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Record #119155:

C-band SAR backscatter from ice on shallow tundra lakes: observations and modelling / H. Wakabayashi, Martin O. Jeffries, Wilford F. Weeks.

Title: C-band SAR backscatter from ice on shallow tundra lakes: observations and modelling / H. Wakabayashi, Martin O. Jeffries, Wilford F. Weeks.
Author(s): Wakabayashi, H.
Jeffries, Martin O.
Weeks, Wilford F.
Date: 1992.
In: Eos : transactions, American Geophysical Union. (1992.), Vol. 73(43, fall meeting supplement) (1992)
Abstract: Abstract only. Field measurements near Barrow, AK, in April 1992 confirmed that areas of weak and strong returns in SAR images corresponded to grounded and floating ice, respectively. Grounded ice was <1 m thick and free-floating ice exceeded 2 m. Analysis of ice cores from seven lakes showed that both grounded and free-floating ice had upper layer of clear bubble-free ice and lower layer containing vertically oriented cylindrical bubbles. Structure of ice is discussed in some detail with reference to backscatter intensity.
Notes:

Eos : transactions, American Geophysical Union. Vol. 73(43, fall meeting supplement) :181 (1992).

Keywords: 551.32 -- Glaciology.
551.326 -- Floating ice.
551.326.85 -- Lake ice.
551.326.3 -- Floating ice, structure and surface features.
548.54 -- Ice crystals, habit and appearance.
519.673 -- Modelling.
E6 -- Glaciology: floating ice.
(*49) -- Alaska.
(*494) -- Alaska, northwestern.
SPRI record no.: 119155

MARCXML

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001 SPRI-119155
005 20220926152746.0
007 ta
008 220926s1992####xx####|##|###|0||#0|eng#d
035 ## ‡aSPRI-119155
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aWakabayashi, H.
245 10 ‡aC-band SAR backscatter from ice on shallow tundra lakes :‡bobservations and modelling /‡cH. Wakabayashi, Martin O. Jeffries, Wilford F. Weeks.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1992.
300 ## ‡ap. 181.
500 ## ‡aEos : transactions, American Geophysical Union. Vol. 73(43, fall meeting supplement) :181 (1992).
520 3# ‡aAbstract only. Field measurements near Barrow, AK, in April 1992 confirmed that areas of weak and strong returns in SAR images corresponded to grounded and floating ice, respectively. Grounded ice was <1 m thick and free-floating ice exceeded 2 m. Analysis of ice cores from seven lakes showed that both grounded and free-floating ice had upper layer of clear bubble-free ice and lower layer containing vertically oriented cylindrical bubbles. Structure of ice is discussed in some detail with reference to backscatter intensity.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.326 -- Floating ice.‡2udc
650 07 ‡a551.326.85 -- Lake ice.‡2udc
650 07 ‡a551.326.3 -- Floating ice, structure and surface features.‡2udc
650 07 ‡a548.54 -- Ice crystals, habit and appearance.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡aE6 -- Glaciology: floating ice.‡2local
651 #7 ‡a(*49) -- Alaska.‡2udc
651 #7 ‡a(*494) -- Alaska, northwestern.‡2udc
700 1# ‡aJeffries, Martin O.
700 1# ‡aWeeks, Wilford F.
773 0# ‡7nnas ‡tEos : transactions, American Geophysical Union. ‡gVol. 73(43, fall meeting supplement) (1992) ‡wSPRI-1028
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220926