Articles | Volume 12, issue 4
https://doi.org/10.5194/cp-12-961-2016
© 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-12-961-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
The influence of volcanic eruptions on the climate of tropical South America during the last millennium in an isotope-enabled general circulation model
Christopher M. Colose
CORRESPONDING AUTHOR
Dept. of Atmospheric & Environmental Sciences, University at Albany,
SUNY, Albany, NY 12222, USA
Allegra N. LeGrande
NASA Goddard Institute for Space Studies, New York, NY 10025, USA
Mathias Vuille
Dept. of Atmospheric & Environmental Sciences, University at Albany,
SUNY, Albany, NY 12222, USA
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Cited
32 citations as recorded by crossref.
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- Southern African temperature responses to major volcanic eruptions since 1883: Simulated by CMIP5 models P. Harvey & S. Grab 10.1002/joc.7135
27 citations as recorded by crossref.
- Recent advances and future avenues in examining the impacts of volcanic aerosols on climate T. Zhou et al. 10.1360/TB-2023-0140
- Tropical Atlantic Response to Last Millennium Volcanic Forcing L. Figueiredo Prado et al. 10.3390/atmos9110421
- 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
- Paleoclimatic investigations using isotopic signatures of the Late Pleistocene-Holocene groundwater of the stratified aquifers in Kuwait C. Sabarathinam et al. 10.1016/j.jhydrol.2020.125111
- Hemispherically asymmetric volcanic forcing of tropical hydroclimate during the last millennium C. Colose et al. 10.5194/esd-7-681-2016
- Current state and future challenges in stable isotope applications of the tropical hydrologic cycle (Invited Commentary) M. Vuille 10.1002/hyp.11490
- Energetic constraints on the time-dependent response of the ITCZ to volcanic eruptions M. Erez & O. Adam 10.1175/JCLI-D-21-0146.1
- Comparison of the oxygen isotope signatures in speleothem records and iHadCM3 model simulations for the last millennium J. Bühler et al. 10.5194/cp-17-985-2021
- Forward modeling of δ18O in Andean ice cores J. Hurley et al. 10.1002/2016GL070150
- The amplifying influence of increased ocean stratification on a future year without a summer J. Fasullo et al. 10.1038/s41467-017-01302-z
- Disproportionately strong climate forcing from extratropical explosive volcanic eruptions M. Toohey et al. 10.1038/s41561-018-0286-2
- The South American monsoon variability over the last millennium in climate models M. Rojas et al. 10.5194/cp-12-1681-2016
- Hydroclimate Responses over Global Monsoon Regions Following Volcanic Eruptions at Different Latitudes M. Zuo et al. 10.1175/JCLI-D-18-0707.1
- Southern African temperature responses to major volcanic eruptions since 1883: Simulated by CMIP5 models P. Harvey & S. Grab 10.1002/joc.7135
- Investigating stable oxygen and carbon isotopic variability in speleothem records over the last millennium using multiple isotope-enabled climate models J. Bühler et al. 10.5194/cp-18-1625-2022
- Towards learned emulation of interannual water isotopologue variations in General Circulation Models J. Wider et al. 10.1017/eds.2023.29
- Ecosystem modeling using artificial neural networks: An archaeological tool L. Burry et al. 10.1016/j.jasrep.2017.07.013
- Southern Hemisphere continental temperature responses to major volcanic eruptions since 1883 in CMIP5 models P. Harvey & S. Grab 10.1007/s00704-021-03810-x
- Wetter Global Arid Regions Driven by Volcanic Eruptions M. Zuo et al. 10.1029/2019JD031171
- Ecosystems dynamics and environmental management: An NDVI reconstruction model for El Alto-Ancasti mountain range (Catamarca, Argentina) from 442 AD through 1980 AD A. Meléndez et al. 10.1016/j.quascirev.2023.108450
- The 852/3 CE Mount Churchill eruption: examining the potential climatic and societal impacts and the timing of the Medieval Climate Anomaly in the North Atlantic region H. Mackay et al. 10.5194/cp-18-1475-2022
- Evaluating uncertainty in aerosol forcing of tropical precipitation shifts A. Peace et al. 10.5194/esd-13-1215-2022
- Variation of centennial precipitation patterns in Kuwait and their relation to climate change S. Radha et al. 10.1007/s10661-022-10587-7
- Comparing proxy and model estimates of hydroclimate variability and change over the Common Era 10.5194/cp-13-1851-2017
- 2,100 years of human adaptation to climate change in the High Andes C. Åkesson et al. 10.1038/s41559-019-1056-2
- A continental reconstruction of hydroclimatic variability in South America during the past 2000 years M. Choblet et al. 10.5194/cp-20-2117-2024
- Dependence of global monsoon response to volcanic eruptions on the background oceanic states M. Zuo et al. 10.1175/JCLI-D-20-0891.1
5 citations as recorded by crossref.
- Reconstructing Earth's surface temperature over the past 2000 years: the science behind the headlines J. Smerdon & H. Pollack 10.1002/wcc.418
- Major Volcanic Eruptions and Their Impacts on Southern Hemisphere Temperatures During the Late 19th and 20th Centuries, as Simulated by CMIP5 Models P. Harvey et al. 10.1029/2020GL087792
- Southern Hemisphere continental temperature responses to major volcanic eruptions since 1883 in CMIP5 models P. Harvey & S. Grab 10.1007/s00704-021-03810-x
- Potential impacts of major nineteenth century volcanic eruptions on temperature over Cape Town, South Africa: 1834–1899 J. Picas & S. Grab 10.1007/s10584-020-02678-6
- Southern African temperature responses to major volcanic eruptions since 1883: Simulated by CMIP5 models P. Harvey & S. Grab 10.1002/joc.7135
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Discussed (final revised paper)
Latest update: 21 Nov 2024
Short summary
Volcanic forcing is the most important source of forced variability during the preindustrial component of the last millennium (~ 850-1850 CE) and is important during the last century.
Here, we focus on the climate impact over South America in a model-based study. Emphasis is given to temperature, precipitation, and oxygen isotope variability (allowing for potential contact made with paleoclimate-based observations)
Here, we focus on the climate impact over South America in a model-based study. Emphasis is given to temperature, precipitation, and oxygen isotope variability (allowing for potential contact made with paleoclimate-based observations)
Volcanic forcing is the most important source of forced variability during the preindustrial...