Cargando…

Greening of the Sahara suppressed ENSO activity during the mid-Holocene

The evolution of the El Niño-Southern Oscillation (ENSO) during the Holocene remains uncertain. In particular, a host of new paleoclimate records suggest that ENSO internal variability or other external forcings may have dwarfed the fairly modest ENSO response to precessional insolation changes simu...

Descripción completa

Detalles Bibliográficos
Autores principales:	Pausata, Francesco S. R., Zhang, Qiong, Muschitiello, Francesco, Lu, Zhengyao, Chafik, Léon, Niedermeyer, Eva M., Stager, J. Curt, Cobb, Kim M., Liu, Zhengyu
Formato:	Online Artículo Texto
Lenguaje:	English
Publicado:	Nature Publishing Group 2017
Materias:	Article
Acceso en línea:	https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5504352/ https://www.ncbi.nlm.nih.gov/pubmed/28685758 http://dx.doi.org/10.1038/ncomms16020

Ejemplares similares

End of Green Sahara amplified mid- to late Holocene megadroughts in mainland Southeast Asia
por: Griffiths, Michael L., et al.
Publicado: (2020)

Rainfall regimes of the Green Sahara
por: Tierney, Jessica E., et al.
Publicado: (2017)

Early Holocene greening of the Sahara requires Mediterranean winter rainfall
por: Cheddadi, Rachid, et al.
Publicado: (2021)

ITCZ shift and extratropical teleconnections drive ENSO response to volcanic eruptions
por: Pausata, Francesco S. R., et al.
Publicado: (2020)

Holocene hydroclimatic variability in the tropical Pacific explained by changing ENSO diversity
por: Karamperidou, Christina, et al.
Publicado: (2022)

Lakeside Cemeteries in the Sahara: 5000 Years of Holocene Population and Environmental Change
por: Sereno, Paul C., et al.
Publicado: (2008)

Inside the “African Cattle Complex”: Animal Burials in the Holocene Central Sahara
por: di Lernia, Savino, et al.
Publicado: (2013)

A predominantly tropical influence on late Holocene hydroclimate variation in the hyperarid central Sahara
por: Van der Meeren, Thijs, et al.
Publicado: (2022)

Pacific warm pool subsurface heat sequestration modulated Walker circulation and ENSO activity during the Holocene
por: Dang, Haowen, et al.
Publicado: (2020)

Enhanced ice sheet melting driven by volcanic eruptions during the last deglaciation
por: Muschitiello, Francesco, et al.
Publicado: (2017)

Dynamics of Green Sahara Periods and Their Role in Hominin Evolution
por: Larrasoaña, Juan C., et al.
Publicado: (2013)

A history of male migration in and out of the Green Sahara
por: Xue, Yali
Publicado: (2018)

Pastoralism may have delayed the end of the green Sahara
por: Brierley, Chris, et al.
Publicado: (2018)

Holocene ENSO variability in the South China Sea recorded by high-resolution oxygen isotope records from the shells of Tridacna spp.
por: Shao, Da, et al.
Publicado: (2020)

Explaining population booms and busts in Mid-Holocene Europe
por: Kondor, Dániel, et al.
Publicado: (2023)

Ancestral mitochondrial N lineage from the Neolithic ‘green’ Sahara
por: Vai, Stefania, et al.
Publicado: (2019)

The spatiotemporal extent of the Green Sahara during the last glacial period
por: Ait Brahim, Yassine, et al.
Publicado: (2023)

The impact of Arctic sea ice loss on mid-Holocene climate
por: Park, Hyo-Seok, et al.
Publicado: (2018)

Mid-Holocene Northern Hemisphere warming driven by Arctic amplification
por: Park, Hyo-Seok, et al.
Publicado: (2019)

Mean sea surface temperature changes influence ENSO-related precipitation changes in the mid-latitudes
por: Yang, Young-Min, et al.
Publicado: (2021)

Response of carbon cycle to drier conditions in the mid-Holocene in central China
por: Huang, Xianyu, et al.
Publicado: (2018)

Underlying causes of Eurasian midcontinental aridity in simulations of mid‐Holocene climate
por: Bartlein, Patrick J., et al.
Publicado: (2017)

The bioarchaeology of mid-Holocene pastoralist cemeteries west of Lake Turkana, Kenya
por: Sawchuk, Elizabeth A., et al.
Publicado: (2019)

Agricultural adaptations to mid-late Holocene climate change in western Türkiye
por: Maltas, Tom, et al.
Publicado: (2023)

Impacts of IOD, ENSO and ENSO Modoki on the Australian Winter Wheat Yields in Recent Decades
por: Yuan, Chaoxia, et al.
Publicado: (2015)

El Sahara : vínculos sociales y retos geoestratégicos
por: Cherkaoui, Mohamed
Publicado: (2008)

Impact of a drier Early–Mid-Holocene climate upon Amazonian forests
por: Mayle, Francis E, et al.
Publicado: (2008)

Regional population collapse followed initial agriculture booms in mid-Holocene Europe
por: Shennan, Stephen, et al.
Publicado: (2013)

Widespread population decline in South America correlates with mid-Holocene climate change
por: Riris, Philip, et al.
Publicado: (2019)

Increased chemical weathering during the deglacial to mid-Holocene summer monsoon intensification
por: Miriyala, Pavan, et al.
Publicado: (2017)

Dark Side Archaeology: Climate Change and Mid-Holocene Saharan Pastoral Adaptation
por: Holl, Augustin F. C.
Publicado: (2020)

Early to Mid-Holocene Palaeoenvironment Change and Sedimentary Evolution in the Xianghu Area, Zhejiang
por: Sha, Longbin, et al.
Publicado: (2020)

A large mid-Holocene estuary was not present in the lower River Murray, Australia
por: Tibby, J., et al.
Publicado: (2021)

The peopling of the last Green Sahara revealed by high-coverage resequencing of trans-Saharan patrilineages
por: D’Atanasio, Eugenia, et al.
Publicado: (2018)

Botanical features of the Algerian Sahara /
por: Cannon, William Austin 1870-
Publicado: (1913)

Africa south of the Sahara, 1995
Publicado: (1994)

The atmospheric electrical index for ENSO modoki: Is ENSO modoki one of the factors responsible for the warming trend slowdown?
por: Kulkarni, Madhuri N., et al.
Publicado: (2016)

Remains of Leatherback turtles, Dermochelys coriacea, at Mid-Late Holocene archaeological sites in coastal Oman: clues of past worlds
por: Frazier, John G., et al.
Publicado: (2018)

A Modal Rendition of ENSO Diversity
por: Chattopadhyay, Rajib, et al.
Publicado: (2019)

Phenological Responses to ENSO in the Global Oceans
por: Racault, M.-F., et al.
Publicado: (2016)

Cannot write session to /tmp/vufind_sessions/sess_vpgbpas24umh5fpjmg6in2tm7g