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For specific-heat measurements at lower temperatures, we can use both quasi-adiabatic and thermal-relaxation methods.
The conductivity was low (10−4 S cm−1) making the measurements at lower temperatures rather difficult.
Simulation results of terminal voltage and surface temperature are in good agreement with actual experimental measurements at lower C rates and dynamic load currents.
Microwave measurements, at lower vertical resolution but lower sensitivity to clouds, are therefore used synergistically with infrared measurements in "cloud-clearing" algorithms to provide global, all-weather atmospheric sounding capability.
From our growing data base of OH and O2 airglow intensity and temperature measurements at lower mid-latitudes, gravity wave information has been extracted by time series spectral analysis.
For a detailed comparison between the COSMIC and IRI-2012 model profiles, the percentage deviation in the electron density as compared to COSMIC RO measurements at lower (200 km), peak (hmF2), and topside (600 km) altitudes has been calculated and are listed in Table 1.
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To extend the measurement at lower energy, it is necessary to limit the extension of the He gas target.
Flexural-mode resonance devices, such as microfabricated AFM cantilevers, may be more reliable since they allow measurement at lower frequencies.
Whereas online and mail surveys, if done appropriately, can often enable more detailed measurement at lower cost, they can also suffer from low response rates, and substantial efforts are required to demonstrate that the included sample adequately represents the target population.
Super-rotation of the ionosphere was observed in zonal drift measurements, particularly at lower latitudes.
This might be caused by higher instabilities in the measurements system at lower frequencies.
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