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Record #158858:
- #158858
Main publication details
MARC recordSummer sea ice characteristics of the Chukchi Sea / Kang Jiancheng, Sun Bo, Sun Junying, Meng Guanglin, Kumiko Goto-Azuma.
| Title: | Summer sea ice characteristics of the Chukchi Sea / Kang Jiancheng, Sun Bo, Sun Junying, Meng Guanglin, Kumiko Goto-Azuma. |
| Author(s): | Jiancheng, Kang. Bo, Sun. Junying, Sun. Guanglin, Meng. Goto-Azuma, Kumiko. |
| Date: | 2001. |
| In: | Chinese Journal of Polar Science. (2001.), Vol. 12(2) (2001) |
| Abstract: | Investigating characteristics of Chukchi Sea sea ice, authors distinguished between melting of surface layer, surface and bottom layers, and total ice, with bottom melting of ice floes most important process. Heated by sun, circulation of warmer water influenced this melting, and balanced fluctuating temperature of sea. Sea ice became mixture of ice and liquid brine. When ice crystals eventually separated, ice collapsed. |
| Notes: | Chinese Journal of Polar Science. Vol. 12(2) :109-118 (2001). |
| Keywords: | 551.326 -- Floating ice. 551.326.1 -- Floating ice, distribution and movement. 551.326.3 -- Floating ice, structure and surface features. 551.326-032.26 -- Floating ice, salinity. 551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc. 622.14 -- Core sampling, ice and snow. 551.465.7 -- Oceanography, energy budget. E6 -- Glaciology: floating ice. (*60) -- Arctic Ocean and adjacent waters. (*682) -- Chukchi Sea. |
| SPRI record no.: | 158858 |
LDR 01728naa#a2200000#a#4500 001 SPRI-158858 005 20240418231645.0 007 ta 008 240418s2001####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-158858 040 ## ‡aUkCU-P‡beng‡eaacr 245 00 ‡aSummer sea ice characteristics of the Chukchi Sea /‡cKang Jiancheng, Sun Bo, Sun Junying, Meng Guanglin, Kumiko Goto-Azuma. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2001. 300 ## ‡ap. 109-118 :‡bdiags., table. 500 ## ‡aChinese Journal of Polar Science. Vol. 12(2) :109-118 (2001). 520 3# ‡aInvestigating characteristics of Chukchi Sea sea ice, authors distinguished between melting of surface layer, surface and bottom layers, and total ice, with bottom melting of ice floes most important process. Heated by sun, circulation of warmer water influenced this melting, and balanced fluctuating temperature of sea. Sea ice became mixture of ice and liquid brine. When ice crystals eventually separated, ice collapsed. 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡a551.326.1 -- Floating ice, distribution and movement.‡2udc 650 07 ‡a551.326.3 -- Floating ice, structure and surface features.‡2udc 650 07 ‡a551.326-032.26 -- Floating ice, salinity.‡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 ‡a551.465.7 -- Oceanography, energy budget.‡2udc 650 07 ‡aE6 -- Glaciology: floating ice.‡2local 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 651 #7 ‡a(*682) -- Chukchi Sea.‡2udc 700 1# ‡aJiancheng, Kang. 700 1# ‡aBo, Sun. 700 1# ‡aJunying, Sun. 700 1# ‡aGuanglin, Meng. 700 1# ‡aGoto-Azuma, Kumiko. 773 0# ‡7nnas ‡tChinese Journal of Polar Science. ‡gVol. 12(2) (2001) ‡wSPRI-143545 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240418