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Record #114730:
Energy exchange over Antarctic sea ice in late winter / G. König-Langlo, B. Ivanov, A. Zachek.
Title: | Energy exchange over Antarctic sea ice in late winter / G. König-Langlo, B. Ivanov, A. Zachek. |
Author(s): | König-Langlo, G. Ivanov, B. Zachek, A. |
Date: | 1991. |
Publisher: | Fairbanks, AK: University of Alaska, Geophysical Institute/Centre for Global Change and Arctic System Research |
In: | International Conference on the Role of the Polar Regions in Global Change : proceedings of a conference held June 11-15, 1990 at the University of Alaska Fairbanks. (1991.), Vol. 1. |
Abstract: | Measurements made in September and October 1989. Average radiation balance of sea-ice surface was zero, i.e. short-wave radiation gains were fully compensated by long-wave radiation losses. Due to turbulent fluxes of sensible and latent heat, atmosphere received 25 W m⁻² energy from ice--ocean system. Since no significant ice melting or freezing was observed, latter must originate mainly from warm deep water which is entrained into oceanic mixed layer. |
Notes: | In: International Conference on the Role of the Polar Regions in Global Change : proceedings of a conference held June 11-15, 1990 at the University of Alaska Fairbanks. Vol. 1. / Gunter Weller, Cindy L. Wilson, Barbara A.B. Severin, eds. |
Keywords: | 551.32 -- Glaciology. 551.326 -- Floating ice. 551.326.7 -- Sea ice. 551.465.7 -- Oceanography, energy budget. 551.463.6 -- Sea water, thermal properties and heat flux. E6 -- Glaciology: floating ice. (*80) -- Southern Ocean. (*7) -- Antarctic regions. |
SPRI record no.: | 114730 |
LDR 02043naa#a2200000#a#4500 001 SPRI-114730 005 20240419015558.0 007 ta 008 240419s1991####akuab##|#####|0||#0#eng#d 035 ## ‡aSPRI-114730 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aKönig-Langlo, G. 245 10 ‡aEnergy exchange over Antarctic sea ice in late winter /‡cG. König-Langlo, B. Ivanov, A. Zachek. 260 ## ‡aFairbanks, AK :‡bUniversity of Alaska, Geophysical Institute/Centre for Global Change and Arctic System Research,‡c1991. 300 ## ‡ap. 325-329 :‡bdiags., map. 500 ## ‡aIn: International Conference on the Role of the Polar Regions in Global Change : proceedings of a conference held June 11-15, 1990 at the University of Alaska Fairbanks. Vol. 1. / Gunter Weller, Cindy L. Wilson, Barbara A.B. Severin, eds. 520 3# ‡aMeasurements made in September and October 1989. Average radiation balance of sea-ice surface was zero, i.e. short-wave radiation gains were fully compensated by long-wave radiation losses. Due to turbulent fluxes of sensible and latent heat, atmosphere received 25 W m⁻² energy from ice--ocean system. Since no significant ice melting or freezing was observed, latter must originate mainly from warm deep water which is entrained into oceanic mixed layer. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡a551.326.7 -- Sea ice.‡2udc 650 07 ‡a551.465.7 -- Oceanography, energy budget.‡2udc 650 07 ‡a551.463.6 -- Sea water, thermal properties and heat flux.‡2udc 650 07 ‡aE6 -- Glaciology: floating ice.‡2local 651 #7 ‡a(*80) -- Southern Ocean.‡2udc 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 700 1# ‡aIvanov, B. 700 1# ‡aZachek, A. 773 0# ‡7nnam ‡aGunter Weller, Cindy L. Wilson, Barbara A.B. Severin, eds. ‡tInternational Conference on the Role of the Polar Regions in Global Change : proceedings of a conference held June 11-15, 1990 at the University of Alaska Fairbanks. ‡dFairbanks, AK : University of Alaska, Geophysical Institute/Centre for Global Change and Arctic System Research, 1991. ‡gVol. 1. ‡wSPRI-114710 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240419