bluuebunny/crossref_metadata_2025_split huggingface dataset:
Tapirs in trouble: estimating Baird's tapir densities in the Sierra Madre de Chiapas, Mexico
Authors: Rivero Marina , de la Torre J. Antonio , Camacho Gamaliel , Naranjo Eduardo J. , Tobler Mathias W. , Jordan Christopher A. , Medellín Rodrigo A. , Reyna-Hurtado Rafael 
Published: September 2021

AbstractSpatial capture–recapture models have been widely used to estimate densities of species where individuals can be uniquely identified, but alternatives have been developed for estimation of densities for unmarked populations. In this study we used camera-trap records from 2018 to estimate densities of a species that does not always have individually identifiable marks, Baird's tapir Tapirus bairdii, in the Sierra Madre de Chiapas, southern Mexico. We compared the performance of the spatial capture–recapture model with spatial mark–resight and random encounter models. The density of Baird's tapir did not differ significantly between the three models. The estimate of density was highest using the random encounter model (26/100 km2, 95% CI 12–41) and lowest using the capture–recapture model (8/100 km2, 95% CI 4–16). The estimate from the spatial mark–resight model was 10/100 km2 (95% CI 8–14), which had the lowest coefficient of variation, indicating a higher precision than with the other models. Using a second set of camera-trap data, collected in 2015–2016, we created occupancy models and extrapolated density to areas with potential occupancy of Baird's tapir, to generate a population estimate for the whole Sierra Madre de Chiapas. Our findings indicate the need to strengthen, and possibly expand, the protected areas of southern Mexico and to develop an action plan to ensure the conservation of Baird's tapir.
Mobile-assisted language learning in older adults: Chances and challenges
Authors: Puebla Cecilia , Fievet Tiphaine , Tsopanidi Marilena , Clahsen Harald 
Published: September 2021

AbstractIn an increasingly ageing, multilingual, and digitalised society, there is still a lack of research on older adults’ adoption and use of mobile technology for supporting their self-directed second language learning. In the present study, we investigated the extent to which seniors residing in Germany (aged 60+) engage in mobile-assisted language learning (MALL) and the factors encouraging or discouraging them from using language learning apps by conducting a web-based survey (n= 208) and a series of in-depth individual interviews (n= 22). Our results show that (1) participants were resistant to fully embrace the potential of MALL despite their active engagement in language learning and extensive use of digital technology, online resources, and mobile devices; and (2) self-perceived digital literacy and openness towards new developments are strong factors favouring the use of language learning apps in older adulthood. We interpret and discuss these results in the light of theoretical accounts of mobile learning and education in (older) adults, emphasising the need to consider the specific requirements of late-life learners in future implementations of language learning apps. Based on our results, we highlight several implications for designers and developers of such apps intended to facilitate full inclusion of seniors as mobile language learners.
Successful birth after ICSI with testicular immotile spermatozoa from a patient with total MMAF in the ejaculates: a case report
Authors: Zhang Liuguang , Li Yuhu , Huang Yuqun , Li Zongqiang 
Published: September 2021

SummaryThere has been no report on the outcome of vitrified blastocyst transfer from a vitrified oocyte injected with immotile testicular spermatozoa with only multiple morphological abnormalities of the sperm flagella (MMAF). A couple diagnosed with MMAF returned to the clinic to attempt pregnancy using their vitrified oocytes. Testicular spermatozoa were injected intracytoplasmically, and the following intracytoplasmic sperm injection results were observed. In the second cycle, surplus vitrified oocytes and testicular retrieved sperm were used, but no pregnancy ensued. In the third cycle, a surplus vitrified blastocyst was transferred, and a healthy female child was delivered, with a birth weight of 3050 g and a birth length of 53 cm. In this report we describe a successful pregnancy achieved in a patient presenting MMAF. The successful pregnancy was obtained from vitrified oocytes microinjected with testicular retrieved sperm in a vitrified blastocyst transfer.
Ectopic autologous transplantation of ovarian tissue as a feasible technique to assess ovarian morphophysiology
Authors: Nascimento Bárbara Rodrigues , Lopes Guilherme Antonio de Gouvêa , Freitas Danielle Storino de , Campos-Junior Paulo Henrique Almeida 
Published: September 2021

SummaryThe cryopreservation of murine ovarian tissue and its transplantation can be a promising technique for the preservation of fertility and an alternative for the future reconstitution of scientific valuable strains of mice. Accordingly, the aim of this study was to describe the entire surgical procedure for ovariectomy and dorsal subcutaneous autotransplantation in mice, and also some data about the efficiency of this procedure. Female C57Bl/6J mice (n = 18) were anaesthetised and bilaterally ovariectomized. After surgery, ovaries were autotransplanted in small subcutaneous pouches in the dorsal region of the forelimbs. The animals were inspected daily and, 23 days after transplantation, euthanasia and recovery of ovarian tissues were performed. Postoperative recovery, oestrous cyclicity, and folliculogenesis progression were evaluated. At 23 days after transplantation, the recovery of the ovaries was feasible, all classes (primordial to antral) of follicles were observed. Additionally, satisfactory efficiency rates were obtained, with 100% of anaesthesia survival rate, survival, graft recovery, folliculogenesis progression and oestrous cyclicity. In general, this short article describes ovarian ectopic autologous transplantation as an effective technique for maintaining rodent oogenesis and endocrine ovarian function. Even more broadly, we can still assume that the application of this technique may reduce the number of breeding matrices and experimental animals in the near future.
The development of aboriginal brain injury coordinator positions: a culturally secure rehabilitation service initiative as part of a clinical trial
Authors: Armstrong Elizabeth , McCoy Kathy , Clinch Rebecca , Merritt Maureen , Speedy Renee , McAllister Meaghan , Heine Kym , Ciccone Natalie , Robinson Melanie , Coffin Juli 
Published: September 2021

Abstract
Brain injury, resulting from stroke and traumatic brain injury, is a common occurrence in Australia, with Aboriginal people affected at a significant rate and impact felt by individuals, families and communities. Access to brain injury rehabilitation services for Aboriginal people is reported to be often limited, with very little support outside the hospital environment. Our research involving Aboriginal brain injury survivors and their families to date has revealed that people often manage ‘on their own’ following such events. Following recommendations from survivors and their families, the Healing Right Way clinical trial, currently underway in Western Australia, has created the role of Aboriginal Brain Injury Coordinator (ABIC) to assist in navigating information and services, particularly after discharge from hospital. Eight positions for this role have been instigated across metropolitan and rural regions in the state. Healing Right Way’s aim is to enhance rehabilitation services and improve quality of life for Aboriginal Australians after brain injury. The ABIC’s role is to provide education, support, liaison and advocacy services to participants and their families over a six-month period, commencing soon after the participant’s stroke or injury has occurred. This paper outlines the development of this role, the partnerships involved, experiences to date and identifies some facilitators and barriers encountered that may impact the role’s ongoing sustainability. Details of components of the planned full Process Evaluation of Healing Right Way related to the ABIC role and the partnerships surrounding it are also provided. In combination with the trial’s ultimate results, this detail will assist in future service planning and provide a model of culturally secure care for stroke and brain injury services that can also inform other sub-acute and primary care models.
HUP‐BMA: An Integration of Hydrologic Uncertainty Processor and Bayesian Model Averaging for Streamflow Forecasting
Authors: Darbandsari Pedram , Coulibaly Paulin 
Published: September 2021

AbstractUncertainty quantification and providing probabilistic streamflow forecasts are of particular interest for water resource management. The hydrologic uncertainty processor (HUP) is a well‐known Bayesian approach used to quantify hydrologic uncertainty based on observations and deterministic forecasts. This uncertainty quantification is model‐specific; however, utilizing information from multiple hydrologic models should be advantageous and should lead to better probabilistic forecasts. Using seven, structurally different, conceptual models, this study first aims at evaluating the effects of implementing different hydrologic models on HUP performance. Second, using the concepts of the Bayesian Model Averaging (BMA) approach, a multimodel HUP‐based Bayesian postprocessor (HUP‐BMA) is proposed where the combination of posterior distributions derived from HUP with different hydrologic models are used to better quantify the hydrologic uncertainty. All postprocessing approaches are applied for medium‐range daily streamflow forecasting (1–14 days ahead) in two watersheds located in Ontario, Canada. The results indicate that the HUP forecasts for short lead‐times are negligibly affected by implementing different hydrologic models, while with increasing lead‐time and flow magnitude, they significantly depend on the quality of the deterministic forecast. Moreover, the superiority of the proposed HUP‐BMA method over HUP is demonstrated based on various verification metrics in both watersheds. Additionally, HUP‐BMA outperformed the original BMA in quantifying hydrologic uncertainty for short lead‐times. However, by increasing lead‐time, considering the effects of initially observed flow on HUP‐BMA formulation may not be beneficial. So, its modified version unconditioned on initial observations is preferred.
Deriving Antarctic Sea‐Ice Thickness From Satellite Altimetry and Estimating Consistency for NASA's ICESat/ICESat‐2 Missions
Authors: Xu Yue , Li Huan , Liu Baojian , Xie Hongjie , Ozsoy‐Cicek Burcu 
Published: September 2021

AbstractWith the launch of the Ice, Cloud and Land Elevation Satellite‐2 (ICESat‐2), densely measuring the Antarctic ocean all year long, monthly sea ice thickness changes can be inspected. However, the consistency between ICESat‐2 and its predecessor ICESat remains unknown if a long‐term change of the Antarctic sea ice thickness is to be examined. Due to the complex physical structure of Antarctic sea ice, an improved One‐Layer Method (OLMi) for sea‐ice thickness retrieval, with an ∼0.3 m uncertainty, is proposed in this study. Using this method, the monthly sea ice variation in each sea sector of Antarctica from ICESat‐2 is inspected, revealing detailed characteristics of Antarctic sea ice over sector scale such as bi‐modal distributions. The different retrieving methods for the total freeboard from ICESat are found to be ∼0.036 m lower than that from ICESat‐2. The circum‐Antarctic sea ice thickness shows a decreasing tendency (2003–2020), especially in summer with −0.014 m/yr.
What Controls the Presence and Characteristics of Aftershocks in Rock Fracture in the Lab?
Authors: Davidsen Jörn , Goebel Thomas , Kwiatek Grzegorz , Stanchits Sergei , Baró Jordi , Dresen Georg 
Published: September 2021

AbstractAftershock cascades are a characteristic feature of natural seismicity, but underlying mechanisms remain debated. Here, we experimentally explore the presence or absence of aftershocks during failure of intact rock and slip on newly created laboratory faults. We show that the overall activity increase and spatial localization of acoustic emission (AE) events during fracture nucleation occurs without temporal (Omori‐type) correlations. Our analysis shows that this absence of aftershock sequences occurs even beyond peak stress and also when a macroscopic fracture has formed post peak‐stress and propagates. Instead, aftershock triggering does occur during post‐fracture stress relaxation along the newly created lab‐fault and in the presence of large‐scale stress heterogeneities, for example, imposed by a saw‐cut notch. The detected aftershocks in these cases can be described by standard seismological relationships such as a modified Omori‐Utsu relation and its associated inter‐event time distribution and productivity relation. Moreover, AE within all experiments follow the Gutenberg‐Richter relation, with smaller ‐values for triggered events compared to non‐triggered events. Performing full‐moment tensor inversions, we find that seismic events with significant isotropic, compaction components play an important role for aftershock triggering. The resulting triggered events tend to have focal mechanisms similar to their trigger. Seismic events with predominant tensile components, on the other hand, show little evidence for aftershock triggering. This opens up a new perspective on aftershocks, going beyond not only the rate‐and‐state paradigm limited to purely frictional sliding or shear events but also the mainshock attribute paradigm where mainshock attributes control aftershock patterns.
Early Warning for Great Earthquakes From Characterization of Crustal Deformation Patterns With Deep Learning
Authors: Lin J.‐T. , Melgar D. , Thomas A. M. , Searcy J. 
Published: September 2021

AbstractAlthough infrequent, large (Mw7.5+) earthquakes can be extremely damaging and occur on subduction and intraplate faults worldwide. Earthquake early warning (EEW) systems aim to provide advanced warning before strong shaking and tsunami onsets. These systems estimate earthquake magnitude using the early metrics of waveforms, relying on empirical scaling relationships of abundant past events. However, both the rarity and complexity of great events make it challenging to characterize them, and EEW algorithms often underpredict magnitude and the resulting hazards. Here, we propose a model, M‐LARGE, that leverages deep learning to characterize crustal deformation patterns of large earthquakes for a specific region in real‐time. We demonstrate the algorithm in the Chilean Subduction Zone by training it with more than six million different simulated rupture scenarios recorded on the Chilean GNSS network. M‐LARGE performs reliable magnitude estimation on the testing data set with an accuracy of 99%. Furthermore, the model successfully predicts the magnitude of five real Chilean earthquakes that occurred in the last 11 years. These events were damaging, large enough to be recorded by the modern high rate global navigation satellite system instrument, and provide valuable ground truth. M‐LARGE tracks the evolution of the source process and can make faster and more accurate magnitude estimation, significantly outperforming other similar EEW algorithms. This is the first demonstration of our approach. Future work toward generalization is outstanding and will include the addition of more training and testing data, interfacing with existing EEW methods, and applying the method to different tectonic settings to explore performance in these regions.
MagIC as a FAIR Repository for America's Directional Archaeomagnetic Legacy Data
Authors: Jones Shelby A. , Blinman Eric , Tauxe Lisa , Cox J. Royce , Lengyel Stacey , Sternberg Robert , Eighmy Jeffrey , Wolfman Daniel , DuBois Robert 
Published: September 2021

AbstractBeginning in 1964, an academic lineage of Robert DuBois and his students, Daniel Wolfman and Jeffrey Eighmy, developed dedicated United States‐based archaeomagnetic research programs. Collectively, they analyzed over 5,377 archaeomagnetic sites, primarily from North America, dated to less than 2,000 years old. Yet despite their decades of effort, few journal publications resulted. Most of their published results are embedded in archeological reports, often without technical data, which limits the data's accessibility. Furthermore, when published, the results are generally averaged at the site level using statistical conventions different from today's standards, limiting the data's comparability and (re)usability. In 2015, we undertook a salvage archival study to digitize the surviving data and metadata from the scientists' individual estates and emeritus collections. We digitized measurement data from more than 51,000 specimens, reinterpreted them using modern conventions, and uploaded them to the FAIR‐adhering magnetic data repository, earthref.org/MagIC. The reinterpreted site‐level results from the three laboratories are mutually consistent, permitting the individual data sets to be combined and analyzed as single regional entities. Through incorporation into the MagIC repository, these legacy data are now accessible for incorporation into archaeomagnetic and global magnetic field modeling efforts, critical to understanding Earth's magnetic field variation through time. In the Four Corners region of the United States Southwest, this digitized archive advances the development of a new regional paleosecular variation curve used in archaeomagnetic dating. This project highlights both the value and complexities of managing legacy data; the many lessons learned to set a precedent for future paleomagnetic data recovery efforts.
High and Variable Drag in a Sinuous Estuary With Intermittent Stratification
Authors: Bo Tong , Ralston David K. , Kranenburg Wouter M. , Geyer W. Rockwell , Traykovski Peter 
Published: September 2021

AbstractIn field observations from a sinuous estuary, the drag coefficient based on the momentum balance was in the range of , much greater than expected from bottom friction alone. also varied at tidal and seasonal timescales. was greater during flood tides than ebbs, most notably during spring tides. The ebb tide was negatively correlated with river discharge, while the flood tide showed no dependence on discharge. The large values of are explained by form drag from flow separation at sharp channel bends. Greater water depths during flood tides corresponded with increased values of , consistent with the expected depth dependence for flow separation, as flow separation becomes stronger in deeper water. Additionally, the strength of the adverse pressure gradient downstream of the bend apex, which is indicative of flow separation, correlated with during flood tides. While generally increased with water depth, decreased for the highest water levels that corresponded with overbank flow. The decrease in may be due to the inhibition of flow separation with flow over the vegetated marsh. The dependence of during ebbs on discharge corresponds with the inhibition of flow separation by a favoring baroclinic pressure gradient that is locally generated at the bend apex due to curvature‐induced secondary circulation. This effect increases with stratification, which increases with discharge. Additional factors may contribute to the high drag, including secondary circulation, multiple scales of bedforms, and shallow shoals, but the observations suggest that flow separation is the primary source.
Interannual Variability of the Latitude of Separation of the Brazil Current: Teleconnections and Oceanic Rossby Waves Propagation
Authors: Bodnariuk Nicolás , Simionato Claudia G. , Saraceno Martín , Osman Marisol , Diaz Leandro B. 
Published: September 2021

AbstractThe latitude of separation of the Brazil Current (LSBC) variability is analyzed with a view to unveiling the physical mechanisms that modulate the turning point of the Brazil Current at low frequencies. The global ocean reanalysis ORAP5.0 spanning the period 1979–2013 is employed for this purpose. Three characteristic periodicities of the LSBC variability are found on the basis of a Singular Spectrum Analysis: 2, 4 and 10 years. Lagged sea surface height (SSH) correlation maps relate these modulations to Rossby wave propagation. According to these maps, the biennial signal might be triggered by the Atlantic Niño and the Indian Ocean Dipole. In the last case, SSH anomalies propagate around the southern tip of Africa, connecting the Indian and Atlantic oceans. Correlation maps suggest that the 4‐year signal is triggered by both the Atlantic Niño and the ENSO in the equatorial Pacific Ocean. The ENSO‐related anomalies travel through the Indonesian Throughflow along the western Australian coast, where Rossby waves are excited. These anomalies propagate to the eastern coast of Madagascar and feed into the Agulhas Current, eventually leaking into the Atlantic basin. Finally, the decadal signal is associated to the leading mode of decadal variability of the South Pacific Ocean. SSH propagating patterns derived from ORAP5.0 data are also obtained with satellite altimetry during the overlapping period (1993–2013), which strengthens confidence in our results. The association of the LSCB modulations to characteristic climate variability modes suggests that the position of the LSCB could be predicted.
Retracted: True Gravity in Atmospheric Ekman Layer Dynamics
Authors: Chu Peter C. 
Published: September 2021

AbstractTrue gravity is a three‐dimensional vector field, g(λ, φ, z) = igλ + jgφ + kgz, with (λ, φ, z) the (longitude, latitude, height) and (i, j, k) the corresponding unit vectors. The longitudinal‐latitudinal component of the true gravity, gh = igλ+jgφ, is neglected completely in meteorology through using the standard gravity (−g0k, g0 = 9.81 m/s2) or the effective gravity [−g(φ)K]. Here, k (or K) is normal to the Earth spherical (or ellipsoidal) surface. Such simplification of g(λ, φ, z) has never been challenged. This study uses the classical atmospheric Ekman layer dynamics as an example to illustrate the importance of gh. The standard gravity (−g0k) is replaced by the true gravity g in the classical atmospheric Ekman layer equation with a constant eddy viscosity (K) and a height‐dependent‐only density ρ(z) represented by an e‐folding stratification. New formulas for the Ekman spiral and Ekman pumping are obtained. The second derivative of the gravity disturbance (T), , causes the Ekman pumping in addition to the geostrophic vorticity (). With from the EIGEN‐6C4 static gravity model, and calculated from July sea level pressure (p) data from the Comprehensive Ocean‐Atmosphere Data Set, the global mean strength of the Ekman pumping over the world oceans is 3.69 cm s−1 due to gh, which is much larger than 0.33 cm s−1 due to the geostrophic vorticity. It implies the urgency to use the true gravity g(λ, φ, z) into atmospheric GCM and weather forecast although the results are obtained from specific density field and gravity model.