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Extra resources for Attic Black-Figure Funerary Plaques
Many early systems operated at 3 cm wavelengths, ideal for detecting snow and wet clouds, but suffering from attenuation during heavier rain events. S. east coast in the mid-1950s lead to the development of the WSR-57 radar, a minimal attenuation 10 cm radar ideal for probing thunderstorms. Similar systems became commonplace worldwide. Conventional radar returns were described in terms of decibels of reﬂectivity (dBZ), which are related to precipitation rate. Several hundred Z/R (reﬂectivity/rainfall) rate algorithms have emerged over the years, so one to one correlations between precipitation rates and reﬂectivity remain elusive.
Geophys. Res. , 27:3829–3832. , and Fukunishi, H. (2003). Activities of sprites and elves in the winter season, Japan. J. Atmos. -Terr. , 65:551–560. Wescott, E. , Stenbaek-Nielsen, H. , Sentman, D. , Heavner, M. , and Sao Sabbas, F. T. (2001). Triangulation of sprites, associated halos and their possible relation to causative lightning and micro-meteors. J. Geophys. , 106(A6):10467–10477. Williams, E. R. (2002). Global electric circuit. In Encyclopedia of Atmospheric Science. Academic Press. Williams, E.
Stenbaek-Nielsen, H. , Sentman, D. , Heavner, M. , and Sao Sabbas, F. T. (2001). Triangulation of sprites, associated halos and their possible relation to causative lightning and micro-meteors. J. Geophys. , 106(A6):10467–10477. Williams, E. R. (2002). Global electric circuit. In Encyclopedia of Atmospheric Science. Academic Press. Williams, E. R. and Heckman, S. J. (1993). The local diurnal variation of cloud electriﬁcation and the global diurnal variation of negative on the Earth. J. Geophys.