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Meteorological Factors

Meteorological Factors are the environmental conditions that influence the atmosphere, including temperature, precipitation, humidity, wind, and atmospheric pressure.
These factors can have significant impacts on various research domains, such as agriculture, public health, and environmental studies.
By understanding and analyzing meteorological factors, researchers can optimize their protocols, enhance reproducibility, and improve the accuracy of their research outcomes.
This holistic, data-driven approach can lead to more robust and insightful findings, ultimately advancing scientific knowledge and discovery.

Most cited protocols related to «Meteorological Factors»

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Publication 2020
COVID 19 Cuboid Bone Diet, Formula Meteorological Factors Transmission, Communicable Disease
In this work, we built an integrated analysis framework (SI Appendix, Fig. S18) to evaluate the air quality improvements and health benefits of clean air actions in China (i.e., the 6 measures listed in Fig. 1) from 2013 to 2017. We first used the WRF-CMAQ model (20 , 21 ) to simulate the variations in PM2.5 concentrations from 2013 to 2017, during which period contributions from anthropogenic and meteorological factors were separated through scenario analysis. We then estimated the accumulated benefits of the 5-y implementation of each major control measure in 2017. Measure-specific emission abatements were quantified by applying the MEIC model (18 ) with data collected from the Ministry of Ecology and Environment of China (SI Appendix, Table S6) as inputs (19 ). Reductions in PM2.5 concentrations introduced by each measure were then evaluated using the WRF-CMAQ model, and the number of PM2.5-attributable excess deaths avoided by each measure was further quantified using the newly developed GEMM (4 (link)).
As shown in SI Appendix, Table S1, the WRF-CMAQ modeling system was utilized to simulate PM2.5 concentrations in 4 groups of scenarios. The BASE scenario group provided baseline simulations from 2013 to 2017, from which variations in PM2.5 concentrations could be derived. With additional information provided by the FixEmis scenarios (scenarios with fixed 2017 emissions and varying meteorological conditions from 2013 to 2017), the contributions of interannual meteorological variations and anthropogenic emission abatements to the 2013–2017 PM2.5 variations were separated. The air quality improvements in 2017 introduced by each measure were further derived based on the MEAS scenario and the NoCtrl scenario groups. Details of the methods and datasets are described in the SI Appendix. To evaluate CMAQ model performance, we compared simulated meteorological parameters, total PM2.5 concentrations, and PM2.5 chemical composition concentrations with ground observations (SI Appendix, sections S3 and S4).
Publication 2019
Biological Models chemical composition Cysteamine Meteorological Factors
In this study, we applied the time-stratified case-crossover (ts-CCO) design, regarded as a self-matched case-control study, which compares the exposure in the case period when events occurred with exposures in nearby referent periods, to examine the differences in exposure which may contribute to the differences in the daily count of cases [18 (link)]. Therefore, a time-stratified case-crossover design was adopted to regulate potential confounders (e.g., age, gender, etc) using self-control and exclude long-term impact of air pollutants (e.g., secular trend, seasonality, etc.) by stratification of time. We used the calendar month as the time stratum, to control the effects of long-term trend, seasonality, and day of the week [17 (link)]. We conducted a quasi-Poisson regression, controlling over-dispersion problem, combined with distributed lag non-linear model (DLNM) to estimate the non-linear and delayed influence of air pollution on IS onset. DLNM is based on the definition of “cross-basis”, a bi-dimensional space of functions to reflect the non-linear exposure-responses and lag structure of the association [19 (link), 20 (link)]. In this study, consequently, the combination of DLNM with the ts-CCO design was employed, which allows estimating the short-term, non-linear and delayed effect of air pollutant using cross-basis functions for depicting the relationship between air pollutant and IS onset along the dimensions of exposure and lag simultaneously based on removing control confounders and long-term trend by ts-CCO design.
A quasi-Poisson regression model combined with time-stratified case-crossover design and DLNM was built as follows:
Yt~Poissonμt
Logμt/Populationye=α+i=1mcbPollutanti,tdf2i1maxlagidf2i+cbTemptdf2m+1maxlagm+1df2m+2+cbRHtdf2m+3maxlagm+2df2m+4+γHolidayt+λStratum where t is the day of observation; Yt is the count of IS cases on t; μt is the expectation of Yt; Populationye is the year-end population size; α is an intercept; Pollutanti, tTempt, and RHt are the ith pollutant concentration, temperature and relative humidity on t, respectively; cb() represents the cross-basis function with three pre-specified parameters of maximal lag maxlagi, degree of freedom for lag-response natural spline df2i − 1, and degree of freedom for exposure-response natural spline df2i for pollutant, temperature or relative humidity; Holiday is used to control the effect of public holidays; Stratum is the time stratum in the time-stratified case-crossover design. We defined natural cubic spline function with 3 df for air pollution and meteorological factors to mimic the exposure-response pattern of air pollution-IS onset associations, as well as lag spaces with 3 df to estimate the lag effects. To capture the complete lag-response curve, the maximal lag of air pollutants was set to 14 days; for the sake of simplification and without loss of generalization, meanwhile, this maximal lag was assigned to the length of the case and control periods. In addition, a 3-day duration was specified to be the maximal lag of meteorological factors. The df and maximum lag days for air pollution determination referred to the Akaike information criterion for quasi-Poisson (Q-AIC), which could produce the relatively superior model.
We initially conducted single-pollutant model to evaluate the association between air pollution and IS onset, and then the significant air pollutants were included in multi-pollutant model. Spearman’s correlation tests were used to estimate the associations between air pollution and meteorological factors, and pollutants with correlation coefficient r > 0.60 were not included in multi-pollutant model simultaneously to address the collinearity between air pollutants. In order to identify the high-risk or low-risk air pollution condition, the influence of extreme air pollution was evaluated and presented as relative risk (RR) by comparing the 99th above or 1st below percentiles of air pollution to the median values. We calculated the single day lag influence and the cumulative lag influence (lag0–1, lag0–6, lag0–8, lag0–10, lag0–12, lag0–13, and lag0–14) to effectively depict the characteristics of the association between air pollution and IS onset. In addition, we conducted stratified analysis to investigate the impact of air pollution on subgroups according to gender (male and female) and age groups (adult: 18–64 years; the elderly: ≥ 65 years).
All analyses were conducted using R version 3.5.1 with the dlnm package for fitting the DLNM, the gnm package for conditional quasi-Poisson regression.
Sensitivity analyses were performed to test the robustness of the selected model, which were as following: df [2 (link)–6 (link)] for air pollution, and df [2 (link)–6 (link)] for lag space were changed; the maximum lag days (12–21 days) for air pollution were extended.
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Publication 2020
Adult Aged Age Groups Air Conditioning Air Pollutants Air Pollution CCL4 protein, human Cuboid Bone Environmental Pollutants Generalization, Psychological Humidity Hypersensitivity Longterm Effects Males Meteorological Factors Woman

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Publication 2020
COVID 19 Forests INSRR protein, human Meteorological Factors Microtubule-Associated Proteins
We estimated the associations between PM10 and daily mortality using a
set of generalised linear models. For each city, we estimated the associations
from the equation in figure 1 using daily time
series data.
Meteorological factors Zi were modeled in the
regressions through a set of natural spline functions
Si. The spline functions allow flexible
relations between meteorological factors and the outcomes. We chose the degrees
of freedom for each meteorological factor (dfZi) based on its best
prediction for air pollution levels. Using degrees of freedom that best predict
air pollution levels is advantageous because they produce unbiased or
asymptotically unbiased estimates of the pollution log-relative risk.15 (link) The optimal degree of freedom for each
natural spline was obtained using a generalised cross validation method that
best predicts PM10 concentrations.16 (link) After controlling for these potential confounding factors, the
data on high frequency PM10 concentrations should provide a plausible
source of external variation.
Since air pollution might affect mortality in a lagged fashion, we examined the
air pollution effects separately for different lag structures (lag of one day,
two days, etc). We also explored heterogeneous air pollution effects by
examining both sexes and different age groups.
To estimate national air pollution effects, we conducted a heterogeneity test and
used random effects meta-analysis to produce estimates of air pollution effects
for each city. In the meta-analysis we used the coefficients of PM10and its standard errors estimated from figure 2 for each city. In a random
effects meta-analysis, the true air pollution effects (βk) are
assumed to vary across different cities and to follow a normal distribution.
Such heterogeneity in air pollution effects may be caused by differences in city
populations, local socioeconomic conditions, and baseline population health.
Specifically, we assumed the true air pollution effects were randomly and
normally distributed around a mean effect (μ) with variance (σ2). We
then estimated the variance between cities using the DerSimonian and Laird
method17 (link) and modified the weights
used to calculate the summary estimate accordingly (fig 2).
Using a set of linear regressions, we conducted exploratory analysis on the
patterns of heterogeneous air pollution effects across the 38 cities. We
investigated whether estimated air pollution effects are associated with a
city’s mean PM10 concentrations, geographical location (north or
south), gross domestic product (GDP) per capita, and several demographic
factors.
Publication 2017
Age Groups Air Pollution Genetic Heterogeneity Head Meteorological Factors Population Health

Most recents protocols related to «Meteorological Factors»

We conducted several sensitivity analyses to check the robustness of our results. Firstly, we repeated the analyses using alternative df values (from 3 df to 4, 5, and 6 df) for mean temperature, relative humidity, and precipitation. Secondly, we used alternative moving average lag structures for all meteorological factors: lag 0–1 (current month and preceding 1 month) and lag 0–2 (current month and preceding 2 months). Thirdly, we refitted the CITS models using data from 2017 to 2020 to avoid inconsistencies in trends between different periods. Finally, for diseases with adequate sample sizes with the elderly, we restricted analyses to people aged between 20 and 54 and people aged above 55, respectively. We used the statistical software R 4.0.1 (Lucent Technologies, Jasmine Mountain, USA) to perform all analyses. A two-sided P-value < 0.05 was considered statistically significant.
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Publication 2023
CCL4 protein, human CIT protein, human Humidity Hypersensitivity Jasminum Meteorological Factors
The Theil-Sen Median (Sen) method was employed to determine the trend of NEP over the study area. This method is a robust nonparametric trend method, which does not require the data to follow a certain distribution (Fensholt et al., 2012 (link); Zhang Z. et al., 2021 (link)). It has been widely used in the trend analysis of long-time data series.
The Sen’s slope value (β) indicates the magnitude of the NEP trend. A positive β value suggests an upward trend and a negative β value suggests a downward trend. The calculation formula for β is as follows:
where β is Sen’s slope value; NEPi and NEPj are NEP in year i and j respectively.
The Mann–Kendall test is used to assess the significance of NEP trends. The test statistics S value is calculated as:
The test statistic Z value was obtained by standardizing S:
Where the function var is calculated as:
where n is the number of sequence samples; m is the number of affiliated groups in the data sequence; ti is the number of input values inside the affiliated group i.
To validate the significance of the trend, the absolute z-score value |Z| is compared with the critical value Z1-α/2 at a given significance level α. if |Z| is higher than Z1-α/2, the trend is considered significant. The Z1-α/2 values were obtained from the standard normal distribution table. For the significance level α of 0.05 and 0.01, the critical Z1-α/2 values are 1.96 and 2.58, respectively
Partial correlation is used to analyze the relationship between NEP and meteorological factors. Its formula is:
where Rij,k is the partial correlation coefficient between variable i and j after variable k is fixed. rij, rih, rjh are correlation coefficients for the variables i and j, j and k, and k and i, respectively.
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Publication 2023
Meteorological Factors
Standard descriptive analysis was conducted to display the distribution of air pollutants, meteorological factors, and daily hospitalizations for respiratory diseases, while the temporal distribution of air pollutants was presented in line charts. Spearman's correlation analysis was used to identify the correlation between air pollutants and meteorological factors.
The generalized additive model was applied to quantify the association between daily ambient CO concentration and daily hospitalizations for respiratory diseases. Quasi-Poisson regression was applied in the model, as daily hospitalizations tended to display an over-dispersed Poisson distribution. A dichotomous variable for public holidays and a categorical variable for the day of the week (DOW) were incorporated into the model to adjust the variation of daily hospitalizations within holidays and each week. Moreover, smoothing terms were used to fit daily hospitalizations in the models to control long-term and seasonal trends of daily hospitalizations and meteorological effects (14 (link)). According to previous studies (15 (link)–17 (link)), we applied 6 degrees of freedom (df) per year for long-term and seasonal trends, 3 df each for the same day's temperature (Tem0) and relative humidity (Humid0). In brief, the model can be represented as follows:
where E(Yt) represents the estimated daily hospitalizations for respiratory diseases at day t. β represents the log-relative risk of hospitalization associated with a 1 mg/m3 increase in ambient CO concentration. s () is the restricted smoothing spline function for variables with the non-linear association, day indicates the variable of the long-term and seasonal trends, and α is the intercept for the model.
Considering the delayed health effects of air pollutants, we estimated the lag effects of different days in both single-day lag from lag0 to lag7 and multi-day lag from lag0 to lag0–7 (moving average from lag0 to lag7). To improve the comparability of the association between CO exposure and risk of hospitalization for total and specific respiratory diseases, we selected the same CO exposure window for different respiratory diseases in exposure–response relationship analysis, stratified analysis, and sensitivity analysis adjusted for co-pollutants.
Based on the same models that estimated the association between CO exposure and risk of hospitalization for respiratory diseases, the smoothing function with 3 df was used to graphically describe the exposure–response relationship between ambient CO concentration and risk of hospitalization for respiratory diseases. Stratified analysis was conducted to assess the potential effect modification by age (minors/adult/elderly), gender (men/women), and season (warm: May–October, cold: November–April) (18 (link), 19 (link)). To further quantify the potential effect modification, we calculated the significant differences between subgroups based on the widely used method (20 (link)). We also investigated whether the association between CO and hospitalizations was still robust to the adjustment for other co-pollutants including PM2.5, PM10, SO2, NO2, and O3. Dual- and multi-pollutant models were performed in this study.
In this study, two-sided P < 0.05 was considered statistically significant. The generalized additive model was conducted in R 4.0.2 within the “mgcv” package (21 (link)). Effect estimates were presented as percentage changes and 95% confidence intervals (CIs) in daily hospitalizations in relation to each 1 mg/m3 increase in ambient CO concentration.
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Publication 2023
Adult Aged Air Pollutants Common Cold Environmental Pollutants Hospitalization Humidity Hypersensitivity Meteorological Factors Respiration Disorders Woman
Several statistical indicators, including correlation coefficient ( R ), root mean square error ( RMSE ), mean bias ( MB ), general error ( GE ), mean fractional bias ( MFB ), and mean fractional error ( MFE ) were used to evaluate the simulation results. The indicators were defined as follows: R=i=1N(XiX¯)(YiY¯)i=1N(XiX¯)2i=1N(YiY¯)2,
RMSE=i=1N(XiYi)2N,
MB=i=1N(XiYi)N,
GE=i=1N|XiYi|N,
MFB=1Ni=1N(XiYi)(Xi/2+Yi)×100%,
MFE=1Ni=1N|XiYi|(Xi/2+Yi)×100%,
where Xi and Yi represent the simulated and observed values, respectively. The indicator of R with a value closer to 1, or MB with a value closer to 0, or RMSE and GE with smaller values indicate a better simulation effect [49 (link)].
In order to quantify the effects of meteorological elements on PM2.5 variations induced by the underlying surface of “water networks”, multiple linear regression is adopted to quantify the contribution of meteorological factors to the change in air pollutants by using the software MATLAB (https://ww2.mathworks.cn/, accessed on 7 February 2023).
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Publication 2023
Air Pollutants Meteorological Factors Plant Roots
The carbon storage and sequestration of the InVEST model (integrated valuation of ecosystem services and trade-offs) is an effective tool for estimating terrestrial carbon storage [18 ]. It divides terrestrial carbon storage into four principal carbon pools, which are AGC (above-ground carbon storage), BGC (below-ground carbon storage), SOC (soil carbon storage), and dead organism carbon storage (Equation (3)) [33 (link)].
Ci=Ciabove+Cibelow+Cisoil+Cidead
Ctotal=i=1nCiSi
In Equations (3) and (4), Ctotal is the total terrestrial carbon storage, Ci represents the total carbon storage of land category i, Cabove refers to above-ground biotic carbon storage, and Cbelow represents below-ground biological carbon storage. Csoil means soil carbon storage with soil depth of 10 cm. Cdead indicates the carbon storage of dead organisms. Si is the total area of land category i [17 ].
Due to the low carbon density content of dead organisms and the difficulty of obtaining data, only the carbon storage of three major carbon pools was studied in this work. To ensure the accuracy of the study results, carbon density data within Jilin Province were used as much as possible, and carbon density values obtained by the same scholar or the same method were used due to the difference in research methods that may have caused deviations in the results [34 ]. The data collected through previous studies were all carbon density data from the 2010s. However, carbon density has the characteristics of changing with time and climate change [13 ]. To enhance the accuracy of carbon storage simulation results, it is necessary to average the carbon density values of secondary land categories with little difference and correct the carbon density by using meteorological factors.
The results of domestic and international studies show that both biological carbon density and soil carbon density are positively correlated with annual average precipitation [35 (link),36 (link)], and most of the established studies have obtained correction coefficients by comparing other regions with clear historical carbon density with the study area [2 ]. Combining the established studies with the needs of this work, the following equations were selected for the correction of carbon density.
Csp=3.3968×P+3996.1 R2=0.11
Cbp=6.7981e0.00541P R2=0.7
Ksp=Csp1/Csp2
Kbp=Cbp1/Cbp2
where Csp is the annual precipitation-corrected soil carbon density data (unit: Mg/hm−2); Cbp is the annual precipitation-corrected biological carbon density data (unit: Mg/hm−2); and P is the annual average precipitation (unit: mm). Ksp is the annual average precipitation correction factor of soil carbon density. Kbp is the annual average precipitation correction factor of biological carbon density; Csp1 and Cbp1 are the carbon density correction factors of Jilin Province. Csp1 and Cbp1 are the correction coefficients for carbon density in Jilin Province. Csp2 and Cbp2 are the correction coefficients for historical carbon density in Jilin Province. The values of the average annual precipitation are 766.6 mm and 811.2 mm, which are the average annual precipitation of Jilin Province in 2020 and of Jilin Province in 2010, respectively. The correction coefficients were substituted into the correction equation and revised to obtain the missing carbon density values for each land category. Considering the difficulty of obtaining carbon density data and the deviation in predicted values, the constant carbon density values selected were used to calculate the changes in carbon storage in historical and future periods in this work (Table 3). The partial carbon density data of 2020 obtained via correction were compared with the carbon density data collected in the field for verification. The measured above-ground carbon density of grassland in western Jilin Province is 19.8 Mg·hm−2, and the soil carbon density is 330.2 Mg·hm−2; the soil carbon density of wetland is 141.7 Mg·hm−2, and the soil carbon density of other lands is 248.1 Mg·hm−2. In a reasonable range, the results can be used to input model parameters.
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Publication 2023
Biological Factors Biopharmaceuticals Carbon Carbon-10 Climate Change colligin-2 Ecosystem Meteorological Factors Wetlands

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Meteorological factors, such as temperature, precipitation, humidity, wind, and atmospheric pressure, play a crucial role in various research domains, including agriculture, public health, and environmental studies.
By understanding and analyzing these environmental conditions, researchers can optimize their protocols, enhance the reproducibility and accuracy of their findings, and uncover valuable insights.
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The integration of meteorological factors into research processes can lead to more robust and insightful findings, ultimately advancing scientific knowledge and discovery.
By embracing a holistic, data-driven approach, researchers can enhance the reliability and impact of their work, making strides in their respective fields.