Articles | Volume 12, issue 8
https://doi.org/10.5194/cp-12-1681-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-12-1681-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
The South American monsoon variability over the last millennium in climate models
Maisa Rojas
CORRESPONDING AUTHOR
Department of Geophysics, University of Chile, Santiago, Chile
Millennium Nucleus PaleoClimate, Santiago, Chile
Paola A. Arias
Department of Geophysics, University of Chile, Santiago, Chile
Grupo de Ingeniería Gestión Ambiental (GIGA), Escuela Ambiental, Facultad de
Ingeniería, Universidad de Antioquia, Medellín, Colombia
Valentina Flores-Aqueveque
Millennium Nucleus PaleoClimate, Santiago, Chile
Anji Seth
Department of Geography, University of Connecticut, Storrs, CT, USA
Mathias Vuille
Department of Atmospheric and Environmental Sciences, University at Albany,
State University of New York, Albany, NY, USA
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25 citations as recorded by crossref.
- Amazon rainforest modulation of water security in the Pantanal wetland I. Bergier et al. 10.1016/j.scitotenv.2017.11.163
- South American precipitation changes simulated by PMIP3/CMIP5 models during the Little Ice Age and the recent global warming period L. Díaz & C. Vera 10.1002/joc.5449
- The joint impacts of Atlantic and Pacific multidecadal variability on South American precipitation and temperature Z. He et al. 10.1175/JCLI-D-21-0081.1
- South American Summer Monsoon variability over the last millennium in paleoclimate records and isotope-enabled climate models R. Orrison et al. 10.5194/cp-18-2045-2022
- The Role of Internal Variability in ITCZ Changes Over the Last Millennium P. Roldán‐Gómez et al. 10.1029/2021GL096487
- Holocene stratigraphic evolution of saline lakes in Nhecolândia, southern Pantanal wetlands (Brazil) M. McGlue et al. 10.1017/qua.2017.57
- Two Millennia of South Atlantic Convergence Zone Variability Reconstructed From Isotopic Proxies V. Novello et al. 10.1029/2017GL076838
- On the Interpretation of the ENSO Signal Embedded in the Stable Isotopic Composition of Quelccaya Ice Cap, Peru J. Hurley et al. 10.1029/2018JD029064
- Central Andean (28–34°S) flood record 0–25 ka from Salinas del Bebedero, Argentina J. Quade et al. 10.1017/qua.2022.1
- Seasonal modulation of the Asian summer monsoon between the Medieval Warm Period and Little Ice Age: a multi model study Y. Kamae et al. 10.1186/s40645-017-0136-7
- The Threat of Multi‐Year Drought in Western Amazonia L. Parsons et al. 10.1029/2017WR021788
- Disentangling the Medieval Climatic Anomaly in Patagonia and its impact on human societies I. Ozán et al. 10.1177/09596836221095993
- High- and low-latitude forcings drive Atacama Desert rainfall variations over the past 16,000 years F. González-Pinilla et al. 10.1126/sciadv.abg1333
- A continental reconstruction of hydroclimatic variability in South America during the past 2000 years M. Choblet et al. 10.5194/cp-20-2117-2024
- Lake Tauca highstand (Heinrich Stadial 1a) driven by a southward shift of the Bolivian High L. Martin et al. 10.1126/sciadv.aar2514
- Late Quaternary environmental dynamics in the Atacama Desert reconstructed from rodent midden pollen records M. de Porras et al. 10.1002/jqs.2980
- Stable Oxygen Isotope Records (δ18O) of a High-Andean Cushion Peatland in NW Argentina (24° S) Imply South American Summer Monsoon Related Moisture Changes During the Late Holocene S. Kock et al. 10.3389/feart.2019.00045
- Late Holocene Precipitation Fluctuations in South America Triggered by Variability of the North Atlantic Overturning Circulation A. Bahr et al. 10.1029/2021PA004223
- Origin and variability of oxygen and hydrogen isotopic composition of precipitation in the Central Andes: A review S. Valdivielso et al. 10.1016/j.jhydrol.2020.124899
- The Choco low‐level jet: past, present and future J. Sierra et al. 10.1007/s00382-020-05611-w
- The Late Intermediate Period in the south-central Andes (AD 1000–1450): Key problems in chronology E. Arkush et al. 10.1016/j.quaint.2023.10.002
- Assessing the hydroclimate changes in Western Himalayas during the Little Ice Age A. Singh et al. 10.1177/09596836231225727
- South Pacific Subtropical High from the late Holocene to the end of the 21st century: insights from climate proxies and general circulation models V. Flores-Aqueveque et al. 10.5194/cp-16-79-2020
- South American monsoon intensification during the last millennium driven by joint Pacific and Atlantic forcing Z. Lyu et al. 10.1126/sciadv.ado9543
- Vegetation and fire variability in the central Cerrados (Brazil) during the Pleistocene-Holocene transition was influenced by oscillations in the SASM boundary belt R. Cassino et al. 10.1016/j.quascirev.2020.106209
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Latest update: 21 Nov 2024
Short summary
Recent work shows that during the most prominent climate anomalies during the last millennium, the Medieval Climate Anomaly (ca. 950–1250) and the Little Ice Age (ca. 1450–1850), the South American monsoon system (SAMS) was drier and wetter, respectively. We investigate if this variability in the SAMS is reproduced in the latest set of climate simulations that cover these periods. Despite weak forcing, through analysis of the large-scale circulation we find this signal in the models.
Recent work shows that during the most prominent climate anomalies during the last millennium,...