TY - JOUR

T1 - Cross-shore currents in the surf zone

T2 - rips or undertow

AU - Aagaard, Troels

AU - Vinther, Niels

PY - 2008

Y1 - 2008

N2 -   While the dynamics and kinematics of various types of mean cross-shore current flows in the surf zone (undertow and rip currents) are fairly well understood, the causes for transitions occurring between these two types of mean circulation patterns remain obscure. On longshore barred beaches, such transitions involve the formation and/or degeneration of rip channels. In this paper, field evidence is presented to suggest that transitions between undertow and rip current (cell) circulations may depend upon the magnitude of the wave-induced onshore mass transport across a longshore bar, rip channel spacing and trough cross-sectional area. The results are based on data obtained from four field experiments on the Danish and Dutch North Sea coasts, which encompassed a range of incident wave energy conditions. Two of the data sets demonstrate transitions between cell and undertow circulations. Calculated onshore-directed mass transports in the two circulation types were plotted against At/yr, where At is trough cross-sectional area and yr is longshore distance from the measurement position to a rip channel. The two types of circulation are separated in parameter space by a straight line with a slope of 1 (ms-1). The observations support the model proposed by DEIGAARD et al. (1999), according to which optimum rip spacings exist that depend on the balance between onshore discharge and longshore pressure gradients caused by irregular bar bathymetry. This simple morphodynamic model indicates that both hydrodynamic conditions and existing bathymetry are critical in determining the type of mean current circulation.

AB -   While the dynamics and kinematics of various types of mean cross-shore current flows in the surf zone (undertow and rip currents) are fairly well understood, the causes for transitions occurring between these two types of mean circulation patterns remain obscure. On longshore barred beaches, such transitions involve the formation and/or degeneration of rip channels. In this paper, field evidence is presented to suggest that transitions between undertow and rip current (cell) circulations may depend upon the magnitude of the wave-induced onshore mass transport across a longshore bar, rip channel spacing and trough cross-sectional area. The results are based on data obtained from four field experiments on the Danish and Dutch North Sea coasts, which encompassed a range of incident wave energy conditions. Two of the data sets demonstrate transitions between cell and undertow circulations. Calculated onshore-directed mass transports in the two circulation types were plotted against At/yr, where At is trough cross-sectional area and yr is longshore distance from the measurement position to a rip channel. The two types of circulation are separated in parameter space by a straight line with a slope of 1 (ms-1). The observations support the model proposed by DEIGAARD et al. (1999), according to which optimum rip spacings exist that depend on the balance between onshore discharge and longshore pressure gradients caused by irregular bar bathymetry. This simple morphodynamic model indicates that both hydrodynamic conditions and existing bathymetry are critical in determining the type of mean current circulation.

KW - Faculty of Science

KW - Skallingen

KW - Cell circulation

KW - Egmond

KW - Skallingen

KW - beach processes

KW - beach morphodynamics

KW - mean currents

U2 - 10.2112/04-357

DO - 10.2112/04-357

M3 - Journal article

VL - 24

SP - 561

EP - 570

JO - Journal of Coastal Research

JF - Journal of Coastal Research

SN - 0749-0208

ER -