Dipòsit Digital de Documents de la UAB 6 registres trobats  La cerca s'ha fet en 0.02 segons. 
1.
21 p, 9.7 MB Sea surface temperature variability in the central-western Mediterranean Sea during the last 2700 years : a multi-proxy and multi-record approach / Cisneros, Mercè (Universitat de Barcelona. Departament de Dinàmica de la Terra i de l’Oceà) ; Cacho, Isabel (Universitat de Barcelona. Departament de Dinàmica de la Terra i de l’Oceà) ; Frigola, J. (Universitat de Barcelona. Departament de Dinàmica de la Terra i de l’Oceà) ; Canals Artigas, Miquel (Universitat de Barcelona. Departament de Dinàmica de la Terra i de l’Oceà) ; Masqué Barri, Pere (Universitat Autònoma de Barcelona. Departament de Física) ; Martrat, Belen (Institut de Diagnosi Ambiental i Estudis de l’Aigua) ; Casado, Marta (Institut de Diagnosi Ambiental i Estudis de l’Aigua) ; Grimalt, Joan O. (Institut de Diagnosi Ambiental i Estudis de l’Aigua) ; Pena, Leopoldo D. (Universitat de Barcelona. Departament de Dinàmica de la Terra i de l’Oceà) ; Margaritelli, Giulia (Istituto per l’Ambiente Marino Costiero) ; Lirer, Fabrizio (Istituto per l’Ambiente Marino Costiero)
This study presents the reconstructed evolution of sea surface conditions in the central-western Mediterranean Sea during the late Holocene (2700 years) from a set of multi-proxy records as measured on five short sediment cores from two sites north of Minorca (cores MINMC06 and HERMC-MR3). [...]
2016 - 10.5194/cp-12-849-2016
Climate of the past, Vol. 12, issue 4 (April 2016) , p. 849-869  
2.
17 p, 12.9 MB Hosed vs. unhosed : interruptions of the Atlantic Meridional overturning circulation in a global coupled model, with and without freshwater forcing / Brown, Nicolas (McGill University. Department of Earth and Planetary Science) ; Galbraith, Eric D. (Universitat Autònoma de Barcelona. Institut de Ciència i Tecnologia Ambientals)
It is well known that glacial periods were punctuated by abrupt climate changes, with large impacts on air temperature, precipitation, and ocean circulation acrossa the globe. However, the long-held idea that freshwater forcing, caused by massive iceberg discharges, was the driving force behind these changes has been questioned in recent years. [...]
2016 - 10.5194/cp-12-1663-2016
Climate of the past, Vol. 12, issue 8 (Aug. 2016) , p. 1663-1679  
3.
11 p, 659.8 KB Salinity changes in the Agulhas leakage area recorded by stable hydrogen isotopes of C37 alkenones during Termination I and II / Kasper, S. (Koninklijk Nederlands Instituut voor Onderzoek der Zee) ; Van der Meer, M. T. J. (Koninklijk Nederlands Instituut voor Onderzoek der Zee) ; Mets, A. (Koninklijk Nederlands Instituut voor Onderzoek der Zee) ; Zahn, Rainer (Universitat Autònoma de Barcelona. Institut de Ciència i Tecnologia Ambientals) ; Sinninghe Damsté, J. S. (Koninklijk Nederlands Instituut voor Onderzoek der Zee) ; Schouten, Stefan (Koninklijk Nederlands Instituut voor Onderzoek der Zee)
At the southern tip of Africa, the Agulhas Current reflects back into the Indian Ocean causing so-called “Agulhas rings” to spin off and release relatively warm and saline water into the South Atlantic Ocean. [...]
2014 - 10.5194/cp-10-251-2014
Climate of the past, Vol. 10, issue 1 (February 2014) , p. 251-260  
4.
18 p, 4.1 MB Productivity response of calcareous nannoplankton to Eocene Thermal Maximum 2 (ETM2) / Dedert, M. (Vrije Universiteit Amsterdam. Cluster Earth & Climate Department of Earth Sciences) ; Stoll, H. M. (Universidad de Oviedo. Departamento de Geologia) ; Kroon, D. (University of Edinburgh. School of GeoSciences) ; Shimizu, N. (Woods Hole Oceanographic Institute) ; Kanamaru, K. (University of Massachusetts at Amherst. Department of Geosciences) ; Ziveri, Patrizia (Universitat Autònoma de Barcelona. Departament de Biologia Animal, de Biologia Vegetal i d'Ecologia)
The Early Eocene Thermal Maximum 2 (ETM2) at ~53. 7 Ma is one of multiple hyperthermal events that followed the Paleocene-Eocene Thermal Maximum (PETM, ~56 Ma). The negative carbon excursion and deep ocean carbonate dissolution which occurred during the event imply that a substantial amount (10³ Gt) of carbon (C) was added to the ocean-atmosphere system, consequently increasing atmospheric CO₂(pCO₂). [...]
2012 - 10.5194/cp-8-977-2012
Climate of the Past, Vol. 8, issue 3 (May 2012) , p. 977-993  
5.
21 p, 3.0 MB Tracking climate variability in the western Mediterranean during the Late Holocene : a multiproxy approach / Nieto Moreno, V. (Instituto Andaluz de Ciencias de la Tierra) ; Martínez Ruiz, F. (Instituto Andaluz de Ciencias de la Tierra) ; Giralt, S. (Institut de Ciències de la Terra Jaume Almera) ; Jiménez Espejo, F. (Instituto Andaluz de Ciencias de la Tierra) ; Gallego Torres, D. (Universidad de Granada. Departamento de Mineralogía y Petrología) ; Rodrigo Gámiz, M. (Instituto Andaluz de Ciencias de la Tierra) ; Garcia i Orellana, Jordi (Universitat Autònoma de Barcelona. Departament de Física) ; Ortega Huertas, M. (Universidad de Granada. Departamento de Mineralogía y Petrología) ; De Lange, G. J. (Utrecht University. Marine Geochemistry and Chemical Oceanography)
Climate variability in the western Mediterranean is reconstructed for the last 4000 yr using marine sediments recovered in the west Algerian-Balearic Basin, near the Alboran Basin. Fluctuations in chemical and mineralogical sediment composition as well as grain size distribution are linked to fluvial-eolian oscillations, changes in redox conditions and paleocurrent intensity. [...]
2011 - 10.5194/cp-7-1395-2011
Climate of the Past, Vol. 7 No. 4 (Dec. 2011) , p. 1395-1414  
6.
12 p, 699.3 KB The impact of the Little ice age on coccolithophores in the central Mediterranea Sea / Incarbona, A. (Università degli Studi di Palermo. Dipartimento di Geologia e Geodesia) ; Ziveri, Patrizia (Universitat Autònoma de Barcelona. Departament de Biologia Animal, de Biologia Vegetal i d'Ecologia) ; Di Stefano, E. (Università degli Studi di Palermo. Dipartimento di Geologia e Geodesia) ; Lirer, F. (Istituto per l’Ambiente Marino Costiero) ; Mortyn, Peter Graham (Universitat Autònoma de Barcelona. Institut de Ciència i Tecnologia Ambientals) ; Patti, B. (Istituto per l’Ambiente Marino Costiero) ; Pelosi, N. (Istituto per l’Ambiente Marino Costiero) ; Sprovieri, M. (Istituto per l’Ambiente Marino Costiero) ; Tranchida, G. (Istituto per l’Ambiente Marino Costiero) ; Vallefuoco, M. (Istituto per l’Ambiente Marino Costiero) ; Albertazzi, S. (Istituto Scienze Marine. Sezione di Geologia Marina) ; Bellucci, L. G. (Istituto Scienze Marine. Sezione di Geologia Marina) ; Bonanno, A. (Istituto per l’Ambiente Marino Costiero) ; Bonomo, S. (Istituto di biomedicina e di immunologia molecolare "Alberto Monroy") ; Censi, P. (Università degli Studi di Palermo. Dipartimento di Fisica e Chimica della Terra) ; Ferraro, L. (Istituto per l’Ambiente Marino Costiero) ; Giuliani, S. (Istituto Scienze Marine. Sezione di Geologia Marina) ; Mazzola, S. (Istituto per l’Ambiente Marino Costiero) ; Sprovieri, R. (Università degli Studi di Palermo. Dipartimento di Geologia e Geodesia)
The Little ice age (LIA) is the last episode of a series of Holocene climatic anomalies. There is still little knowledge on the response of the marine environment to the pronounced cooling of the LIA and to the transition towards the 20th century global warming. [...]
2010 - 10.5194/cp-6-795-2010
Climate of the Past, Vol. 6 No. 6 (Dec. 2010) , p. 795-805  

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