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The present study examines, in the context of physical education (PE) classes, if having the opportunity to report disadvantages before performing a physical test could reduce students' self-reported level of fear of failure. Forty-six students (31 males, M[subscript age] = 14.2 years and 15 females, M[subscript age] = 12.5 years) from a middle school and a high school in France participated in the study. A repeated measures design (intra-individual) was used, such that the fear of failure was measured before and after students were given (week 1) or not given (week 2) the opportunity to report disadvantages that could impair their future performance. The main results indicated that when students had the opportunity to report disadvantages, their self-reported level of fear of failure declined before performing the physical test. Conversely, when they had no opportunity to report disadvantages, their self-reported level of fear of failure increased. Implications for educational psychologists and teachers are discussed.

The purpose of the present experiment was to investigate whether the motivational climates (MCs) drawn from achievement goal and self-determination theories would affect perceived competence and the use of claimed self-handicapping. Specifically, this study examined the effects of performance MC, mastery MC and need-supportive MC on these two variables. In the context of high school physical education, 37 participants had the opportunity to claim handicaps before performing an isometric resistance task in a given MC. This procedure was repeated three times at one-week intervals so that all participants were assigned to each of the three MCs. Consistent with our hypotheses, students claimed handicaps less in the need-supportive than in the performance MC. In addition, when data from girls and boys were separated, girls reported significantly greater perceived competence in the need-supportive MC than in the performance and mastery MCs. The theoretical and applied implications of these finding are discussed.

The vast majority of coastal dunes in Europe have been stabilized by increasing vegetation cover since the mid‐20th century. However, some systems may experience a remobilization phase, generally occurring locally and further propagating alongshore, the drivers of which remain poorly documented. This study investigates the evolutionary paths (stabilization/destabilization/remobilization) from 1945 to 2020 of a 2 km‐long modern coastal transgressive dunefield located in southwest France with a holistic approach (GPR profiles, aerial photographs and LiDAR topographic data). Results show a landward migration of the transgressive dune by approximately 233 ± 7.5 m, through two distinct stages of rapid landward migration from 10 to 23 m/yr (Stage I: 1949–1959 and Stage III: 2000–2021) separated by an approximately 40‐year stage of slow to no migration, but with substantial windward slope deflation (Stage II). The onset of Stage II is due to the fixation of vegetation by human action between 1950 and 1959. The onset of Stage III is hypothesized to be driven by long and sustained upper backshore/dune toe erosion beginning in 1968 due to a massive shoal welding that locally disturbed the longshore drift. It induced a destabilization of the dune and erosion of the vegetation cover over some decades. A non‐synchronization is therefore observed between the start of the perturbation (1968), then the migration (2000), in line with the hysteresis concept of Tsoar (2005). This study shows that almost all of the sedimentary volume of the 1945 dune has been remobilized by translation to shape the dune system in its current form. The 2.2 km dunefield has grown by approximately 673 000 ± 190 000 m3 during the 2005–2020 period. Among this volume, there is a new foredune that was built from 2005 between the upper beach and the transgressive dune (volume in 2020 of about 394 000 ± 68 000 m3). [ABSTRACT FROM AUTHOR]

Numerous studies have been devoted to recurved and hooked spits in micro‐ and meso‐tidal environments, but none have really focused on the peculiar right‐angle plan shape exhibited by some spit hooks. The morphodynamics of a complex multi‐hooked spit in a macrotidal inlet in Normandy, France, have been investigated using aerial photographs and 12 topographic LiDAR surveys from 2000 to 2017, complemented by hydrodynamic data. Merville Spit is a 2.5 km‐long hooked spit, composed of four 'nested' ridges each with a right‐angle hook at its tip, that has developed in the vicinity of the sand‐rich outlet of the Orne River. Monitoring of the two last ridges shows that ridge formation starts with the attachment of the tip of a swash bar to the fulcrum point of the previous ridge, and ends following its westward elongation and counter‐clockwise rotation when its hook impinges on the Orne outlet. The main factor controlling ridge plan‐view shape is swash bar dynamics in the vicinity of the spit. The offshore wave direction has no significant impact on ridge and hook behaviour due to the large number of swash bars on the ebb‐tidal delta. Over the study period, between 5 and 10 swash bars massively assured sand supply to the upper foreshore, favouring the growth of existing ridges, but also enabling the building of a new ridge. The bars contribute to imparting hook right angles at the tips of the ridges by creating local wave refraction or by providing a sheltering effect. Strong tidal currents in the Orne channel act as a hydrodynamic barrier that stops hook elongation at the edge of the river's outlet. The similar behaviour of the two studied ridges has been synthesized into a new and original conceptual model of complex multi‐hooked spit formation and evolution under the influence of swash bars. [ABSTRACT FROM AUTHOR]

Abstract: The morphodynamics of an intertidal bar located on an ebb delta of a megatidal inlet system in Normandy, France, was examined during four short experiments under low to high energy wave conditions and spring or neap tide contexts. Although there have been numerous studies on ebb-tidal bar morphology and on the processes affecting such bars, these concern only microtidal or mesotidal settings, and are mainly based on observations. No detailed work involving hydrodynamic conditions embracing the whole tidal cycle has been carried out so far on the mechanisms of onshore migration of these coastal accumulation features, especially along macro and megatidal coasts. In this study, the morphological response of the bar was coupled with the residence times and intensities of each hydrodynamic process (swash, surf, shoaling waves) over a representative bar cross-shore profile, and sediment transport patterns deduced from fluorescent tracer. The results show that the bar migrated exclusively shoreward during moderate to storm conditions (Hs>0.7 m at the bottom of the bar seaward slope). During low energy wave conditions, no bar movement was observed. Swash action was not the dominant process, mainly due to its duration, which did not exceed 8 min in the course of a semi-diurnal tidal cycle. The movement of sediments and the bar morphology is induced mainly by surf processes and their associated currents. The increase in the significant wave height disturbed the general mean current behaviour, which was parallel to the bar crest during low energy conditions. Under surf conditions, mean flows are directed onshore, with an absence of bed return flow; this allows sediment to be transported towards the bar crest causing a landward bar migration. An offshore-directed cross-shore current (not favourable for bar migration) is recorded with larger water depths and no breaking waves (shoaling conditions). This study also highlights the influence of the tidal water level fluctuations in such a large tidal range setting, which induce a rapid shift in processes (such as bed shear and sediment re-working) across the shore-normal profile. These conditions explain the relative low rate of migration of the bar over the delta platform (about 33 m/year). This rate is much less than those reported from micro-mesotidal environments. Calculations of bed shear stress also show that the mean currents alone are not responsible for onshore bar movement, notwithstanding the megatidal character of the field site. [Copyright &y& Elsevier]

Robin, N.; Billy, J.; Castelle, B.; Hesp, P.; Laporte-Fauret, Q.; Nicolae-Lerma, A.; Marieu, V.; Rosebery, D.; Bujan, S.; Destribats, B., and Michalet., 2020. Beach-dune recovery from the extreme 2013-2014 storms erosion at Truc Vert Beach, Southwest France: New insights from ground-penetrating radar. In: Malvárez, G. and Navas, F. (eds.), Global Coastal Issues of 2020. Journal of Coastal Research, Special Issue No. 95, pp. 588–592. Coconut Creek (Florida), ISSN 0749-0208. Foredunes are efficient natural coastal defenses acting as protective barriers during storm events. A striking example is the response of coastal dunes along the Aquitaine Coast (SW France) to the 2013-2014 winter, which was the most energetic winter since at least the mid-20th century in most of the NE Atlantic. The aim of this study is to analyze the (partial) foredune recovery from the 2013-2014 winter at Truc Vert beach using ground-penetrating radar (GPR) and through the coastal dune internal structure. Geophysical data was compared with semi-monthly DGPS topographic data of the beach, UAV-photogrammetry and Airborne LiDAR surveys of the coastal dune. Three main recovery phases were identified from the 2013-2014 winter: (i) aggradation of the upper-beach and dune front-crest during the post-storm summer; (ii) distinct phases of incipient dune-foot development with dune-crest stability during the following year, and (iii) since 2016, aggradation of both dune-foot and dune front-crest tending towards an equilibrium profile. This study shows that GPR surveys, combined with chronological topographic data, is an efficient tool to provide comprehensive understanding of the beach-dune system evolution at a decadal scale. This approach opens new perspectives to document foredune recovery timing and magnitude along sandy coasts. [ABSTRACT FROM AUTHOR]

Balouin, Y.; Bourrin, F.; Meslard, F.; Palvadeau, E., and Robin, N., 2020. Assessing the role of storm waves and river discharge on sediment bypassing mechanisms at the Têt river mouth in the Mediterranean (southeast France). In: Malvárez, G. and Navas, F. (eds.), Global Coastal Issues of 2020. Journal of Coastal Research, Special Issue No. 95, pp. 351–355. Coconut Creek (Florida), ISSN 0749-0208. River mouths along sandy coastlines are influenced by alongshore transport of littoral sands and the interaction of hydrodynamics processes at the river mouth. These interaction are responsible for opening/closure of river outlets and subsequent episodes of sand bypassing by spitbreaching. Here, we study these mechanisms of alongshore sediment bypassing at a river mouth along the French Mediterranean coast. Over the last 6 years, bypassing processes were found to be associated with spit elongation and spit breaching. Hydrodynamics measurements were implemented in order to assess the respective role of river jet and wave conditions on these opening/breaching episodes. Results tends to point on one major mechanism: spit overtoping that induces breaching. For the floods events analysed, the river jet has apparently only a very low contribution to this opening. [ABSTRACT FROM AUTHOR]

Foredunes provide many environmental and ecosystem services including protection from wave erosion and flooding hazards during storm events. While the impact of human interventions on the short-term evolution of coastal dunes is reasonably well understood, less is known about their contemporary influence on current wind and sediment dynamics several decades after implementation. The coastal dunes in Leucate (SE, France) have been anthropogenically constructed and are dominated by offshore wind conditions. Since their construction 20 years ago, a distinct variation in their longshore morphology has developed that is inherited from its original construction. The northern part of the dune has a symmetrical profile with a 28° degree stoss slope, 30° lee slope and a single crest. The southern part is asymmetric, with a gentler stoss slope (12°), 26° lee slope, and a double crest. To explore the potential geomorphic impacts of this distinct difference in morphology, several numerical simulations with varying wind speeds and direction were conducted. We used Computational Fluid Dynamics (CFD) to explore the spatial variations of the near surface wind flow, shear stress and aeolian sediment transport. show that for each scenario, near surface wind speed accelerated toward the dune crest on the windward slope of the dune. The maximum wind speed varied with incident wind direction, the highest speeds occurring when incident wind flow was perpendicular to the dune crest. The double crest in the southern section of the dune affected the wind flow by inducing two consecutive speeds-up zones, with a greater maximum wind speed than on the single crested dune. Wind flow separation was observed where a steep lee slope was present (single crested dune), and only during perpendicular winds. This suggests that the shape of the dune and the direction of the wind are key parameters rather than wind speed. The area affected by reversed separated flow was spatially limited and did not extend beyond the dune toe but was below the threshold for aeolian sediment transport. Elsewhere in the lee of the dune, the wind was only deflected by an order of 15° for the oblique winds (310 and 330°), and less than 10° for the perpendicular wind (290°) on the southern part. In these locations, the shear velocity exceeded the threshold, notably on the southern dune, which coincided with the formation of undulating aeolian deposits in the lee of vegetation on the dune crest. The spatial differences observed in wind flow and aeolian sediment transport processes on this human-made dune were directly inherited from differences in their construction two decades ago. These results demonstrate the importance of the constructed dune profile, due to its potential impact on the long-term evolution of the landscape and the sediment budget of the system. • Dune construction methods impact their morphology even after several decades. • A relatively small coastal dune can lead to airflow separation. • The pattern of wind flow perturbation depends on dune shape and wind direction. [ABSTRACT FROM AUTHOR]

Introduction: There are little data regarding elective referral to the military specialist, especially considering common pathologies such as spinal diseases, which, in the French forces, involve military neurosurgeons. An overview of the management of the military patient referred to neurosurgery consultation, especially considering spinal diseases that both constitute an operational healthissue in the forces and appear of special interest. The objective was to describe the reasons, demographics, and care pathways, addressed to the neurosurgeon., Materials and Methods: This retrospective, single-center study focused on all military patients referred for neurosurgery consultation at Sainte Anne Military Hospital in Toulon. Extracted data included demographic characteristics, army, unit, military specialty, the reason for referral, the diagnosis by the neurosurgeon, treatment, and outcome., Results: From January 2018 to December 2019, 352 patients were referred for neurosurgical consultation by the unit general practitioner. Spinal disease (n = 297, 91%) was the most frequent reason. Lumbar degenerative disk disease accounted for 20% of consultations, regardless of the patient's unit or specialty. Most of the patients seen in consultation received nonsurgical management (n = 271, 82.6%). These patients mainly presented with cervical or lumbar degenerative disk disease (n = 99, 36.5%) or cervical or lumbar herniated discs (n = 57, 21.0%). Ninety-eight patients (29.9%) were referred exclusively for medical fitness assessment. Few patients experienced full resolution of their presenting complaint after management (n = 9, 2.8%)., Conclusions: This descriptive study demonstrates the predominance of degenerative spinal diseases in military patients referred to neurosurgery. It reflects the importance of the medical and military competence required to maintain operational capability upstream and downstream of war traumatology. The description of the care pathways invites us to define more proactive multidisciplinary pathways for the management of these diseases in the armed forces., (© The Association of Military Surgeons of the United States 2023. All rights reserved. For permissions, please e-mail: journals.permissions@oup.com.)