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Teleconnected ocean forcing of Western North American droughts and pluvials during the last millennium ArchiMer
Routson, Cody C.; Woodhouse, Connie A.; Overpeck, Jonathan T.; Betancourt, Julio L.; Mckay, Nicholas P..
Western North America (WNA) is rich in hydroclimate reconstructions, yet questions remain about the causes of decadal-to-multidecadal hydroclimate variability. Teleconnection patterns preserved in annually-resolved tree-ring reconstructed drought maps, and anomalies in a global network of proxy sea surface temperature (SST) reconstructions, were used to reassess the evidence linking ocean forcing to WNA hydroclimate variability over the past millennium. Potential forcing mechanisms of the Medieval Climate Anomaly (MCA) and individual drought and pluvial events including two multidecadal-length MCA pluvials were evaluated. We show strong teleconnection patterns occurred during the driest (wettest) years within persistent droughts (pluvials), implicating...
Tipo: Text Palavras-chave: Western North America; Drought; Pluvial; Synthesis; Climate change; Multi-proxy.
Ano: 2016 URL: https://archimer.ifremer.fr/doc/00496/60719/65283.pdf
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A global mean sea surface temperature dataset for the Last Interglacial (129–116 ka) and contribution of thermal expansion to sea level change ArchiMer
Turney, Chris S. M.; Jones, Richard T.; Mckay, Nicholas P.; Van Sebille, Erik; Thomas, Zoë A.; Hillenbrand, Claus-dieter; Fogwill, Christopher J..
A valuable analogue for assessing Earth's sensitivity to warming is the Last Interglacial (LIG; 129–116 ka), when global temperatures (0 to +2 ∘C) and mean sea level (+6 to 11 m) were higher than today. The direct contribution of warmer conditions to global sea level (thermosteric) is uncertain. We report here a global network of LIG sea surface temperatures (SST) obtained from various published temperature proxies (e.g. faunal and floral plankton assemblages, Mg ∕ Ca ratios of calcareous organisms, and alkenone UK′37). We summarize the current limitations of SST reconstructions for the LIG and the spatial temperature features of a naturally warmer world. Because of local δ18O seawater changes, uncertainty in the age models of marine cores, and differences...
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Ano: 2020 URL: https://archimer.ifremer.fr/doc/00663/77549/79436.pdf
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