TY - JOUR
T1 - Ocean-atmosphere dynamics linked to 800–1050 CE drying in mesoamerica
AU - Bhattacharya, Tripti
AU - Chiang, John C.H.
AU - Cheng, Wei
N1 - Funding Information:
This material is based upon work supported by the National Science Foundation Graduate Research Fellowship under Grant No. DGE 1106400. Additional funding comes from NSF DDRIG No. BCS-13333370, and a U.C. Museum of Paleontology Graduate Research Award (2013–2014, 2014–2015) and NOAA grants NA16OAR4310171 to J.C.H. Chiang and NA16OAR4310169 to W. Cheng. We thank Jeff Knight for help with HadCM3 output. We thank current and past members of the U.C. Berkeley Climate ‘Supergroup,’ David Wahl, Roger Byrne, Ben Cook, and others for helpful suggestions and discussions.
Publisher Copyright:
© 2017 Elsevier Ltd
PY - 2017/8/1
Y1 - 2017/8/1
N2 - Proxy records from the last millennium in Mesoamerica suggest a widespread interval of drought at some point between the 7th and 13th centuries CE. In some records, this time period represents the driest proxy values in the last few millennia. There is currently no clear dynamical explanation for these droughts, nor consensus as to whether they were spatiotemporally coherent over the region. We perform several analyses to develop a novel hypothesis to explain these droughts that is consistent with our knowledge of the dynamics of the climate system. We use Bayesian age modeling techniques and a synthesis of regional proxy records to suggest that there is robust evidence of drying between 800 and 1050 CE, with the sites showing dry conditions clustered in southern central America. By studying control simulations of two general circulation models (GCMs), we suggest that this pattern may be diagnostic of hydroclimate changes associated with multidecadal variability in the Atlantic Basin. Models and instrumental data suggest that cooling of tropical Atlantic SSTs and strengthening of the North Atlantic Subtropical High drives a pattern of multidecadal drought with negative rainfall anomalies in southern central America and positive anomalies in northern Mexico. This process could have resulted in the droughts observed in the proxy record. Our work offers a novel hypothesis about the dynamics of multidecadal drought in Mesoamerica, and builds on previous efforts to synthesize proxy records from the region.
AB - Proxy records from the last millennium in Mesoamerica suggest a widespread interval of drought at some point between the 7th and 13th centuries CE. In some records, this time period represents the driest proxy values in the last few millennia. There is currently no clear dynamical explanation for these droughts, nor consensus as to whether they were spatiotemporally coherent over the region. We perform several analyses to develop a novel hypothesis to explain these droughts that is consistent with our knowledge of the dynamics of the climate system. We use Bayesian age modeling techniques and a synthesis of regional proxy records to suggest that there is robust evidence of drying between 800 and 1050 CE, with the sites showing dry conditions clustered in southern central America. By studying control simulations of two general circulation models (GCMs), we suggest that this pattern may be diagnostic of hydroclimate changes associated with multidecadal variability in the Atlantic Basin. Models and instrumental data suggest that cooling of tropical Atlantic SSTs and strengthening of the North Atlantic Subtropical High drives a pattern of multidecadal drought with negative rainfall anomalies in southern central America and positive anomalies in northern Mexico. This process could have resulted in the droughts observed in the proxy record. Our work offers a novel hypothesis about the dynamics of multidecadal drought in Mesoamerica, and builds on previous efforts to synthesize proxy records from the region.
KW - Central America
KW - Climate dynamics
KW - Drought
KW - Holocene
KW - Paleoclimatology
KW - Proxy-model synthesis
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U2 - 10.1016/j.quascirev.2017.06.005
DO - 10.1016/j.quascirev.2017.06.005
M3 - Article
AN - SCOPUS:85020841481
SN - 0277-3791
VL - 169
SP - 263
EP - 277
JO - Quaternary Science Reviews
JF - Quaternary Science Reviews
ER -