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10.1038/srep12243 http://scihub22266oqcxt.onion/10.1038/srep12243 C4513290!4513290!26206616     free     free     free Deprecated: Implicit conversion from float 211.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 211.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 211.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 211.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 211.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534       Sci+Rep 2015 ; 5 (ä): ä Nephropedia Template TP {{tp|p=26206616|t=2015. Stratospheric Ozone destruction by the Bronze-Age Minoan eruption (Santorini Volcano, Greece) |pdf=|usr=}}{{26206616}} gab.com Text Stratospheric Ozone destruction by the Bronze-Age Minoan eruption (Santorini Volcano, Greece) JO: Sci Rep http://www.kidney.de/pget.php?&tw=1&pmid=26206616 #FOAvip The role of volcanogenic halogen-bearing (i.e. chlorine and bromine) compounds in stratospheric ozone chemistry and climate forcing is poorly constrained. While the 1991 eruption of Pinatubo resulted in stratospheric ozone loss, it was due to heterogeneous chemistry on volcanic sulfate aerosols involving chlorine of anthropogenic rather than volcanogenic origin, since co-erupted chlorine was scavenged within the plume. Therefore, it is not known what effect volcanism had on ozone in pre-industrial times, nor what will be its role on future atmospheres with reduced anthropogenic halogens present. By combining petrologic constraints on eruption volatile yields with a global atmospheric chemistry-transport model, we show here that the Bronze-Age ?Minoan? eruption of Santorini Volcano released far more halogens than sulfur and that, even if only 2% of these halogens reached the stratosphere, it would have resulted in strong global ozone depletion. The model predicts reductions in ozone columns of 20 to >90% at Northern high latitudes and an ozone recovery taking up to a decade. Our findings emphasise the significance of volcanic halogens for stratosphere chemistry and suggest that modelling of past and future volcanic impacts on Earth?s ozone, climate and ecosystems should systematically consider volcanic halogen emissions in addition to sulfur emissions. Twit Text FOAVip Stratospheric Ozone destruction by the Bronze-Age Minoan eruption (Santorini Volcano, Greece) ????Sci Rep http://www.kidney.de/pget.php?&tw=1&pmid=26206616 #FOAvip Twit Text # Free Paper on # # # # # LINK http://www.kidney.de/pget.php?&tw=1&pmid=26206616 #FOAvip English Wikipedia <ref>{{Cite pmid|26206616}}</ref> Stratospheric Ozone destruction by the Bronze-Age Minoan eruption (Santorini Volcano, Greece) #MMPMID26206616 Cadoux A; Scaillet B; Bekki S; Oppenheimer C; Druitt TH Sci Rep 2015[]; 5 (ä): ä PMID26206616show ga The role of volcanogenic halogen-bearing (i.e. chlorine and bromine) compounds in stratospheric ozone chemistry and climate forcing is poorly constrained. While the 1991 eruption of Pinatubo resulted in stratospheric ozone loss, it was due to heterogeneous chemistry on volcanic sulfate aerosols involving chlorine of anthropogenic rather than volcanogenic origin, since co-erupted chlorine was scavenged within the plume. Therefore, it is not known what effect volcanism had on ozone in pre-industrial times, nor what will be its role on future atmospheres with reduced anthropogenic halogens present. By combining petrologic constraints on eruption volatile yields with a global atmospheric chemistry-transport model, we show here that the Bronze-Age ?Minoan? eruption of Santorini Volcano released far more halogens than sulfur and that, even if only 2% of these halogens reached the stratosphere, it would have resulted in strong global ozone depletion. The model predicts reductions in ozone columns of 20 to >90% at Northern high latitudes and an ozone recovery taking up to a decade. Our findings emphasise the significance of volcanic halogens for stratosphere chemistry and suggest that modelling of past and future volcanic impacts on Earth?s ozone, climate and ecosystems should systematically consider volcanic halogen emissions in addition to sulfur emissions. äStratospheric Ozone destruction by the Bronze-Age Minoan eruption (San(epmc).pdf DeepDyve Pubget Overpricing