This change can produce small variations in the average
daily temperatures measured.
Not exact matches
«With our moorings we
measure current velocities,
temperatures, salinities and pressures every 15 minutes, from which meaningful
daily values of the [meridional overturning circulation] strength can be derived,» Kanzow says.
* Metabolic
Temperature Graph ™: A method for
measuring and interpreting
daily temperatures to gain insight into metabolic energy issues associated with both adrenal and thyroid function.
The difference is that while BMR only
measures basic processes of breathing, blood circulation, and
temperature regulation in a completely resting state, RMR also includes energy expended by digestion and non-exercise
daily movements, like getting dressed and lifting your fork to your mouth.
We take careful
measures to ensure our
Daily Digestive Enzymes are stored in
temperature - controlled facilities.
I am curious though, is your data based on the
measured daily low
temperature?
Shows that a suite of modeled and derived
measures (produced from
daily maximum — minimum
temperatures) linking plant development (phenology) with its basic climatic drivers provide a reliable and spatially extensive method for monitoring general impacts of global warming on the start of the growing season
The world wide surface station
measured average
daily rising temp and falling temp is 17.465460 F / 17.465673 F for the period of 1950 to 2010, not only is the falling
temperatures slightly larger than rising
temperatures, 17.4 F is only 50 % -70 % of a typical clear sky
temperature swing of 25F to 30F, which can be as large as +40 F depending on location and humidity.
«As you
measure the high and low
daily temperatures each year, it normally becomes more difficult to break a record after a number of years.
So one could
measure the
daily fluctuation in
temperature range.
Again, an indirect
measure is used — this time it was changes in
daily temperature range (DTR) between urban and rural stations.
It seems like the best thing to do would be to
measure the difference between the measurement of choice (
daily high, presumably, since we're in the business of talking about black - swan high -
temperature events this time of year) and the trend line rather than a flat baseline.
Temperatures aloft can be
measured in a number of ways, two of which are useful for climate monitoring: by radiosondes (balloon - borne instrument packages, including thermometers, released
daily or twice
daily at a network of observing stations throughout the world), and by satellite measurements of microwave radiation emitted by oxygen gas in the lower to mid-troposphere, taken with an instrument known as the Microwave Sounding Unit (MSU).5 The balloon measurements are taken at the same Greenwich mean times each day, whereas the times of day of the satellite measurements for a given location drift slowly with changes in the satellite orbits.
New analyses of
daily maximum and minimum land - surface
temperatures for 1950 to 1993 continue to show that this
measure of diurnal
temperature range is decreasing very widely, although not everywhere.
Thermometers that
measure daily maximum and minimum
temperatures are usually housed in Stevenson screens — the familiar white - painted, louvered boxes placed a few feet above the ground.
There is consistence [70] between the estimates of the ISCCP, the global albedo, the insolation
measured at the surface and the length of the
daily insolation observed in many places: all of them are likely to explain the
temperature changes.
That is not to say that there may not be noticeable impacts on shorter term
measures — local and seasonal trends and possibly
daily temperature range (DTR) effects for example.
Crazy statistical inference of the week We can
measure a higher
daily average
temperature while accumulating less heat due to the biases created by the minimum.
In no way is this comparable to the manufacture of data where no measurements have been taken or the substitution of one
measured variable (
daily mean land air
temperature) with another (instantaneous SST observations) whose sampling method varies, is exceedingly uneven geographically, and no credible, alias - free time - series can be obtained.
UAH and RSS aren't thermometers
measuring temperatures at a fixed time and place every day (or even the
daily high or low).
But is
temperature uncertainty reported as if it derives from the average anomaly and not derived from the
measured daily Tmin and Tmax?
In a nutshell, Zhao's technique, published in Geophysical Research Letters, extrapolates the
temperature of the ocean's innards by using satellites to
measure the
daily sloshings of the seas that are created by the moon.
I apologize for reposting my comment: The Met Office says «The «mean
daily temperature» is the average
temperature in each 24 hour period,
measured at 1.5 metres above ground level.»
Measured daily air
temperatures by the DMI at 80 north latitude through EVERY summer since 1958 have remained steady between 1958 and 2000, and, in fact, have declined between 2000 and 2012 — which included record low sea ice extents in 2007 and 2012.