In
calculating no trend between «windy» and «calm» days (with wind data obtained from NCEP / NCAR Reanalysis), Parker (2006), in effect, states that there is no modulation to speak of — in and of itself, that is a remarkable statement, or else there is no UHI to speak of.
Not exact matches
Calculate gross
trend momentum factor return as the difference in average (equal - weighted) actual returns
between quintiles / deciles with the highest and lowest expected returns.
Calculating an overall
trend in climate - related deaths is difficult due to the irregularity of severe storms, Boersma says, though the link
between extreme weather and chick death demonstrates that as extreme weather increases in coming years, chick death will increase in turn.
I am very cuious if you found a variance
between Upper Air and Surface warming... I
calculated total amospheric refraction temperatures, ie from data extracted by analyzing optical effects, some of my results show an impressive yearly warming
trend, much stronger than the surface based one.
These five ozone metrics are
calculated for all urban and non-urban ozone monitoring stations (section 4.2) available in the TOAR database, as present - day averages for 2010 — 2014 (section 5), as well as
trends between 2000 — 2014 (section 6).
Given these
trends, we decided to revisit the issue of teacher diversity, and we
calculated again our groundbreaking «Teacher Diversity Index,» an approach we pioneered in our first paper that ranks states on the percentage - point difference
between teachers of color and students of color.
-- I
calculated potential intensity
trends over the period 1980 - 2012 & The disparity
between the reanalysis potential intensity
trends over the past 30 years and the projected
trends over this century suggests either that most of the observed increase in potential intensity (and actual intensity of high category storms) is due to natural variability,....»
I am very cuious if you found a variance
between Upper Air and Surface warming... I
calculated total amospheric refraction temperatures, ie from data extracted by analyzing optical effects, some of my results show an impressive yearly warming
trend, much stronger than the surface based one.
«We have examined
trends in ocean mass
calculated from 6 yr of GRACE data and found differences of up to 1 mm yr − 1
between estimates derived from different GRACE processing centre solutions.
For purposes of the scenario, the hypothetical
calculated trend line for those seven consecutive peak years is chosen to run at +0.03 per decade starting from 1998, thus producing the «seven consecutive hottest peak years on record»
between 1998 and 2028.»
Some — instead of
calculating the
trend — simply draw a line
between these two years *, and for unapparent ** reasons that is not just opportunistic climate skeptics, but also real climate scientists with a funny definition of decades.
That graph doesn't show your extrapolated
trend thus it doesn't show the disparity
between the extrapolated and
calculated trend.
Basically, I
calculated the temperature
trend for each gridbox
between 60N and 60S, averaged the longitudinal values, and plotted a scaled image by latitude and depth.
The difference
between this and the NSIDC September average extent is
calculated and estimated with a linear
trend.
The research looked at growth
trends in the aviation industry and
calculated that emissions from the sector would rise rapidly
between now and 2050, assuming these
trends continued.
Obviously, neither the difference
between two maxima nor the
calculated regression during an arbitrarily selected period is an acceptable measure of
trend either.
«
Calculating the annual average temperature of the 119 temperature gauges in Nepal located at elevations on
between 72 m and 4100 m, reveals an upward
trend in values from 1961 — 1996 at a rate of almost 7C per 100 years (or 0.07 C / year)»
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.
These were used for comparing troposphere and surface
trends in the CCSP report that is a reference point for both Douglass and Santer, as shown in their Table 1 below...... As a first exercise, I
calculated the lapse rate
trend between these three surface indices (collated into TRP averages) and RSS T2LT (and T2, as well as corresponding UAH results.)
The ~ 0.14 C / decade
trend difference
between the well and poorly sited stations is significant as well: Our chance of obtaining the same results by random chance is
calculated by J - NG, using Monte Carlo methodic, at 0.00000.
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.
It is also evident that natural variations added to warming
between 1976 and 1998 — even if you simply remove the ENSO end states from the record and then
calculate trend.
These are both defendable choices, but when
calculating global mean anomalies in a situation where the Arctic is warming up rapidly, there is an obvious offset
between the two records (and indeed GISTEMP has been
trending higher).
This can be seen at: The formula used was: dCair = 0.5415 * F (emissions) / 0.21 + 3 * dtemp This resulted in a mean difference of
trends (observed -
calculated) = 0.00; correlation
between the series = 0.65; R ^ 2 = 0.42 (which is poor); stdev of the
calculated and observed series = 0.55 ppmv It looks like that the
calculated CO2 increase / variations are leading the observed ones.
By lagging the CO2 result from temperature changes one year, the
calculated variation was lagging the observed: The same coefficients were used, no difference in
trends and stdev, correlation
between the series = 0.732; R ^ 2 = 0.536 (which is fair).
• Successfully met self and company sales targets by a 100 %
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