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10.1038/srep32984 http://scihub22266oqcxt.onion/10.1038/srep32984 C5016737!5016737!27609585     free     free     free Deprecated: Implicit conversion from float 233.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 233.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 233.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 233.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 233.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 233.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534       Sci+Rep 2016 ; 6 (ä): ä Nephropedia Template TP {{tp|p=27609585|t=2016. Paradoxical cold conditions during the medieval climate anomaly in the Western Arctic |pdf=|usr=}}{{27609585}} gab.com Text Paradoxical cold conditions during the medieval climate anomaly in the Western Arctic JO: Sci Rep http://www.kidney.de/pget.php?&tw=1&pmid=27609585 #FOAvip In the Northern Hemisphere, most mountain glaciers experienced their largest extent in the last millennium during the Little Ice Age (1450 to 1850 CE, LIA), a period marked by colder hemispheric temperatures than the Medieval Climate Anomaly (950 to 1250 CE, MCA), a period which coincided with glacier retreat. Here, we present a new moraine chronology based on 36Cl surface exposure dating from Lyngmarksbrĉen glacier, West Greenland. Consistent with other glaciers in the western Arctic, Lyngmarksbrĉen glacier experienced several advances during the last millennium, the first one at the end of the MCA, in ~1200 CE, was of similar amplitude to two other advances during the LIA. In the absence of any significant changes in accumulation records from South Greenland ice cores, we attribute this expansion to multi-decadal summer cooling likely driven by volcanic and/or solar forcing, and associated regional sea-ice feedbacks. Such regional multi-decadal cold conditions at the end of the MCA are neither resolved in temperature reconstructions from other parts of the Northern Hemisphere, nor captured in last millennium climate simulations. Twit Text FOAVip Paradoxical cold conditions during the medieval climate anomaly in the Western Arctic ????Sci Rep http://www.kidney.de/pget.php?&tw=1&pmid=27609585 #FOAvip Twit Text # Free Paper on # # # # # LINK http://www.kidney.de/pget.php?&tw=1&pmid=27609585 #FOAvip English Wikipedia <ref>{{Cite pmid|27609585}}</ref> Paradoxical cold conditions during the medieval climate anomaly in the Western Arctic #MMPMID27609585 Jomelli V; Lane T; Favier V; Masson-Delmotte V; Swingedouw D; Rinterknecht V; Schimmelpfennig I; Brunstein D; Verfaillie D; Adamson K; Leanni L; Mokadem F Sci Rep 2016[]; 6 (ä): ä PMID27609585show ga In the Northern Hemisphere, most mountain glaciers experienced their largest extent in the last millennium during the Little Ice Age (1450 to 1850 CE, LIA), a period marked by colder hemispheric temperatures than the Medieval Climate Anomaly (950 to 1250 CE, MCA), a period which coincided with glacier retreat. Here, we present a new moraine chronology based on 36Cl surface exposure dating from Lyngmarksbrĉen glacier, West Greenland. Consistent with other glaciers in the western Arctic, Lyngmarksbrĉen glacier experienced several advances during the last millennium, the first one at the end of the MCA, in ~1200 CE, was of similar amplitude to two other advances during the LIA. In the absence of any significant changes in accumulation records from South Greenland ice cores, we attribute this expansion to multi-decadal summer cooling likely driven by volcanic and/or solar forcing, and associated regional sea-ice feedbacks. Such regional multi-decadal cold conditions at the end of the MCA are neither resolved in temperature reconstructions from other parts of the Northern Hemisphere, nor captured in last millennium climate simulations. äParadoxical cold conditions during the medieval climate anomaly in the(epmc).pdf DeepDyve Pubget Overpricing