We air - deploy buoys that
measure the temperature profile of the upper ocean continuously and report the data via Satellite.
The measured temperature profile of the atmosphere is such evidence, the IR measurements on the surface and from satellites are such evidence.
Not exact matches
Now, by combining his measurements with the
temperature profiles measured by the Finnish Meteorological Institute, Professor Laine has found an explanation for the mechanism that creates the sound.
The radar wind profiler / radio acoustic sounding system (RWP / RASS), available in 915 - MHz (for U.S. deployments) and 1290 - MHz (for foreign deployments),
measures wind
profiles and backscattered signal strength between (nominally) 0.1 km and 5 km and virtual
temperature profiles between 0.1 km and 2.5 km.
Using a
temperature gun to
measure homemade and restaurant meals, he started creating
temperature profiles for a variety of foods.
Argo: Argo is a global array of 3,800 free - drifting
profiling floats that
measures the
temperature and salinity of the upper 2000 m of the ocean.
The initial objective of the Argo program was to operate 3200
profiling floats in the ice - free waters from 60 ° N to 60 ° S to
measure pressure,
temperature, and salinity in the upper 2000 meters of the ocean.
It
measures the vertical
profile of pressure,
temperature and humidity (PTU) as the balloon ascends through the atmosphere.
Winds are estimated by using an upward - looking Doppler radar, while
temperature and moisture
profiles are evaluated by using a vertically pointing radiometer that
measures electromagnetic emissions of selected wavelengths at various heights in the troposphere.
The
measured local vertical
profile of
temperature in the air is called the environmental lapse rate.»
The radar wind profiler
measures wind
profiles, backscattered signal strength, and virtual
temperature profiles.
«The Microwave Limb Sounder (MLS) experiments
measure naturally - occurring microwave thermal emission from the limb (edge) of Earth's atmosphere to remotely sense vertical
profiles of atmospheric gases,
temperature, pressure, and cloud ice.
We can repeat our earlier observation that CET instrumental to 1659 - this time augmented by the reconstruction using historical records to 1538, demonstrates a
temperature profile that looks quite different to significant periods of the remainder of the Northern Hemisphere if the official version of extended climate - as epitomised by the «Hockey stick» - is taken as the appropriate set of data which it should be
measured against.
What they should do, I think, is estimate the uncertainty in the frequency domain, and jitter those spectra and see how the
temperature profiles differ across a collection of jitters from the
measured data.
First, there is the «true» OLR, which can be
measured from space or calculated for observed or specified atmospheric conditions (
temperature profile, well - mixed GHG mixing ratios, humidity
profile).
The instrument
measures naturally occurring microwave thermal emission from the edge of Earth's atmosphere to remotely sense vertical
profiles of atmospheric gases,
temperature, pressure and cloud ice.