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Record #117870:

[Radiative temperature of ice surface in Svalbard, 1991] / Shuhei Takahashi, Hiroyuki Enomoto, Shun'ichi Kobayashi, Kumiko Azuma.

Title: [Radiative temperature of ice surface in Svalbard, 1991] / Shuhei Takahashi, Hiroyuki Enomoto, Shun'ichi Kobayashi, Kumiko Azuma.
Author(s): Takahashi, Shuhei.
Enomoto, Hiroyuki.
Kobayashi, Shun'ichi.
Azuma, Kumiko.
Date: 1992.
Publisher: Mombetsu: Okhotsk Sea & Cold Ocean Research Association
Language: Japanese.
In: Seventh International Symposium on Okhotsk Sea & Sea Ice; abstracts; 2-5 February 1992, Mombetsu, Hokkaido, Japan. (1992.),
Abstract: Radiative temperature of bare-ice surfaces was higher than that of snow surface, though both surface were melting with temperatures that should be 0°C. Temperature difference can be explained by difference of reflection characteristics due to condition of surface. Bare-ice surface would tend to reflect solar radiation, which snow surface would not do because of its rough surface.
Notes:

In: The Seventh International Symposium on Okhotsk Sea & Sea Ice; abstracts; 2-5 February 1992, Mombetsu, Hokkaido, Japan / Okhotsk Sea & Cold Ocean Research Association.

English abstract, p. 286.

Keywords: 551.32 -- Glaciology.
551.324 -- Land ice.
551.324.414 -- Land ice, radiation to and from.
551.578.46 -- Snow cover and snow patches.
551.521 -- Radiation, atmospheric.
E5 -- Glaciology: land ice.
(*32) -- Svalbard.
(*324) -- Spitsbergen.
SPRI record no.: 117870

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245 00 ‡a[Radiative temperature of ice surface in Svalbard, 1991] /‡cShuhei Takahashi, Hiroyuki Enomoto, Shun'ichi Kobayashi, Kumiko Azuma.
260 ## ‡aMombetsu :‡bOkhotsk Sea & Cold Ocean Research Association,‡c1992.
300 ## ‡ap. 286-289 :‡bill.
500 ## ‡aIn: The Seventh International Symposium on Okhotsk Sea & Sea Ice; abstracts; 2-5 February 1992, Mombetsu, Hokkaido, Japan / Okhotsk Sea & Cold Ocean Research Association.
500 ## ‡aEnglish abstract, p. 286.
520 3# ‡aRadiative temperature of bare-ice surfaces was higher than that of snow surface, though both surface were melting with temperatures that should be 0°C. Temperature difference can be explained by difference of reflection characteristics due to condition of surface. Bare-ice surface would tend to reflect solar radiation, which snow surface would not do because of its rough surface.
546 ## ‡aIn Japanese.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.414 -- Land ice, radiation to and from.‡2udc
650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc
650 07 ‡a551.521 -- Radiation, atmospheric.‡2udc
650 07 ‡aE5 -- Glaciology: land ice.‡2local
651 #7 ‡a(*32) -- Svalbard.‡2udc
651 #7 ‡a(*324) -- Spitsbergen.‡2udc
700 1# ‡aTakahashi, Shuhei.
700 1# ‡aEnomoto, Hiroyuki.
700 1# ‡aKobayashi, Shun'ichi.
700 1# ‡aAzuma, Kumiko.
773 0# ‡7c2am ‡aOkhotsk Sea & Cold Ocean Research Association. ‡tSeventh International Symposium on Okhotsk Sea & Sea Ice; abstracts; 2-5 February 1992, Mombetsu, Hokkaido, Japan. ‡dMombetsu : Okhotsk Sea & Cold Ocean Research Association, 1992. ‡wSPRI-117855
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