It's important to remember that, as this is a systematic review study, it provides large -
scale average values rather than specific diet strategies.
Not exact matches
The
scale for this question was reversed, with 1 corresponding to «strongly agree» and 7 to «strongly disagree;» the
average response
value was 4.4.
Because the neutron decays on a time
scale similar to the period for BBN, accurate simulations of the BBN era require thorough knowledge of the neutron lifetime, the
average time required for a neutron to decay, but this
value is still not precisely known.
Responding on a
scale of 1 to 7, with 1 corresponding to «strongly disagree,» 4 to «neither agree nor disagree,» and 7 to «strongly agree,» the
average response
value was 4.5.
Our effective temperature
scale is between 0 - 200 K cooler than that expected from the Infrared Flux Method, depending on the adopted extinction map, which provides evidence for a lower
value on
average than that inferred for the Kepler Input Catalog (KIC).
If the Department believes percent proficient is also important for reporting purposes, these
values could be reported alongside the
average scale scores.
The
value advantage may or may not continue in the future, and even if it does continue it is impossible to know whether the
scale of the outperformance will remain similar to its historical
average.
C is not constant for the dT» / dt equation to apply because heat penetrates through different parts of the climate system (different depths of the ocean in particular) over different time
scales (also, if T» is supposed to be at some reference location or the global
average at some vertical level, T» at other locations will vary; C will have to be an effective C
value, the heat per unit change in the T» at the location (s) where T» occurs)
For temperature
scales where there are negative
values in the data set, root mean square will not produce a meaningful result because negative and positive
values of the same magnitude contribute the same positive amount to the
average.
Hunter and Brown calculated an
average acceleration in the central projection of the IPCCs AR4 A1FI emission scenario (including
scaled - up ice sheet discharge) of 0.002 mm per year over the period 1990 — 2010 (see the
value plotted at 2000 in their Fig. 1, ref.
The NCAR 2000 black carbon global emission is set at the
average of the GISS and GFDL 2000
values, and follows this
scaling in the future, for illustrative purposes.
The recent decadal
average is up around 1 C on this
scale, and well above the 2004
value indicated in the graph, and hence above the mean across all decades.
This product is a global -
scale climate diagnostic tool and provides a big picture overview of
average global temperatures compared to a reference
value.
The corresponding working quasilinear wave equation for the barotropic azonal stream function Ψm ′ of the forced waves with m = 6, 7, and 8 (m waves) with nonzero right - hand side (forcing + eddy friction) yields (34) u˜ ∂ ∂ x (∂ 2Ψm ′ ∂ x2 + ∂ 2Ψm ′ ∂ y2) + β˜ ∂ Ψm ′ ∂ x = 2Ω sin ϕ cos2 ϕT˜u˜ ∂ Tm ′ ∂ x − 2Ω sin ϕcos2 ϕHκu˜ ∂ hor, m ∂ x − (kha2 + kzH2)(∂ 2Ψm ′ ∂ x2 + ∂ 2Ψm ′ ∂ y2), [S3] where x = aλ and y = a ln -LSB-(1 + sin ϕ) / cos ϕ] are the coordinates of the Mercator projection of Earth's sphere, with λ as the longitude, H is the characteristic
value of the atmospheric density vertical
scale, T˜ is a constant reference temperature at the EBL, Tm ′ is the m component of azonal temperature at this level, u˜ = u ¯ / cos ϕ, κ is the ratio of the zonally
averaged module of the geostrophic wind at the top of the PBL to that at the EBL (53), hor, m is the m component of the large -
scale orography height, and kh and kz are the horizontal and vertical eddy diffusion coefficients.
Accounting for the characteristic spatial
scale ΔA of the relevant Airy function (see Basic Necessary Conditions and Assumptions) at the waveguide's boundaries, the
averaging of [S18] over Δ yields the following estimate for A˜m, max, at typical
values of l0 ≈ (0.3 − 0.5) × 10 − 6 m − 2, ΔQRA / Δ ≈ 0.3 − 0.5, and ΔA / Δ ≈ 0.2 − 0.25: A˜m, max ≈ K2 -LSB-(K2 + l02 + l04) / (m / a) 2] Kl0u ¯ 0ΔQRA2 Δ.
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.
Values are also averaged over successive four - month periods, to enable variations on upwards of the seasonal time scale to be seen more clearly than if monthly values had been pl
Values are also
averaged over successive four - month periods, to enable variations on upwards of the seasonal time
scale to be seen more clearly than if monthly
values had been pl
values had been plotted.
• The huge negative
values of coefficients of efficiency at those
scales show that model predictions are much poorer that an elementary prediction based on the time
average.
Citigroup recently produced a report that suggested they amounted to around 1 per cent of the
value of the Australian Stock Exchange — about the same
scale as the
average daily movement on the index.
In fact the Mauna Loa or global CO2 rise is much faster than linear... the differences between the mauna loa / global are negligible for the purpose of radiative transfer, and the difference in
average CO2 concentration between an «
average global» data - set and the Mauna Loa record since 1980 (for monthly
values) is only 0.65 ppm (and with a correlation coefficient r greater than 0.99) indicating that the Mauna Loa record is representative of global -
scale CO2 concentration as you'd expect with a well - mixed gas.
Might the «weather» of orbital cycles be impacted by K / T but not the «climate» — perhaps the trajectories of obliquity, precession and eccentricity would become completely different given sufficient time, but maybe with the same general character — periods and amplitudes and
average values being similar enough that a casual glance at any given time segment (on the necessary
scale to characterize the orbital cycle «climate») wouldn't look like anything different.
A survey of Twitter users from MarketingProfs referenced by eMarketer reports that, on a
scale from 1 to 5 (with 1 for strongly disagree and 5 and for strongly agree), the phrase «I find it exciting to learn new things from people»
averaged a score of 4.65 and «I
value getting information in a timely manner»
averaged 4.58.
Before plotting and interpreting the distributions, let me quantify the qualitative
values I used earlier: on a 0 to 10
scale, a bad movie is somewhere between 0 and 3, an
average one between 3 and 7, and a good one between 7 and 10.
Test — retest reliability of these
scales is high over a period
averaging 8 days (r
values =.82 — .93) and internal consistencies are adequate (α
values =.63 — .79; Achenbach & Rescorla, 2001).
All indexes are deseasonalized,
scaled to have an
average value of 100 for the period 2013 - 2015, and are adjusted for Redfin market share.
NeighborhoodScout is the only source for real estate
value trends and forecasts at a
scale 10X smaller than the
average ZIP code.