Meso-scale aeolian sediment input to coastal dunes: The nature of aeolian transport events

被引:95
|
作者
Delgado-Fernandez, Irene [1 ]
Davidson-Arnott, Robin [1 ]
机构
[1] Univ Guelph, Dept Geog, Guelph, ON N1G 2W1, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
Meso-scale; Event frequency; Event magnitude; Foredune budget; PRINCE-EDWARD-ISLAND; SAND TRANSPORT; SURFACE MOISTURE; WATER-CONTENT; AIR-FLOW; BEACH; WIND; FOREDUNE; DYNAMICS; THRESHOLDS;
D O I
10.1016/j.geomorph.2010.11.005
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Observations of aeolian transport in coastal areas have focused on short-term experiments because of limitations imposed by instrumentation. This paper uses a case study at Greenwich Dunes, Prince Edward Island National Park, Canada, to analyze how sediment transport takes place at the beach over periods of weeks to months. A monitoring station provided hourly time series of vegetation cover, shoreline position, fetch distances, surficial moisture content, presence of ice and snow, wind speed and direction and transport processes over nine months. Analysis shows that high wind speeds may not generate any net transport into the dunes because of the limitations imposed by snow/ice cover, moisture, and short fetch distances. Despite extreme winds during intense storms, such events often lead to wave scarping rather than aeolian sediment input to the foredunes. When sediment was transported on the beach, the magnitude was regulated by a combination of factors including: angle of wind approach, fetch distance, moisture content, and duration of the wind event. In particular, angle of wind approach (and therefore fetch distance) may demote a high magnitude wind event with strong transport potential to one with no transport at all, which poses challenges for predicting the effects of individual storms over the course of several months. A significant proportion of sediment delivery to the foredunes was associated with wind events of low to medium magnitude. It is suggested here that large magnitude wind events have low probabilities of resulting in transport towards the foredune because factors such as wave inundation play an increasing role in preventing sediment movement across the beach. This has implications for modelling and management, and highlights differences between the magnitude and frequency of aeolian transport events in the coastal environment compared to those in deserts and to fluvial sediment transport. (C) 2010 Elsevier B.V. All rights reserved.
引用
收藏
页码:217 / 232
页数:16
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