Previous versions of the RSS dataset have used a diurnal climatology derived from general circulation model output to remove the effects of drifting
local measurement time.
Not exact matches
I made dinner rolls for the 1st
time and they were a little denser than I wanted... was wondering if the xanthem gum was the culprit... so I looked up adjusting xanthem gum for dense bread and it brought me here... your article says if bread is rubbery it might have too much xanthem... I have perfected my cupcakes they are light fluffy and moist... and good enough that I was able to sell them at a
local cafe for 3.00 a piece and could not keep up... anyway the xanthem gum
measurements for cakes is supposed to be 1/2 tsp per cup and I only use 1/4 tsp per cup... so I am thinking if I reduce the xanthem in the rolls it would produce an airier roll... as everyone knows gluten free flours can be expensive... and I wanted to avoid making a failed batch as bread and cake are a bit different... the 1st batch tased great... just won't leave much room for food due to density... as is the problem with lots of gluten free stuff... am I on the right track?
The first full day of MAMM flying kicked off at 9 am
local time, as the FAAM Atmospheric Research Aircraft (ARA) took to the skies to begin the morning's
measurements of wetland emissions.
Here, we report on
local and global changes in MHW characteristics over
time as recorded by satellite and in situ
measurements of sea surface temperature (SST) and defined using a quantitative MHW framework, which allows for comparisons across regions and events1.
While there remain disparities among different tropospheric temperature trends estimated from satellite Microwave Sounding Unit (MSU and advanced MSU)
measurements since 1979, and all likely still contain residual errors, estimates have been substantially improved (and data set differences reduced) through adjustments for issues of changing satellites, orbit decay and drift in
local crossing
time (i.e., diurnal cycle effects).
While there remain disparities among different tropospheric temperature trends estimated from satellite Microwave Sounding Unit (MSU and advanced MSU)
measurements since 1979, and all likely still contain residual errors, estimates have been substantially improved (and data set differences reduced) through adjustments for issues of changing satellites, orbit decay and drift in
local crossing
time (i.e., diurnal cycle effects).
«Temperature Tools The temperature log can be used to give a useful profile of the thermal conductivity of rocks adjacent to the borehole and a
measurement of the
local geothermal gradient when the borehole is allowed to stabilize for a period of
time (at least several days) after drilling ceases, assuming there is no convection in the borehole.
As a side note, Callendar was the man who did throw out a lot of
local CO2
measurements made by chemical methods to show a curve for what he thought that the real increase of CO2 over
time was until then.
Then, after 1960 where the blanket of temp readings expanded, became more dense and more synchronized to
Time of Day for the
measurements (i.e., became more accurate), the reality was finally expose — tree rings DO NOT correlate to temperature at all but are driven more by other
local factors (like days above freezing and not the amount of delta above freezing, freezing or some other minimal temp being a point where growth occurs).
In addition to treating cloud transmission based only on the
measurements at the
local time of the TOMS observations, the results from other satellites and weather assimilation models can be used to estimate atmospheric UV irradiance transmission throughout the day.
And even if they corrected their methods; which they can't do, because it would take all the money on the planet to buy enough thermometers; it is all for naught, since there is no physical cause and effect connection between a
local surface or near surface Temperature
measurement, and the energy flows that are occurring at that location at that
time; so mean global temperature tells us nothing about whether the earth is gaining or losing total energy.
I can take
measurements of solar insolation starting at sunrise and ending at
local noon, extrapolate it into the future, and then claim the earth will be melted in a short
time.
Once the
local effects are understood, it should be a much simpler matter to integrate them over
time and space using satellite cloud
measurements to a more generalized climate sensitivity over various bands / latitudes of the earth.
The
measurements on the right were taken just before midday «
local solar
time».
Observation
times also changed during the war years from 6 - hourly
measurements to a thrice - daily regime with many more
measurements made at 8 am and 8 pm
local time with another
measurement at noon.
Pilot balloon
measurements during BoDEx point to a marked diurnal cycle in the wind speed such that the LLJ accelerates over a near frictionless inversion by night but is mixed down to the surface by extreme radiative heating through modification of eddy viscosity to produce a surface - wind - speed maximum by ≈ 1100
local time (32).
The sales rep also said one of his
local suppliers had some slabs in stock, so the turnaround
time after
measurement would only be a few days.