The drag coefficient, bottom roughness, and wave-breaking in the nearshore

被引:56
作者
Feddersen, F
Gallagher, EL
Guza, RT
Elgar, S
机构
[1] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA
[2] USN, Postgrad Sch, Dept Oceanog, Monterey, CA 93943 USA
[3] Woods Hole Oceanog Inst, AOPE, Woods Hole, MA 02543 USA
基金
美国国家科学基金会;
关键词
nearshore; bed roughness; drag coefficient; circulation;
D O I
10.1016/S0378-3839(03)00026-7
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The bottom drag coefficient in the nearshore has been suggested to depend on bottom roughness (bedforms) or alternatively on wave breaking. The hypothesis that bottom drag coefficient depends on bottom roughness is tested with 2 months of field observations collected on a sandy ocean beach during the Duck94 field experiment. Both the drag coefficient (estimated from alongshore momentum balances) and bottom roughness (estimated from fixed altimeters) are larger within the surfzone than in the region farther seaward. Although the drag coefficient increases with roughness seaward of the surfzone, no relationship was found between the drag coefficient and roughness-related quantities within the surfzone. These results suggest that breaking-wave generated turbulence increases the surfzone drag coefficient. (C) 2003 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:189 / 195
页数:7
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