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Record #122822:
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MARC recordAnalysis of synthetic aperture radar data collected over the southwestern Greenland ice sheet / Kenneth C. Jezek, Mark R. Drinkwater, J.P. Crawford, Robert A. Bindschadler, R. Kwok.
| Title: | Analysis of synthetic aperture radar data collected over the southwestern Greenland ice sheet / Kenneth C. Jezek, Mark R. Drinkwater, J.P. Crawford, Robert A. Bindschadler, R. Kwok. |
| Author(s): | Jezek, Kenneth C. Drinkwater, Mark R. Crawford, J. P. Bindschadler, Robert A. Kwok, R. |
| Date: | 1993. |
| In: | Journal of Glaciology. (1993.), Vol. 39(131) (1993) |
| Abstract: | Presents and discusses airborne SAR data collected on 31 August 1989. Offers descriptive model of way in which snow facies are manifest in SAR imagery, depending on wetness of snow. On basis of results, it is predicted that P-band backscatter intensity will decrease up-glacier above dry-snow line, where ice lenses are less numerous, and that there will be strong seasonal dependence in backscatter associated with snowmelt. |
| Notes: | Journal of Glaciology. Vol. 39(131) :119-132 (1993). |
| Keywords: | 551.32 -- Glaciology. 551.321.7 -- Snow cover, measurement of properties. 551.578.46 -- Snow cover and snow patches. 551.578.461 -- Snow cover, methods of reporting and coding. 53.087.23 -- Remote sensing. 528.715 -- Aerial surveys. E10 -- Glaciology: snow and avalanches. (*38) -- Greenland. |
| SPRI record no.: | 122822 |
LDR 01623naa#a2200000#a#4500 001 SPRI-122822 005 20231128172759.0 007 ta 008 231128s1993####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-122822 040 ## ‡aUkCU-P‡beng‡eaacr 245 00 ‡aAnalysis of synthetic aperture radar data collected over the southwestern Greenland ice sheet /‡cKenneth C. Jezek, Mark R. Drinkwater, J.P. Crawford, Robert A. Bindschadler, R. Kwok. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1993. 300 ## ‡ap. 119-132 :‡bill., diags., table, maps. 500 ## ‡aJournal of Glaciology. Vol. 39(131) :119-132 (1993). 520 3# ‡aPresents and discusses airborne SAR data collected on 31 August 1989. Offers descriptive model of way in which snow facies are manifest in SAR imagery, depending on wetness of snow. On basis of results, it is predicted that P-band backscatter intensity will decrease up-glacier above dry-snow line, where ice lenses are less numerous, and that there will be strong seasonal dependence in backscatter associated with snowmelt. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.321.7 -- Snow cover, measurement of properties.‡2udc 650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc 650 07 ‡a551.578.461 -- Snow cover, methods of reporting and coding.‡2udc 650 07 ‡a53.087.23 -- Remote sensing.‡2udc 650 07 ‡a528.715 -- Aerial surveys.‡2udc 650 07 ‡aE10 -- Glaciology: snow and avalanches.‡2local 651 #7 ‡a(*38) -- Greenland.‡2udc 700 1# ‡aJezek, Kenneth C. 700 1# ‡aDrinkwater, Mark R. 700 1# ‡aCrawford, J. P. 700 1# ‡aBindschadler, Robert A. 700 1# ‡aKwok, R. 773 0# ‡7nnas ‡tJournal of Glaciology. ‡gVol. 39(131) (1993) ‡wSPRI-20534 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231128