skip to primary navigation skip to content
 

 

You are not currently logged in

SPRI library catalogue

View a record

Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.

Please search for material in iDiscover for up-to-date information about the library collection.


Record #154781:

Heat transport in McMurdo Sound first-year fast ice / H.J. Trodahl, and 6 others.

Title: Heat transport in McMurdo Sound first-year fast ice / H.J. Trodahl, and 6 others.
Author(s): Trodahl, H. J.
Date: 2000.
In: Journal of Geophysical Research. (2000.), Vol. 105(C5) (2000)
Abstract: Uses relationship of rate of change of internal energy density to divergence of heat current density rather than wave attenuation predicted by thermal diffusion equation in data reduction for analyzing heat transport through sea ice at McMurdo Sound, Antarctica. Weak temperature dependence is similar to that predicted by models in literature, but magnitude is small by about 10% than usual predicted value for climate and sea ice models. Sudden rise of growth rate is shown coinciding with appearance of platelet ice in time and depth. Discusses radiative solar heating at depth.
Notes:

Journal of Geophysical Research. Vol. 105(C5) :11, 347-11, 358 (2000).

Keywords: 551.32 -- Glaciology.
551.326 -- Floating ice.
551.326.7 -- Sea ice.
551.322 -- Ice and snow.
536.2 -- Heat, transmission.
519.673 -- Modelling.
E6 -- Glaciology: floating ice.
(*7) -- Antarctic regions.
(*881.1) -- McMurdo Sound.
SPRI record no.: 154781

MARCXML

LDR 01580naa#a2200000#a#4500
001 SPRI-154781
005 20220926145504.0
007 ta
008 220926s2000####xx#a##|##|###|0||#0|eng#d
035 ## ‡aSPRI-154781
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aTrodahl, H. J.
245 10 ‡aHeat transport in McMurdo Sound first-year fast ice /‡cH.J. Trodahl, and 6 others.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2000.
300 ## ‡ap. 11, 347-11, 358 :‡bdiags.
500 ## ‡aJournal of Geophysical Research. Vol. 105(C5) :11, 347-11, 358 (2000).
520 3# ‡aUses relationship of rate of change of internal energy density to divergence of heat current density rather than wave attenuation predicted by thermal diffusion equation in data reduction for analyzing heat transport through sea ice at McMurdo Sound, Antarctica. Weak temperature dependence is similar to that predicted by models in literature, but magnitude is small by about 10% than usual predicted value for climate and sea ice models. Sudden rise of growth rate is shown coinciding with appearance of platelet ice in time and depth. Discusses radiative solar heating at depth.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.326 -- Floating ice.‡2udc
650 07 ‡a551.326.7 -- Sea ice.‡2udc
650 07 ‡a551.322 -- Ice and snow.‡2udc
650 07 ‡a536.2 -- Heat, transmission.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡aE6 -- Glaciology: floating ice.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*881.1) -- McMurdo Sound.‡2udc
773 0# ‡7nnas ‡tJournal of Geophysical Research. ‡gVol. 105(C5) (2000) ‡wSPRI-35252
916 ## ‡a149162 -- 2014/03/12 -- CC
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220926 ‡bCC