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Linear trend estimation
Linear trend estimation
from Wikipedia

Linear trend estimation is a statistical technique used to analyze data patterns. Data patterns, or trends, occur when the information gathered tends to increase or decrease over time or is influenced by changes in an external factor. Linear trend estimation essentially creates a straight line on a graph of data that models the general direction that the data is heading.

Fitting a trend: Least-squares

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Given a set of data, there are a variety of functions that can be chosen to fit the data. The simplest function is a straight line with the dependent variable (typically the measured data) on the vertical axis and the independent variable (often time) on the horizontal axis.

The least-squares fit is a common method to fit a straight line through the data. This method minimizes the sum of the squared errors in the data series . Given a set of points in time and data values observed for those points in time, values of and are chosen to minimize the sum of squared errors

.

This formula first calculates the difference between the observed data and the estimate , the difference at each data point is squared, and then added together, giving the "sum of squares" measurement of error. The values of and derived from the data parameterize the simple linear estimator . The term "trend" refers to the slope in the least squares estimator.

Data as trend and noise

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To analyze a (time) series of data, it can be assumed that it may be represented as trend plus noise:

where and are unknown constants and the 's are randomly distributed errors. If one can reject the null hypothesis that the errors are non-stationary, then the non-stationary series is called trend-stationary. The least-squares method assumes the errors are independently distributed with a normal distribution. If this is not the case, hypothesis tests about the unknown parameters and may be inaccurate. It is simplest if the 's all have the same distribution, but if not (if some have higher variance, meaning that those data points are effectively less certain), then this can be taken into account during the least-squares fitting by weighting each point by the inverse of the variance of that point.

Commonly, where only a single time series exists to be analyzed, the variance of the 's is estimated by fitting a trend to obtain the estimated parameter values and thus allowing the predicted values

to be subtracted from the data (thus detrending the data), leaving the residuals as the detrended data, and estimating the variance of the 's from the residuals — this is often the only way of estimating the variance of the 's.

Once the "noise" of the series is known, the significance of the trend can be assessed by making the null hypothesis that the trend, , is not different from 0. From the above discussion of trends in random data with known variance, the distribution of calculated trends is to be expected from random (trendless) data. If the estimated trend, , is larger than the critical value for a certain significance level, then the estimated trend is deemed significantly different from zero at that significance level, and the null hypothesis of a zero underlying trend is rejected.

The use of a linear trend line has been the subject of criticism, leading to a search for alternative approaches to avoid its use in model estimation. One of the alternative approaches involves unit root tests and the cointegration technique in econometric studies.

The estimated coefficient associated with a linear trend variable such as time is interpreted as a measure of the impact of a number of unknown or known but immeasurable factors on the dependent variable over one unit of time. Strictly speaking, this interpretation is applicable for the estimation time frame only. Outside of this time frame, it cannot be determined how these immeasurable factors behave both qualitatively and quantitatively.

Research results by mathematicians, statisticians, econometricians, and economists have been published in response to those questions. For example, detailed notes on the meaning of linear time trends in the regression model are given in Cameron (2005);[1] Granger, Engle, and many other econometricians have written on stationarity, unit root testing, co-integration, and related issues (a summary of some of the works in this area can be found in an information paper[2] by the Royal Swedish Academy of Sciences (2003)); and Ho-Trieu & Tucker (1990) have written on logarithmic time trends with results indicating linear time trends are special cases of cycles.

Noisy time series

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It is harder to see a trend in a noisy time series. For example, if the true series is 0, 1, 2, 3, all plus some independent normally distributed "noise" e of standard deviation E, and a sample series of length 50 is given, then if E = 0.1, the trend will be obvious; if E = 100, the trend will probably be visible; but if E = 10000, the trend will be buried in the noise.

Consider a concrete example, such as the global surface temperature record of the past 140 years as presented by the IPCC.[3] The interannual variation is about 0.2 °C, and the trend is about 0.6 °C over 140 years, with 95% confidence limits of 0.2 °C (by coincidence, about the same value as the interannual variation). Hence, the trend is statistically different from 0. However, as noted elsewhere,[4] this time series doesn't conform to the assumptions necessary for least-squares to be valid.

Goodness of fit (r-squared) and trend

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Illustration of the effect of filtering on r2. Black = unfiltered data; red = data averaged every 10 points; blue = data averaged every 100 points. All have the same trend, but more filtering leads to higher r2 of fitted trend line.

The least-squares fitting process produces a value, r-squared (r2), which is 1 minus the ratio of the variance of the residuals to the variance of the dependent variable. It says what fraction of the variance of the data is explained by the fitted trend line. It does not relate to the statistical significance of the trend line (see graph); the statistical significance of the trend is determined by its t-statistic. Often, filtering a series increases r2 while making little difference to the fitted trend.

Advanced models

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Thus far, the data have been assumed to consist of the trend plus noise, with the noise at each data point being independent and identically distributed random variables with a normal distribution. Real data (for example, climate data) may not fulfill these criteria. This is important, as it makes an enormous difference to the ease with which the statistics can be analyzed so as to extract maximum information from the data series. If there are other non-linear effects that have a correlation to the independent variable (such as cyclic influences), the use of least-squares estimation of the trend is not valid. Also, where the variations are significantly larger than the resulting straight line trend, the choice of start and end points can significantly change the result. That is, the model is mathematically misspecified. Statistical inferences (tests for the presence of a trend, confidence intervals for the trend, etc.) are invalid unless departures from the standard assumptions are properly accounted for, for example, as follows:

In R, the linear trend in data can be estimated by using the 'tslm' function of the 'forecast' package.

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Medical and biomedical studies often seek to determine a link between sets of data, such as of a clinical or scientific metric in three different diseases. But data may also be linked in time (such as change in the effect of a drug from baseline, to month 1, to month 2), or by an external factor that may or may not be determined by the researcher and/or their subject (such as no pain, mild pain, moderate pain, or severe pain). In these cases, one would expect the effect test statistic (e.g., influence of a statin on levels of cholesterol, an analgesic on the degree of pain, or increasing doses of different strengths of a drug on a measurable index, i.e. a dose - response effect) to change in direct order as the effect develops. Suppose the mean level of cholesterol before and after the prescription of a statin falls from 5.6 mmol/L at baseline to 3.4 mmol/L at one month and to 3.7 mmol/L at two months. Given sufficient power, an ANOVA (analysis of variance) would most likely find a significant fall at one and two months, but the fall is not linear. Furthermore, a post-hoc test may be required. An alternative test may be a repeated measures (two way) ANOVA or Friedman test, depending on the nature of the data. Nevertheless, because the groups are ordered, a standard ANOVA is inappropriate. Should the cholesterol fall from 5.4 to 4.1 to 3.7, there is a clear linear trend. The same principle may be applied to the effects of allele/genotype frequency, where it could be argued that a single-nucleotide polymorphism in nucleotides XX, XY, YY are in fact a trend of no Y's, one Y, and then two Y's.[3]

The mathematics of linear trend estimation is a variant of the standard ANOVA, giving different information, and would be the most appropriate test if the researchers hypothesize a trend effect in their test statistic. One example is levels of serum trypsin in six groups of subjects ordered by age decade (10–19 years up to 60–69 years). Levels of trypsin (ng/mL) rise in a direct linear trend of 128, 152, 194, 207, 215, 218 (data from Altman). Unsurprisingly, a 'standard' ANOVA gives p < 0.0001, whereas linear trend estimation gives p = 0.00006. Incidentally, it could be reasonably argued that as age is a natural continuously variable index, it should not be categorized into decades, and an effect of age and serum trypsin is sought by correlation (assuming the raw data is available). A further example is of a substance measured at four time points in different groups:

# mean SD
1 1.6 0.56
2 1.94 0.75
3 2.22 0.66
4 2.40 0.79

This is a clear trend. ANOVA gives p = 0.091, because the overall variance exceeds the means, whereas linear trend estimation gives p = 0.012. However, should the data have been collected at four time points in the same individuals, linear trend estimation would be inappropriate, and a two-way (repeated measures) ANOVA would have been applied.

See also

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Notes

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References

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Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
Linear trend estimation is a statistical technique used to identify and quantify the rate of linear change in a over an independent variable, such as time, by fitting a straight line that best represents the underlying pattern in the observations. This method assumes a constant capturing gradual increases or decreases in the mean of the data, often applied to to detect systematic shifts amid random variation. The primary approach employs ordinary least squares (OLS) regression, which determines the and intercept by minimizing the sum of squared vertical deviations between observed data points and the fitted line. Key aspects of linear trend estimation include assessing to determine if the detected trend deviates meaningfully from zero, typically via t-tests on the slope adjusted for effective sample size in the presence of . For instance, the is calculated as the divided by its , compared against critical values from the t-distribution with accounting for via formulas like Neff=N1r1+rN_{eff} = N \frac{1 - r}{1 + r}, where rr is the lag-1 . Assumptions underlying OLS include uncorrelated errors and a constant trend, though violations like or outliers necessitate robust alternatives such as the Theil-Sen estimator, which is non-parametric and less sensitive to extreme values. Applications span environmental sciences, where it evaluates changes in variables like or , and other domains requiring trend detection in sequential . One proposed criterion for a statistically meaningful trend is a coefficient of determination of r20.65r^2 \geq 0.65 alongside significance (p0.05p \leq 0.05), as defined by Bryhn and Dimberg (2011).

Core Concepts

Definition and Purpose

Linear trend estimation is a statistical method that identifies and quantifies a straight-line relationship between an independent variable, such as time, and a dependent variable, modeling gradual changes or patterns of growth and decline at a constant rate over the independent variable. This approach assumes that the underlying pattern in the data can be adequately captured by a , where the dependent variable changes by a fixed amount for each unit increase in the independent variable. The primary purpose of linear trend estimation is to simplify complex datasets by extracting the dominant linear signal, which facilitates forecasting future values, testing hypotheses about underlying relationships, and detecting anomalies or deviations from the expected pattern. By focusing on this core linear component, it enables analysts to discern long-term directions in data without being overwhelmed by short-term fluctuations or noise. The origins of linear trend estimation trace back to the early in astronomy, where developed the method of in 1805 to fit linear models to observational data on planetary orbits. These methods evolved significantly in the late through contributions from statisticians like , who formalized regression concepts in the , integrating them into broader statistical theory. Unlike nonlinear trend models, such as exponential or ones, linear trend estimation specifically assumes a constant rate of change, making it suitable for data exhibiting steady progression rather than accelerating or decelerating patterns. This distinction ensures its applicability to scenarios where the relationship is approximately straight-line, though it may require transformation or alternative models for curved trends.

Mathematical Model

The mathematical model for linear trend estimation is formulated as a simple linear regression, where the goal is to describe the relationship between an observed response variable and a single predictor, often time. For nn observations, the model is given by Yi=β0+β1Xi+ϵi,i=1,2,,n,Y_i = \beta_0 + \beta_1 X_i + \epsilon_i, \quad i = 1, 2, \dots, n, where YiY_i represents the observed response at the ii-th point, XiX_i is the predictor variable (such as a time index tit_i), β0\beta_0 is the intercept parameter denoting the of YY when X=0X = 0, β1\beta_1 is the parameter indicating the change in YY per unit increase in XX, and ϵi\epsilon_i is the random error term capturing unexplained variation. This model assumes in the parameters, meaning the E(YiXi)=β0+β1XiE(Y_i | X_i) = \beta_0 + \beta_1 X_i holds without higher-order terms in the predictors. The errors ϵi\epsilon_i are assumed to be independent across observations, with constant variance (homoscedasticity, Var(ϵi)=σ2\text{Var}(\epsilon_i) = \sigma^2 for all ii), and normally distributed with mean zero (ϵiN(0,σ2)\epsilon_i \sim N(0, \sigma^2)) to facilitate such as confidence intervals and hypothesis tests. The parameter β1\beta_1 is interpreted as the average change in the response YY for each one-unit increase in the predictor XX, representing the rate of the linear trend; for instance, in time series contexts, it quantifies the trend's slope over time. Similarly, β0\beta_0 provides the baseline level of YY at X=0X = 0. While this section focuses on the simple linear trend with one predictor, the framework extends to multiple linear regression by including additional predictors in the equation, though such cases involve more complex estimation. The parameters β0\beta_0 and β1\beta_1 are typically estimated using methods like ordinary least squares, as detailed in subsequent sections.

Estimation Techniques

Ordinary Least Squares Fitting

Ordinary least squares (OLS) fitting is the foundational method for estimating the parameters of a linear trend model, originally developed by in 1805 and further justified by in 1809 as a technique for minimizing prediction errors in observational data. This approach assumes a simple Yi=β0+β1Xi+ϵiY_i = \beta_0 + \beta_1 X_i + \epsilon_i, where the goal is to find estimates β0^\hat{\beta_0} and β1^\hat{\beta_1} that best approximate the underlying trend by treating the errors ϵi\epsilon_i as random deviations. The objective of OLS is to minimize the sum of squared residuals, defined as S=i=1n(YiY^i)2S = \sum_{i=1}^n (Y_i - \hat{Y}_i)^2, where Y^i=b0+b1Xi\hat{Y}_i = b_0 + b_1 X_i represents the predicted value for each observation. This minimization criterion arises from the principle of selecting parameter values that make the model's predictions as close as possible to the observed data in a least-squares sense, effectively reducing the overall prediction error. To derive the OLS estimators, one can use the method of normal equations, which involves taking partial derivatives of SS with respect to b0b_0 and b1b_1, setting them to zero, and solving the resulting system. The partial derivative with respect to b0b_0 yields (Yib0b1Xi)=0\sum (Y_i - b_0 - b_1 X_i) = 0, and with respect to b1b_1 yields Xi(Yib0b1Xi)=0\sum X_i (Y_i - b_0 - b_1 X_i) = 0. Solving these equations provides the closed-form solutions: b1=nXiYiXiYinXi2(Xi)2,b_1 = \frac{n \sum X_i Y_i - \sum X_i \sum Y_i}{n \sum X_i^2 - (\sum X_i)^2}, b0=Yˉb1Xˉ,b_0 = \bar{Y} - b_1 \bar{X}, where nn is the number of observations, Xˉ\bar{X} and Yˉ\bar{Y} are the sample means of XX and YY, and the sums are taken over all i=1i = 1 to nn. These formulas ensure that the fitted line passes through the point (Xˉ,Yˉ)(\bar{X}, \bar{Y}) and has a slope proportional to the covariance between XX and YY divided by the variance of XX. The step-by-step procedure for OLS fitting begins with data preparation, which involves paired observations (Xi,Yi)(X_i, Y_i) and ensuring they are suitable for linear modeling, such as checking for outliers or missing values. Next, compute the necessary sums: nn, Xi\sum X_i, Yi\sum Y_i, XiYi\sum X_i Y_i, and Xi2\sum X_i^2. Using these, apply the closed-form formulas to estimate b0b_0 and b1b_1. Finally, construct the trend line equation Y^=b0+b1X\hat{Y} = b_0 + b_1 X and visualize it by plotting the line against the points to assess the fit. Geometrically, the OLS trend line represents the straight line that minimizes the sum of the squared vertical distances from each data point to the line, providing the best linear unbiased approximation under the model's assumptions. This interpretation highlights how OLS projects the data onto a one-dimensional subspace in the plane spanned by and XX, orthogonalizing the residuals perpendicular to that subspace. OLS fitting is widely implemented in statistical software, such as the lm() function in for linear models and scipy.stats.linregress() in Python for computations.

Alternative Estimation Methods

While ordinary least squares (OLS) assumes homoscedastic errors, alternative methods address violations such as heteroscedasticity, non-normality, or outliers in linear trend estimation. Weighted least squares (WLS) extends OLS by incorporating weights to account for heteroscedasticity, where error variances differ across observations. Typically, weights are set as wi=1/σi2w_i = 1 / \sigma_i^2, where σi2\sigma_i^2 is the variance of the ii-th , giving higher influence to more precise data points. The slope estimator is given by b^1=wi(XiYi)wiXiwiYiwiwiXi2(wiXi)2wi.\hat{b}_1 = \frac{\sum w_i (X_i Y_i) - \frac{\sum w_i X_i \sum w_i Y_i}{\sum w_i}}{\sum w_i X_i^2 - \frac{(\sum w_i X_i)^2}{\sum w_i}}. This method is particularly useful when precision varies, such as in time series with increasing volatility. Computationally, WLS often requires iterative if weights depend on unknown variances, starting with OLS residuals to approximate σi2\sigma_i^2. (MLE) provides a framework for under specified distributions, offering inferential advantages beyond point estimates. Under the assumption of normally distributed errors, MLE coincides with OLS for the slope and intercept. However, it extends to other distributions, such as Poisson for count data trends. The for the normal is L(β,σ)=i=1n12πσ2exp(ϵi22σ2),L(\beta, \sigma) = \prod_{i=1}^n \frac{1}{\sqrt{2\pi \sigma^2}} \exp\left( -\frac{\epsilon_i^2}{2\sigma^2} \right),
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