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The secular variation curves in Fig. 7 confirm that the decrease ranges between 0 and 55 nT/year, with faster changes in the south (HER, SWP) than the north (TSU, MAU).
Due to local climatic conditions, frontal precipitation system and the topography controlling the precipitation, the δ18O content of atmospheric water decrease ranges from −0.15 to −0.5‰ per 100 m rise in altitude (Clark and Fritz 1997).
When aggregating precipitation data from the four RCMs for the four future periods and comparing to the period 1981 2000, winter precipitation decrease ranges between 7.2% (period 2041 2060) and 14.0% (period 2081 2100) and temperature increase ranges between 2.06 (period 2021 2040) and 3.80 °C (period 2081 2100).
Wyss and Habermann (1988) summarized seventeen cases of precursory seismic quiescence to main shocks with magnitudes ranging from M = 4.7 to 8.0, and found that (1) the rate of decrease ranges from 45%to90%0%, and (2) the duration of the precursors ranges from 15 to 75 months.
For quarterly SSD runs, the workload decrease ranges from 49.1%% (12.5 % signal loss) to 75.0 % (50.0%% signal loss).
Applying a signal threshold of N ≥ 5, results were as follows: For quarterly SSD runs, the workload decrease ranges from 13.8%0.0%.0 % signal loss) to 83.3 % (37.5 % signal loss).
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This represents a decrease ranging from 15 to 25% compared to the results obtained with MEA and MDEA.
A 25% reduction in RBF as induced by occluder inflation was associated with a median 32% decrease in RBV (range: 31% to 47%) and a 33% decrease (range: 45% decrease to a 18% increase) in mTT resulting in an overall 2% decrease (range: 43% decrease to 2% increase) in PI.
These results were confirmed using media containing a decrease range of phosphate concentrations.
The decrease ranged from 3.2 to 10.0%.
For the selection model, the decrease ranged from 13% for escitalopram to 26% for paroxetine.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com