bluuebunny/crossref_metadata_2025_split huggingface dataset:
Physically Consistent Responses of the Global Atmospheric Hydrological Cycle in Models and Observations
Authors: Allan Richard P. , Liu Chunlei , Zahn Matthias , Lavers David A. , Koukouvagias Evgenios , Bodas-Salcedo Alejandro 
Published: January 2013

Abstract
Robust and physically understandable responses of the global atmospheric water cycle to a warming climate are presented. By considering interannual responses to changes in surface temperature (T), observations and AMIP5 simulations agree on an increase in column integrated water vapor at the rate 7 %/K (in line with the Clausius–Clapeyron equation) and of precipitation at the rate 2–3 %/K (in line with energetic constraints). Using simple and complex climate models, we demonstrate that radiative forcing by greenhouse gases is currently suppressing global precipitation (P) at ∼−0.15 %/decade. Along with natural variability, this can explain why observed trends in global P over the period 1988−2008 are close to zero. Regional responses in the global water cycle are strongly constrained by changes in moisture fluxes. Model simulations show an increased moisture flux into the tropical wet region at 900 hPa and an enhanced outflow (of smaller magnitude) at around 600 hPa with warming. Moisture transport explains an increase in P in the wet tropical regions and small or negative changes in the dry regions of the subtropics in CMIP5 simulations of a warming climate. For AMIP5 simulations and satellite observations, the heaviest 5-day rainfall totals increase in intensity at ∼15 %/K over the ocean with reductions at all percentiles over land. The climate change response in CMIP5 simulations shows consistent increases in P over ocean and land for the highest intensities, close to the Clausius−Clapeyron scaling of 7 %/K, while P declines for the lowest percentiles, indicating that interannual variability over land may not be a good proxy for climate change. The local changes in precipitation and its extremes are highly dependent upon small shifts in the large-scale atmospheric circulation and regional feedbacks.
How Do Partners Find out About the Risk of Huntington's Disease in Couple Relationships?
Authors: Keenan Karen Forrest , Simpson Sheila A. , Miedzybrodzka Zosia , Alexander David A. , Semper June 
Published: January 2013

AbstractWhilst a growing body of work has explored family communication about Huntington's disease and how at‐risk individuals learn about their risk, the experience of telling a partner and partners’ experiences of finding out about this potentially devastating hereditary illness have received little attention. This study describes the experiences of partners in finding out about Huntington's disease and any impact on couple's relationships/marriages. We undertook a thematic analysis of qualitative interviews which explored the dynamics of partners’ marriages after predictive testing and partners’ views of genetic counseling. A main theme from partners’ accounts was how they found out about their spouse's risk of Huntington's disease and the impact this had on marital relations. The analysis revealed four types of disclosure experiences: (1) marital secrets; (2) alerting, but not telling; (3) knowing and seeing; (4) marital ignorance. Our findings demonstrate that partners’ experiences of (non)disclosure about the risk of HD within marriages is an important factor which contributes to couples’ coping or marital problems. Exploring how spouses found out about their partner's risk of HD will illuminate issues about a couple's past and future patterns of communication and their coping strategies. A practical and ethical implication is the extent to which genetic counselors should inform partners about the course and nature of Huntington's disease when a partner is the support person for the individual being tested.
Development of the tibiofemoral angle in a cohort of Nigerian children during the first 3 years of life
Authors: Oyewole Olufemi O. , Akinpelu Aderonke O. , Odole Adesola C. 
Published: January 2013

Purpose Findings from cross-sectional studies of knee angle development in Nigerian children vary in values and in the age at which the varus angle changes to the valgus angle. This study was conducted to describe knee angle development and to determine the age when the knee angle changes from the varus to the valgus angle. Methods This was a longitudinal survey of 152 Nigerian children recruited within 3 weeks of life and followed up monthly until age 3 years. Their knee angle was measured using clinical methods. Results The mean tibio-femoral/varus knee angle (13.2 ± 3.8°) at birth–3 weeks of life decreased sharply to 5.6 ± 0.7° at 9 months, increased slightly to 6.3 ± 1.1° at 13 months, and then decreased again up to age 18 months (0.3 ± 2.1°). The mean valgus knee angle increased from −2.4 ± 2.5° at 19 months of life to −8.5 ± 2.5° at 27 months and then decreased to −7.7 ± 2.2° at 36 months. Intercondylar/intermalleolar distances (ICD/IMD) showed a similar pattern, changing from an extreme varus knee (ICD) at birth–3 weeks of life (2.5 ± 0.7 cm), decreasing to 0.6 ± 0.2 cm at 9 months, increasing to 0.8 ± 0.5 cm at 12 months, and decreasing to 0.1 ± 0.4 cm at 15 months. The mean IMD increased from −0.1 ± 0.8 cm at 16 months of life to −2.0 ± 1.5 cm at 29 months and then decreased up to 36 months. Our tri-modal analysis showed that the transition from the varus to the valgus angle was between 18 and 19 months. Conclusion Our findings suggest that the developmental pattern of the knee angle in Nigerian children is at maximal varus at birth, neutral at 18 months of life, and valgus at 19 months, with the valgus angle continuing to increase up to 36 months.
Endometrial ablation for the treatment of heavy menstrual bleeding in obese women
Authors: Madsen Annetta M. , El‐Nashar Sherif A. , Hopkins Matthew R. , Khan Zaraq , Famuyide Abimbola O. 
Published: January 2013

AbstractObjectiveTo compare the efficacy and safety of endometrial ablation (EA) among obese versus non‐obese women.MethodsA retrospective cohort study of 666 women who underwent EA at the Mayo Clinic, Rochester, USA, between January 1, 1998, and December 31, 2005, was conducted. Obesity was defined as a body mass index (BMI, calculated as weight in kilograms divided by the square of height in meters) of 30 or above. Outcome measures included treatment failure and amenorrhea. Regression models were used to compare outcomes and adjust for known confounders.ResultsThe mean BMI was 29.6 ± 7.7; 263 women (39.5%) were classified as obese. No difference was observed in treatment failure at 5 years between the obese and non‐obese cohorts (11.6% vs 9.7%) with an adjusted hazard ratio of 0.96 (95% confidence interval [CI], 0.60–1.53; P = 0.878). The crude 12‐month amenorrhea rate was higher among non‐obese than obese women (24.3% vs 17.5%); however, this difference was not significant after adjusting for known predictors of amenorrhea. The odds ratio was 1.28 (95% CI, 0.75–2.19; P = 0.366). Adverse events were rare and comparable between the cohorts.ConclusionThe use of EA is a safe and effective option for women with obesity.
Chloritoid in the bottom sediments of the Akademichesky Ridge of Lake Baikal, an indicator of eolian transportation
Authors: Vologina E.G. , Fedotov A.P. 
Published: January 2013

Abstract
We present results of study of Holocene and Late Pleistocene deposits recovered on the underwater Akademichesky Ridge in Lake Baikal. The change in mineral composition and grain size in the bottom sediment core is closely consistent with the change of major diatom complexes marking the Holocene–Late Pleistocene boundary. A high content of chloritoid (up to 14.6%) has been found among the heavy minerals of the sand fraction of Late Pleistocene clays. The concentration of chloritoid in Holocene mud is no higher than 1.2%. The source of chloritoid is chloritoid shales of the Anaya Formation (Upper Proterozoic), widespread in the watershed of the Primorsky Ridge in the upper reaches of the Lena and Anaya Rivers. Chloritoid was transported to the area of the Akademichesky Ridge by predominant western and northwestern winds, which is also evidenced from the absence of mechanical impacts on the surface of its grains. The high contents of chloritoid in the Late Pleistocene sediments are due to the more intense eolian transportation at that time as compared with the Holocene.
Hydrocarbon migration in the Zagros Basin, offshore Iran, for understanding the fluid flow in the Oligocene–Miocene carbonate reservoirs
Authors: Shariatinia Z. , Haghighi M. , Feiznia S. , Alizai A.H. , Levresse G. 
Published: January 2013

AbstractKuh-e Mond Field is a conventional heavy oil resource in the Zagros foreland Basin, Iran, produced from the fractured carbonates partially filled by dolomite, calcite, and anhydrite cement. Vitrinite reflectance data from carbonate reservoir suggest low-maturation levels corresponding to paleotemperatures as low as 50 °C. The observed maturation level (&lt;0.5% Rmax) does not exceed values for simple burial maturation based on the estimated burial history. Oil inclusions within fracture-filled calcite and dolomite cement indicate the key role of these fractures in oil migration.The fluid inclusion temperature profiles constructed from the available data revealed the occurrence of petroleum in dolomite, calcite, and anhydrite and characterize the distinct variations in the homogenization temperatures (Th). Fluid inclusions in syntectonic calcite veins homogenize between 22 °C and 90 °C, showing a salinity decrease from 22 to 18 eq. wt.% NaCl. Fluid inclusions in anhydrite homogenize at &lt;50 °C, showing that the pore fluids became warmer and more saline during burial. The Th range in the calcite-dolomite cement depicts a change in water composition; therefore, we infer these cements precipitated from petroleum-derived fluids. The microthermometry data on the petroleum fluid inclusions suggest that the reservoir was filled with heavy black oils and high-salinity waters and indicate that undersaturated oil was present in a hydrostatically pressured reservoir.The Th data do not support vertical migration of hot fluids througout the section, but extensive lateral fluid migration, most likely, drove tectonically dewatering in the south or west of the pool.
Distortions of impedance and tipper tensors due to three-dimensional perturbations of the earth and field
Authors: Plotkin V.V. 
Published: January 2013

Abstract
Magnetotelluric (MT) sounding measurements are conducted, as a rule, along a single profile or mutiple profiles, and data are interpreted using 1D and 2D earth models. In a real situation, the earth is three-dimensional, and the primary field may vary laterally. This implies that 1D and 2D inversions of MT data contain some error, up to the appearance of false structures. In this study, analytical methods are used to obtain expressions for the effect of small deviations of the earth and the primary field from the Tikhonov–Cagniard model on the impedance and tipper tensor components (sensitivity functions which determining the size of the zone near the sounding point within which the perturbations affect the impedance and tipper at this point).
Chemical Cold Packs May Provide Insufficient Enthalpy Change for Treatment of Hyperthermia
Authors: Phan Samson , Lissoway John , Lipman Grant S. 
Published: January 2013

Objective Heat illness is a common ailment that, if left untreated, is associated with high morbidity and mortality. Chemical cold packs (CCPs) and ice packs are widely used in the pre-hospital setting and by those with limited resources, yet no controlled studies have compared the cooling of ice to that of CCPs. This study determined the theoretical cooling of CCPs on a benchtop model, comparing the results to similarly sized ice packs, and is the first known comparison of these hyperthermia treatments. Methods The CCPs used in Stanford University's Emergency Department were activated in an insulated volume of water (2 L), and temperature was recorded at 1-second intervals in a controlled environment (41°C at 20% humidity). The procedure was repeated with 1-quart ice packs. Results The CCPs resulted in a 5.25°C degree temperature drop, with a time constant (time to 63% of initial temperature—a common engineering characterization metric) of 1.72 minutes for the test volume. Ice packs resulted on average in a 19.8°C temperature change, with a time constant of 26.8 minutes. The CCPs provide less overall temperature change and were shorter lived. Application of 6 CCPs on a 50th percentile male (weight 86.6 kg, height 1.7 m), assuming ideal heat transfer, would result in less than 0.5°C temperature change. Similarly configured ice packs would result in a 2.5°C change. Conclusions Experiments demonstrate that CCPs are inferior to similarly sized ice packs for thermal regulation, and lose their effectiveness more quickly. These findings support the consideration of ice packs as an alternative to chemical cold packs when cooling hyperthermic patients.
Interphasial energy transfer and particle dissipation in particle-laden wall turbulence
Authors: Zhao Lihao , Andersson Helge I. , Gillissen Jurriaan J. J. 
Published: January 2013

AbstractTransfer of mechanical energy between solid spherical particles and a Newtonian carrier fluid has been explored in two-way coupled direct numerical simulations of turbulent channel flow. The inertial particles have been treated as individual point particles in a Lagrangian framework and their feedback on the fluid phase has been incorporated in the Navier–Stokes equations. At sufficiently large particle response times the Reynolds shear stress and the turbulence intensities in the spanwise and wall-normal directions were attenuated whereas the velocity fluctuations were augmented in the streamwise direction. The physical mechanisms involved in the particle–fluid interactions were analysed in detail, and it was observed that the fluid transferred energy to the particles in the core region of the channel whereas the fluid received kinetic energy from the particles in the wall region. A local imbalance in the work performed by the particles on the fluid and the work exerted by the fluid on the particles was observed. This imbalance gave rise to a particle-induced energy dissipation which represents a loss of mechanical energy from the fluid–particle suspension. An independent examination of the work associated with the different directional components of the Stokes force revealed that the dominating energy transfer was associated with the streamwise component. Both the mean and fluctuating parts of the Stokes force promoted streamwise fluctuations in the near-wall region. The kinetic energy associated with the cross-sectional velocity components was damped due to work done by the particles, and the energy was dissipated rather than recovered as particle kinetic energy. Componentwise scatter plots of the instantaneous velocity versus the instantaneous slip-velocity provided further insight into the energy transfer mechanisms, and the observed modulations of the flow field could thereby be explained.
Turbulence in transient channel flow
Authors: He S. , Seddighi M. 
Published: January 2013

AbstractDirect numerical simulations (DNS) are performed of a transient channel flow following a rapid increase of flow rate from an initially turbulent flow. It is shown that a low-Reynolds-number turbulent flow can undergo a process of transition that resembles the laminar–turbulent transition. In response to the rapid increase of flow rate, the flow does not progressively evolve from the initial turbulent structure to a new one, but undergoes a process involving three distinct phases (pre-transition, transition and fully turbulent) that are equivalent to the three regions of the boundary layer bypass transition, namely, the buffeted laminar flow, the intermittent flow and the fully turbulent flow regions. This transient channel flow represents an alternative bypass transition scenario to the free-stream-turbulence (FST) induced transition, whereby the initial flow serving as the disturbance is a low-Reynolds-number turbulent wall shear flow with pre-existing streaky structures. The flow nevertheless undergoes a ‘receptivity’ process during which the initial structures are modulated by a time-developing boundary layer, forming streaks of apparently specific favourable spacing (of about double the new boundary layer thickness) which are elongated streamwise during the pre-transitional period. The structures are stable and the flow is laminar-like initially; but later in the transitional phase, localized turbulent spots are generated which grow spatially, merge with each other and eventually occupy the entire wall surfaces when the flow becomes fully turbulent. It appears that the presence of the initial turbulent structures does not promote early transition when compared with boundary layer transition of similar FST intensity. New turbulent structures first appear at high wavenumbers extending into a lower-wavenumber spectrum later as turbulent spots grow and join together. In line with the transient energy growth theory, the maximum turbulent kinetic energy in the pre-transitional phase grows linearly but only in terms of${u}^{\ensuremath{\prime} } $, whilst${v}^{\ensuremath{\prime} } $and${w}^{\ensuremath{\prime} } $remain essentially unchanged. The energy production and dissipation rates are very low at this stage despite the high level of ${u}^{\ensuremath{\prime} } $. The pressure–strain term remains unchanged at that time, but increases rapidly later during transition along with the generation of turbulent spots, hence providing an unambiguous measure for the onset of transition.
Estimating wall-shear-stress fluctuations given an outer region input
Authors: Mathis Romain , Marusic Ivan , Chernyshenko Sergei I. , Hutchins Nicholas 
Published: January 2013

AbstractA model for the instantaneous wall-shear-stress distribution is presented for zero-pressure-gradient turbulent boundary layers. The model, based on empirical and theoretical considerations, is able to reconstruct a statistically representative fluctuating wall-shear-stress time-series,${ \tau }_{w}^{\ensuremath{\prime} } (t)$, using only the low-frequency content of the streamwise velocity measured in the logarithmic region, away from the wall. Results, including spectra and second-order moments, show that the model is capable of successfully capturing Reynolds number trends as observed in other studies.
Tidal conversion and turbulence at a model ridge: direct and large eddy simulations
Authors: Rapaka Narsimha R. , Gayen Bishakhdatta , Sarkar Sutanu 
Published: January 2013

AbstractDirect and large eddy simulations are performed to study the internal waves generated by the oscillation of a barotropic tide over a model ridge of triangular shape. The objective is to go beyond linear theory and assess the role of nonlinear interactions including turbulence in situations with low tidal excursion number. The criticality parameter, defined as the ratio of the topographic slope to the characteristic slope of the tidal rays, is varied from subcritical to supercritical values. The barotropic tidal forcing is also systematically increased. Numerical results of the energy conversion are compared with linear theory and, in laminar flow at low forcing, they agree well in subcritical and supercritical cases but not at critical slope angle. In critical and supercritical cases with higher forcing, there are convective overturns, turbulence and significant reduction (as much as 25 %) of the radiated wave flux with respect to laminar flow results. Analysis of the baroclinic energy budget and spatial modal analysis are performed to understand the reduction. The near-bottom velocity is intensified at critical angle slope leading to a radiated internal wave beam as well as an upslope bore of cold water with a thermal front. In the critical case, the entire slope has turbulence while, in the supercritical case, turbulence originates near the top of the topography where the slope angle transitions through the critical value. The phase dependence of turbulence within a tidal cycle is examined and found to differ substantially between the ridge slope and the ridge top where the beams from the two sides cross.
Dynamic contact angle of a liquid spreading on an unsaturated wettable porous substrate
Authors: Shikhmurzaev Yulii D. , Sprittles James E. 
Published: January 2013

AbstractThe spreading of an incompressible viscous liquid over an isotropic homogeneous unsaturated porous substrate is considered. It is shown that, unlike the dynamic wetting of an impermeable solid substrate, where the dynamic contact angle has to be specified as a boundary condition in terms of the wetting velocity and other flow characteristics, the ‘effective’ dynamic contact angle on an unsaturated porous substrate is completely determined by the requirement of existence of a solution, i.e. the absence of a non-integrable singularity in the spreading fluid’s pressure at the ‘effective’ contact line. The obtained velocity dependence of the ‘effective’ contact angle determines the critical point at which a transition to a different flow regime takes place, where the fluid above the substrate stops spreading whereas the wetting front inside it continues to propagate.
Flow visualization using momentum and energy transport tubes and applications to turbulent flow in wind farms
Authors: Meyers Johan , Meneveau Charles 
Published: January 2013

AbstractAs a generalization of the mass–flux based classical stream tube, the concept of momentum and energy transport tubes is discussed as a flow visualization tool. These transport tubes have the property that no fluxes of momentum or energy exist over their respective tube mantles. As an example application using data from large eddy simulation, such tubes are visualized for the mean-flow structure of turbulent flow in large wind farms, in fully developed wind-turbine-array boundary layers. The three-dimensional organization of energy transport tubes changes considerably when turbine spacings are varied, enabling the visualization of the path taken by the kinetic energy flux that is ultimately available at any given turbine within the array.
Flexible scraping of viscous fluids
Authors: Seiwert Jacopo , Quéré David , Clanet Christophe 
Published: January 2013

AbstractWe study the thickness ${h}_{d} $ of the liquid film left on a wet surface after scraping it with an elastic wiper (length $L$, rigidity $B$) moved at a velocity $V$. The scraper is clamped vertically at a given distance above the substrate, and ${h}_{d} $ is maximal when the tip of the scraper is just tangent to the surface. We show experimentally and theoretically that this maximum thickness is ${h}_{\mathit{max}} \simeq 0. 33L \mathop{ (\eta V{L}^{2} / B)}\nolimits ^{3/ 4} , $ where $\eta $ is the liquid viscosity. The deposition law is found to be sensitive to the shape of the wiper: the film thickness can also be tuned by using wipers with a permanent curvature, and varying this curvature.