Calculated trends do not predict the future trends.
Not exact matches
As I have mentioned previously I simply run a nightly scan of Long and Short stock candidates hitting 52 week highs / lows and keep note of these stocks and over the course of the coming days and weeks I look for which stocks keep hitting the parameters of my scans before taking a closer look at the chart, once I see there is a clean smooth
trend be it going up or down I then
calculate from that afternoons closing price and where the stop loss would need to be positioned on the first day the trade is placed in line with my risk management and then simply wait for the open the following day to open the trade then my system
does the rest.
No worry of
calculating stops, software
does it automatically, never second guess the
trend again.
No worry of
calculating your stops, the software
does it automatically, never second guess the
trend again.
The F test in Excel
does the maths, (Hank, 233) and has the additional bonus of
calculating the range of
trend lines within which the true
trend probably falls.
We don't compare observations with the same time period in the models (i.e. the same start and stop dates), but to all model projections of the same time length (i.e. 60 - month to 180 - month)
trends from the projected data from 2001 - 2020 (from the A1B run)(the
trends of a particular length are
calculated successively, in one month steps from 2001 to 2020).
when he started
doing his «analysis» he still didn t understand how a
trend line is
calculated.
Nowhere
did we «use 1910 - 2009
trends as the basis for
calculating 1880 - 2009 exceedence probabilities», and I can't think why
doing this would make sense.
I
calculated the 1979 - 1999
trends (as
done by Douglass et al) for each of the individual simulations.
How gentlemanly is it that he falsely claims «Rahmstorf confirms my critique (see the thread), namely, they used 1910 - 2009
trends as the basis for
calculating 1880 - 2009 exceedence probabilities,» when I have
done nothing of the sort?
The data are available and anyone can
calculate the different
trends, I don't think I have any special method or anything, but for completeness the 1950 - 2006
trend went from 0.097 deg C / dec to 0.068 deg C / dec (mean of all realisations) a 31 % drop (uncertainties on OLS
trends + / -0.017 deg C / dec; for 100 different realisations of HadSST3 the range of
trends is [0.0458,0.0928] deg C / dec).
One merely
calculates the least - squares linear - regression
trend over successively longer periods to see whether the slope of the
trend progressively increases (as it must if the curve is genuinely exponential) or whether, instead, it progressively declines towards linearity (as it actually
does).
# 144, Alastair,
Calculating the rate of GW is a complicated affair, I don't think that most who have came up with a
trend have claimed absolute certainty.
You could use 1m by 2050 as the benchmark and
calculate the GIMBI from there: thus by
trending (you
do nt have to use straight line) sea level rise to that date and valuing every additional piece of new information as it happens the
trend will be affected and therefore GIMBI.
I don't know how this was
calculated, but it seems to be a claim that «AR1 + linear
trend» is valid.
Our analysis shows that the 6 groups we mentioned above that have being
calculating the «global warming»
trends didn't
do a good enough job in accounting for these biases.
If he
did it the standard way, then he simply took the data and
calculated the probability of obtaining the same
trend, or a more extreme one, if there was no warming - i.e. if temperatures really
did follow a random walk.
In fact, it doesn't mention
calculating a linear
trend at all.
That graph doesn't show your extrapolated
trend thus it doesn't show the disparity between the extrapolated and
calculated trend.
In Part 1A and Part 1B we looked at how surface temperature
trends are
calculated, the importance of using Temperature Anomalies as your starting point before
doing any averaging and why this can make our temperature record more robust.
Perhaps I can find a way to expand the satellite hole in the modern record to
calculate a
trend but that doesn't sound too easy.
They
do not refer to
calculating trends.
Obvious mistakes would be
calculating the autocorrelations from a period which
does not show an approximately linear
trend, or using unrealistically short periods.
It doesn't really change much from
trends calculated for SAT in the 1910 to 1945 period; the numbers to 2 significant digits are between 0.15 and 0.14 C / decade.
Then in order to think that this
calculated value is important, you have to ignore the statistical range that shows that the chance of the cooling
trend being real doesn't pass textbook standard tests.
I
calculated the cycles using 1850 - 1950, as you
did, and then used a
trend of 0.42 for the entire reconstruction.
I
do not need a «robust analysis of uncertainty» to conclude that the accepted
trends are
calculated from garbage data, and can have no possible result other than to produce a much higher
trend than an analysis that properly accounted for these factors.
And when you properly
calculate the
trends, that from 1979 - 2008 NOAA ConUS 12 - mo averages (annual figures)
does not compare well to the UAH
trend (actually from 12/1978 to present), being 39 % higher.
How
do the
trends change when
calculating the
trends for the different classes from gridded data?
For example, changes in time of observation, adjustment for a move of a station that was previously sited next to a heat source to a better location (that now allows the station to be classed as Class 1 or 2), switch to a different temperature measurement device or system, etcetera, could explain why smaller classes of raw data don't track well with the overall
trend calculated from homogenized station
trend data.
George Turner (00:53:27): So if you're just looking at
trends and discarding stations, how
do you
calculate an average global temperature, or compare one year to another, based on
trends?
So if you're just looking at
trends and discarding stations, how
do you
calculate an average global temperature, or compare one year to another, based on
trends?
We don't use PCA to
calculate the
trend on the instrumental temperature record.
I don't know whether it would be closer if
calculated statistically from the real data instead of eyeballed, as the satellite
trend was.
But I
do know the difference between a simple linear interpolation and principal component analysis, and I can
calculate the two standard deviations range of uncertainty on a white noise linear
trend.
How
do you know how accurate the long term temp
trend against which you are
calculating the anomaly is?
The stated model
trends do not match linear
trends calculated from the MMH archive.
Well, one would have to believe that the folks of the GWPF don't even know how to
calculate a temperature
trend, if one wants to believe they
did it in good faith.
Monckton — quoted by Bickmore «One merely
calculates the least - squares linear - regression
trend over successively longer periods to see whether the slope of the
trend progressively increases (as it must if the curve is genuinely exponential) or whether, instead, it progressively declines towards linearity (as it actually
does).»
McCulloch accuses Steig et al. of appropriating his «finding» that Steig et al.
did not account for autocorrelation when
calculating the significance of
trends.
Even with a 6000 Mt / °C, that is about 3 ppmv / °C (I
calculated 2 - 4 ppmv), that doesn't change the
trend, as that is a two - way reaction on temperature.