003) Self-regularization by projection for noisypseudodifferential equations of negative order, Numer. Math. 95 (1), 123-143.Dahmen W, Kunoth A, Schneider R (2002) Wavelet least squares methods for boundary valueproblems. SIAM J. Numer. Anal. 39 (6), 1985--2013.Harbrecht H, Paiva F, Pérez C, Schneider R (2002) Biorthogonal wavelet approximation for thecoupling of FEM-BEM, Numer. Math. 92 (2), 325-356.A60
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Contents1 General Information about
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1 General Information about the Clu
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1.2 Research Program1.2.1 Summary/Z
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1.2.2.2 ObjectivesThe Future Ocean
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will address the emerging new resea
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Topics Objectives DisciplinesA1 Exa
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development of these new initiative
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Project Objective IndustryPartnersO
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Continued excellence in the field o
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The establishment of several new po
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1.4.1 Integrated School of Ocean Sc
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ensure that emerging innovations wi
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Institute / DisciplineAcademic Leve
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their orientation according to the
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1.7.2 Structural Evolution and Qual
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organisms to elevated CO 2 and decr
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ist wahrscheinlich stärker als wä
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out by the proponents and will esta
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Rückkopplungsschleife weitere Erw
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enthic biota of gas release or the
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Synthese, aufbauend auf einer Kombi
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(4) a determination of the impact o
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Einflüsse. Um deren Auswirkungen b
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on longer time scales. The latter t
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the expertise which already exists
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2. State-of-the-artThe changing com
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• Field and laboratory investigat
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Erwärmung der Ozeane kann zur Frei
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Valuing the Ocean: Research focus a
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submarine earthquakes, slumps and s
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Fischerei ist eine der wichtigsten
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ecosystems. In particular, the foll
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Hochdurchsatztechnologien die Evolu
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microbial diversity on their barrie
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transient three-dimensional fluid f
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modeling, which describe chemical a
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Erdbeben, submarine Hangrutschungen
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Simons 2003) to investigate shallow
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damit zusammenhängender Meeresspie
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B5(1) Sea-Level Rise and Physical-M
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Pickrill RA, Todd BJ (2003) The mul
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Onate E, Piazzese J (2005) Decision
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echtlichen und ökonomischen Rahmen
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marine resources, such as energy ex
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2. State-of-the-artThe variety of n
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and will benefit from expertise in
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Die Plattform 2 stellt die analytis
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4. New Cluster TechnologiesIn order
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(iv) Proteomanalysetechniken und (v
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4. New Cluster TechnologiesA specia
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Illustration of existing/emerging a
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physical parameters (e.g. lowered a
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etabliert, das insbesondere auf wis
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2.4.3.2 Central Funds for Transfer
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International School of Ocean Scien
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Description Year of purchase Amount
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3.2 Auxiliary Support3.2.1 Total Fu
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Suess E, Torres ME, Bohrmann G, Col
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Schreiber, StefanVisbeck, MartinSri
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4.3 Third-Party FundingNo. FundingB
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f,rylheonRaytheon Anschütz GmbHPos