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10.1073/pnas.1422270112 http://scihub22266oqcxt.onion/10.1073/pnas.1422270112 C4403187!4403187 !25825740     free     free     free Warning: file_get_contents(https://eutils.ncbi.nlm.nih.gov/entrez/eutils/elink.fcgi?dbfrom=pubmed&id=25825740 &cmd=llinks): Failed to open stream: HTTP request failed! 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Extreme rainfall activity in the Australian tropics reflects changes in the El Niņo/Southern Oscillation over the last two millennia |pdf=|usr=}}{{25825740 }} gab.com Text Extreme rainfall activity in the Australian tropics reflects changes in the El Niņo/Southern Oscillation over the last two millennia JO: Proc Natl Acad Sci U S A http://www.kidney.de/pget.php?&tw=1&pmid=25825740 #FOAvip Assessing temporal variability in extreme rainfall events before the historical era is complicated by the sparsity of long-term "direct" storm proxies. Here we present a 2,200-y-long, accurate, and precisely dated record of cave flooding events from the northwest Australian tropics that we interpret, based on an integrated analysis of meteorological data and sediment layers within stalagmites, as representing a proxy for extreme rainfall events derived primarily from tropical cyclones (TCs) and secondarily from the regional summer monsoon. This time series reveals substantial multicentennial variability in extreme rainfall, with elevated occurrence rates characterizing the twentieth century, 850-1450 CE (Common Era), and 50-400 CE; reduced activity marks 1450-1650 CE and 500-850 CE. These trends are similar to reconstructed numbers of TCs in the North Atlantic and Caribbean basins, and they form temporal and spatial patterns best explained by secular changes in the dominant mode of the El Niņo/Southern Oscillation (ENSO), the primary driver of modern TC variability. We thus attribute long-term shifts in cyclogenesis in both the central Australian and North Atlantic sectors over the past two millennia to entrenched El Niņo or La Niņa states of the tropical Pacific. The influence of ENSO on monsoon precipitation in this region of northwest Australia is muted, but ENSO-driven changes to the monsoon may have complemented changes to TC activity. Twit Text FOAVip Extreme rainfall activity in the Australian tropics reflects changes in the El Niņo/Southern Oscillation over the last two millennia ????Proc Natl Acad Sci U S A http://www.kidney.de/pget.php?&tw=1&pmid=25825740 #FOAvip Twit Text # Free Paper on # # # # # LINK http://www.kidney.de/pget.php?&tw=1&pmid=25825740 #FOAvip English Wikipedia <ref>{{Cite pmid|25825740 }}</ref> Extreme rainfall activity in the Australian tropics reflects changes in the El Niņo/Southern Oscillation over the last two millennia #MMPMID25825740 Denniston RF ; Villarini G ; Gonzales AN ; Wyrwoll KH ; Polyak VJ ; Ummenhofer CC ; Lachniet MS ; Wanamaker AD Jr ; Humphreys WF ; Woods D ; Cugley J Proc Natl Acad Sci U S A 2015[Apr]; 112 (15 ): 4576-81 PMID25825740 show ga Assessing temporal variability in extreme rainfall events before the historical era is complicated by the sparsity of long-term "direct" storm proxies. Here we present a 2,200-y-long, accurate, and precisely dated record of cave flooding events from the northwest Australian tropics that we interpret, based on an integrated analysis of meteorological data and sediment layers within stalagmites, as representing a proxy for extreme rainfall events derived primarily from tropical cyclones (TCs) and secondarily from the regional summer monsoon. This time series reveals substantial multicentennial variability in extreme rainfall, with elevated occurrence rates characterizing the twentieth century, 850-1450 CE (Common Era), and 50-400 CE; reduced activity marks 1450-1650 CE and 500-850 CE. These trends are similar to reconstructed numbers of TCs in the North Atlantic and Caribbean basins, and they form temporal and spatial patterns best explained by secular changes in the dominant mode of the El Niņo/Southern Oscillation (ENSO), the primary driver of modern TC variability. We thus attribute long-term shifts in cyclogenesis in both the central Australian and North Atlantic sectors over the past two millennia to entrenched El Niņo or La Niņa states of the tropical Pacific. The influence of ENSO on monsoon precipitation in this region of northwest Australia is muted, but ENSO-driven changes to the monsoon may have complemented changes to TC activity. äExtreme rainfall activity in the Australian tropics reflects changes i(epmc).pdf DeepDyve Pubget Overpricing