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The monitoring of coastal sand dunes requires regular high-resolution aerial photography along hundreds of kilometers of coastal strips. Light detection and ranging (LiDAR) is now the most widely used method for detailed topographic and vegetation studies. The aim of this work is to show how the full-waveform shapes returned from single or multiple targets can carry information relating to low-vegetation cover and ground roughness of dunes. This work focuses on marram grass, widely involved in the development of mobile dunes. Low-growing plants often exhibit identical pigmentary composition and can only be distinguished by the height of their foliage, which modifies the shape of the LiDAR waveform around the main returns at the top of the foliage. We show that ray tracing of full LiDAR waveforms on the regular grid of pixels of hyperspectral images, acquired synchronously, can resolve the confusion between low-vegetation gradients and bare sand by analyzing the waveform damping induced by cumulating microdiffusion on foliage height, but also with glint effects on the surface roughness of compact materials. Analysis of successive shorelines of wet to dry sand, sand to pioneer couch grass, and couch grass to consolidating marram grass can thereby be conducted routinely.

Vegetation surveys were conducted on a variety of coastal foredunes in a largely natural region along the Gulf County region of the Florida panhandle. Species presence, absence and percentage cover were surveyed on 12 foredune profiles during different seasons. The vegetation data were analyzed using the Shannon-Wiener Diversity Index and Sorensen Index. Uniola sp. and Andropgon sp. were the dominant species on foredunes. Uniola sp. was found predominantly on the gulfward facing or stoss slopes, and Andropgon sp. was found to be dominant on the inland or lee slopes of foredunes. While they are present on all foredunes, their presence and percentage cover are dominant on rapidly prograding coasts. Prograding/accretional beaches had higher Sorensen Index values (i.e. higher similarities) than did the foredune-vegetation profiles on eroding beaches. Diversity as indicated by the Shannon-Wiener analysis (H') is greatest on the highest, and generally eroding dunes. Foredune diversity increased with foredune height, and the tallest foredunes were found on shorelines with relatively low erosion rates, where dunes were slowly translating landwards, cannibalizing older dunes, and moving into areas colonized by late successional species, such as Quercus sp. These observations of foredune species richness, diversity, profile similarities, and the use of ecological indices can provide excellent proxy evidence of shoreline dynamics, and in particular the degree of beach erosion and accretion, in the absence of historical erosion/accretion data. [ABSTRACT FROM AUTHOR]

ABSTRACT Wind flow and sand transport intensity were measured on the seaward slope of a vegetated foredune during a 16 h storm using an array of sonic anemometers and Wenglor laser particle counters. The foredune had a compound seaward slope with a wave-cut scarp about 0.5 m high separating the upper vegetated portion from the lower dune ramp, which was bare of vegetation. Wind direction veered from obliquely offshore at the start of the event to obliquely onshore during the storm peak and finally to directly onshore during the final 2 h as wind speed dropped to below threshold. Sand transport was initially inhibited by a brief period of rain at the start of the event but as the surface dried and wind speed increased sand transport was initiated over the entire seaward slope. Transport intensity was quite variable both temporally and spatially on the upper slope as a result of fluctuating wind speed and direction, but overall magnitudes were similar over the whole length. Ten-minute average transport intensity correlates strongly with mean wind speed measured at the dune crest, and there is also strong correlation between instantaneous wind speed and transport intensity measured at the same locations when the data are smoothed with a 10 s running mean. Transport on the beach for onshore winds is decoupled from that on the seaward slope above the small scarp when the wind angle is highly oblique, but for wind angles <45° from shore perpendicular some sand is transported onto the lower slope. Copyright © 2012 John Wiley & Sons, Ltd. [ABSTRACT FROM AUTHOR]

In coastal foredunes, the cyst nematode Heterodera arenaria has been supposed to play a role in degeneration of the pioneer grass Ammophila arenaria (marram grass). However, recent field surveys and field inoculation experiments suggested that the abundance of this cyst nematode is controlled by the host plant. Here, we test pathogenicity of H. arenaria by inoculating a range of densities of second-stage juveniles (J2) onto A. arenaria in sterilised soil. Plant root biomass was reduced after 6 weeks of growth, but not after 13 weeks, when cyst formation was completed. Shoot biomass was not influenced. In the field, H. arenaria occurred in sand and on roots of Elymus farctus and A. arenaria in mobile dunes, but not on A. arenaria in stable dunes. Although we observed Heterodera cysts and juveniles in later succession stages, this cyst nematode appeared to be H. hordecalis. In a host suitability test, H. arenaria produced cysts on E. farctus and A. arenaria, while there were almost no cysts produced when J2 had been added to the later succession species Festuca rubra ssp. arenaria, Carex arenaria, Elymus athericus and Calamagrostis epigejos. Heterodera arenaria did not negatively affect its natural host plants. However, H. arenaria reduced root growth of one later succession plant species, E. athericus, which was a poor host for H. arenaria. The effects of H. arenaria inoculation on plant biomass production did not differ when J2 were added to plants growing in non-sterilised soil. We conclude that H. arenaria is specialised on the pioneer grasses E. farctus and A. arenaria, and also on mobile dunes as a habitat. Our results confirm recent suggestions that H. arenaria may cause little direct growth reduction to its natural host plants. [ABSTRACT FROM AUTHOR]

Remote sensing techniques and fixed-site observations were used to evaluate vegetation, habitat and physiographic characteristics of coastal fore dunes in southern Brazil during the last 50 years. The results demonstrated a gradual increase of edaphic stability and biological diversity in fore dunes during several decades, followed by a rapidand profound attenuation of these attributes. The changes in regional hydrology, as a result of long-term and large-scale impoundment andmore recent and localized drainage activities, are appointed as the major cause for foredune modifications in this part of the southwestern Atlantic. [ABSTRACT FROM AUTHOR]