Zobrazeno 1 - 10
of 86
pro vyhledávání: '"Antje H L Voelker"'
Publikováno v:
Atmosphere, Vol 13, Iss 9, p 1378 (2022)
In order to better understand interglacial climate variability within the 41 kyr world, we produced high-resolution climate records for interglacial Marine Isotope Stage (MIS) 47 (1424–1452 ka) at IODP Site U1387 (36°48′ N, 7°43′ W) on the so
Externí odkaz:
https://doaj.org/article/f4c308635c5142ac8fc73176d179f700
Autor:
Qianqian Su, Stéphanie Desprat, Maria Fernanda Sanchez Goñi, Fatima F Abrantes, Joan O. Grimalt, Ricardo M. Trigo, Qiuzhen Yin, Teresa Rodrigues, Antje H L Voelker, Filipa Naughton, Dulce Oliveira, Montserrat Alonso-Garcia
Marine Isotope Stage (MIS) 13, ~500 ky ago, represents a Quaternary interglacial of primary interest due to the unexpected enhancement of monsoon systems under a cool climate characterised by low atmospheric CO2 and larger ice volume than the present
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1c17b47782ca1b0256b59e0c6240a22f
https://doi.org/10.5194/egusphere-egu21-11408
https://doi.org/10.5194/egusphere-egu21-11408
Autor:
Michael Schulz, Joanna J Waniek, Michal Kucera, Lukas Jonkers, Andreia Rebotim, Antje H L Voelker
Stable oxygen isotopes (δ18O) of planktonic foraminifera are one of the most used tools to reconstruct environmental conditions of the water column. Since different species live and calcify at different depths in the water column, the δ18O of sedim
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::151a4af3636067160f6cdf4ef9d1d8b0
https://doi.org/10.5194/egusphere-egu21-10173
https://doi.org/10.5194/egusphere-egu21-10173
In the past decades a northward expansion of North Atlantic subtropical water masses1-3 and warming of subtropical mode water4,5 (350 – 400 m depth) has been observed. Paleoceanographic records from interglacials prior to 400 ka (‘early Brunhes
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::10917d05238a8806a4349bf8ed3cf8a2
https://doi.org/10.5194/egusphere-egu21-350
https://doi.org/10.5194/egusphere-egu21-350
Autor:
Carlos S. Melo, Ana C. Rebelo, Antje H L Voelker, Joana Pombo, Ricardo Cordeiro, Ana Hipólito, António M. Santos, Lara Baptista, Patrícia Madeira, Sérgio P. Ávila, Andrea Z. Botelho
Publikováno v:
Repositório Científico de Acesso Aberto de Portugal
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
instacron:RCAAP
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
instacron:RCAAP
The marine topshell Phorcus sauciatus is currently found along the temperate-subtropical shores of the Northeast Atlantic Ocean. Although present in the Iberian Peninsula, Madeira, and Canaries for centuries, P. sauciatus has only recently reached an
Publikováno v:
Repositório Científico de Acesso Aberto de Portugal
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
instacron:RCAAP
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
instacron:RCAAP
Reconstruction of the Mediterranean Outflow Water (MOW) dynamics in the geologic past contributes to exploring its influence on the North Atlantic Ocean circulation and global climate. The middle Pleistocene transition (MPT) is one of the most import
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1fe699b9c012c687b8738662fed1c75d
Autor:
Pedro Silva, Anxo Mena, Filipa Naughton, David Casas, Emilia Salgueiro, Gemma Ercilla, Manuel Teixeira, Cristina Roque, Fatima F Abrantes, Antje H L Voelker, Pedro Terrinha
Publikováno v:
Repositório Científico de Acesso Aberto de Portugal
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
instacron:RCAAP
Digital.CSIC. Repositorio Institucional del CSIC
instname
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
instacron:RCAAP
Digital.CSIC. Repositorio Institucional del CSIC
instname
17 pages, 11 figures, 1 table
The Sines Contourite Drift (SCD), located in the Alentejo margin, southwest Iberian continental margin, has been through many depositional phases in result of climatic variations and bottom current oscillations, whi
The Sines Contourite Drift (SCD), located in the Alentejo margin, southwest Iberian continental margin, has been through many depositional phases in result of climatic variations and bottom current oscillations, whi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::309c8da33a07ad46a095444c95dcfef5
Publikováno v:
Naafs, B D A, Voelker, A H L, Karas, C, Andersen, N & Sierro, F J 2020, ' Repeated near-collapse of the Pliocene sea surface temperature gradient in the North Atlantic ', Paleoceanography and Paleoclimatology, vol. 35, no. 5, e2020PA003905 . https://doi.org/10.1029/2020PA003905
Repositório Científico de Acesso Aberto de Portugal
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
instacron:RCAAP
Repositório Científico de Acesso Aberto de Portugal
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
instacron:RCAAP
Sea surface temperature (SST) is used to infer past changes in the state of the climate system. Here we use a combination of newly generated and published organic paleothermometer records, together with novel high‐resolution benthic foraminiferal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::551af1b9fc46f0b7526dc0c33dc6686b
https://research-information.bris.ac.uk/ws/files/231776426/Gradient_paper_final_3_.pdf
https://research-information.bris.ac.uk/ws/files/231776426/Gradient_paper_final_3_.pdf
Autor:
B. David A. Naafs, Henning Kuhnert, Nils Andersen, Antje H L Voelker, Francisco Javier Sierro
The early Pliocene, with atmospheric CO2 concentrations at levels similar to today, is seen as a case study for Earth’s future climate evolution. During this period the progressive closing of the Central American Seaway led to increased poleward he
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::88aa1acdfbf128ad6caf256488647c55
https://doi.org/10.5194/egusphere-egu2020-10667
https://doi.org/10.5194/egusphere-egu2020-10667
Ocean circulation plays an essential role in Earth’s climate and the global carbon cycle. A prerequisite for improving confidence in future climate projections is the accurate numerical modeling of past deep ocean circulation changes. Unfortunately
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6a450ede136942ce8357fa02fd7a0750
https://doi.org/10.5194/egusphere-egu2020-19759
https://doi.org/10.5194/egusphere-egu2020-19759