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10.1038/srep37832 http://scihub22266oqcxt.onion/10.1038/srep37832 C5121654!5121654 !27883066     free     free     free Warning: file_get_contents(https://eutils.ncbi.nlm.nih.gov/entrez/eutils/elink.fcgi?dbfrom=pubmed&id=27883066 &cmd=llinks): Failed to open stream: HTTP request failed! HTTP/1.1 429 Too Many Requests in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 215 Warning: imagejpeg(C:\Inetpub\vhosts\kidney.de\httpdocs\phplern\27883066 .jpg): Failed to open stream: No such file or directory in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 117       Sci+Rep 2016 ; 6 (ä): 37832 Nephropedia Template TP {{tp|p=27883066 |t=2016. Meteotsunamis in the Laurentian Great Lakes |pdf=|usr=}}{{27883066 }} gab.com Text Meteotsunamis in the Laurentian Great Lakes JO: Sci Rep http://www.kidney.de/pget.php?&tw=1&pmid=27883066 #FOAvip The generation mechanism of meteotsunamis, which are meteorologically induced water waves with spatial/temporal characteristics and behavior similar to seismic tsunamis, is poorly understood. We quantify meteotsunamis in terms of seasonality, causes, and occurrence frequency through the analysis of long-term water level records in the Laurentian Great Lakes. The majority of the observed meteotsunamis happen from late-spring to mid-summer and are associated primarily with convective storms. Meteotsunami events of potentially dangerous magnitude (height > 0.3?m) occur an average of 106 times per year throughout the region. These results reveal that meteotsunamis are much more frequent than follow from historic anecdotal reports. Future climate scenarios over the United States show a likely increase in the number of days favorable to severe convective storm formation over the Great Lakes, particularly in the spring season. This would suggest that the convectively associated meteotsunamis in these regions may experience an increase in occurrence frequency or a temporal shift in occurrence to earlier in the warm season. To date, meteotsunamis in the area of the Great Lakes have been an overlooked hazard. Twit Text FOAVip Meteotsunamis in the Laurentian Great Lakes ????Sci Rep http://www.kidney.de/pget.php?&tw=1&pmid=27883066 #FOAvip Twit Text # Free Paper on # # # # # LINK http://www.kidney.de/pget.php?&tw=1&pmid=27883066 #FOAvip English Wikipedia <ref>{{Cite pmid|27883066 }}</ref> Meteotsunamis in the Laurentian Great Lakes #MMPMID27883066 Bechle AJ ; Wu CH ; Kristovich DA ; Anderson EJ ; Schwab DJ ; Rabinovich AB Sci Rep 2016[Nov]; 6 (ä): 37832 PMID27883066 show ga The generation mechanism of meteotsunamis, which are meteorologically induced water waves with spatial/temporal characteristics and behavior similar to seismic tsunamis, is poorly understood. We quantify meteotsunamis in terms of seasonality, causes, and occurrence frequency through the analysis of long-term water level records in the Laurentian Great Lakes. The majority of the observed meteotsunamis happen from late-spring to mid-summer and are associated primarily with convective storms. Meteotsunami events of potentially dangerous magnitude (height > 0.3?m) occur an average of 106 times per year throughout the region. These results reveal that meteotsunamis are much more frequent than follow from historic anecdotal reports. Future climate scenarios over the United States show a likely increase in the number of days favorable to severe convective storm formation over the Great Lakes, particularly in the spring season. This would suggest that the convectively associated meteotsunamis in these regions may experience an increase in occurrence frequency or a temporal shift in occurrence to earlier in the warm season. To date, meteotsunamis in the area of the Great Lakes have been an overlooked hazard. äMeteotsunamis in the Laurentian Great Lakes (epmc).pdf DeepDyve Pubget Overpricing