Combination of insolation and ice-sheet forcing drive enhanced humidity in northern subtropical regions during MIS 13
Marine Isotope Stage (MIS) 13, ∼533–478 ka, has received particular attention due to the unexpected enhancement of monsoon systems under a cool climate characterized by lower atmospheric CO2 and larger ice volume than many other interglacials. Key questions remain about its regional expression (inte...
| Autores: | , , , , , , , , , , , |
|---|---|
| Tipo de documento: | artigo |
| Estado: | Versión aceptada para publicación |
| Data de publicação: | 2020 |
| País: | España |
| Recursos: | Consejo Superior de Investigaciones Científicas (CSIC) |
| Repositório: | DIGITAL.CSIC. Repositorio Institucional del CSIC |
| OAI Identifier: | oai:digital.csic.es:10261/221055 |
| Acesso em linha: | http://hdl.handle.net/10261/221055 |
| Access Level: | Acceso aberto |
| Palavra-chave: | Mid-Brunhes event Interglacial MIS 13 Mediterranean vegetation Model-data comparison Insolation Ice-sheets |
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| dc.title.none.fl_str_mv |
Combination of insolation and ice-sheet forcing drive enhanced humidity in northern subtropical regions during MIS 13 |
| title |
Combination of insolation and ice-sheet forcing drive enhanced humidity in northern subtropical regions during MIS 13 |
| spellingShingle |
Combination of insolation and ice-sheet forcing drive enhanced humidity in northern subtropical regions during MIS 13 Oliveira, Dulce Mid-Brunhes event Interglacial MIS 13 Mediterranean vegetation Model-data comparison Insolation Ice-sheets |
| title_short |
Combination of insolation and ice-sheet forcing drive enhanced humidity in northern subtropical regions during MIS 13 |
| title_full |
Combination of insolation and ice-sheet forcing drive enhanced humidity in northern subtropical regions during MIS 13 |
| title_fullStr |
Combination of insolation and ice-sheet forcing drive enhanced humidity in northern subtropical regions during MIS 13 |
| title_full_unstemmed |
Combination of insolation and ice-sheet forcing drive enhanced humidity in northern subtropical regions during MIS 13 |
| title_sort |
Combination of insolation and ice-sheet forcing drive enhanced humidity in northern subtropical regions during MIS 13 |
| dc.creator.none.fl_str_mv |
Oliveira, Dulce Desprat, Stéphanie Rodrigues, Teresa Yin, Qiuzhen Naughton, Filipa Trigo, Ricardo M. Su, Qianqian Grimalt, Joan O. Alonso-García, Montserrat Voelker, Antje H. L. Abrantes, Fátima Sánchez Goñi, Maria Fernanda |
| author |
Oliveira, Dulce |
| author_facet |
Oliveira, Dulce Desprat, Stéphanie Rodrigues, Teresa Yin, Qiuzhen Naughton, Filipa Trigo, Ricardo M. Su, Qianqian Grimalt, Joan O. Alonso-García, Montserrat Voelker, Antje H. L. Abrantes, Fátima Sánchez Goñi, Maria Fernanda |
| author_role |
author |
| author2 |
Desprat, Stéphanie Rodrigues, Teresa Yin, Qiuzhen Naughton, Filipa Trigo, Ricardo M. Su, Qianqian Grimalt, Joan O. Alonso-García, Montserrat Voelker, Antje H. L. Abrantes, Fátima Sánchez Goñi, Maria Fernanda |
| author2_role |
author author author author author author author author author author author |
| dc.contributor.none.fl_str_mv |
Ministerio de Ciencia e Innovación (España) Grimalt, Joan O. [0000-0002-7391-5768] Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72] |
| dc.subject.none.fl_str_mv |
Mid-Brunhes event Interglacial MIS 13 Mediterranean vegetation Model-data comparison Insolation Ice-sheets |
| topic |
Mid-Brunhes event Interglacial MIS 13 Mediterranean vegetation Model-data comparison Insolation Ice-sheets |
| description |
Marine Isotope Stage (MIS) 13, ∼533–478 ka, has received particular attention due to the unexpected enhancement of monsoon systems under a cool climate characterized by lower atmospheric CO2 and larger ice volume than many other interglacials. Key questions remain about its regional expression (intensity, climate variability, length), and underlying forcing factors, in particular at the mid-latitudes. Here we examine the SW Iberian vegetation, terrestrial climate and sea surface temperature (SST) variability during MIS 13 by combining pollen and biomarker data from IODP Site U1385 with climate-model experiments. We show, for the first time, that despite strong precessional forcing, MIS 13 stands out for its large forest expansions with a reduced Mediterranean character alternating with muted forest contractions, indicating that this stage is marked by a cool-temperate climate regime with high levels of humidity. Results of our data-model comparison reveal that MIS 13 orbitally driven SW Iberian climate and vegetation changes are modulated by the relatively strong ice-sheet forcing. We find that the Northern Hemisphere ice-sheets prescribed at the MIS 13 climate optimum reinforce the insolation effect by increasing the tree fraction and both winter and summer precipitation. We propose that the interactions between ice-sheets and major atmospheric circulation systems may have resulted in the persistent influence of the mid-latitude cells over the SW Iberian region, which led to intensified moisture availability and reduced seasonality, and, in turn, to a pronounced expansion of the temperate forest. |
| publishDate |
2020 |
| dc.date.none.fl_str_mv |
2020 2020 2020 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article http://purl.org/coar/resource_type/c_6501 Postprint info:eu-repo/semantics/acceptedVersion |
| format |
article |
| status_str |
acceptedVersion |
| dc.identifier.none.fl_str_mv |
http://hdl.handle.net/10261/221055 |
| url |
http://hdl.handle.net/10261/221055 |
| dc.language.none.fl_str_mv |
Inglés |
| language_invalid_str_mv |
Inglés |
| dc.relation.none.fl_str_mv |
#PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/RTI2018-099489-B-I00. Q. https://doi.org/10.1016/j.quascirev.2020.106573 Sí |
| dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess |
| eu_rights_str_mv |
openAccess |
| dc.publisher.none.fl_str_mv |
Elsevier |
| publisher.none.fl_str_mv |
Elsevier |
| dc.source.none.fl_str_mv |
reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC instname:Consejo Superior de Investigaciones Científicas (CSIC) |
| instname_str |
Consejo Superior de Investigaciones Científicas (CSIC) |
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DIGITAL.CSIC. Repositorio Institucional del CSIC |
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DIGITAL.CSIC. Repositorio Institucional del CSIC |
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| _version_ |
1869421405113679872 |
| spelling |
Combination of insolation and ice-sheet forcing drive enhanced humidity in northern subtropical regions during MIS 13Oliveira, DulceDesprat, StéphanieRodrigues, TeresaYin, QiuzhenNaughton, FilipaTrigo, Ricardo M.Su, QianqianGrimalt, Joan O.Alonso-García, MontserratVoelker, Antje H. L.Abrantes, FátimaSánchez Goñi, Maria FernandaMid-Brunhes eventInterglacial MIS 13Mediterranean vegetationModel-data comparisonInsolationIce-sheetsMarine Isotope Stage (MIS) 13, ∼533–478 ka, has received particular attention due to the unexpected enhancement of monsoon systems under a cool climate characterized by lower atmospheric CO2 and larger ice volume than many other interglacials. Key questions remain about its regional expression (intensity, climate variability, length), and underlying forcing factors, in particular at the mid-latitudes. Here we examine the SW Iberian vegetation, terrestrial climate and sea surface temperature (SST) variability during MIS 13 by combining pollen and biomarker data from IODP Site U1385 with climate-model experiments. We show, for the first time, that despite strong precessional forcing, MIS 13 stands out for its large forest expansions with a reduced Mediterranean character alternating with muted forest contractions, indicating that this stage is marked by a cool-temperate climate regime with high levels of humidity. Results of our data-model comparison reveal that MIS 13 orbitally driven SW Iberian climate and vegetation changes are modulated by the relatively strong ice-sheet forcing. We find that the Northern Hemisphere ice-sheets prescribed at the MIS 13 climate optimum reinforce the insolation effect by increasing the tree fraction and both winter and summer precipitation. We propose that the interactions between ice-sheets and major atmospheric circulation systems may have resulted in the persistent influence of the mid-latitude cells over the SW Iberian region, which led to intensified moisture availability and reduced seasonality, and, in turn, to a pronounced expansion of the temperate forest.Financial support was provided by the Portuguese Foundation for Science and Technology (FCT) through the project CLIMHOL (PTDC/AAC-CLI/100157/2008), ULTImATum (IF/01489/2015), SAICT-45-2017-02 projects (WARM WORLDS: 29897 and HOLMODRIVE: 29029), CCMAR FCT Research Unit - project UIDB/04326/2020, D. Oliveira’s contract (CEECIND/02208/2017), F. Naughton’s contract (IF/01489/2015), T. Rodrigues’s contract (WarmWorld- PTDC/CTA-GEO/29897/2017), Voelker’s contract (IF/01500/2014), and WarmClim, a LEFE-INSU IMAGO project. D. Oliveira acknowledges the fundng provided by the L’Oréal Portugal Medal of Honour for Women in Science 2018 from L’Oréal, FCT and UNESCO. M. Alonso-Garcia acknowledges funding from FCT through the CINNAMOW project (PTDC/MAR-PRO/3396/2014) and the Spanish Ministry of Science through the grant RTI2018-099489-B-I00. Q. Yin is a Research Associate of the Belgian National Fund for Scientific Research (FRS-FNRS). Computational resources have been provided by the supercomputing facilities of the Université catholique de Louvain (CISM/UCL) and the Consortium des Equipements de Calcul Intensif en Fédération Wallonie Bruxelles (CECI) funded by FRS-FNRS. We would like to thank the scientists and technicians of IODP Expedition 339, the Bremen Core Repository, L. Devaux for technical assistance, V. Hanquiez for drawing Fig. 1., and two anonymous reviewers for their constructive comments.Peer reviewedElsevierMinisterio de Ciencia e Innovación (España)Grimalt, Joan O. [0000-0002-7391-5768]Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]202020202020info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501Postprintinfo:eu-repo/semantics/acceptedVersionhttp://hdl.handle.net/10261/221055reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)Inglés#PLACEHOLDER_PARENT_METADATA_VALUE#info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/RTI2018-099489-B-I00. Q.https://doi.org/10.1016/j.quascirev.2020.106573Síinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/2210552026-05-22T06:33:51Z |
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15,811543 |