bluuebunny/crossref_metadata_2025_split huggingface dataset:
Pencegahan Kekerasan Dalam Rumah Tangga Terhadap Perempuan Dan Anak di Desa Mojorejo
Authors: Sari Rahayu  , Hilmi Jauhar  , Fachry Lazuardy  , Nur Mochamad  , Rachmatus Ananda  , Hany Pratondo  , Apriliana Priska  , Romadhoni Dika  , Arnold Gabriel  , Paulanda Putri  , Yulita Alfiana  , Riyanto Riyanto  , Kurnia Renita  , Sistyaningsih Retno  , Tya Yania  , Arya Galuh  , Riko Mochammad  , Duwy Putry  , Khoirudin Khoirudin  , Nadya Agnes  , Aditya Rivan  , Shukri Muhamad  , Arifin Arifin  
Published: September 2024

The service's goal is to promote public understanding of domestic violence prevention and build awareness among the inhabitants of Mojorejo Village. Counseling activities in the community are motivated by phenomena that occur in the community. The problem of domestic violence itself is actually a problem that often occurs in married life, but some people do not consider what they experience as an act that is wrong in the eyes of the law. Therefore, the community needs to be given an understanding of domestic violence, so that if it occurs or experiences domestic violence, the victim can take legal steps. The method used is a participatory method which is expected to play an active role in legal counseling activities in the form of; Lecture on the Socialization of Law Number 23 of 2004 concerning Domestic Violence; Legal counseling regarding the material of Law Number 23 of 2004 concerning Domestic Violence; Question and answer session about domestic violence through mediation.
Workshop Bagi Pelajar MAN 1 Pangkalpinang Untuk Menjadi Content Kreator
Authors: Ade Septryanti  , Syafrul Irawadi  , Hilyah Magdalena  , Harrizki Arie Pradana  , Yuri Prima Fittryani  
Published: September 2024

Social media is currently very popular with the millennial generation, where the current millennial generation is required to have very high creativity and can produce content. A good content is produced because of the existence of personal branding and good public speaking from a creator. In the workshop students are given directions and techniques for how to build personal branding and public speaking in public, besides that students are taught how to make and produce a video to be recognized by many people. The community service activity was held at MAN 1 Pangkalpinang which was attended by 40 students. Students who were so excited when they received the material and were very active in asking questions.asked questions when the resource person gave the material.
ТЕСТАМЕНТ ВАСИЛЯ ЗАГОРОВСЬКОГО 1577 р. У НАУКОВІЙ РЕЦЕПЦІЇ МИХАЙЛА ГРУШЕВСЬКОГО
Authors: Галів Микола 
Published: September 2024

Мета статті – розкрити особливості рецепції Михайлом Грушевським такого історичного джерела як заповіт Василя Загоровського 1577 р. Завдання дослідження передовсім полягає у визначенні тих проблемно-змістових компонентів джерела, які найбільше зацікавили видатного українського історика, а також у з’ясуванні оцінки М. Грушевським тестаменту брацлавського каштеляна як літературного твору. Методологія дослідження спирається на принципи історизму, системності, авторської об’єктивності, а також на методи критики історичних та історіографічних джерел. Наукова новизна дослідження полягає у тому, що вперше здійснено аналіз наукової рецепції М. Грушевським такого історичного джерела, як тестамент волинського шляхтича, брацлавського каштеляна Василя Загоровського від 11 липня 1577 р. Висновки. Отже, заповіт волинського шляхтича Василя Загоровського від 11 липня 1577 р. відомий в історичній науці доволі давно: уперше був опублікований ще 1859 р. Цей документ став об’єктом наукових і літаратурних зацікавлень Й. Ролле, О. Федорова-Чеховського, О. Фотинського, С. Томашівського, а відтак і М. Грушевського, котрий доволі широко використав його в шостому томі “Історії України-Руси”. Український історик охарактеризував особу автора документа, обставини появи і мову історичного джерела. Вченого у тестаменті Василя Загоровського найбільше зацікавили такі проблемно-змістові аспекти: 1) політичні і національні візії автора; 2) родинні цінності Загоровського-молодшого, його ставлення до власної родини, типові аспекти сімейного життя української шляхти; 3) інструкція щодо освіти та виховання дітей Василя Загоровського; 4) оформлення заповідачем благодійних фундацій для церкви, при якій мали діяти шпиталь і школа; 5) розпорядження щодо слуг і підданих брацлавського каштеляна. М. Грушевський значну увагу приділив літературній цінності зазначеного тестаменту, поставивши його в один ряд з “Повчанням дітям…” Володимира Мономаха, хоча був невисокої думки про літературні таланти Василя Загоровського. Важливо, що сама стратегія опрацювання М. Грушевським цього джерела дає змогу оприявнити і його погляди на джерелознавчу методологію, яка містила не лише позитивістські, але й неокантіанські техніки.
САМОДІЯЛЬНІ ГРОМАДСЬКІ ОРГАНІЗАЦІЇ ІВАНО-ФРАНКІВСЬКОЇ ОБЛАСТІ УКРАЇНСЬКОЇ РСР (1960 – 1970)
Authors: МАЛЯРЧУК Олег , ГРИВНАК Богдан , ПАЛАГНЮК Михайло 
Published: September 2024

Мета дослідження – на основі архівних матеріалів і літератури охарактеризувати механізм створення та роботу самодіяльних громадських організацій радянської тоталітарної системи часів так званого “розвинутого соціалізму”, напрацьований досвід на прикладі Івано-Франківської області західного регіону Української РСР. Методологія дослідження ґрунтується на принципах історизму, об’єктивності, системності. При проведенні дослідження застосовувались загальнонаукові (аналіз і синтез, абстрагування) та конкретно- наукові методи. Наукова новизна полягає у тому, що на основі вивчення офіційних інформацій райвиконкомів, розпоряджень Івано-Франківського облвиконкому розкрито функціонування низової ланки радянських органів через роботу самодіяльних громадських організацій, які були невід’ємною складовою політичної системи та здійснювали “радянське будівництво” на місцях і формували “фасад демократії”. Висновки. Життя усіх громадян в СРСР перебувало під тотальним ідеологічним та правоохоронним контролем. Керівництво країни проявляло неабияку винахідливість у справі виховання громадян на радянських цінностях та залучення місцевого активу під керівництвом комуністичної партії, радянського уряду до сільської, селищної, міської, районної, обласної управлінської ланки. Право керувати на місцях надавалося тільки членам партії та перевіреним особам. Розгалужена мережа самодіяльних громадських організацій охоплювала активістів за місцем проживання, навчання, у кожному трудовому колективі та дублювала і контролювала як органи тогочасного низової управлінської ланки, так й повсякденне життя громадян. Ухилитися від нагляду і так званої “суспільно корисної праці” було практично нереально. Самодіяльні громадські товариства створювалися й функціонували за принципом “демократичного централізму”, тобто жорсткої підпорядкованості комуністичній партії і політиці в СРСР.
Primers on Adventurous Psychology and Risk Perception Bias among Cybercrime Helpers
Authors: Zhang Sunan 
Published: September 2024

In the context of the growing prevalence of the Internet, the incidence of cybercrime is increasing at a rapid pace. This has led to the emergence of cybercrime helpers, who have become a significant and pervasive phenomenon that cannot be overlooked. This paper addresses the psychological characteristics of those who engage in cybercrime. A combination of literature study and empirical research allows for a preliminary analysis of the risk-taking psychology and risk perception bias of cybercrime helpers. It also provides new ideas and directions for the study of curbing cybercrime and offers prevention and intervention strategies targeting the psychological level of low-age and social individuals. The study revealed that the risk-taking psychology and risk perception bias of cybercrime helpers are closely intertwined, influencing each other to prompt criminal behaviour. The findings offer implementation strategies with practical value for cybercrime governance.
Documenter la relocalisation forcée d’une communauté innue (Québec)
Authors: Jérôme Laurent , Bacon Joséphine , Lalo Maxime , Mark Mathias 
Published: September 2024

Dans cet article, nous présenterons l’histoire de la relocalisation forcée d’une communauté innue (Pakua-Shipi, Saint-Augustin, Québec) qui a débuté dans les années 1950, avec des regroupements basés sur des stratégies matrimoniales, et qui s’est achevée dans les années 1970, avec la construction de nouvelles maisons. Cette recherche collaborative, entamée en 2011 avec la communauté de Pakua-Shipi, a pour objectif de documenter les événements entourant ce projet de relocalisation, mais aussi le rôle des principaux acteurs engagés dans ce processus, soit des agents du ministère des Affaires indiennes, des missionnaires Oblats et des Innus. Alors que la méthode du storytelling a mis en valeur le point de vue et l’expérience des aînés ayant vécu les événements, le travail en archives a donné un nouvel éclairage aux sources orales en révélant les motivations et le rôle ambigu des autorités politiques et religieuses. Nous proposons trois objectifs d’analyse et de réflexion : 1) documenter les cinq séquences de la relocalisation, soit la préparation, la déportation, les conditions d’arrivée dans la communauté d’accueil (Unamen Shipu, La Romaine) et les voyages retours ; 2) comprendre les rôles respectifs des agents fédéraux et du missionnaire Alexis Joveneau (o.m.i.) ; 3) analyser les liens entre récits innus et correspondances officielles, dont la compréhension nous apparaît indispensable à la reconstitution de l’expérience coloniale.
The particle carriers of field‐aligned currents in the Earth's magnetotail during a substorm
Authors: Cheng Z. W. , Zhang J. C. , Shi J. K. , Kistler L. M. , Dunlop M. , Dandouras I. , Fazakerley A. 
Published: March 2016

AbstractAlthough the particle carriers of field‐aligned currents (FACs) in the Earth's magnetotail play an important role in the transfer of momentum and energy between the solar wind, magnetosphere, and ionosphere, the characteristics of the FAC carriers have been poorly understood. Taking advantage of multiinstrument magnetic field and plasma data collected by the four spacecraft of the Cluster constellation as they traversed the northern plasma sheet boundary layer in the magnetotail on 14 September 2004, we identified the species type and energy range of the FAC carriers for the first time. The results indicate that part of tailward FACs is carried by energetic keV ions, which are probably originated from the ionosphere through outflow, and they are not too small (~2 nA/m2) to be ignored. The earthward (tailward) FACs are mainly carried by the dominant tailward (earthward) motion of electrons, and higher‐energy electrons (from ~0.5 to 26 keV) are the main carriers.
The response of mesospheric NO to geomagnetic forcing in 2002–2012 as seen by SCIAMACHY
Authors: Sinnhuber M. , Friederich F. , Bender S. , Burrows J. P. 
Published: March 2016

AbstractDaily NO number density, retrieved from measurements of the Scanning Imaging Absorption Spectrometer for Atmospheric Chartography (SCIAMACHY) from 2002 to 2012 for polar summer in the mesosphere, is used to investigate the response of NO to geomagnetic activity, as expressed by the auroral electrojet (AE) index. Applying the superposed epoch analysis, we observe a clear response of NO to strong geomagnetic forcing at geomagnetic latitudes 55–75°N/S and altitudes above 66 km. The 27 day solar rotation cycle is observed, indicating that some of the observed geomagnetic events are related to solar coronal holes. We find a linear relationship between anomalies of AE and NO at geomagnetic latitudes 55–70°N/S and 70–74 km altitude. A clear auroral oval‐like structure is observed on days of strong geomagnetic forcing in both hemispheres, with small longitudinal inhomogeneities, which might be related to the South Atlantic Anomaly or the magnetic local time. The NO lifetime and production rate per AE anomaly has been derived from a least squares fit to the observations. Comparisons of results from a simple model using this empirical NO production and a lifetime varying from 1.2 days in summer to 10 days in winter to SCIAMACHY observations show good agreement. In particular, the strength and interannual variability of the wintertime maximum is well captured. This suggests that direct production of NO in the upper mesosphere above 72 km contributes substantially to the so‐called energetic particle precipitation indirect effect.
Aftershocks triggered by fluid intrusion: Evidence for the aftershock sequence occurred 2014 in West Bohemia/Vogtland
Authors: Hainzl S. , Fischer T. , Čermáková H. , Bachura M. , Vlček J. 
Published: March 2016

AbstractThe West Bohemia/Vogtland region, central Europe, is well known for its repeating swarm activity. However, the latest activity in 2014, although spatially overlapping with previous swarm activity, consisted of three classical aftershock sequences triggered by ML3.5, 4.4, and 3.5 events. To decode the apparent system change from swarm‐type to mainshock‐aftershock characteristics, we have analyzed the details of the major ML4.4 sequence based on focal mechanisms and relocated earthquake data. Our analysis shows that the mainshock occurred with rotated mechanism in a step over region of the fault plane, unfavorably oriented to the regional stress field. Most of its intense aftershock activity occurred in‐plane with classical characteristics such as (i) the maximum magnitude of the aftershocks is significantly less than the mainshock magnitude and (ii) the decay can be well fitted by the Omori‐Utsu law. However, the absolute number of aftershocks and the fitted Omori‐Utsu c and p parameters are much larger than for typical sequences. By means of the epidemic‐type aftershock sequence model, we show that an additional aseismic source with an exponentially decaying strength triggered a large fraction of the aftershocks. Corresponding pore pressure simulations with an exponentially decreasing flow rate of the fluid source show a good agreement with the observed spatial migration front of the aftershocks extending approximately with
. Thus, we conclude that the mainshock opened fluid pathways from a finite fluid source into the fault plane explaining the unusual high rate of aftershocks, the migration patterns, and the exponential decrease of the aseismic signal.
Geodetic observations of postseismic creep in the decade after the 1999 Izmit earthquake, Turkey: Implications for a shallow slip deficit
Authors: Hussain Ekbal , Wright Tim J. , Walters Richard J. , Bekaert David , Hooper Andrew , Houseman Gregory A. 
Published: March 2016

AbstractThe relationship between aseismic slip and tectonic loading is important for understanding both the pattern of strain accumulation along a fault and its ability to generate large earthquakes. We investigate the spatial distribution and temporal evolution of aseismic creep on the western North Anatolian Fault (NAF) using time series analysis of Envisat interferometric synthetic aperture radar (InSAR) data, covering the full extent of the 1999 Izmit and Düzce earthquake ruptures and spanning 2002–2010. Discontinuities in the line‐of‐sight velocity across the fault imply that fault creep reaches the Earth's surface at an average fault‐parallel rate of ∼5 mm/yr along an ∼80 km section of the NAF. By combining InSAR and published GPS velocities, we are able to extract the vertical and east‐west components of motion and show that the Adapazari basin is subsiding at a rate of ∼6 mm/yr. Vertical motions have biased previous estimates of creep in this region. The displacement time series close to the fault is consistent with an afterslip model based on rate‐and‐state friction, which predicts a rapid deceleration in fault creep rate after the Izmit earthquake to a near‐steady state ∼5 mm/yr after 5 years. Projecting our model 200 years into the future we find that the cumulative displacement of 1–1.3 m is insufficient to account for the shallow coseismic slip deficit observed in previous studies. Distributed off‐fault deformation in the shallow crust or transient episodes of faster slip are likely required to release some of the long‐term strain during the earthquake cycle.
Recent changes in sea ice area flux through the Beaufort Sea during the summer
Authors: Howell Stephen E. L. , Brady Michael , Derksen Chris , Kelly Richard E. J. 
Published: March 2016

AbstractOver the annual cycle, sea ice is sequestered from the Canadian Basin and transported through the Beaufort Sea toward the Chukchi Sea. In recent years, the Beaufort Sea has experienced considerable ice loss during the summer, which may be indicative of recent changes to this process. In order to investigate this, we quantify the sea ice area flux using RADARSAT from 1997 to 2014 at three gates in Beaufort Sea: the Canadian Basin (entrance), mid‐Beaufort (midpoint), and Chukchi (exit). There was a mean annual flux of 42 ± 56 × 103 km2 at the Canadian Basin gate, 94 ± 92 × 103 km2 at the mid‐Beaufort gate and −83 ± 68 × 103 km2 at the Chukchi gate (positive and negative flux signs correspond to ice inflow and outflow, respectively). The majority of ice transport in Beaufort Sea was found to occur from October to May providing replenishment for ice lost during the summer months. The cross‐strait gradient in sea level pressure explains ∼40% of the variance in the ice area flux at the gates. Remarkably, the mean July–October net sea ice area flux at the Chukchi gate decreased by ∼80% from 2008 to 2014 relative to 1997–2007 and became virtually ice‐free every year since 2008. This reduction was associated with younger (thinner) ice that was unable to survive the summer melt season when either being sequestered from the Canadian Basin and transported through Beaufort Sea during the melt season (2008–2011) or remaining immobile and present in the vicinity of the Chukchi gate during the melt season (2012–2014).
Long‐term characterization of the Pacific ITCZ using TRMM, GPCP, and ERA‐Interim
Authors: Wodzicki K. R. , Rapp A. D. 
Published: March 2016

AbstractAn objective, automated Intertropical Convergence Zone (ITCZ) identification and characterization algorithm is developed and applied to European Centre for Medium‐Range Weather Forecasts Reanalysis Interim (ERA‐Interim) variables, and Tropical Rainfall Measuring Mission (TRMM) Microwave Imager (TMI) and Global Precipitation Climatology Project (GPCP) rain rates (RRs) to create 15 and 36 year climatologies, respectively, in the tropical Pacific ocean. Characteristics derived from the algorithm include ITCZ latitude, northern and southern ITCZ convection boundaries and extent, and precipitation intensity. The climatological location of the ITCZ was found near 8°N, consistent with previous studies, with a preferred southern boundary location of 4°N. The northern ITCZ boundary did not exhibit a preferred boundary with locations between 7° and 15°N having similar frequencies of occurrence. The northern and southern extents of the ITCZ were symmetric in the central Pacific and asymmetric in the east Pacific. Long‐term trends in the ITCZ width and precipitation intensity showed significant narrowing and intensifying. Separation of characteristics by season and location (i.e., central and eastern Pacific) revealed negative trends in ITCZ width in both domains, with trends in the east Pacific weaker than those in the central Pacific. Trends in precipitation intensity near the center of the ITCZ indicate a strong intensification, with slightly stronger trends in the central Pacific than in the east Pacific. These findings show that while the location of the ITCZ has not changed significantly over the past three decades, the ITCZ has narrowed and convection has intensified.
Exploiting sparsity and field conditioning in subsurface microwave imaging of nonweak buried targets
Authors: Bevacqua Martina , Crocco Lorenzo , Donato Loreto Di , Isernia Tommaso , Palmeri Roberta 
Published: March 2016

AbstractAn efficient inverse scattering strategy is proposed to achieve dielectric characterization of buried objects in lossy soils. The approach takes advantage of Virtual Experiments and Compressive Sensing to obtain quantitative reconstructions of nonweak targets which are nonsparse in the pixel representation basis, commonly adopted in microwave imaging. In addition, an original strategy is adopted to overcome the relevant information lack arising when data are gathered under aspect‐limited configurations, such as in ground penetrating radar (GPR) surveys. The proposed strategy significantly outperforms the results achievable with the “state of the art” standard approaches since it allows to achieve nearly optimal reconstructions within a linear framework and without increasing the overall computational burden. Numerical examples with simulated data are given to show the feasibility of the proposed strategy.
Numerical experiments to explain multiscale hydrological responses to mountain pine beetle tree mortality in a headwater watershed
Authors: Penn Colin A. , Bearup Lindsay A. , Maxwell Reed M. , Clow David W. 
Published: March 2016

AbstractThe effects of mountain pine beetle (MPB)‐induced tree mortality on a headwater hydrologic system were investigated using an integrated physical modeling framework with a high‐resolution computational grid. Simulations of MPB‐affected and unaffected conditions, each with identical atmospheric forcing for a normal water year, were compared at multiple scales to evaluate the effects of scale on MPB‐affected hydrologic systems. Individual locations within the larger model were shown to maintain hillslope‐scale processes affecting snowpack dynamics, total evapotranspiration, and soil moisture that are comparable to several field‐based studies and previous modeling work. Hillslope‐scale analyses also highlight the influence of compensating changes in evapotranspiration and snow processes. Reduced transpiration in the Grey Phase of MPB‐induced tree mortality was offset by increased late‐summer evaporation, while overall snowpack dynamics were more dependent on elevation effects than MPB‐induced tree mortality. At the watershed scale, unaffected areas obscured the magnitude of MPB effects. Annual water yield from the watershed increased during Grey Phase simulations by 11 percent; a difference that would be difficult to diagnose with long‐term gage observations that are complicated by inter‐annual climate variability. The effects on hydrology observed and simulated at the hillslope scale can be further damped at the watershed scale, which spans more life zones and a broader range of landscape properties. These scaling effects may change under extreme conditions, e.g., increased total MPB‐affected area or a water year with above average snowpack.