M o u n t a i n

We a t h e r

a n d

S n o w p a c k

ACKNOWLEDGMENTS^{Fukuzawa, T. and E. Akitaya. 1993. Depth- hoar crystal growth}
The authorswouldlike toexpress ourthankstoDr.K.^{in the surface layer under high temperature gradient.Annals of}
NishimuraofInstituteofLowTemperatureScience,^{Glaciology ,18 , 39- 45.}
HokkaidoUniversity,forhelpfulsuggestions.We are^{Lang, R. M., B. R. Leo, and R. L. Brown. 1984. Observations on}
gratefultothe staff of the TeshioExperimentalForests^{the growth process and strength characteristics of surface hoar.}
of Hokkaido University fortheirlogistic support.This^{ProceedingsInternationalSnowScienceWorkshop ,Aspen,}
researchwassupportedbythefundforavalanchere-^{Colorado, 188- 195.}
searchoftheMinistryofEducation,Science,CultureOzeki, T. and E. Akitaya. 1996. Field observations of sun crust
and Sports,Japan.formation in Hokkaido, Japan.Arctic and Alpine Research ,28
(2), 244- 248.

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Hachikubo, A. and E. Akitaya. 1997. The effect of wind on sur-^{Agric.Handb.489,USDAForestService,FortCollins,Colo-}
face hoar growth on snow.J. Geophys. Res. , submitted.^{rado, 254 pp.}
Hachikubo, A., T.Fukuzawa and E.Akitaya. 1995. Formation^{Takeuchi, K., and J. Kondo. 1981.Atmosphere near the Ground}
rate of surface hoar crystals under various wind velocities.Pro-^{Surface.Tokyo University Press, Tokyo, 226 pp. [In Japanese]}
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Utah, 132- 137.

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