首页> 外文会议>Coastal sediments'03: crossing disciplinary boundaries >Conceptualu001fbeach-stateu001fmodelu001fforu001ftheu001finneru001fbaru001fofu001fau001fstorm-dominated,u001fu001fmicro/mesou001ftidalu001frangeu001fcoastu001fatu001fWanganui,u001fNewu001fZealand
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Conceptualu001fbeach-stateu001fmodelu001fforu001ftheu001finneru001fbaru001fofu001fau001fstorm-dominated,u001fu001fmicro/mesou001ftidalu001frangeu001fcoastu001fatu001fWanganui,u001fNewu001fZealand

机译:u001fbeach-state u001fmodel u001ffor u001fthe u001finner u001fbar u001fof u001fa u001fstorm主导的 u001f u001fmicro / meso u001ftidal u001frange u001fcoast u001fat u001fWanganui,

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摘要

Plan-viewu001fmorphologicalu001fconfigurationsu001fwereu001fidentifiedu001fforu001ftheu001finneru001fsub-tidalu001frnbaru001f atu001fWanganui,u001fNewu001f Zealand,u001f andu001f configurationu001f behaviouru001fwasu001f relatedu001f tou001fwaveu001frnheight,u001f longshoreu001f currentu001f (inu001f termsu001f ofu001f longshoreu001f windu001fcomponents),u001f tidalu001f rangeu001f (inu001frntermsu001f ofu001f neapu001f tide-springu001f tideu001f variation),u001f andu001f antecedentu001f morphologyu001f tou001f deriveu001f au001frnconceptualu001fmodelu001fforu001fthisu001ftypeu001fofu001fcoast.u001fu001fTheu001fWanganuiu001fcoastu001fisu001fcharacterisedu001fbyu001ffineu001frnsand,u001fmultipleu001fsandu001fbars,u001ffrequentu001fstormu001fwaves,u001flongshoreu001fcurrent,u001fau001fneapu001ftidalu001frangeu001fofu001fu001frn0.8u001f mu001f andu001f au001f springu001f tidalu001f rangeu001f ofu001f 2.4u001f m.u001f Transverseu001f configurationsu001f occuru001f moreu001frnfrequentlyu001fandu001fwereu001fmoreu001fpersistentu001fthanu001ftheu001fotheru001f3u001ftypesu001fofu001fconfigurationu001fusedu001finu001ftheu001frnstudy:u001f linear,u001fundulatingu001fandu001fsubdued.u001fu001fTheu001fpredominantu001fclassu001ftransitionsu001fconsistu001fofu001frntransverseu001f configurationsu001f changingu001f tou001f subduedu001f andu001f undulating;u001f undulatingu001frnconfigurationsu001f changingu001f tou001f transverse;u001f linearu001f configurationsu001f changingu001f tou001f undulating,u001frnandu001fsubduedu001fconfigurationsu001fchangingu001ftou001ftransverse.u001fConfigurationu001fchangeu001ftou001ftransverse,u001frnundulatingu001f andu001f linearu001f occuru001f underu001f loweru001f (neap)u001f tidalu001f conditions,u001f withu001f linearityu001frnincreasingu001fwithu001fincreasingu001fwaveu001fheightu001fandu001fstrengthu001fofu001ftheu001flongshoreu001fcurrent.u001fChangeu001ftou001frnsubduedu001fconfigurationsu001fcorrespondsu001fwithu001fhigheru001f(spring)u001ftides,u001floweru001fwaveu001fheightu001fandu001frnweakeru001f longshoreu001f current.u001f u001f Theu001f directionu001f ofu001f longshoreu001f currentsu001f alsou001f influencesu001frnconfigurationu001f change.u001f u001f Inu001f particular,u001f theu001f formationu001f ofu001f transverseu001f configurationsu001f areu001frnfacilitatedu001f byu001f longshoreu001f currentsu001f alignedu001f withu001f theu001f obliqueu001f ripu001f currentsu001f whichu001frncharacteriseu001ftheu001fWanganuiu001fcoast.u001fu001fByu001fcontrast,u001ftheu001fformationu001fofu001fsubduedu001fandu001fundulatingu001frnconfigurationsu001f appearu001f tou001f beu001f facilitatedu001f byu001f longhoreu001f currentsu001f opposingu001f obliquelyu001frnorientatedu001fripu001fcurrents.u001fu001fMorphologicalu001ffeedbacku001fenablesu001ftransverseu001fconfigurationsu001ftou001frnresistu001f greateru001f waveu001f heightu001f andu001f strongeru001f longshoreu001f currentu001f thanu001f occuru001f duringu001f theiru001frnformation.u001fWhileu001fundulatingu001fandu001flinearu001fconfigurationsu001fremainu001fcoherentu001fduringu001fhigheru001frntidalu001frange,u001fbar-crestsu001fbroadenu001finu001ftheu001fcross-shoreu001fdirectionu001fwithu001ftheu001foppositeu001foccurringu001frnduringu001ftimesu001fofu001floweru001ftidalu001frange.u001fTransverseu001fconfigurationsu001fmayu001falsou001fpersistu001fduringu001frnhigheru001ftidalu001frange;u001fhowever,u001finu001fthisu001fsituationu001fbar-crestu001fbroadeningu001fandu001fchannelu001finfillu001fcanu001frnresultu001finu001fau001fclassu001fchangeu001ftou001fsubduedu001fconfigurations.
机译:计划 - viewu001fmorphologicalu001fconfigurationsu001fwereu001fidentifiedu001fforu001ftheu001finneru001fsub-tidalu001frnbaru001f atu001fWanganui,u001fNewu001f新西兰,u001f andu001f configurationu001f behaviouru001fwasu001f relatedu001f tou001fwaveu001frnheight,u001f longshoreu001f currentu001f(inu001f termsu001f ofu001f longshoreu001f windu001fcomponents),u001f tidalu001f rangeu001f(inu001frntermsu001f ofu001f neapu001f潮springu001f tideu001f变化),u001f andu001f antecedentu001f morphologyu001f tou001f deriveu001f au001frnconceptualu001fmodelu001fforu001fthisu001ftypeu001fofu001fcoast。 u001fu001fTheu001fWanganuiu001fcoastu001fisu001fcharacterisedu001fbyu001ffineu001frnsand,u001fmultipleu001fsandu001fbars,u001ffrequentu001fstormu001fwaves,u001flongshoreu001fcurrent,u001fau001fneapu001ftidalu001frangeu001fofu001fu001frn0.8u001f mu001f andu001f au001f springu001f tidalu001f rangeu001f ofu001f 2.4u001f m.u001f Transverseu001f configurationsu001f occuru001f moreu001frnfrequentlyu001 fandu001fwereu001fmoreu001fpersistentu001fthanu001ftheu001fotheru001f3u001ftypesu001fofu001fconfigurationu001fusedu001finu001ftheu001frnstudy:u001f线性,u001fundulatingu001fandu001fsubdued.u001fu001fTheu001fpredominantu001fclassu001ftransitionsu001fconsistu001fofu001frntransverseu001f configurationsu001f changingu001f tou001f subduedu001f andu001f起伏; u001f undulatingu001frnconfigurationsu001f changingu001f tou001f横向; u001f linearu001f configurationsu001f changingu001f tou001f起伏,u001frnandu001fsubduedu001fconfigurationsu001fchangingu001ftou001ftransverse.u001fConfigurationu001fchangeu001ftou001ftransverse,u001frnundulatingu001f andu001f linearu001f occuru001f underu001f loweru001f(NEAP)u001f tidalu001f条件,u001f withu001f linearityu001frnincreasingu001fwithu001fincreasingu001fwaveu001fheightu001fandu001fstrengthu001fofu001ftheu001flongshoreu001fcurrent.u001fChangeu001ftou001frnsubduedu001fconfigurationsu001fcorrespondsu001fwithu001fhigheru001f (春天) 001ftides,u001floweru001fwaveu001fheightu001fandu001frnweakeru001f longshoreu001f current.u001f u001f Theu001f directionu001f ofu001f longshoreu001f currentsu001f alsou001f influencesu001frnconfigurationu001f change.u001f u001f Inu001f特别地,u001f theu001f formationu001f ofu001f transverseu001f configurationsu001f areu001frnfacilitatedu001f byu001f longshoreu001f currentsu001f alignedu001f withu001f theu001f obliqueu001f ripu001f currentsu001f whichu001frncharacteriseu001ftheu001fWanganuiu001fcoast.u001fu001fByu001fcontrast,u001ftheu001fformationu001fofu001fsubduedu001fandu001fundulatingu001frnconfigurationsu001f appearu001f tou001f beu001f facilitatedu001f byu001f longhoreu001f currentsu001f对立的u001f倾斜的u001定向的u001fripu001fcurrents.u001fu001f形态学u001ffeedbacku001fenablesu001ftransverseu001fconfigurationsu001ftou001frnresistu001f更大的u001f waveu001f高度u001f和u001f更强的u001f longshoreu001f当前u001fi ru001frnformation.u001fWhileu001fundulatingu001fandu001flinearu001fconfigurationsu001fremainu001fcoherentu001fduringu001fhigheru001frntidalu001frange,u001fbar-crestsu001fbroadenu001finu001ftheu001fcross-shoreu001fdirectionu001fwithu001ftheu001foppositeu001foccurringu001frnduringu001ftimesu001fofu001floweru001ftidalu001frange.u001fTransverseu001fconfigurationsu001fmayu001falsou001fpersistu001fduringu001frnhigheru001ftidalu001frange; u001fhowever,u001finu001fthisu001fsituationu001fbar-crestu001fbroadeningu001fandu001fchannelu001finfillu001fcanu001frnresultu001finu001fau001fclassu001fchangeu001ftou001fsubduedu001fconfigurations。

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