作者: Carl L. Amos
DOI: 10.1016/S0070-4571(05)80030-5
关键词: Salt marsh 、 Typhoon 、 Tidal irrigation 、 Hydrology 、 Geology 、 Siliciclastic 、 Storm 、 Mean High Water 、 Sediment 、 Erosion 、 Oceanography
摘要: Publisher Summary In this chapter the term “Tidal Flats”, defines tidal flat as “sandy to muddy or marshy flats emerging during low tide and submerging high tide”. This definition can be ambiguous positions of tides are time-variable. The frequency inundation, Waves play a strong role in resuspension sediments on flats. A series papers written effects storms, hurricanes typhoons non-periodic occurrences wave magnitude means that even sheltered regions subject influence at times. degree is often visible across form erosion seaward edges salt marshes mud flats, development sandy beaches top marsh mean water spring (MHWST) level. varying influences waves apparent zonation associated sediment texture.