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10.1098/rsta.2015.0224 http://scihub22266oqcxt.onion/10.1098/rsta.2015.0224 C5004054!5004054!27550759     free     free     free Deprecated: Implicit conversion from float 209.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 209.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 209.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 209.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534       Philos+Trans+A+Math+Phys+Eng+Sci 2016 ; 374 (2077): ä Nephropedia Template TP {{tp|p=27550759|t=2016. Eclipse-induced wind changes over the British Isles on the 20 March 2015 |pdf=|usr=}}{{27550759}} gab.com Text Eclipse-induced wind changes over the British Isles on the 20 March 2015 JO: Philos Trans A Math Phys Eng Sci http://www.kidney.de/pget.php?&tw=1&pmid=27550759 #FOAvip The British Isles benefits from dense meteorological observation networks, enabling insights into the still-unresolved effects of solar eclipse events on the near-surface wind field. The near-surface effects of the solar eclipse of 20 March 2015 are derived through comparison of output from the Met Office?s operational weather forecast model (which is ignorant of the eclipse) with data from two meteorological networks: the Met Office?s land surface station (MIDAS) network and a roadside measurement network operated by Vaisala. Synoptic-evolution relative calculations reveal the cooling and increase in relative humidity almost universally attributed to eclipse events. In addition, a slackening of wind speeds by up to about 2?knots in already weak winds and backing in wind direction of about 20° under clear skies across middle England are attributed to the eclipse event. The slackening of wind speed is consistent with the previously reported boundary layer stabilization during eclipse events. Wind direction changes have previously been attributed to a large-scale ?eclipse-induced cold-cored cyclone?, mountain slope flows, and changes in the strength of sea breezes. A new explanation is proposed here by analogy with nocturnal wind changes at sunset and shown to predict direction changes consistent with those observed.This article is part of the themed issue ?Atmospheric effects of solar eclipses stimulated by the 2015 UK eclipse?. Twit Text FOAVip Eclipse-induced wind changes over the British Isles on the 20 March 2015 ????Philos Trans A Math Phys Eng Sci http://www.kidney.de/pget.php?&tw=1&pmid=27550759 #FOAvip Twit Text # Free Paper on # # # # # LINK http://www.kidney.de/pget.php?&tw=1&pmid=27550759 #FOAvip English Wikipedia <ref>{{Cite pmid|27550759}}</ref> Eclipse-induced wind changes over the British Isles on the 20 March 2015 #MMPMID27550759 Gray SL; Harrison RG Philos Trans A Math Phys Eng Sci 2016[Sep]; 374 (2077): ä PMID27550759show ga The British Isles benefits from dense meteorological observation networks, enabling insights into the still-unresolved effects of solar eclipse events on the near-surface wind field. The near-surface effects of the solar eclipse of 20 March 2015 are derived through comparison of output from the Met Office?s operational weather forecast model (which is ignorant of the eclipse) with data from two meteorological networks: the Met Office?s land surface station (MIDAS) network and a roadside measurement network operated by Vaisala. Synoptic-evolution relative calculations reveal the cooling and increase in relative humidity almost universally attributed to eclipse events. In addition, a slackening of wind speeds by up to about 2?knots in already weak winds and backing in wind direction of about 20° under clear skies across middle England are attributed to the eclipse event. The slackening of wind speed is consistent with the previously reported boundary layer stabilization during eclipse events. Wind direction changes have previously been attributed to a large-scale ?eclipse-induced cold-cored cyclone?, mountain slope flows, and changes in the strength of sea breezes. A new explanation is proposed here by analogy with nocturnal wind changes at sunset and shown to predict direction changes consistent with those observed.This article is part of the themed issue ?Atmospheric effects of solar eclipses stimulated by the 2015 UK eclipse?. äEclipse-induced wind changes over the British Isles on the 20 March 20(epmc).pdf DeepDyve Pubget Overpricing