bluuebunny/crossref_metadata_2025_split huggingface dataset:
The modernity of tradition: Women and ‘healthy progress’ in late colonial Java and Sumatra
Authors: Formichi Chiara 
Published: March 2022

AbstractWriting in the Malay-language press from the late 1910s to the 1930s, literate women in colonial Java and Sumatra engaged deeply with understandings of modernity mediated through concepts of healthfulness and hygiene. Piecing together the views of writers who participated in conversations about health, child-rearing, child-feeding, and socio-political progress, and situating them against the backdrop of both imperial policies of hygienic modernity and systems of indigenous knowledge, this article argues that these women deployed their own agency and negotiation efforts to articulate a singular paradigm of progress. The article focuses on practices of infant-feeding, showing that these literate colonized women's conscious manipulation of the colonial discourse on scientific modernity was grounded in their awareness of the racial project of control of their own bodies. The promotion of ‘traditional’ breastfeeding was a way to affirm a path to progress that shared the underlying conditions for, but not the modalities of, Western modernity. Examining the processes of negotiation and subversion that emerged in these women's writings provides a productive space to question and reframe scholarly understandings of ‘modernity’ as a category of analysis.
Lung flukes of the genusParagonimus: ancient and re-emerging pathogens
Authors: Blair David 
Published: March 2022

AbstractThe title of this article refers to Table 1 in Zhou (2022, Infectious diseases of poverty: progress achieved during the decade gone and perspectives for the future. Infectious Diseases of Poverty 11, 1), in which it is indicated thatParagonimusspecies, like many other foodborne trematodes, are ancient pathogens that are also re-emerging to cause disease in modern times. This article provides a general overview ofParagonimusspecies and the disease they cause. This is followed by comments on several specific topics of current interest: taxonomy and distribution of members of the genus; details of the life cycle; global and regional prevalence of paragonimiasis; genomics of lung flukes and possible effects of global environmental change. Unresolved questions relating to these topics are discussed and gaps in knowledge identified.
Reconstruction in left main coronary artery atresia with bypass graft obstruction
Authors: Miwa Koji , Iwai Shigemitsu , Nagashima Toshiaki 
Published: March 2022

AbstractPaediatric coronary artery bypass surgery with internal thoracic artery grafting is the optimal choice for left main coronary artery atresia; we report successful reconstruction in a patient with bypass graft obstruction. The pulmonary trunk was transected to expose the left main coronary stem, which was opened beyond the obstruction and the incision extended through the left main coronary artery to the circumflex bifurcation and left anterior descending artery. A funnel-shaped coronary ostium was created with a glutaraldehyde-treated autologous pericardium onlay patch. Surgical reconstruction is a good alternative for left main coronary artery atresia with graft obstruction and preserves the remaining internal thoracic artery for future use.
Analysis of Disaster Medical Response: The Sejong Hospital Fire
Authors: Choi Daihai , Lim Jangsun , Cha Myeong-Il , Choi Changshin , Woo Seungyoul , Jeong Seongmi , Hwang Seong Youn , Kim Inbyung , Yang Heebum 
Published: March 2022

AbstractThis paper provides a field report on a fire that broke out on January 26, 2018 at Sejong Hospital in Miryang, South Korea, engendering the establishment of a committee to investigate the hospital fire response. This field report analyzes the disaster medical response. The official records of the disaster response from each institution were examined. On-site surveys were conducted through interviews with government officials and other health care workers regarding communication during the disaster response without using a separate questionnaire. All medical records were abstracted from hospital charts. There were 192 casualties: 47 victims died, seven were seriously injured, and 121 suffered minor injuries. Emergency Medical Services (EMS) arrived three minutes after the fire started, while news of the fire reached the National Emergency Medicine Operation Center based in Seoul in 12 minutes. The first disaster medical assistance team (DMAT) was dispatched 63 minutes after the National Emergency Medicine Operation Center was notified. The disaster response was generally conducted in accordance with disaster medical support manuals; however, these response manuals need to be improved. Close cooperation among various institutions, including nearby community public health centers, hospitals, fire departments, and DMATs, is necessary. The response manuals should be revised for back-up institutions, as the relevant information is currently incomplete.
A cognitive behavioural therapy smartphone app for adolescent depression and anxiety: co-design of ClearlyMe
Authors: Li S.H. , Achilles M.R. , Spanos S. , Habak S. , Werner-Seidler A. , O’Dea B. 
Published: March 2022

Abstract
Adolescence is associated with heightened vulnerability to symptoms of depression and anxiety. In-person and computerised cognitive behavioural therapy (CBT) are effective treatment options, yet uptake and engagement remain low. Smartphone delivery of CBT offers an alternative, highly accessible method of delivering CBT. However, there is no freely available CBT smartphone application (app) specifically designed to reduce depression and anxiety symptoms in adolescents. The aim of this study was to design a new CBT smartphone app (ClearlyMe) that targets depressive and anxiety symptoms in adolescents. We engaged in a rigorous co-design process with adolescents (n=36), parents (n=15), and mental health professionals (n=32). Co-design involved: (1) discovery of users’ needs, views and preferences by conducting focus groups, (2) defining app features through ideation workshops and user consultations, (3) designing therapeutic CBT content and visual features, and (4) testing prototypes. Users were involved at every step and the process was iterative, with findings carried forward to ensure continued refinement of concepts and features. We found a preference for vibrant, cheerful colours and illustrations and non-endorsement of gamification and chatbots, which contrasted with findings from other studies. Preferences were largely consistent between the three user groups. However, adolescents preferred an app that could be used autonomously without professional support, whereas mental health professionals desired a product for use as a therapy adjunct to support CBT skill development. The importance of co-design, and particularly the inclusion of all stakeholders throughout the entire co-design process, is discussed in relation to the design of ClearlyMe.

Key learning aims

(1)
To understand the co-design process that underpins the development of a new CBT smartphone app for youth with elevated symptoms of depression and anxiety.

(2)
To understand adolescent, parent and mental health professionals’ key preferences regarding the features and functionality of a CBT smartphone app for adolescents with elevated symptoms of depression and anxiety.

(3)
To understand how ClearlyMe has been designed as both a therapy adjunct and stand-alone program, and how it can be incorporated into day-to-day clinical practice.
The 2018–2020 Multi‐Year Drought Sets a New Benchmark in Europe
Authors: Rakovec Oldrich , Samaniego Luis , Hari Vittal , Markonis Yannis , Moravec Vojtěch , Thober Stephan , Hanel Martin , Kumar Rohini 
Published: March 2022

AbstractDuring the period 2018–2020, Europe experienced a series of hot and dry weather conditions with significant socioeconomic and environmental consequences. Yet, the extremity of these multi‐year dry conditions is not recognized. Here, we provide a comprehensive spatio‐temporal assessment of the drought hazard over Europe by benchmarking past exceptional events during the period from 1766 to 2020. We identified the 2018–2020 drought event as a new benchmark having an unprecedented intensity that persisted for more than 2 years, exhibiting a mean areal coverage of 35.6% and an average duration of 12.2 months. What makes this event truly exceptional compared with past events is its near‐surface air temperature anomaly reaching +2.8 K, which constitutes a further evidence that the ongoing global warming is exacerbating present drought events. Furthermore, future events based on climate model simulations Coupled Model Intercomparison Project v5 suggest that Europe should be prepared for events of comparable intensity as the 2018–2020 event but with durations longer than any of those experienced in the last 250 years. Our study thus emphasizes the urgent need for adaption and mitigation strategies to cope with such multi‐year drought events across Europe.
Seismic Volcanostratigraphy: The Key to Resolving the Jan Mayen Microcontinent and Iceland Plateau Rift Evolution
Authors: Blischke Anett , Brandsdóttir Bryndís , Stoker Martyn S. , Gaina Carmen , Erlendsson Ögmundur , Tegner Christian , Halldórsson Sæmundur A. , Helgadóttir Helga M. , Gautason Bjarni , Planke Sverre , Koppers Anthony A. P. , Hopper John R. 
Published: March 2022

AbstractVolcanostratigraphic and igneous province mapping of the Jan Mayen microcontinent (JMMC) and Iceland Plateau Rift (IPR) region have provided new insight into the development of rift systems during breakup processes. The microcontinent's formation involved two breakup events associated with seven distinct tectono‐magmatic phases (∼63–21 Ma), resulting in a fan‐shaped JMMC‐IPR igneous domain. Primary structural trends and anomalous magmatic activity guided initial opening (∼63–56 Ma) along a SE‐NW trend from the European margin and along a WNW‐ESE trend from East Greenland. The eastern margin of the microcontinent formed during the first breakup (∼55–53 Ma), with voluminous subaerial volcanism and emplacement of multiple sets of SSW–NNE‐aligned seaward‐dipping reflector sequences. The more gradual, second breakup (∼52–23 Ma) consisted of four northwestward migrating IPR (I–IV) rift zones along the microcontinent's southern and western margins. IPR I and II (∼52–36 Ma) migrated obliquely into East Greenland, interlinked via segments of the Iceland‐Faroe Fracture Zone, in overlapping sub‐aerial and sub‐surface igneous formations. IPR III and IV (∼35–23 Ma) formed a wide igneous domain south and west of the microcontinent, accompanied by uplift, regional tilting, and erosion as the area moved closer to the Iceland hotspot. The proto‐Kolbeinsey Ridge formed at ∼22–21 Ma and connected to the Reykjanes Ridge via the Northwest Iceland Rift Zone, near the center of the hotspot. Eastward rift transfers, toward the proto‐Iceland hotspot, commenced at ∼15 Ma, marking the initiation of segmented rift zones comparable to present‐day Iceland.
Measurement and Scaling of Lake Surface Skin Temperatures
Authors: Hondzo Miki , You Jiaqi , Taylor Jackie , Bartlet Garret , Voller Vaughan R. 
Published: March 2022

AbstractWater temperature microprofiles at the air‐water interface of a stratified lake were measured concurrently with moderate wind speeds of 0.8–8.2 ms−1 above the lake surface. The day‐time measurements revealed the cool skin effect of water surface temperatures that triggers the cooling of the lake surface and the occurrence of natural convection. Natural convection velocity scale mediates the thickness of the diffusive thermal sublayer and the corresponding net heat flux at the interface. The diffusive thermal sublayer thickness ranged from 0.7 to 3.6 mm. The temperature microprofiles and proposed parameterization of skin‐to‐bulk temperatures enable similarity scaling of temperature microprofiles over the diffusive thermal sublayer thickness. The proposed parameterizations allow for the estimation of diffusive thermal sublayer thickness and skin‐to‐bulk temperature difference in the presence of natural convection. Our results have the potential to facilitate the validation and integration of satellite‐derived lake surface temperatures.
The Most Intense Deflation of the Last Two Decades at Mt. Etna: The 2019–2021 Evolution of Ground Deformation and Modeled Pressure Sources
Authors: Bruno V. , Aloisi M. , Gambino S. , Mattia M. , Ferlito C. , Rossi M. 
Published: March 2022

AbstractWe analyze Global Navigation Satellite System (GNSS) and tilt data from the permanent monitoring networks of Etna volcano starting just after the 24 December 2018 eruption to an unusual two‐month period of deflation in February–March, 2021, which coincided with the occurrence of 17 lava fountain episodes. Based on changes in slope in the GNSS displacement time series, we divide the period starting 7 months after the eruption into five phases, spanning the continued inflation of the edifice punctuated by short periods of effusive and strombolian activity (four phases) and a 2‐month phase of intensive deflation. Our model indicates a progressive deepening of the internal pressure sources followed by a fast ascending source starting two‐months before the first 2021 paroxysms. We explain these results in light of a recent volcanological model on the nature and behavior of magma ascending through the Etnean feeding system.
Exospheric Temperature Measured by NASA‐GOLD Under Low Solar Activity: Comparison With Other Data Sets
Authors: Park Jaeheung , Evans Joseph S. , Eastes Richard W. , Lumpe Jerry D. , van den Ijssel Jose , Englert Christoph R. , Stevens Michael H. 
Published: March 2022

AbstractExospheric temperature is one of the key parameters in constructing thermospheric models and has been extensively studied with in situ observations and remote sensing. The Global‐scale Observations of the Limb and Disk (GOLD) at a geosynchronous vantage point provides dayglow limb images for two longitude sectors, from which we can estimate the terrestrial exospheric temperature since 2018. In this paper, we investigate climatological behavior of the exospheric temperature measured by GOLD. The temperature has positive correlations with solar and geomagnetic activity and exhibits a morning‐afternoon asymmetry, both of which agree with previous studies. We have found that the arithmetic sum of F10.7 (solar) and Ap (geomagnetic) indices is highly correlated with the exospheric temperature, explaining ∼64% of the day‐to‐day variability. Furthermore, the exospheric temperature has good correlation with thermospheric parameters (e.g., neutral temperature, O2 density, and NO emission index) sampled at various heights above ∼130 km, in spite of the well‐known thermal gradient below ∼200 km. However, thermospheric temperature at altitudes around 100 km is not well correlated with the GOLD exospheric temperature. The result implies that effects other than thermospheric heating by solar Extreme Ultraviolet and geomagnetic activity take control below a threshold altitude that exists between ∼100 and ∼130 km.
Surface‐Wave Tomography of the Central‐Western Mediterranean: New Insights Into the Liguro‐Provençal and Tyrrhenian Basins
Authors: Magrini Fabrizio , Diaferia Giovanni , El‐Sharkawy Amr , Cammarano Fabio , van der Meijde Mark , Meier Thomas , Boschi Lapo 
Published: March 2022

AbstractThe complex tectonic setting of the central‐western Mediterranean has interested geoscientists for decades, but its geodynamic evolution remains a matter of debate. We rely on 807 seismometers from southern Europe and northern Africa to measure Rayleigh and Love phase velocities in the period range ∼5–200 s, based on teleseismic earthquakes and seismic ambient noise. By nonlinear joint inversion of the phase‐velocity maps, we obtain a 3‐D shear‐wave velocity (VS) model of the study area. At shallow depths, our model correlates with surface geology and reveals the presence of a sedimentary cover in the Liguro‐Provençal basin, as opposed to the Tyrrhenian basin where this is either very thin or absent. At ∼5‐km depth, high velocities below the Magnaghi, Vavilov, and Marsili seamounts point to an exhumed, scarcely serpentinized mantle. These are replaced by lower velocities at larger depths, likely connected to the presence of partial melt. At 50–60‐km depth, a very heterogeneous structure characterizes the Tyrrhenian basin, with low velocities pointing to the presence of fluids due to the lateral mantle inflow from the Ionian slab edges, and higher velocities associated with a relatively dry upper mantle. Such heterogeneity disappears at depths ≳75 km, replaced by more uniform velocities which are ∼2% lower than those found in the Liguro‐Provençal basin. We infer that, at the same depths, the Tyrrhenian basin is characterized by a larger concentration of fluids and possibly higher temperatures.
Boreal Summer Negative Correlation Relationship Between Interannual SST and Precipitation Anomalies in the Tropical and Subtropical Western North Pacific
Authors: Xue Wei , Sun Xuguang , Yang Xiu‐Qun 
Published: March 2022

AbstractWestern North Pacific (WNP) is a key region for ENSO development and its effect on East Asian summer monsoon. Different from most other tropical oceanic areas, sea surface temperature (SST) and precipitation anomalies over the WNP are negatively correlated in boreal summer, indicating the ocean is mainly driven by the atmosphere rather than the opposite over there. Two interannual variability modes of such negative correlation relationship are revealed with SVD method, called tropical and subtropical WNP air‐sea coupled modes (WNP‐TCM and WNP‐STCM) in terms of their locations accordingly. Their core regions are both consistent with the near‐zero line of low‐level zonal wind, corresponding to the Northwest Pacific monsoon trough and the west ridge of WNP subtropical high, respectively. In WNP‐TCM, precipitation anomaly is caused by local vorticity anomaly, which is the result of Matsuno‐Gill response to SST anomalies with the reversed signs in central equatorial Pacific and eastern equatorial Indian Ocean. In WNP‐STCM, it is produced by local divergence anomaly, which is remotely forced by SST anomalies with the same signs in equatorial Pacific and Indian Ocean through anomalous Hadley circulation. SST anomalies in the two modes are both controlled by ocean thermal process, especially the solar radiation anomaly. The key factors determining such unique WNP air‐sea interaction are the weak latent heat flux and horizontal SST advection anomalies, which are both closely related to the near‐zero low‐level zonal wind. In addition, WNP‐TCM often happens in ENSO developing summer whereas WNP‐STCM usually appears in ENSO decaying summer.
Observational Characteristics of Wintertime Extreme Surface Turbulent Heat Flux Events in the North Pacific Subtropical Region
Authors: Huang Jing , Zhang Yang , Hu Haibo , Yang Xiu‐Qun , Ren Xuejuan 
Published: March 2022

AbstractSurface turbulent heat flux is the most direct variable denoting air‐sea interactions. In wintertime North Pacific, in addition to the Kuroshio‐Oyashio extension (KOE) region, high‐resolution observations show that the North Pacific subtropical region (NPSR) is also characterized with high surface heat flux, whose characteristics need systematic investigation. In this study, the extreme surface turbulent heat flux events in the NPSR are investigated using daily observational data. Our results show that the extreme events exhibit dipolar changes of surface flux over NPSR and KOE regions, lasting for several days. Though with a spatially correlated pattern, the occurrence of extreme events in NPSR and KOE is found greatly independent. In the extreme events, both surface sensible and latent heat fluxes display evident changes in north NPSR, while in south NPSR the change in surface latent heat flux dominates. The formation of extreme events in the NPSR is mainly determined by anomalous atmospheric circulation. Changes in the intensity of subtropical high influence the surface air wind speed, humidity, and temperature, contributing to the formation of extreme events in the NPSR. Our results further suggest that the processes through which the extreme events affect the atmospheric precipitation may be different in south and north NPSR. In south NPSR, the change of precipitation in extreme events is very likely attributed to the change of surface latent heat flux. In north NPSR, the change of water vapor transport by atmospheric circulations is found to play a major role.
Four Year Study of the Schumann Resonance Regular Variations Using the Sierra Nevada Station Ground‐Based Magnetometers
Authors: Rodríguez‐Camacho J. , Salinas A. , Carrión M. C. , Portí J. , Fornieles‐Callejón J. , Toledo‐Redondo S. 
Published: March 2022

AbstractWe present a study of the Schumann resonance (SR) regular variations (March 2013–February 2017) using the ground‐based magnetometers from the Sierra Nevada station, Spain (37°02′N, 3°19′W). The study is based on the fitting parameters obtained by the Lorentzian fit, calculated for each 10‐min interval record, namely, peak amplitudes, peak frequencies, width of the resonances, and the power spectrum integral for the first three SR modes. We consider three time‐scales in the study: seasonal, monthly, and daily variations. The processed data collected by the Sierra Nevada station are also made public with this work. The general characteristics of the long‐term evolution of the SR are confirmed, but discrepancies appear that require further study comparing recent measurements from different stations. Signatures of the influences of the El Niño phenomenon and the solar cycle to SR have been found.
What Determine the Performance of the ENSO‐East Asian Winter Monsoon Relationship in CMIP6 Models?
Authors: Wang Zhenzhen , Wu Renguang , Gong Hainan , Jia XiaoJing , Dai Panxi 
Published: March 2022

AbstractThis study evaluates the relationship between El Niño‐Southern Oscillation (ENSO) and the East Asian winter monsoon (EAWM) in 26 Coupled Model Intercomparison Project Phase 6 (CMIP6) models. Of particular concern is the plausible factors for the model's capability of simulating the ENSO‐EAWM relationship. Results show that the model's ability of simulating the ENSO‐EAWM relationship is more dependent upon the longitudinal extension of ENSO‐related equatorial Pacific sea surface temperature (SST) anomalies than the amplitude of the equatorial central‐eastern Pacific SST anomalies. The influence of the amplitude of ENSO on the simulation of the ENSO‐EAWM relationship depends on the westward extension of ENSO‐related equatorial Pacific SST anomalies. Another factor for the model's ability of simulating the ENSO‐EAWM relationship is the SST anomalies in the tropical western North Pacific (WNP). A westward extension of the equatorial Pacific SST anomalies shifts the west branch of anomalous Walker circulation too far westward, which causes westward displaced anomalous ascending (descending) motion around the Philippines through modulating regional meridional vertical circulation in El Niño (La Niña) years. The weak SST anomalies in the tropical WNP lead to the failure of inducing anomalous lower‐level anticyclone (cyclone) over the Philippine Sea through a Rossby wave response in El Niño (La Niña) years. The accompanying weak anomalous lower‐level southwesterly (northeasterly) winds along the west flank of the anomalous anticyclone (cyclone) account for the weak ENSO‐EAWM relationship.