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Daily mean values of different solar and geomagnetic activity indices, and more than 1400 nights of airglow brightness and rotational temperature measurements (mostly from El Leoncito, 31.8°S) are available for this study.
The daily mean values of MD measurements were calculated for each patient.
All the quantities shown in this section are derived from the daily mean values determined as follows.
The probability distribution of temperature has been calculated from the daily mean values in the investigated 20-year time periods based on the normal distribution function.
Night and daily mean values have been plotted for each parameter and graphics, as Figures 1, 2, 3 and 4 shown, have been obtained for each sampling site.
Whereas observed daily mean values overlapped with the upper range of literature values, maximum single leaf-deposition values greatly exceeded those previously reported.
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We also show that severe geomagnetic storms can increase ODR by up to 117% (from daily mean value).
The positions of the statistical auroral oval are superposed in solid white lines for conditions from very quiet (IQ = 0) to very disturbed (IQ = 6), proportionally to the daily mean value of the Kp index.
The positions of the statistical auroral oval (Feldstein and Starkov 1967; Holzworth and Meng 1975) are superposed in white line for conditions from very quiet (IQ = 0) to disturbed (IQ = 6), proportionally to the daily mean value of the Kp index.
Summary statistics were determined, and AUCtau was compared to the AUCtau in adults when treated with darunavir/ritonavir 800/100 mg once daily (mean value of 93.0 μg·h/ml and a geometric mean value of 89.7 μg·h/ml, determined from ARTEMIS data [data on file]).
The observed, daily mean temperature values of the Wetzstein site were filtered for optimal soil water and light conditions and normalized (see Methods: Observational data and data filtering).
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