scholarly journals Acoustic scattering in an elastic medium as it relates to sea ice and the determination of effective moduli

1995 ◽  
Vol 97 (5) ◽  
pp. 3336-3336
Author(s):  
Henry A. Laible ◽  
Subramaniam D. Rajan
Keyword(s):  
Sea Ice ◽  
Elastic Medium ◽  
Acoustic Scattering ◽  
Effective Moduli

Quantitative determination of tip undercooling of faceted sea ice with in situ experiments

2021 ◽  
Author(s):  
Tongxin Zhang ◽  
Zhijun Wang ◽  
Lilin Wang ◽  
Junjie Li ◽  
Jincheng Wang
Keyword(s):  
Sea Ice ◽  
Quantitative Determination ◽  
In Situ Experiments

scholarly journals Determination of surface turbulent fluxes over leads in Arctic sea ice

1997 ◽  
Vol 102 (C2) ◽  
pp. 3331-3343 ◽  
Author(s):  
Afshan Alam ◽  
Judith A. Curry
Keyword(s):  
Sea Ice ◽  
Turbulent Fluxes ◽  
Arctic Sea Ice ◽  
Arctic Sea

Determination Of Elastic Moduli Of Sea Ice

2005 ◽  
Author(s):  
K.L. Williams ◽  
R. Stein ◽  
T. Wen ◽  
R.E. Francois
Keyword(s):  
Sea Ice ◽  
Elastic Moduli

Determination of sea ice motion from satellite images

1992 ◽  
pp. 343-354 ◽  
Author(s):  
Benjamin Holt ◽  
D. Andrew Rothrock ◽  
Ronald Kwok
Keyword(s):  
Sea Ice ◽  
Satellite Images

scholarly journals Determination of sea ice processes using geophone arrays

1995 ◽  
Vol 97 (5) ◽  
pp. 3334-3335
Author(s):  
Peter J. Stein ◽  
Steven E. Euerle
Keyword(s):  
Sea Ice

scholarly journals Characteristics of Altimetry Signatures Over Sea Ice (Abstract)

1987 ◽  
Vol 9 ◽  
pp. 240
Author(s):  
N.F. McIntyre ◽  
S.W. Laxon
Keyword(s):  
Sea Ice ◽  
Continental Margin ◽  
Small Proportion ◽  
The Arctic ◽  
Antarctic Sea Ice ◽  
Surface Measurements ◽  
Characteristic Sequences ◽  
Data Coverage ◽  
Ice Edge

We report characteristics of Seasat altimetry signatures recorded over Antarctic sea ice. Up to four discrete zones can at times be seen in characteristic sequences in the Weddell and Ross Seas, and elsewhere. They are substantially larger than those reported in the Arctic, covering up to 2500 km at the time of maximum ice extent in 1978. Transitions between them can be abrupt, with marked changes occurring in less than a few kilometres. Some zones were found to persist through the 3 month satellite lifetime; others exhibited intermittent variations. Repeat data coverage has enabled temporal as well as spatial patterns to be investigated. Interpretation of the geophysical cause of the patterns observed has been limited by available data. Some comparisons may be made with surface measurements of nadir back-scatter on first- and multi-year floes but these account for only a small proportion of the altimetry returns studied. Correlations with the NOAA Navy Ice Charts show significant disparities in the determination of the ice edge which may relate to the sensitivity of the altimeter to the presence of fresh ice or ice in very small quantities. Similar signatures can be found next to small coastal leads at the continental margin, an area known to be important for the growth of new ice.

scholarly journals Direct determination of the air-sea CO2 gas transfer velocity in Arctic sea ice regions

2017 ◽  
Vol 44 (8) ◽  
pp. 3770-3778 ◽  
Author(s):  
John Prytherch ◽  
Ian M. Brooks ◽  
Patrick M. Crill ◽  
Brett F. Thornton ◽  
Dominic J. Salisbury ◽  
...  
Keyword(s):  
Sea Ice ◽  
Direct Determination ◽  
Arctic Sea Ice ◽  
Gas Transfer ◽  
Transfer Velocity ◽  
Co2 Gas ◽  
Gas Transfer Velocity ◽  
Arctic Sea

Laboratory and field measurements of acoustic scattering from sea ice

1988 ◽  
Vol 84 (S1) ◽  
pp. S123-S123
Author(s):  
K. C. Jezek ◽  
T. K. Stanton ◽  
A. J. Gow ◽  
M. Lange
Keyword(s):  
Sea Ice ◽  
Acoustic Scattering ◽  
Field Measurements
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