Miracle-dz/UniFAR-FTUs huggingface dataset:
Stock price prediction on Indonesia stock market with the influence of external factors using recurrent neural network with attention mechanism

: In recent years, more businesses and individuals have started to rely on data as their decision-making factor. Past data has been very useful in making the next decision about business activities in many business sectors, such as in investing activities. Many people invest in stocks without capable knowledge to analyze a proper performance of the stocks as there are a lot of factors affecting the value of stocks. To predict the value of the stock close value, deep learning especially recurrent neural network is applicable to predict the stock price. Previous research only involves the stock price data and vanilla recurrent neural network. This research predicts the stock price with the influence of external factors using recurrent neural network with attention mechanism. A block each for LSTM and attention mechanism model is created and can be repeated several times as needed. The AALI stock price data chosen to represent one of the biggest sectors in Indonesia, with 10 external factors related to the stocks. The result shows that the additional method of using external data with feature selection and attention mechanism helps to improve the model performance in predicting the stock prices. With the right combination through tuning the model, a single block
Public Awareness Toward Healthy Life: Sample from Iraqi Community 2020

Background: People must develop a healthy lifestyle to have a longer and healthier life. Objective: to study the Public awareness toward healthy life of Iraqi community, and it relation with some of demographic variables. Method & persons: A cross-sectional study conducted from 20th June – 20th September 2022, through online questionnaire (google form) distributed through any available channels (e-mails, Viber, Chat, Messenger, WhatsApp, Telegram, Facebook groups) Results: Nine hundred and fifty-six Iraqi persons enrolled in this study, with age mean and standard deviation 32.67± 11.954; the highest percentage of participants 589(51.2%) aged ≤ 29 years, females 577(60.4%), currently married 480(50.2%), medical & health field worker 458(47.9%), while all the non- medical persons 498, (52.1%), {students 212(22.2%), government non-medical worker 146(15.3%). most of the participants 812(84.9%) had once to twice brushing their teeth, and 408(42.7%) had sometimes using Dental floss, while 376(39.3%) of them never using dental floss, and only 39(41.1%)of the participant had regular teeth examination also good overall teeth health only in 387(40.5%). Acceptant-lifestyle 767(80.2%), and only 15(1.6%) had food & water intake poor lifestyle, while in overall-checkup the majority had poor overall-checkup 561(58.7%), then acceptable overall checkup 290(30.3%). Conclusion: Most of the participant had acceptance lifestyle in concerned food and water but had poor Overall checkup for vision, teeth, blood pressure, sugar, lipid and Regular doctor checkup in general.
How well does a 1/4° global circulation model simulate large-scale oceanic observations?

Numerical high-resolution ocean general circulation models have experienced a revolutionary development during the last decade. Today they are run globally in realistic configuration with realistic surface boundary forcing. To fully use the results of those models in understanding various aspects of the ocean general circulation and to combine ocean observations with models (state estimation) in a manner consistent with the data and model dynamics, stringent model-data comparisons are a necessary first step. In this paper a quantitative model-data comparison is carried out for the global Parallel Ocean Climate Model (POCM), known also as the Semtner and Chervin model, with nominal lateral resolution of 1/4°. The focus is on various aspects of the simulated large-scale circulation and their relation to the TOPEX/POSEIDON sea surface height (SSH) observations and World Ocean Circulation Experiment (WOCE) hydrography. Comparisons are made for (1) the global mean sea surface circulation and absolute slopes, (2) rms SSH variability and eddy kinetic energy, (3) the simulation of the observed seasonal cycle in SSH, (4) two-dimensional frequency-wavenumber spectra of the large-scale fluctuations, as well as (5) the hydrography for WOCE sections. Recent improvements in external surface forcing fields including daily wind-stress fields and sea surface heat fluxes lead to a significant improvement in the overall agreement of the simulated and observed large-scale mean circulation and its variability. However, simulated amplitudes of variability remain low by about a factor of 2 to 4 over a broad spectral range, including the long wavelengths and periods. Both the causes and consequences of this low variability remain obscure.
An Examination of the Complex Pharmacological Properties of the Non-Selective Opioid Modulator Buprenorphine

The goal of this review is to provide a recent examination of the pharmacodynamics as well as pharmacokinetics, misuse potential, toxicology, and prenatal consequences of buprenorphine. Buprenorphine is currently a Schedule III opioid in the US used for opioid-use disorder (OUD) and as an analgesic. Buprenorphine has high affinity for the mu-opioid receptor (MOR), delta (DOR), and kappa (KOR) and intermediate affinity for the nociceptin (NOR). Buprenorphine’s active metabolite, norbuprenorphine, crosses the blood–brain barrier, is a potent metabolite that attenuates the analgesic effects of buprenorphine due to binding to NOR, and is responsible for the respiratory depressant effects. The area under the concentration curves are very similar for buprenorphine and norbuprenorphine, which indicates that it is important to consider this metabolite. Crowding sourcing has identified a buprenorphine street value (USD 3.95/mg), indicating some non-medical use. There have also been eleven-thousand reports involving buprenorphine and minors (age < 19) at US poison control centers. Prenatal exposure to clinically relevant dosages in rats produces reductions in myelin and increases in depression-like behavior. In conclusion, the pharmacology of this OUD pharmacotherapy including the consequences of prenatal buprenorphine exposure in humans and experimental animals should continue to be carefully evaluated.
Sediments and History of Holocene Transgression, Continental Shelf, Northwest Gulf of Mexico

The continental shelf of the northwest Gulf of Mexico, between the Mexican border and the Mississippi Delta, is a smooth, gently sloping sediment-covered plain interrupted by occasional hills or banks. Many of these banks probably represent the surface expressions of salt domes protruding through the sediment cover. The width to the edge of the shelf at about 65 fathoms ranges from 50 to 130 miles. Drowned barriers relict from lowered sea level are found on the nondepositional part of the shelf. The Holocene (Recent) sediments are divided into marine transgressive basal nearshore sands and shelf facies muds (silty clays and clayey silts). The basal sands are exposed at the surface near the shore line and across almost the entire shelf off the Rio Grande, off east Texas, and off western-most Louisiana. The shelf facies overlies the basal facies off central Texas and off most of Louisiana. The thickness of the Holocene Series is probably less than 20 feet in much of the area where the basal facies has not yet been buried under the shelf facies, but is several hundred feet thick on the shelf in the vicinity of the Mississippi Delta. Texturally about half of the surface sediments are polymodal mixtures of thin overlapping sediment masses deposited on the shelf during different periods of postglacial time. The mixing has been by burrowing organisms and the strong wave surges associated with hurricane waves, the former having produced irregularly interlayered and mottled sands and muds and the latter homogeneously mixed polymodal sediments. The sandy sediments are subarkoses everywhere, except off the central Texas coast where they are orthoquartzites. Some of the sediments contain mixed shallow and deeper shelf faunas. Most of the sand-size particles in the outer shelf silty clays are Foraminifera and fragments of echinoids. Glauconite is locally abundant in the relict basal sands of the outer shelf. The sediments on the shelf are the products of the marine transgression following the Wisconsin glaciation. The chronology of this transgression has been traced back 17,000 years by radiocarbon dates of shells of nearshore organisms. The sequence of events has been interpreted in the light of textural and mineralogical characteristics of the sediments and from the physiography of the drowned barriers of the east Texas shelf area. These ridges, which slope for long distances down the middle and inner shelf at acute angles to the contours, represent barrier spits deposited at the mouths of rivers during brief periods of regression. Two and possibly three periods of temporary regression interrupting the transgression are suggested. One of these, occurring at about the mid-point of the tr nsgression, correlates well with the Two Creeks interstadial and the advance of the Mankato glaciers of North America. The wind pattern appears to have changed during these periods of regression and reversed the current directions in parts of the gulf.
Evolution of lavas in the Late Ordovician/Early Silurian Solund‐Stavfjord Ophiolite Complex, West Norway

The geochemistry of the volcanic sequence of the Late Ordovician/Early Silurian Solund‐Stavfjord Ophiolite Complex (SSOC) of the Western Norwegian Caledonides has been investigated along 12 stratigraphic sections spaced over a lateral distance of ∼60 km. The metabasalts commonly show a cyclic organization, comprising sheet flows followed by pillow lavas and with volcanic breccias at the top of some volcanic units. The proportions of the volcanic rock types vary considerably along‐axis, even within short distances. The robust nature of the sheeted dike complex, the proportion and regional distribution of the various volcanic rocks, the aphyric nature of the metabasalts, as well as the predominance of Fe‐Ti basalts suggest that the SSOC formed at an intermediate to fast spreading ridge, probably within a back‐arc basin. The variations in the concentrations of the incompatible (e.g., Zr) and compatible (e.g., Cr) elements in the lavas are substantial, i.e., from 49–384 ppm and 66–443 ppm, respectively. Nd isotopic ratios show only minor variations, suggesting that the lavas were generated from an isotopically uniform source. The variations in the incompatible elements (represented by Zr) define stratigraphic units ∼25 to 150 m thick, with either gradual decreases or increases in Zr concentrations, while Cr may show different trends. The different Zr‐Cr covariations are interpreted in the light of a numerical model in which fractional crystallization and mixing of various magmas are the principal processes. Through upwardly Zr‐increasing units, Cr generally decreases and estimated magma densities increase, compatible with progressive fractional crystallization. However, through upwardly Zr‐decreasing units, Cr and estimated magma densities either increase or decrease, trends that are attributed to hybridization in frequently replenished magma chambers. Within short lateral distances (<1 km), the geochemical stratigraphy changes dramatically, excluding eruption from a homogeneous, axially continuous magma chamber. Instead, we propose that the volcanic sequence was fed from small, separate magma lenses that evolved independently of each other.
In situ Observation of ilmenite‐perovskite phase transition in MgSiO3 using synchrotron radiation

In situ observations of the ilmenite‐perovskite transition in MgSiO3 were carried out in a multianvil high‐pressure apparatus interfaced with synchrotron radiation. The phase boundary between ilmenite and perovskite in the temperature range of 1300–1600 K was determined to be P (GPa) = 28.4(±0.4) ‐ 0.0029(± 0.0020)T (K) based on Jamieson's equation of state of gold [Jamieson et al., 1982] and P (GPa) = 27.3(±0.4) ‐ 0.0035(±0.0024)T (K) based on Anderson's equation of state of gold [Anderson et al., 1989]. The consistency of our results, using Jamieson's equation of state, with previous studies obtained by quench methods leads us to conclude that the 660 km seismic discontinuity in the mantle can be attributed a phase transition to perovskite phase. However, the phase boundary based on the Anderson's equation of state implies that the depth of the 660‐km seismic discontinuity does not match the pressure of this transition.
Predictable signals of seasonal precipitation in the Yangtze–Huaihe River Valley

An effort is made to identify the ‘more predictable’ signals in seasonal precipitation in the Eastern Yangtze–Huaihe River Valley of China based on the observations recorded for the period of 1951–2004 at a network of 23 stations in this region. A recently developed methodology for decomposing the interannual variance of seasonal mean climate fields is applied to precipitation time series at the stations. This allows the total interannual variance to be separated into the variance of a slow component, or predictable signal, and the variance of a more noisier component of rainfall associated with intraseasonal variability. The potential predictability (signal‐to‐total ratio) is generally moderate in this region and is lower during winter from January to March (JFM) and higher in summer from May to July (MJJ) and autumn from November to January (NDJ). Empirical orthogonal function (EOF) analysis is then applied to the predictable‐, intraseasonal‐ and total‐covariance matrices, respectively. Leading EOF modes of the total component more often resemble the EOF modes of the intraseasonal component when the potential predictability is lower and vice versa. Temporal variation of the leading modes in the predictable components is more closely linked to the interannual variability of Eastern Pacific sea surface temperature (SST) in early summer (MJJ), North Atlantic SST in late summer (JAS) and El Niño/Southern oscillation in late autumn (NDJ). The rainfall SST connections found in these seasons persist throughout the entire 54‐year period. The predictable rainfall modes also have apparent linkages to the intensity and position of the Western Pacific subtropical high during the early summer and late autumn with more rainfall occurring in the region when the height pattern is more intensive and extends further west. During the late summer, the predictable rainfall variability is accompanied by a large variation of tropospheric advection from north of the region, indicating the impact of an anomalous atmospheric circulation associated with the variation of summer North Atlantic Oscillation.
Cytokine-Induced iNOS in A549 Alveolar Epithelial Cells: A Potential Role in COVID-19 Lung Pathology

Background. In COVID-19, an uncontrolled inflammatory response might worsen lung damage, leading to acute respiratory distress syndrome (ARDS). Recent evidence points to the induction of inducible nitric oxide synthase (NOS2/iNOS) as a component of inflammatory response since NOS2 is upregulated in critical COVID-19 patients. Here, we explore the mechanisms underlying the modulation of iNOS expression in human alveolar cells. Methods. A549 WT and IRF1 KO cells were exposed to a conditioned medium of macrophages treated with SARS-CoV-2 spike S1. Additionally, the effect of IFNγ, IL-1β, IL-6, and TNFα, either alone or combined, was addressed. iNOS expression was assessed with RT-qPCR and Western blot. The effect of baricitinib and CAPE, inhibitors of JAK/STAT and NF-kB, respectively, was also investigated. Results. Treatment with a conditioned medium caused a marked induction of iNOS in A549 WT and a weak stimulation in IRF1 KO. IFNγ induced NOS2 and synergistically cooperated with IL-1β and TNFα. The inhibitory pattern of baricitinb and CAPE indicates that cytokines activate both IRF1 and NF-κB through the JAK/STAT1 pathway. Conclusions. Cytokines secreted by S1-activated macrophages markedly induce iNOS, whose expression is suppressed by baricitinib. Our findings sustain the therapeutic efficacy of this drug in COVID-19 since, besides limiting the cytokine storm, it also prevents NOS2 induction.
A theoretical study of the seasonal and solar cycle variations of stable aurora red arcs

SAR arc statistic provide information on the seasonal and solar cycle variations in the subauroral region electron temperature peak and associated magnetospheric energy source. There are two sources of long-term (solar cycle and seasonal) variability in the magnitude of the subauroral region electron temperature peak and associated SAR are emission intensity: (1) the neutral atmosphere and ionosphere and (2) the magnetospheric energy source. The results of this study indicate that the observed seasonal variation in SAR are intensities can be explained reasonably well by seasonal variations in the neutral atmosphere and ionosphere. True solstice effect are unlikely to result from difference in a near-equatorial magnetospheric heat source since the same heat source supplies both the summer and the winter hemispheres at opposite ends of a common flux tube. Observed solar cycle variations in SAR are intensity for a fixed ring current strength (as represented by the D sub st index) are not consistent with variations predicted solely on the basis of a solar cycle changes in the neutral atmosphere and ionosphere. A reduction of the magnetospheric heat flux by a factor of between 5 and 20 from solar maximum to solar minimum conditions is necessary to bring model electron temperaturesmore » and 6300 emission intensity into agreement with observational results for moderately disturbed conditions D sub st approx - 80 gamma. The required reduction in the magnetospheric energy source with decreasing solar cycle is attributed to compositional changes in the magnetospheric plasma. « less
Stratigraphy of the eastern and central United States

This volume discusses stratigraphic sequences in thirty states, listing and describing a great many formations, citing original places of definition and other references, together with synonyms. Fossil lists are given for the more important formations. There are about eighty correlation charts made especially for the book, as well as similar tables taken from other strati-graphic reports, and many state geologic maps. The stratigraphy discussed is chiefly of the Paleozoic formations; however, along the Atlantic Coastal Plain considerable of the well-known Mesozoic and Cenozoic marine history is also presented. The marine Mesozoic formations in the western part of the central states are also described. PART I follows an introductory chapter on stratigraphic terminology. This first main section deals with New York State. PART II covers the eleven states lying across the Appalachian Geosyncline, beginning with Pennsylvania and New Jersey, going across Maryland and Old and Little Virginia, East Tennessee, the western parts of the Caro-linas, Georgia, and northern Alabama, and the small part of Mississippi that shows the Paleozoic formation. PART III deals with the states of the Atlantic Coastal Plain, and completes the geological history of the Appalachian province. The territory covered includes the land beneath the marine waters off the New Eng
Assessing the Amount of Data per Second to Measure Tactical Variables in Team Sports

Sampling frequency of microsensors that measure the position of the players in team sports is a variable that could affect the accuracy of the measurement. The aim of the present study was to assess the impact of the sampling frequency on the measurement of a collective tactical behaviour variable: the total area (TA). Sixteen young U16 male soccer players participated in the study. They carried out three controlled tasks. Tactical variable was measured by a radio ultra-wide band technology (IMU; WIMU PROTM, RealTrack Systems, Almeria, Spain). For TA different sampling frequencies were applied (i.e. 1 Hz, 2 Hz, 4 Hz and 10 Hz). Trivial differences (p 0.05) were found between the TA values across the different amounts of inserted data per second across Task 1 (ES= 0.04-0.08), Task 2 (ES= 0.01-0.09) and Task 3 (ES= -0.03-0.04). Also High to perfect ICCs (0.91-1) and linear correlations (r= 0.961-1; p 0.01) were found among the TA values obtained through all sampling frequencies. The sampling frequency (i.e. 1 Hz, 2 Hz, 4 Hz and 10 Hz) does not affect the measurement of total area during tactical behaviour analysis but does significantly affect the change in centroid position measurement. Thus, it is recommended the use of 1 Hz to measure TA, but further studies should analyse the impact of lower than 1 Hz and greater than 10 Hz sampling frequencies to measure this collective tactical behavior.
A 275-GHz InP HBT H-Band Amplifier With Transmission Line-Based Capacitively Coupled Resonator Matching Technique

This article presents transmission line-based capacitively coupled resonator matching techniques for THz amplifiers and demonstrates the idea in a three-stage differential H-band amplifier in indium phosphide (InP) 250-nm double heterojunction bipolar transistor technology for a general-purpose waveguide gain block. We propose two types of symmetrical capacitively coupled resonator matching circuits with transmission lines, which are effective for replacing low-quality lumped elements at subterahertz frequencies. For high stability and high gain, the cascode topology was optimized with series and shunt interdevice matching circuits. The amplifiers were fabricated in two versions; one with folded rat-race baluns for on-chip measurement and the other with on-chip dipole couplers for split-block waveguide packaging. From 252 to 295 GHz and 258 to 293 GHz, the measured peak gains were 23 dB in the on-wafer amplifier and 20.8 dB in the packaged amplifier, respectively, achieved with a 3.6-V supply at 46 mA and a 3.0-V supply at 37 mA.
Fluid induced seismicity guided by a continental fault: Injection experiment of 2004/2005 at the German Deep Drilling Site (KTB)

Recent hydraulic experiments at the KTB site have shown that seismicity induced by long‐term fluid injection directly into a continental crustal fault remains guided by this fault. The seismicity is triggered by pressure perturbations as low as 0.01–1 bars at the hypocenters. A combination of sequential one‐year fluid extraction (2002/2003) and one‐year fluid injection (2004/2005) experiments has shown that only positive pore pressure perturbation (i.e., injections) was able to induce the seismicity. Moreover, the onset of seismicity roughly coincides with the time of compensation of the extracted fluid volume by the following injection. This confirms that the pressure diffusion is a dominant mechanism of seismicity triggering by fluid injections. The probed fault shows a significant anisotropy and non‐linearity of its hydraulic behaviour. Its hydraulic diffusivity is up to one order of magnitude larger than that of surrounding rocks.
In situ detection of stratosphere‐troposphere exchange of cirrus particles in the midlatitudes

Airborne trace gas, microphysical, and radiation measurements were performed during the AIRcraft TOwed Sensor Shuttle ‐ Inhomogeneous Cirrus Experiment over northern Germany in 2013. Based on high‐precision nitrous oxide (N2O) and carbon monoxide (CO) in situ data, stratospheric air could be identified, which contained cirrus cloud particles. Consistent with the stratospheric N2O data, backward trajectories indicate that the sampled air masses crossed the dynamical tropopause in the last 3 h before the measurement. These air masses contained cirrus particles, which were formed during slow ascent in the troposphere and subsequently mixed with stratospheric air. From the CO‐N2O correlation the irreversibility of this transport is deduced. To our knowledge, this is the first in situ detection of cirrus particles mixed with stratospheric air in the midlatitudes.