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  1. 学術雑誌掲載済論文
  2. 洋雑誌

Effects of snow physical parameters on spectral albedo and bidirectional reflectance of snow surface

https://kitami-it.repo.nii.ac.jp/records/7576
80d0a41a-dd1b-4eb9-8954-45df696b455d
名前 / ファイル ライセンス アクション
(2000)JGR.pdf (2000)JGR.pdf (3.5 MB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2014-01-18
タイトル
言語 en
タイトル Effects of snow physical parameters on spectral albedo and bidirectional reflectance of snow surface
言語
言語 eng
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ journal article
アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
著者 Aoki, Teruo

× Aoki, Teruo

WEKO 38688

en Aoki, Teruo

Search repository
Aoki, Tadao

× Aoki, Tadao

WEKO 38689

en Aoki, Tadao

Search repository
Fukabori, Masashi

× Fukabori, Masashi

WEKO 38690

en Fukabori, Masashi

Search repository
Hachikubo, Akihiro

× Hachikubo, Akihiro

WEKO 38691

en Hachikubo, Akihiro

Search repository
Tachibana, Yoshihiro

× Tachibana, Yoshihiro

WEKO 38692

en Tachibana, Yoshihiro

Search repository
Nishio, Fumihiko

× Nishio, Fumihiko

WEKO 38693

en Nishio, Fumihiko

Search repository
抄録
内容記述タイプ Abstract
内容記述 Observationso f spectrala lbedo and bidirectionalr eflectancei n the wavelength
region of X = 0.35-2.5 tzm were made together with snow pit work on a flat snowfield in
eastern Hokkaido, Japan. The effects of snow impurities, density, layer structure, and
grain size attained by in situ and laboratorym easurementsw ere taken into accounti n
snow models for which spectral albedos were calculated using a multiple-scattering model
for the atmosphere-snows ystem.C omparisonso f these theoretical albedosw ith measured
ones suggest hat the snowi mpuritiesw ere concentrateda t the snow surfaceb y dry fallout
of atmospheric aerosols. The optically equivalent snow grain size was found to be of the
order of a branch width of dendrites or of a dimension of narrower portion of broken
crystalsT. his sizew as smallert han both the mean grain size and the effectiveg rain size
obtainedf rom micrographsb y image processingT. he observationarl esultsf or the
bidirectionalr eflectiond istributionf unction( BRDF) normalizedb y the radiancea t the
nadir showed that the anisotropic reflection was very significant in the near-infrared
region,e speciallyfo r X > 1.4 tzm,w hile the visiblen ormalizedB RDF (NBRDF) patterns
were relatively flat. Comparison of this result with two kinds of theoretical NBRDFs,
where one havingb een calculatedu sing single-scatteringp arametersb y Mie theory and
the other usingt he samep arameterse xceptf or Henyey-Greenstein(H G) phasef unction
obtained from the same asymmetry factor as in the Mie theory, showed that the observed
NBRDF agreed with the theoretical one using the HG phase function rather than with
that using the Mie phase function, while the albedos calculated with both phase functions
agreed well with each other
書誌情報 JOURNAL OF GEOPHYSICAL RESEARCH

巻 105, 号 D8, p. 10219-10236
出版者
出版者 American Geophysica Ulnion
著者版フラグ
値 publisher
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
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