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Record #152525:
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MARC recordCrystal-growth rates in firn and shallow ice at high-accumulation sites / Jun Li, T.H. Jacka.
| Title: | Crystal-growth rates in firn and shallow ice at high-accumulation sites / Jun Li, T.H. Jacka. |
| Author(s): | Li, Jun. Jacka, T. H. |
| Date: | 1999. |
| In: | Annals of Glaciology. (1999.), Vol. 29 (1999) |
| Abstract: | Examines crystal size and c-axis orientation fabrics in two ice cores drilled at Law Dome, East Antarctica. Snow accumulation rates are particularly high compared to other Antarctic sites. Finds relatively high deformation rates generated in shallow ice as consequence of high accumulation rates, progress to dynamic recrystallization taking over from normal crystal growth as dominant crystal-growth mechanism, leading to rapid increase in crystal size. |
| Notes: | Annals of Glaciology. Vol. 29 :169-175 (1999). Sixth International Symposium on Antarctic Glaciology (ISAG-6), 5--9 September 1998, Lanzhou, China, T.H. Jacka (Editor) |
| Keywords: | 551.32 -- Glaciology. 551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc. 622.14 -- Core sampling, ice and snow. 551.322 -- Ice and snow. 548 -- Crystallography. 548.2 -- Ice, granular structure. Anisotropy. 551.578.46 -- Snow cover and snow patches. 551.324 -- Land ice: Law Dome. E4 -- Glaciology: physics and chemistry of ice. (*7) -- Antarctic regions. (*747.3) -- Budd Coast. |
| SPRI record no.: | 152525 |
LDR 01731naa#a2200000#a#4500 001 SPRI-152525 005 20231205014741.0 007 ta 008 231205s1999####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-152525 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aLi, Jun. 245 10 ‡aCrystal-growth rates in firn and shallow ice at high-accumulation sites /‡cJun Li, T.H. Jacka. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1999. 300 ## ‡ap. 169-175 :‡bdiags., table. 500 ## ‡aAnnals of Glaciology. Vol. 29 :169-175 (1999). 500 ## ‡aSixth International Symposium on Antarctic Glaciology (ISAG-6), 5--9 September 1998, Lanzhou, China, T.H. Jacka (Editor) 520 3# ‡aExamines crystal size and c-axis orientation fabrics in two ice cores drilled at Law Dome, East Antarctica. Snow accumulation rates are particularly high compared to other Antarctic sites. Finds relatively high deformation rates generated in shallow ice as consequence of high accumulation rates, progress to dynamic recrystallization taking over from normal crystal growth as dominant crystal-growth mechanism, leading to rapid increase in crystal size. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc.‡2udc 650 07 ‡a622.14 -- Core sampling, ice and snow.‡2udc 650 07 ‡a551.322 -- Ice and snow.‡2udc 650 07 ‡a548 -- Crystallography.‡2udc 650 07 ‡a548.2 -- Ice, granular structure. Anisotropy.‡2udc 650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc 650 07 ‡a551.324 -- Land ice: Law Dome.‡2udc 650 07 ‡aE4 -- Glaciology: physics and chemistry of ice.‡2local 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 651 #7 ‡a(*747.3) -- Budd Coast.‡2udc 700 1# ‡aJacka, T. H. 773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 29 (1999) ‡wSPRI-60773 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231205