909 research outputs found
Science results from sixteen years of MRO SHARAD operations
In operation for >16 years to date, the Mars Reconnaissance Orbiter (MRO) Shallow Radar (SHARAD) sounder
has acquired data at its nominal 300â450 m along-track and 3-km cross-track resolution covering >55% of the
Martian surface, with nearly 100% overlap in coverage at that scale in the polar regions and in a number of
smaller mid-latitude areas. While SHARAD data have opened a new window into understanding the interior
structures and properties of Martian ices, volcanics, and sedimentary deposits up to a few kilometers in depth,
they have also led to new revelations about the deeper interior and the behavior of the planetâs ionosphere. Here
we summarize the data collected by SHARAD over this time period, the methods used in the analysis of that data,
and the resulting scientific findings. The polar data are especially rich, revealing complex structures that
comprise up to several dozen reflecting interfaces that extend to depths of 3 km, which inform the evolution of
Martian climate in the late Amazonian period. SHARAD observations of mid-latitude lobate debris aprons and
other glacier-like landforms detect strong basal reflections and low dielectric loss, confirming that they are icerich
debris-covered glaciers. In other mid-latitude terrains, SHARAD data demonstrate the presence of widespread
ground ices, likely at lower concentrations. SHARAD signals also probe non-icy materials, mapping out
stacked lava flows, probing low-density materials thought to be ash-fall deposits, and occasionally penetrating
sedimentary deposits, all of which reveal the structures and interior properties diagnostic of emplacement
processes. SHARAD signals are impacted by their passage through the Martian ionosphere, revealing variations
in time and space of the total electron content linked with the remanent magnetic field. Advanced techniques
developed over the course of the mission, which include subband and super-resolution processing, coherent and
incoherent summing, and three-dimensional (3D) radar imaging, are enabling new discoveries and extending the
utility of the data. For 3D imaging, a cross-track spacing at the nominal 3-km resolution is more than sufficient to
achieve good results, but finer spacing of 0.5 km or less significantly improves the spatially interpolated radar
images. Recent electromagnetic modeling and a flight test show that SHARADâs signal-to-noise ratio can be
greatly improved with a large (~120âŠ) roll of the spacecraft to reduce interference with the spacecraft body. Both
MRO and SHARAD are in remarkably fine working order, and the teams look forward to many more years in
which to pursue improvements in coverage density, temporal variability in the ionosphere, and data quality that
promise exciting new discoveries at Mars
Radar sounder evidence of thick, porous sediments in Meridiani Planum and implications for iceâfilled deposits on Mars
Meridiani Planum is one of the most intensely studied regions on Mars, yet little is known about the physical properties of the deposits below those examined by the Opportunity rover. We report the detection of subsurface echoes within the Meridiani Planum deposits from data obtained by the Mars Advanced Radar for Subsurface and Ionospheric Sounding (MARSIS) instrument. The delay time between the surface and subsurface returns is indicative of materials with a real dielectric constant of 3.6 ± 0.6. The real dielectric constant is strongly modulated by bulk density. Newly derived compaction relationships for Mars indicate that the relatively low dielectric constant of the Meridiani Planum deposits is consistent with a thick layer of iceâfree, porous, basaltic sand. The unique physiographic and hydrologic setting of Meridiani Planum may have provided an ideal sediment trap for eolian sands. The relatively low gravity and the cold, dry climate that has dominated Mars for billions of years may have allowed thick eolian sand deposits to remain porous and only weakly indurated. Minimally compacted sedimentary deposits may offer a possible explanation for other nonpolar region units with low apparent bulk dielectric constants
âWe Used to Say Rats Fell from the Sky After a Flood:â Temporary Recovery of Muskrat Following Ice Jams in the Peace-Athabasca Delta
Elders and Indigenous land users in the Peace-Athabasca Delta (PAD) have observed a dramatic decline in the relative abundance of muskrat in recent decades (~1935â2014). The main explanation for the decline has been reduction in suitable habitat as a result of decades with reduced frequency of ice-jam flooding on the Peace River. Under favourable conditions, ice jams can cause flooding of perched basins within the PAD that would otherwise receive no recharge from floodwaters. To examine whether abundance of muskrat in the PAD is driven by flooding, we tested the predictions that the density of muskrat (estimated by winter counts of houses) (1) was inversely related to the number of years since major ice jam floods and (2) increased with water depth. An ongoing collaborative monitoring program initiated in 2011, combined with analysis of data from past surveys (1973â2015), allowed Indigenous land users and scientists to document a 10 to 100-fold increase in the density of muskrat houses in 24 basins, over the two years following ice-jam flood events in the PAD. During 1973â2015, in the periods between major floods, density of houses dropped by approximately 79% for every year after a significant flood. In 27 basins surveyed from 2011 to 2015, density of muskrat houses increased by two orders of magnitude in the two years following a flood in the spring of 2014. Density of muskrat houses had a non-linear relationship with estimated depth of water at the time of fall freeze-up; the highest densities of muskrat houses were in basins with about 60 â 250 cm of water at the time of freeze-up. The depth of snow at the time of surveys did not have a strong relationship with the density of muskrat houses. However, few houses were counted in basins with more than 20 cm of snow, likely because deeper snow made it more difficult to conduct surveys and spot houses. Factors other than an increase in the depth of water at fall freeze-up may provide the mechanisms by which flooding affects muskrat. Density of muskrat houses is clearly tied to ice-jam flooding in the PAD. However, the local mechanisms by which floods affect muskrat are best understood by Indigenous land users and remain poorly understood by Western science. Indigenous peoples continue to regard muskrat as an indicator of ecological and cultural health of the PAD. This study highlights the value of consistent ecological monitoring that includes Indigenous knowledge.Les aĂźnĂ©s et les utilisateurs des terres autochtones du delta des riviĂšres de la Paix et Athabasca ont observĂ© une baisse draconienne de lâabondance du rat musquĂ© au cours des derniĂšres dĂ©cennies (~1935-2014). La principale explication du dĂ©clin est la diminution dâabris convenables, et ce, en raison de plusieurs dĂ©cennies marquĂ©es par la frĂ©quence rĂ©duite dâinondations causĂ©es par des embĂącles dans la riviĂšre de la Paix. Dans des conditions favorables, les embĂącles peuvent causer lâinondation des bassins perchĂ©s au sein du delta des riviĂšres de la Paix et Athabasca qui autrement ne recevraient pas de recharge des eaux de crue. Afin dâexaminer si lâabondance du rat musquĂ© dans le delta des riviĂšres de la Paix et Athabasca est favorisĂ©e par les inondations, nous avons testĂ© des prĂ©visions selon lesquelles la densitĂ© du rat musquĂ© (estimĂ©e par le nombre dâabris en hiver) 1) Ă©tait inversement liĂ©e au nombre dâannĂ©es depuis les derniĂšres importantes inondations causĂ©es par des embĂącles et 2) augmentait avec la profondeur de lâeau. Un programme collaboratif de suivi continu lancĂ© en 2011, combinĂ© Ă lâanalyse de donnĂ©es des relevĂ©s antĂ©rieurs (1973-2015), a permis aux utilisateurs des terres autochtones et aux scientifiques de multiplier de 10 Ă 100 fois la densitĂ© dâabris du rat musquĂ© dans 24 bassins, au cours des deux annĂ©es suivant des Ă©vĂ©nementsdâinondation causĂ©s par des embĂącles dans le delta des riviĂšres de la Paix et Athabasca. Entre 1973 et 2015, durant les pĂ©riodes se situant entre les inondations importantes, la densitĂ© dâabris a diminuĂ© dâenviron 79 % chaque annĂ©e suivant une inondation importante. Dans 27 bassins sondĂ©s entre 2011 et 2015, la densitĂ© dâabris du rat musquĂ© a augmentĂ© de deux ordres de grandeur au cours des deux annĂ©es ayant suivi une inondation survenue au printemps de 2014. La densitĂ© dâabris du rat musquĂ© avait une relation non linĂ©aire avec la profondeur de lâeau estimĂ©e au moment de la prise des glaces en automne; les plus fortes densitĂ©s dâabris du rat musquĂ© se trouvaient dans les bassins ayant de 60 Ă 250 cm dâeau au moment de la prise des glaces. La profondeur de la neige au moment des relevĂ©s nâavait pas de relation solide avec la densitĂ© dâabris du rat musquĂ©. Cependant, nous avons comptĂ© peu dâabris dans les bassins comptant plus de 20 cm de neige, probablement parce quâil Ă©tait plus difficile dâeffectuer des relevĂ©s et de trouver les abris dans la neige plus Ă©paisse. Des facteurs autres que lâaugmentation de la profondeur de lâeau au moment de la prise des glaces en automne pourraient fournir les mĂ©canismes par lesquels les inondations se rĂ©percutent sur les rats musquĂ©s. La densitĂ© dâabris du rat musquĂ© est manifestement liĂ©e aux inondations causĂ©es par des embĂącles dans le delta des riviĂšres de la Paix et Athabasca. Toutefois, les utilisateurs des terres autochtones comprennent mieux les mĂ©canismes locaux par lesquels les inondations se rĂ©percutent sur les rats musquĂ©s, tandis quâils demeurent mal compris par la science occidentale. Les peuples autochtones continuent de considĂ©rer le rat musquĂ© comme un indicateur de la santĂ© Ă©cologique et culturelle du delta des riviĂšres de la Paix et Athabasca. Cette Ă©tude fait ressortir la valeur dâun suivi Ă©cologique constant qui tient compte des connaissances autochtones
Implementing a whole-school relationships and sex education intervention to prevent dating and relationship violence: evidence from a pilot trial in English secondary schools
Adolescent dating and relationship violence is associated with health harms and is an important topic for sex education. School-based interventions addressing this have been effective in the USA, but schools in England confront pressures that might hinder implementation. We assessed the feasibility of, and contextual enablers/barriers to implementing Project Respect, a whole-school intervention. We conducted a pilot trial with process evaluation in six English secondary schools. Intervention comprised: training; policy-review; mapping and patrolling âhotspotsâ; parent information; help-seeking app; and a curriculum (including student-led campaigns) targeting dating violence. Process evaluation included assessments of fidelity and interviews with the trainer and school staff. Schools delivered training and lessons partially or completely and made parent and app information available. Two schools conducted policy reviews; none patrolled hotspots or implemented campaigns. Implementation was strengthened where staff saw dating violence as a priority. Delivery was undermined where staff were insufficiently involved, lacked time for planning or struggled to timetable lessons, and where new school challenges undermined engagement. School-based health interventions must work to build staff buy-in and ensure they do not overburden schools. Dating and relationship violence might best be addressed in this context as a broader aspect of sex education
Quantifying interactions between accommodation and vergence in a binocularly normal population
AbstractStimulation of the accommodation system results in a response in the vergence system via accommodative vergence cross-link interactions, and stimulation of the vergence system results in an accommodation response via vergence accommodation cross-link interactions. Cross-link interactions are necessary in order to ensure simultaneous responses in the accommodation and vergence systems. The crosslink interactions are represented most comprehensively by the response AC/A (accommodative vergence) and CA/C (vergence accommodation) ratios, although the stimulus AC/A ratio is measured clinically, and the stimulus CA/C ratio is seldom measured in clinical practice. The present study aims to quantify both stimulus and response AC/A and CA/C ratios in a binocularly normal population, and determine the relationship between them. 25 Subjects (mean±SD age 21.0±1.9years) were recruited from the university population. A significant linear relationship was found between the stimulus and response ratios, for both AC/A (r2=0.96, p<0.001) and CA/C ratios (r2=0.40, p<0.05). Good agreement was found between the stimulus and response AC/A ratios (95% CI â0.06 to 0.24MA/D). Stimulus and response CA/C ratios are linearly related. Stimulus CA/C ratios were higher than response ratios at low values, and lower than response ratios at high values (95% CI â0.46 to 0.42D/MA). Agreement between stimulus and response CA/C ratios is poorer than that found for AC/A ratios due to increased variability in vergence responses when viewing the Gaussian blurred target. This study has shown that more work is needed to refine the methodology of CA/C ratio measurement
A school intervention for 13- to 15-year-olds to prevent dating and relationship violence: the Project Respect pilot cluster RCT
Background âDating and relationship violenceâ is intimate partner violence during adolescence. Among dating adolescents in England, 66â75% of girls and 32â50% of boys report victimisation. Multicomponent school-based interventions might reduce dating and relationship violence. We optimised and piloted Project Respect, a new intervention in secondary schools in England, and study methods, to assess the value of a Phase III randomised controlled trial. Objectives To optimise Project Respect and to then conduct a pilot randomised controlled trial in southern England, addressing whether or not progression to a Phase III trial is justified in terms of prespecified criteria. To assess which of two dating and relationship violence scales is optimal, to assess response rates and to consider any necessary refinements. Design Optimisation activities aimed at intervention development and a pilot randomised controlled trial. Setting Optimisation in four secondary schools across southern England, varying by region and local deprivation. A pilot cluster randomised controlled trial in six other such schools (four intervention schools and two control schools), varying by region, attainment and local deprivation. Participants School students in years 8â10 at baseline and staff. Interventions Schools were randomised to the intervention or control arm in a 2 : 1 ratio; intervention comprised staff training, mapping âhotspotsâ in school for dating and relationship violence, modifying staff patrols, school policy review, informing parents and carers, an application supporting student help-seeking, and a classroom curriculum for students in years 9 and 10 (including student-led campaigns). Main outcome measures Prespecified criteria for progression to Phase III of the trial, concerning acceptability, feasibility, fidelity and response rates. Primary health outcomes were assessed using the Safe Dates and short Conflicts in Adolescent Dating Relationships Inventory measures collected and analysed by individuals who were masked to allocation. Feasibility of economic analysis was assessed. Data sources Baseline and follow-up student and staff surveys, interviews, observations and logbooks. Results The intervention was optimised and approved by the Study Steering Committee. The student response rates in intervention and control groups were 1057 (84.8%) and 369 (76.6%) at baseline, and 1177 (76.8%) and 352 (83.4%) at follow-up, respectively. Safe Dates and the short Conflicts in Adolescent Dating Relationships Inventory had high levels of completion and reliability. At follow-up, prevalence of past-year dating and relationship violence victimisation was around 35% (Safe Dates scale and short Conflicts in Adolescent Dating Relationships Inventory). Staff response rates were very low. Training occurred in all four schools, with suboptimal fidelity. The curriculum was delivered with optimal fidelity in three schools. Other components were delivered inconsistently. Dating and relationship violence was addressed in control schools via violence prevention and responses, but not systematically. Intervention acceptability among students and staff was mixed. An economic evaluation would be feasible. Limitations One school did not undertake baseline surveys. Staff survey response rates were low and completion of the logbook was patchy. Conclusions Our findings suggest that progression to a Phase III trial of this intervention is not indicated because of limited fidelity and acceptability. Future work High prevalence of dating and relationship violence highlights the ongoing need for effective intervention. Potential intervention refinements would include more external support for schools and enhanced curriculum materials. Any future randomised controlled trials could consider having a longer lead-in from randomisation to intervention commencement, using the short Conflicts in Adolescent Dating Relationships Inventory as the primary outcome and not relying on staff surveys. Trial registration Current Controlled Trials ISRCTN65324176. Funding This project was funded by the National Institute for Health Research (NIHR) Public Health Research programme and will be published in full in Public Health Research; Vol. 8, No. 5. See the NIHR Journals Library website for further project information
Publisher Correction: Reporting guideline for the early-stage clinical evaluation of decision support systems driven by artificial intelligence: DECIDE-AI (Nature Medicine, (2022), 28, 5, (924-933), 10.1038/s41591-022-01772-9)
In the version of this article initially published, a list of the DECIDE-AI expert group members and their affiliations was omitted and has now been included in the HTML and PDF versions of the article. *A list of authors and their affiliations appears online
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