Characteristics of sea ice floe size distribution in the seasonal ice zone

The size distribution of sea ice floes was observed by coordinated Landsat imagery and video monitoring conducted from an icebreaker and a helicopter for an area 38 km × 26 km in seasonal sea ice in the southern Sea of Okhotsk in February 2003. The combination of imagery on several scales allowed me...

Full description

Saved in:
Bibliographic Details
Published inGeophysical research letters Vol. 33; no. 2
Main Authors Toyota, Takenobu, Takatsuji, Shinya, Nakayama, Masashige
Format Journal Article
LanguageEnglish
Published Washington, DC Blackwell Publishing Ltd 01.01.2006
American Geophysical Union
Subjects
Online AccessGet full text
ISSN0094-8276
1944-8007
DOI10.1029/2005GL024556

Cover

More Information
Summary:The size distribution of sea ice floes was observed by coordinated Landsat imagery and video monitoring conducted from an icebreaker and a helicopter for an area 38 km × 26 km in seasonal sea ice in the southern Sea of Okhotsk in February 2003. The combination of imagery on several scales allowed measurements of ice floes over three orders of magnitude, from 1 m to 1.5 km. Two different regimes were observed: floes larger than about 40 m have a power‐law number density with an exponent of −1.87, in the lower range of earlier results. Below 40 m, the power law exponent is −1.15. The cause of these two different regimes is hypothesized to lie in the effects of swell on floes of different sizes and thicknesses. The importance of the floe size distribution for lateral melting is elucidated.
Bibliography:ark:/67375/WNG-JHCVT96C-N
istex:B12B5C735C1A8EB1A50BB70E249F2304C6E17A99
ArticleID:2005GL024556
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ObjectType-Article-2
ObjectType-Feature-1
ISSN:0094-8276
1944-8007
DOI:10.1029/2005GL024556