“…Under stable conditions, the vertical structure of the atmosphere is characterized by thin, strongly stable non-turbulent "sheets" separated by thicker, less stable, and often weakly turbulent "layers" (Woods, 1969(Woods, , 1968Gage and Green, 1978;Röttger and Liu, 1978). These sheet and layer (S&L) structures are often observed in temperature, humidity, and horizontal winds within the lower troposphere (Balsley et al, , 2006Chimonas, 1999;Mahrt, 1999;Xing-Sheng et al, 1983;Kantha et al, 2019) and into the edge of the stratosphere (Barat, 1982;Fairall et al, 1991;Gage and Balsley, 1980;Röttger, 1980;Woodman and Guillen, 1974). The S&L structures are known to play an important role in the transport and mixing of heat, momentum, and constituents (Barat, 1982;Chimonas, 1999;Dalaudier et al, 1994;Hunt et al, 1985), as well as important roles in optical (Coulman et Published by Copernicus Publications on behalf of the European Geosciences Union.…”