Not exact matches
While «operating earnings» are not even defined under Generally Accepted Accounting Principles, and «forward operating earnings» only surfaced as a creature of Wall Street
in the early 1980's, it's
simple enough to impute historical values of forward operating earnings because they are almost completely explained by observable earnings and employment
data — see Long - term Evidence on the Fed
Model and Forward Operating Earnings.
In short, for a very simple model, it fits the data remarkably well, explaining 88.5 % of the variance in English by - election results (an R2 of 0.885 in stats parlance
In short, for a very
simple model, it fits the
data remarkably well, explaining 88.5 % of the variance
in English by - election results (an R2 of 0.885 in stats parlance
in English by - election results (an R2 of 0.885
in stats parlance
in stats parlance).
The researchers from Wageningen University & Research, Bogor Agricultural University
in Indonesia, University of East Anglia and the Center for International Forestry Research analysed the spatially distributed pattern of hydrological drought, that is the drought
in groundwater recharge,
in Borneo using a
simple transient water balance
model driven by monthly climate
data from the period 1901 - 2015.
The team chose to focus on a relatively
simple, well - known material
in order to expand the range of pressure it could simulate and attempt to validate the
model with experimental
data.
Using historical
data from horizontal wells
in the Barnett Shale formation
in North Texas, Tad Patzek, professor and chair
in the Department of Petroleum and Geosystems Engineering
in the Cockrell School of Engineering; Michael Marder, professor of physics
in the College of Natural Sciences; and Frank Male, a graduate student
in physics, used a
simple physics theory to
model the rate at which production from the wells declines over time, known as the «decline curve.»
On the other hand, a number of
simple models including some pioneer one - parameter ones proposed more than 30 years ago have remained
in agreement with all observational
data up to recent few months.
As a whole, now the conceptual transition occurs from proving the inflationary paradigm
in general and testing some of its
simplest models to applying it for investigation of particle physics at super-high energies and of the actual history of the Universe
in the remote past using observational
data.
The presentations include: Seasons: A
simple introduction to place the learning into context Writing an Autumn Report (Non - chronological report) A Week
in Autumn (Poetry with a Grammar Focus) Halloween - A Revolting Recipe - writing instructions Halloween Literacy Bundle - variety of language tasks Autumn Handwriting (to be used with interactive board for
modelling handwriting) Autumn Maths (number, handling
data and some area activities) with answer slides Scarecrow Art There are also some online links provided within the presentations to engage the learners.
Vertical Planning Task: Is a
simple, yet powerful process for gathering
data around what teachers and students are do when asked to use mathematics to
model a real - life situation presented
in the form of a word problem.
This
model is a
simple and intuitive valuation - dependent
model, as illustrated by the log - linear line of best fit
in Figure 1.3 At each point
in time, we calibrate the
model only to the historically observed
data available at that time; no look - ahead information is
in the
model calibration.
However, the goal
in scientific
modeling is not mere explanation but rather predictive power, and generally the
simpler model that explains the
data adequately has greater predictive power.
Here, we elucidate this question by using 26 years of satellite
data to drive a
simple physical
model for estimating the temperature response of the ocean mixed layer to changes
in aerosol loadings.
Three IPCC climate
models, recent NASA Aqua satellite
data, and a
simple 3 - layer climate
model are used together to demonstrate that the IPCC climate
models are far too sensitive, resulting
in their prediction of too much global warming
in response to anthropogenic greenhouse gas emissions.
Some of them are optimal fingerprint detection studies (estimating the magnitude of fingerprints for different external forcing factors
in observations, and determining how likely such patterns could have occurred
in observations by chance, and how likely they could be confused with climate response to other influences, using a statistically optimal metric), some of them use
simpler methods, such as comparisons between
data and climate
model simulations with and without greenhouse gas increases / anthropogenic forcing, and some are even based only on observations.
To make matters more difficult, even a
simple mechanistic
model (AFRC Wheat) containing good science
in it sub-modules, struggles if fed less than perfect
data : http://www.nottingham.ac.uk/environmental-modelling/Roger%20Payne.pdf Given the imperfect nature of real - world
data, could AFRC wheat ever be shown to be wrong?
Your
model must match the
data to be credible, while my
simple analysis of the Solar effect alone does not need to match the
data perfectly,
in my paper I say that only approximately 50 % of the warming since 1900 is related to the sun and from 1600 to 1900 the match is quite good, indeed!
It used a
simple mathematical
model, and IPCC
data, to suggest that even if CO2 concentrations
in the atmosphere doubled, which might take the rest of the century, average global temperature would not rise by much more than 1 degree Celsius.
Yes, I understand it isn't that
simple but still
in every sense of the word the Hansen and IPCC
models are «fit» to the
data they have and then we are subsequently assured the
models work great because they fit the
data they fitted it to.
Within economics
modelling, attempts to
model the feedback mechanisms that occur
in the real economy are also really difficult — we know, for example, that investment
in new technologies will act as an incentive for the existing technologies it hopes to substitute to become more efficient (the sailing ship effect — i.e.
in the 50 years after the introduction of the steam ship, sailing ships made more efficiency improvements than they had
in the previous 3 centuries) but how to quantify something even as
simple as this is not easy BUT we have learnt a few ways to give sensible (order of magnitude) figures with time lags, the learning by doing effect and phased -
in substitution effects based on massive amounts of
data.
Carbon budgets have been estimated by a number of different methods, including complex ESMs (shown
in yellow),
simple climate
models employed by Integrated Assessment Models (IAMs, shown in red), and by using observational data on emissions and warming through present to «constrain» the ESM results (shown in
models employed by Integrated Assessment
Models (IAMs, shown in red), and by using observational data on emissions and warming through present to «constrain» the ESM results (shown in
Models (IAMs, shown
in red), and by using observational
data on emissions and warming through present to «constrain» the ESM results (shown
in blue).
A
simple model, following the example of the 14C
data with a one year mixing time, would suggest a delay of 12 6 months for CO2 changes
in concentration
in the Northern Hemisphere to appear
in the Southern Hemisphere.»
Discussion of «pulsed stratospheric spraying» creating less noisy
data for analysis of effects gave me a
simple idea — If the input to the
models assume that stratospheric spraying has been ongoing for decades, then plug into these
models the temperature
data accrued
in the three days after 9/11 when, as reported at the time, the mean temperature over the US landmass «inexplicably» rose by 2 degrees C.
in only three days while all aircraft were grounded, then the actual effect of stratospheric manipulations over US will emerge.
In fact, my
model is a hindcast of the
data, not a
simple fitting of the
data.
This understanding must translate eventually into more satisfying confrontations with
data if it to make a contribution to science, but this can be a multi-step process... Fitting
simple models to a GCM should make it easier to criitique the GCM (or at least that aspect of the GCM that is being fit
in this way) since one can critique the
simple model instead.
He and a colleague published a peer - reviewed paper
in which they used a
simple climate
model to show that these chaotic variations could cause patterns
in satellite
data that would lead climatologists to believe the climate is significantly more sensitive to external forcing than it really is.
Estimates of natural variability from an AOGCM provide a critical input
in deriving, by comparing temperature estimates from the
simple model with observations, a likelihood function for the parameters jointly at each possible combination of parameter settings (and
in one or two cases AOGCMs provide surrogates for some of the observational
data).
The goal of the exercise is to construct a
simple model [amplitude modulation of a single cycle] that accounts for the peaks
in the
data.
There IS a heat source and a physical reality, that requires no forcing to give it super powers as with puny CO2 the palnts gobble up as much as they can get of,
in fact.And explains the stable ice age and the Milankovitch linked interglacials, and how that sawtooth between repeated and predicatble limits can be driven using known energy sources, specific heats and masses, plus
simple deterministic physics, no statistical
models or Piltdown Mann
data set approaches.
General Introduction Two Main Goals Identifying Patterns
in Time Series
Data Systematic pattern and random noise Two general aspects of time series patterns Trend Analysis Analysis of Seasonality ARIMA (Box & Jenkins) and Autocorrelations General Introduction Two Common Processes ARIMA Methodology Identification Phase Parameter Estimation Evaluation of the
Model Interrupted Time Series Exponential Smoothing General Introduction
Simple Exponential Smoothing Choosing the Best Value for Parameter a (alpha) Indices of Lack of Fit (Error) Seasonal and Non-seasonal
Models With or Without Trend Seasonal Decomposition (Census I) General Introduction Computations X-11 Census method II seasonal adjustment Seasonal Adjustment: Basic Ideas and Terms The Census II Method Results Tables Computed by the X-11 Method Specific Description of all Results Tables Computed by the X-11 Method Distributed Lags Analysis General Purpose General
Model Almon Distributed Lag Single Spectrum (Fourier) Analysis Cross-spectrum Analysis General Introduction Basic Notation and Principles Results for Each Variable The Cross-periodogram, Cross-density, Quadrature - density, and Cross-amplitude Squared Coherency, Gain, and Phase Shift How the Example
Data were Created Spectrum Analysis — Basic Notations and Principles Frequency and Period The General Structural
Model A
Simple Example Periodogram The Problem of Leakage Padding the Time Series Tapering
Data Windows and Spectral Density Estimates Preparing the
Data for Analysis Results when no Periodicity
in the Series Exists Fast Fourier Transformations General Introduction Computation of FFT
in Time Series
The simplicity of the PDSI, which is calculated from a
simple water - balance
model forced by monthly precipitation and temperature
data, makes it an attractive tool
in large - scale drought assessments, but may give biased results
in the context of climate change6.
Is it
simple interpolation using the output gridded
data or sub-grid processes running live
in the
model to determine what should be the temperature at the specific height?
In the case of complicated models of Earth's atmosphere and oceans, it is true that it is not simple to do controlled experiments, so we must substitute model predictions against reality to judge the model (and by «prediction» I mean what happens in the future, not a data - snooped hind - cast
In the case of complicated
models of Earth's atmosphere and oceans, it is true that it is not
simple to do controlled experiments, so we must substitute
model predictions against reality to judge the
model (and by «prediction» I mean what happens
in the future, not a data - snooped hind - cast
in the future, not a
data - snooped hind - cast).
Actually,
in Dr Mann's case, it's not easy when
simple data handling and statistical
modeling is your day job - hence, all his problems with California bristlecones, double - counted lone Gaspà © cedars, upside - down Finnish lake sediments, transposed eastern and western hemispheres, invented statistical methods, truncated late 20th - century tree - rings, etc, etc..
In simple terms the red assumption is compatable with a slab ocean thermal
model and I don't think that is an appropriate
model and seems incompatable with the
data.
The
data reveal streamlined subglacial bedforms that define a zone of paleo — ice stream convergence, but,
in contrast to previous
models, do not show a
simple downflow progression of bedform types along paleo — ice stream troughs.
If you have a
simple model that you are fitting to some
data, there is no problem
in describing
in detail how you decided on the
model, the free parameters, the fitting procedure, the
data used, etc. it can be more of a challenge to make the development path of a climate simulator fully transparent.
He proposes a relationship between the Pacific Decadal Oscillation (PDO) and clouds by considering a variety of combinations of initial ocean temperature, ocean thickness, cloud feedback, and forcing by clouds (neglecting forcing by CO2 and the water vapor feedback entirely)
in a
simple energy balance
model, and finds a relationship between PDO and clouds using 9 years of satellite
data.
The whole point of a dimension reduction
model is to mathematically represent the
data in simpler form.
The whole point of a dimension reduction
model is to mathematically represent the
data in a
simpler form.
In addition to saved time on simple data entry, HomeSmart's model puts operational standards in place for all aspects of the busines
In addition to saved time on
simple data entry, HomeSmart's
model puts operational standards
in place for all aspects of the busines
in place for all aspects of the business.