@article{oai:kitami-it.repo.nii.ac.jp:00007575,
 author = {Hachikubo, Akihiro and Akitaya, Eizi},
 issue = {D4},
 journal = {JOURNAL OF GEOPHYSICAL RESEARCH},
 month = {2016-11-22},
 note = {Field observations of surface hoax formation were carried out with
the measurementso f water vapor condensationr ate, snows urfacet emperature, air
temperature, humidity, wind speed, and net radiation. Large surface hoar crystals
wereo bservetdo formu ndert he breezyw ind,I to 2 m s- i, at 0.1m high. The
condensationra te increasedli nearly with the producto f the vapor pressureg radient
and the wind speed. The bulk transferc oefficienot f water vapor Ce was roughly
constant when the surface hoar crystals were small, whereas it showed some increase
as the hoarc rystalsg rewt o severaml illimeterisn height.A possiblcea useo f this
increase in Ce is that the developed surface hoar crystals modify the aerodynamic
roughnessa nd consequentliyn creaseth e turbulentt ransfero f water vapor.},
 pages = {4367--4373},
 title = {Effect of wind on surface hoar growth on snow},
 volume = {102},
 year = {}
}