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CONCLUSIONS<br />
The record snowfall in February <strong>an</strong>d March 1960 across <strong>the</strong> Sou<strong>the</strong>rn Appalachi<strong>an</strong>s occurred in<br />
<strong>as</strong>sociation with highly <strong>an</strong>omalous 500 hPa circulation <strong>an</strong>d 850 hPa temperatures. The persistence<br />
of a 500 hPa trough over <strong>the</strong> e<strong>as</strong>tern U.S. w<strong>as</strong> <strong>as</strong>sociated with a sou<strong>the</strong><strong>as</strong>terly displaced storm<br />
track that kept temperatures well below normal. As a result, <strong>the</strong> 1959–60 snow se<strong>as</strong>on still holds<br />
<strong>the</strong> <strong>an</strong>nual snowfall record (265 cm) <strong>an</strong>d maximum snow depth record (112 cm) for Boone, NC,<br />
<strong>an</strong>d countless o<strong>the</strong>r locations across <strong>the</strong> region. Miller Type A cyclones, Miller Type B cyclones,<br />
<strong>an</strong>d NWFS events were responsible for nearly all of <strong>the</strong> total snowfall across <strong>the</strong> region. However,<br />
NWFS made <strong>the</strong> greatest contribution to snowfall totals across <strong>the</strong> higher elevations <strong>an</strong>d along<br />
northwestern slopes, where snow fell on average every o<strong>the</strong>r day during <strong>the</strong> period. A small<br />
number of exceptionally heavy events produced <strong>the</strong> record snowfall in <strong>the</strong> Georgia <strong>an</strong>d Carolina<br />
foothills in contr<strong>as</strong>t with <strong>the</strong> elevated are<strong>as</strong> to <strong>the</strong> north <strong>an</strong>d west where numerous, relatively light<br />
NWFS events contributed subst<strong>an</strong>tially to <strong>the</strong> total snowfall. Un<strong>an</strong>swered questions include <strong>the</strong><br />
causes of <strong>the</strong> <strong>an</strong>omalous <strong>an</strong>d persistent 500 hPa circulation pattern. In particular, <strong>the</strong> role of<br />
hemispheric teleconnections versus persistent snow cover across <strong>the</strong> region in forcing this pattern<br />
needs to be explored. The influence of favorable air trajectories extending downwind from <strong>the</strong><br />
Great Lakes in periods of NWFS also deserves fur<strong>the</strong>r scrutiny, particularly since <strong>the</strong>se have been<br />
tied to enh<strong>an</strong>ced snowfall in <strong>the</strong> Sou<strong>the</strong>rn Appalachi<strong>an</strong>s (Perry <strong>an</strong>d Konrad 2005). L<strong>as</strong>tly, given<br />
<strong>the</strong> deep snowpack <strong>an</strong>d reports of flooding during rapid melting at <strong>the</strong> end of March (Ludlum<br />
1960b), <strong>an</strong> investigation of <strong>the</strong> hydrological signific<strong>an</strong>ce (e.g. SWE estimations <strong>an</strong>d flooding<br />
reports) of February <strong>an</strong>d March 1960 is also warr<strong>an</strong>ted.<br />
ACKNOWLEDGMENTS<br />
Peter Robinson, Tom Whitmore, Walt Martin, Tom Schmidlin, Laurence Lee, <strong>an</strong>d Michael<br />
Mayfield provided valuable feedback on <strong>the</strong> design of <strong>the</strong> study. Julie Whichard from <strong>the</strong> North<br />
Carolina Department of Tr<strong>an</strong>sportation kindly provided archived photos. Addie Mae Love, Louiva<br />
Ward, <strong>an</strong>d Howell Cooke shared <strong>the</strong>ir m<strong>an</strong>y memories.<br />
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