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Correlations for heat capacity, vapor pressure, and liquid viscosity
Correlations for heat capacity, vapor pressure, and liquid viscosity

Environmental and geographical factors affecting the Iberian
Environmental and geographical factors affecting the Iberian

... of correctly predicted negative cases to the total number of negative cases), was used to measure the performance of models. To compare observed and predicted maps, the continuous probability variable generated by logistic regression should be converted to a binary one (presence /absence), selecting ...
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Multivariate Data Analysis
Multivariate Data Analysis

... Logistic regression: - the underlying distribution is binomial and LS do not suffice for estimating α and β. Maximum likelihood: an iterative procedure to compute values of α and β which maximize the probability that the observed values of the dependent variable in the data set may be predicted from ...
Surrogate model of BNS waveforms for measuring the EOS
Surrogate model of BNS waveforms for measuring the EOS

... • Fixed cost of ~50 ms for computing surrogate (not optimized) • Additional cost for resampling to desired frequencies (interpolation) • Faster than all waveforms in LALSuite (written in C) below ~18 Hz ...
Introduction to Nonparametric Analysis
Introduction to Nonparametric Analysis

Regression Towards the Mean
Regression Towards the Mean

Mixture Models - CMU Statistics
Mixture Models - CMU Statistics

... In Chapter 18, we looked at principal components analysis, which finds linear structures with q space (lines, planes, hyper-planes, . . . ) which are good approximations to our p-dimensional data, q � p. In Chapter 19, we looked at factor analysis, where which imposes a statistical model for the dis ...
MSword - Forest Measurements and Biometrics
MSword - Forest Measurements and Biometrics

...  Is this a measurement error? E.g., a tree height of 100 m is very unlikely  Is a transcription error? E.g. for adult person, a weight of 20 lbs was entered rather than 200 lbs.  Is there something very unusual about this point? e.g., a bird has a short beak, because it was damaged. Try to fix th ...
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Year 7 - Nrich

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Economic Duration Data and Hazard Functions

... mathematically equivalent specification in terms of a probabilitydistribution.The two specifications involve the same parameters and are simply two different ways of describing the same system of probabilities. Thus, the hazardfunction approach does not identify new parameters. As we will see, the l ...
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Data Streams: Algorithms and Applications

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Text Analysis and Sentiment Polarity on FIFA World

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Luca Centurioni - Surface current observations with satellite tracked drifting buoys (remote presentation)

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A Sequential Choice Model of Recreation Behavior

Using SAS Software in the Design and Analysis of Two-Level Fractional Factorial Experiments
Using SAS Software in the Design and Analysis of Two-Level Fractional Factorial Experiments

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Least Squares Regression Line

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Confidence sets for model selection by F

Precipitation downscaling with SDSM over Rio de la Plata basin
Precipitation downscaling with SDSM over Rio de la Plata basin

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STATISTICAL ANALYSIS OF RESIDENTIAL HOUSING PRICES IN

Estimating the Cost of Construction of Light Water - IOSR-JEN
Estimating the Cost of Construction of Light Water - IOSR-JEN

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Data assimilation

Data assimilation is the process by which observations are incorporated into a computer model of a real system. Applications of data assimilation arise in many fields of geosciences, perhaps most importantly in weather forecasting and hydrology. The most commonly used form of data assimilation proceeds by analysis cycles. In each analysis cycle, observations of the current (and possibly past) state of a system are combined with the results from a numerical model (the forecast) to produce an analysis, which is considered as 'the best' estimate of the current state of the system. This is called the analysis step. Essentially, the analysis step tries to balance the uncertainty in the data and in the forecast. The result may be the best estimate of the physical system, but it may not the best estimate of the model's incomplete representation of that system, so some filtering may be required. The model is then advanced in time and its result becomes the forecast in the next analysis cycle. As an alternative to analysis cycles, data assimilation can proceed by some sort of nudging process, where the model equations themselves are modified to add terms that continuously push the model towards observations.
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