Open AccessOn the effective aerodynamic and scalar roughness length of Weddell Sea ice
Author(s) -
Weiss Alexandra I.,
King John,
LachlanCope Tom,
Ladkin Russ
Publication year - 2011
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2011jd015949
Subject(s) - sea ice , arctic ice pack , geology , sea ice thickness , sea ice concentration , roughness length , antarctic sea ice , sea ice growth processes , atmospheric sciences , climatology , oceanography , wind speed , wind profile power law
We study the effective aerodynamic roughness length z 0 _eff and scalar roughness length for temperature z T _eff over different compact sea ice types in the Antarctic Weddell Sea by aircraft measurements during two austral summer seasons. z 0 _eff and z T _eff are highly variable in the Weddell Sea ice area. The averaged value of in all main sea ice areas was smaller than the averaged value of . The ratio between the two roughness lengths was relatively small for new/young sea ice with / ≈ 2, but the ratio became significantly large for the multiyear pack ice with / ≈ 227. For the pack ice area, with sea ice concentration ranging between 95% to 100%, we determined a median = 4.1 × 10 −03 m and a median = 1.8 × 10 −05 m. In the new, young sea ice area, with sea ice concentration ranging between 98% and 100%, we observed a median = × 10 −04 m and a median = 2.2 × 10 −04 m. These values of and differ from published observations conducted in a pack ice and new, young sea ice area in the northern hemisphere, such as the Arctic. Most model parameterizations require the roughness lengths as constant values as boundary input parameters. Our study shows that by using the and values of this study, instead of commonly used sea ice roughness length values, the accuracy of parameterized heat and momentum fluxes in the Weddell Sea ice area can significantly be improved.