bluuebunny/crossref_metadata_2025_split huggingface dataset:
Addressing reproductive health knowledge, infertility and coping strategies among rural women in India
Authors: Patra Shraboni , Unisa Sayeed 
Published: July 2020

AbstractAn awareness of fertility and the factors affecting it is crucial to dealing with infertility, though little research has been conducted in the context of rural India. This study assessed Indian women’s perceived causes of, and strategies for coping with, infertility and the associations with levels of reproductive health knowledge in rural areas. Primary data were collected through mapping and listing in high infertility prevalence districts of West Bengal in 2014–15. A total of 159 women aged 20–49 years who had ever experienced infertility were interviewed. A Reproductive Health Knowledge Index (RHKI) was computed to indicate respondent’s level of reproductive health knowledge, and to show its association with perceived causes of infertility and coping with infertility. The highest mean RHKI score was observed among women in the lowest age group (RHKI=5.75, p<0.001), those with a higher level of education (RHKI=9.39, p<0.001) and those who had exposure to any media (RHKI=5.88, p<0.001). Women with a poor wealth index (RHKI=2.11, p<0.01) and those from Scheduled Caste, Scheduled Tribe and Other Backward Class communities (RHKI=4.20, p<0.05) had lower RHKI scores than richer women and those from General Caste communities. Women with a higher RHKI score were more likely to give biology (98.0%, p<0.001), old age (94.1%, p<0.01) and repeated abortions/accident/injury (92.2%, p<0.001) as reasons for infertility, whereas women with a low RHKI were more likely to give religious (73.2%, p<0.001) and old-age-related causes (75.0%, p<0.01) of infertility. Women with a high RHKI score were more likely to opt for modern allopathic treatments (RHKI=7.04, p<0.001), whereas those with a low RHKI score were more likely to seek treatment from religious and superstitious practitioners, use home remedies or receive no treatment at all (RHKI=1.66, p<0.001). Appropriate reproductive health knowledge is crucial if rural Indian women are to correctly assess their infertility problems and choose effective coping strategies.
Emergent STEM lecturer identities: The shaping effects of EMI in action in an internationalised and Englishised HE context
Authors: Block David 
Published: July 2020

AbstractThis paper examines the emergent identities of three STEM (science, technology, engineering and mathematics) lecturers, focusing especially on how they construct themselves with regard to their disciplines and how researchers construct them as potential English language teachers. It begins with essential background information before discussing identity as a key construct. The paper then moves to the presentation of a Foucauldian-inflected version of positioning theory which is employed as a means of understanding the construction of English-medium instruction (EMI) STEM lecturer identities. In the second half of the paper, there is a discussion of three case-studies of EMI STEM lecturers, which shows how each orientates to his or her subject discipline, and the prospect of acting, on occasion, as an English language teacher. Specifically, there is a detailed consideration of how EMI lecturers position themselves in their contacts with researchers and in their teaching; how their self-positionings are consistent or not with how researchers position them; and how self-positionings are similar or different across EMI lecturers. The paper ends with a discussion of what conclusions can be drawn from the research findings.
Experimental Validation of an Adaptive Controller for Manipulators on a Dynamic Platform
Authors: Rodriguez Reina Andres , Nguyen Kim-Doang , Dankowicz Harry 
Published: July 2020

SUMMARYThis paper reports on laboratory and field experimental results for controlled robotic manipulators operating on moving platforms with unmodeled dynamics. The aim is to validate theoretical predictions for the dependence on control parameters of an adaptive control strategy. In addition, the results provide insight into different discretizations of the continuous-time formulation, suggesting the most suitable discretization scheme for hardware implementation. The second set of experimental results, obtained from an implementation of the control framework for synchronization and consensus in networks of robotic manipulators, similarly validate theoretical predictions on the sensitivity to network communication delays.
Trajectories of co-occurring psychopathology symptoms in autism from late childhood to adulthood
Authors: McCauley James B. , Elias Rebecca , Lord Catherine 
Published: July 2020

AbstractGiven high rates of co-occurring conditions in youth and adults with autism spectrum disorder (ASD), it is critical to examine the developmental trajectories of these symptoms of psychopathology. Using data from a cohort of participants (n= 194), most of whom were first assessed for ASD in very early childhood, we investigated the trajectories of co-occurring depressive, anxiety, and attention-deficit hyperactivity disorder (ADHD) symptoms from late childhood to adulthood. Additionally, childhood predictors and adult outcomes associated with these symptom trajectories were examined. Using group-based trajectory modeling, we found two distinct classes of individuals exhibiting each of these co-occurring symptom patterns: one class exhibited fairly low symptoms across time, and one class with elevated symptoms with varied fluctuation across time (ADHD symptoms starting high but decreasing, anxiety symptoms high and stable, and depressive symptoms fluctuating but peaking at clinically significant levels in young adulthood). All high trajectory classes were associated with age 9 adaptive skills; verbal IQ predicted higher anxiety and depressive symptom classes. After accounting for verbal IQ, all high symptom trajectory classes were negative predictors of objective adult outcomes. These findings call for wide-ranging considerations of the needs of individuals across ability levels, autism symptoms, and behavioral and emotional challenges.
Average Ionospheric Middle and Low Latitudes Nighttime Zonal Currents Deduced From CHAMP
Authors: Zhou Yun‐Liang , Lühr Hermann , Alken Patrick 
Published: July 2020

AbstractBy utilizing magnetic field measurements collected by CHAMP during the years 2001–2009, average characteristics of nighttime ionospheric zonal currents at middle and low latitudes are investigated. We provide for the first time the detailed dependencies of these currents on location, local time, season, and the level of solar activity. The main results obtained are (1) the nighttime zonal ionospheric currents at F‐region altitude, derived from the vertical magnetic component, exhibit on average height‐integrated current densities up to 10 mA/m. The amplitude varies quasi‐linearly with F10.7 flux level. (2) During equinoxes symmetric current systems at F‐region altitude are found in the two hemispheres. After sunset, eastward currents dominate at low latitudes, fading away toward midnight. After midnight regions of eastward currents are observed at midlatitude. During solstice seasons, eastward currents are enhanced in the summer hemisphere; westward currents are stronger in local winter. (3) Longitudinal variations of F‐region currents show clear wave‐1 patterns. This is related to the effect of the stationary planetary wave‐1 and the diurnal nonmigrating tide, D0. This dominant tidal signal, enhancing eastward currents over the Pacific region, appears at middle and low latitudes and during all seasons. (4) At the magnetic equator, signs of the equatorial electrojet (EEJ) are evident after 02:30 MLT. Intensity of westward currents in the narrow band increases toward sunrise. Longitudinal variations of the EEJ show a similar wave‐1 pattern as F‐region currents. Here the westward current density is enhanced over Africa/India. The EEJ wave‐1 modulation is strongest around June solstice.
Precision Measurements of Radar Transverse Scattering Speeds From Meteor Phase Characteristics
Authors: Mazur Michael , Pokorný Petr , Brown Peter , Weryk Robert J. , Vida Denis , Schult Carsten , Stober Gunter , Agrawal Anamika 
Published: July 2020

AbstractIn this paper, we describe an improved technique for using the backscattered phase from meteor radar echo measurements just prior to the specular point (t0) to calculate meteor speeds and their uncertainty. Our method, which builds on earlier work of Cervera et al. (1997, https://doi.org/10.1029/96RS03638), scans possible speeds in the Fresnel distance‐time domain with a dynamic, sliding window and derives a best‐speed estimate from the resultant speed distribution. We test the performance of our method, called pre‐t0 speeds by sliding‐slopes technique (PSSST), on transverse scattered meteor echoes observed by the Middle Atmosphere Alomar Radar System (MAARSY) and the Canadian Meteor Orbit Radar (CMOR) and compare the results to time‐of‐flight and Fresnel transform speed estimates. Our novel technique is shown to produce good results when compared to both model and speed measurements using other techniques. We show that our speed precision is ±5% at speeds less than 40 km/s, and we find that more than 90% of all CMOR multistation echoes have PSSST solutions. For CMOR data, PSSST is robust against the selection of critical phase value and poor phase unwrapping. Pick errors of up to ±6 pulses for meteor speeds less than about 50 km/s produce errors of less than ±5% of the meteoroid speed. In addition, the width of the PSSST speed Kernel density estimate (KDE) is used as a natural measure of uncertainty that captures both noise and t0 pick uncertainties.
Experimental Investigation on the Movability of Water in Shale Nanopores: A Case Study of Carboniferous Shale From the Qaidam Basin, China
Authors: Yang Shugang , Yu Qingchun 
Published: July 2020

AbstractThe movability of water in shale nanopores intensely affects the transport and storage of other fluids and plays an important role in the geological water cycle. To investigate the movability of water, three shale samples were used to conduct flow experiments using the steady state and step‐by‐step depressurization method. The experimental results show that the movability of water strongly depends on the pressure gradient. Two water‐related mechanisms, shear fluidity and electroviscous effect, are primarily responsible for the difference in movability between free water and bound water. The flow of water in these samples deviates from Darcy's law, and the threshold pressure gradient (TPG) is observed. When the pressure gradient is higher than the TPG, water starts to flow, and the permeability increases with increasing pressure gradient. Based on the analysis of the solid‐liquid interfacial forces, the water in the shale was quantitatively classified into four types (L1, L2, L3, and L4) according to its movability. The calculation results indicate that most of the water, which could be up to 74.46–89.73%, is immovable under the experimental conditions. The proportion of movable water increases with increasing pressure gradient, and the relation can be expressed by a quadratic function. The moving ratio was defined as the ratio of the volume of water involved in flow to the total pore volume. The correlation between the moving ratio and permeability is a power function with exponents ranging from 1.16 to 1.43, indicating that water permeability is sensitive to the moving ratio.
Turbulence‐Based Model for Subthreshold Aeolian Saltation
Authors: Rana Santosh , Anderson William , Day Mackenzie 
Published: July 2020

AbstractSand transport initiation and cessation occurs when the surface shear velocity exceeds a fluid threshold and falls below an impact threshold, respectively. Even when average shear velocity is below fluid threshold, turbulent fluctuations can initiate saltation, leading to turbulence‐driven transport intermittency. We leveraged the dynamic properties of large‐eddy simulation to recover a shear velocity time series due to atmospheric turbulence and recover a probability density function for saltation based on the frequency of events where wind has previously exceeded fluid threshold but not yet dropped below impact threshold. By conditionally sampling, we can quantitatively predict the frequency of intermediate saltation. Results show that a compensated, subthreshold shear velocity exhibits linear dependence upon the actual shear velocity. This compensated shear velocity compares favorably against field data. Model performance under terrestrial and Mars conditions is also shown.
Ocean Tide Loading Effects on InSAR Observations Over Wide Regions
Authors: Yu Chen , Penna Nigel T. , Li Zhenhong 
Published: July 2020

AbstractRecent and future Interferometric Synthetic Aperture Radar (InSAR) missions provide spatially wide and temporally continuous observations capturing relative ground motions over great distances which enable nationwide or continent‐wide deformation mapping. To achieve this, long wavelength errors, which increase with distance and are coupled with geophysical deformation, must be corrected. We predict the ocean tide loading (OTL) effect on Sentinel‐1 interferograms globally for all ascending and descending acquisitions, and they are largest in coastal regions. Then, interferograms over southwest Britain are investigated, with the OTL correction having a similar noise reduction effect as when correcting for tropospheric delay (27% standard deviation reduction for tropospheric delay and 46% for combined tropospheric delay and OTL). OTL corrections contribute considerably to the noise reduction of the InSAR time series, with the time series standard deviation reducing by 33% after correcting tropospheric errors and 52% after also applying OTL corrections.
A Closure of the Mongol‐Okhotsk Ocean by the Middle Jurassic: Reconciliation of Paleomagnetic and Geological Evidence
Authors: Yi Zhiyu , Meert Joseph G. 
Published: July 2020

AbstractThe late Mesozoic closure of the Mongol‐Okhotsk Ocean (MOO) is critical for understanding the tectonics of East Asia. There is a considerable mismatch (~40 million years) between the timing of MOO closure based on paleomagnetic data and geological evidence. We review paleomagnetic data from Mongolia, Siberia, and North China and argue that previously published apparent polar wander paths (APWPs) for North China and Siberia are insufficient to constrain the timing of MOO closure. Our new analysis incorporates newly published paleomagnetic data from North China and a refined geochronology for the key Siberian poles. We combine this with an updated global APWP incorporating large‐scale Jurassic true polar wander and argue that the MOO was closed by the Middle Jurassic. This temporal shift is compatible with geology‐based models. The Middle Jurassic reconstruction of Eurasia suggests that the East Asian blocks had become a quasi‐rigid part of Pangea prior to breakup.
Triggering the Indian Ocean Dipole From the Southern Hemisphere
Authors: Zhang Lian‐Yi , Du Yan , Cai Wenju , Chen Zesheng , Tozuka Tomoki , Yu Jin‐Yi 
Published: July 2020

AbstractThis study identifies a new triggering mechanism of the Indian Ocean Dipole (IOD) from the Southern Hemisphere. This mechanism is independent from the El Niño‐Southern Oscillation (ENSO) and tends to induce the IOD before its canonical peak season. The joint effects of this mechanism and ENSO may explain different lifetimes and strengths of the IOD. During its positive phase, development of sea surface temperature cold anomalies commences in the southern Indian Ocean, accompanied by an anomalous subtropical high system and anomalous southeasterly winds. The eastward movement of these anomalies enhances the monsoon off Sumatra‐Java during May–August, leading to an early positive IOD onset. The pressure variability in the subtropical area is related with the Southern Annular Mode, suggesting a teleconnection between high‐latitude and midlatitude climate that can further affect the tropics. To include the subtropical signals may help model prediction of the IOD event.
Development of Hierarchical Ensemble Model and Estimates of Soil Water Retention With Global Coverage
Authors: Zhang Yonggen , Schaap Marcel G. , Wei Zhongwang 
Published: July 2020

AbstractCorrect quantification of mass and energy exchange processes between land surface and atmosphere requires an accurate description of unsaturated soil hydraulic properties. Soil pedotransfer functions (PTFs) have been widely used to predict soil hydraulic parameters. Here, 13 PTFs were grouped according to input data requirements and evaluated against a well‐documented database (National Cooperative Soil Survey Characterization [NCSS]) covering the continental United States (87.7% of data) and other regions of the globe (12.3% of data). Weighted ensembles were shown to have improved performance over individual PTFs in terms of evaluation criteria. Validation of moisture content estimated from the ensemble models against observations showed promising results. Global maps of soil water retention data from the ensemble models as well as their uncertainty were provided. Our full 13‐member ensemble model provides more accurate estimates than PTFs that are currently being used in Earth system models, which may, therefore, provide improved water fluxes and reduce uncertainty of the estimations.
The Modulation of Plasma and Waves by Background Electron Density Irregularities in the Inner Magnetosphere
Authors: Yue Chao , Ma Qianli , Jun Chae‐Woo , Bortnik Jacob , Zong Qiugang , Zhou Xuzhi , Jang Eunjin , Reeves Geoffrey D. , Spence Harlan E. , Wygant John R. 
Published: July 2020

AbstractThe background cold electron density plays an important role in plasma and wave dynamics. Here, we investigate an event with clear modulation of the particle fluxes and wave intensities by background electron density irregularities based on Van Allen Probes observations. The energies at the peak fluxes of protons and Helium ions of 100 eV to several keV are well correlated with the total electron density variation. Intense electromagnetic ion cyclotron (EMIC) and magnetosonic (MS) waves are simultaneously observed in the high‐density regions and disappear in low‐density regions. Based on the linear theory of wave growth, the EMIC waves are generated by the ~10 keV protons, while most MS waves are generated by the positive gradient of proton phase space density at several hundred eV in the high‐density regions. Our results indicate the importance of background plasma density structures in generation of plasma waves by unstable ion distributions.
Impact of Eurasian Ice Sheet and North Atlantic Climate Dynamics on Black Sea Temperature Variability During the Penultimate Glacial (MIS 6, 130–184 ka BP)
Authors: Wegwerth Antje , Kaiser Jérôme , Dellwig Olaf , Arz Helge W. 
Published: July 2020

AbstractUnderstanding hemisphere‐wide millennial‐scale temperature variability during past glacials in response to ice sheet dynamics and orbital forcing is one of the key targets for Quaternary climate research. While an inland propagation of abrupt temperature changes into Eurasia from the North Atlantic realm during the last glacial (Weichselian) receives increasingly broad support, much less is known regarding the penultimate glacial (Saalian) temperature variability, especially from a continental interior perspective. Here, we present a TEX86‐derived lake surface temperature (LST) record from the former Black Sea “Lake” covering nearly the entire Marine Isotope Stage (MIS) 6. While orbital‐scale LST cooling likely relates to meltwater discharge from the retreating Eurasian Ice Sheet during insolation maxima, millennial‐scale LST variability suggests interstadial warming in phase with Greenland and northern Mediterranean Sea temperature records during the first half of MIS 6. Although summer insolation reached an interglacial‐like level during this period, we propose that the reduced extent of the Eurasian Ice Sheet associated with northward shifted atmospheric fronts was ultimately responsible for the inland propagation of Dansgaard‐Oeschger‐like temperature variability. During the second half of MIS 6, temperature patterns across the North Atlantic‐Eurasian corridor were more variable and less comparable with each other, likely because of the larger continental ice sheet weakening northern hemisphere atmospheric teleconnections. Temperature records across the North Atlantic‐Eurasian realm suggest a weaker atmospheric teleconnection during MIS 6 compared to MIS 3, likely related to a stronger imprint of the Eurasian Ice Sheet on the continental and regional climate.
Improved Characterization of DNAPL Source Zones via Sequential Hydrogeophysical Inversion of Hydraulic‐Head, Self‐Potential and Partitioning Tracer Data
Authors: Kang Xueyuan , Kokkinaki Amalia , Kitanidis Peter K. , Shi Xiaoqing , Revil André , Lee Jonghyun , Soueid Ahmed Abdellahi , Wu Jichun 
Published: July 2020

AbstractHigh‐resolution characterization of hydraulic properties and dense nonaqueous phase liquid (DNAPL) contaminant source is crucial to develop efficient remediation strategies. However, DNAPL characterization suffers from a limited number of borehole data in the field, resulting in a low‐resolution estimation. Moreover, high‐resolution DNAPL characterization requires a large number of unknowns to be estimated, presenting a computational bottleneck. In this paper, a low‐cost geophysical approach, the self‐potential method, is used as additional information for hydraulic properties characterization. Joint inversion of hydraulic head and self‐potential measurements is proposed to improve hydraulic conductivity estimation, which is then used to characterize the DNAPL saturation distribution by inverting partitioning tracer measurements. The computational barrier is overcome by (a) solving the inversion by the principal component geostatistical approach, in which the covariance matrix is replaced by a low‐rank approximation, thus reducing the number of forward model runs; (b) using temporal moments of concentrations instead of individual concentration data points for faster forward simulations. To assess the ability of the proposed approach, numerical experiments are conducted in a 3‐D aquifer with 104 unknown hydraulic conductivities and DNAPL saturations. Results show that with realistic DNAPL sources and a limited number of hydraulic heads, the traditional hydraulic/partitioning tracer tomography roughly reconstructs subsurface heterogeneity but fails to resolve the DNAPL distribution. By adding self‐potential data, the error is reduced by 24% in hydraulic conductivity estimation and 68% in DNAPL saturation characterization. The proposed sequential inversion framework utilizes the complementary information from multi‐source hydrogeophysical data sets, and can provide high‐resolution characterizations for realistic DNAPL sources.