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He said he leaned toward the restrained and ascetic in design, in keeping with the principles expressed by the German industrial designer Dieter Rams in his book "Die leise Ordnung der Dinge," or "The Gentle Order of Things" — meaning things can have a very quiet value without flourishes or "shouting".
This is another reason that the magnetotail (where the field intensity is much weaker than in the main body) cannot store the magnetic energy of more than 2 × 1022 ergs; if the lobe field could accumulate 2 × 1022 ergs between 10 and 20 Re, the magnetic field intensity would have to increase 30 ∼ 50%% from a quiet value; there has been no report of such a change of the lobe field.
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She saw her similarities to her father, besides the physical ones (she has his mouth, chin and long slender fingers): he was quiet, valued privacy and didn't like huge parties.
12.4°N, 1.5°W) covering a solar cycle, we have presented preliminary results from the analysis of solar dependence of six different classifications of the data: (i) daily values, (ii) monthly mean, (iii) daily quiet values (with Ap ⩽ 20), (iv) monthly-quiet-mean values, (v) monthly median, and (vi) monthly-quiet-median values.
The exceptions are: the sharp daytime hmF2 increase by ~ 100 km observed at Irkutsk on September 13, which is not reproduced by GSM TIP; the daytime hmF2 quiet values observed at Yakutsk, which is much smaller than the GSM TIP values.
GPS TEC increased by a factor of 2.2 in comparison with quiet day value (from 8.6 to 19 TECU).
The GPS-TEC started to increase between 04 30 and 09 30 UT and remained higher than the quiet mean value between 07:00 and 17:00 UT on 25 October 2011.
The IRI-model TEC on the storm day is found to be the same as the quiet mean value, indicating that the IRI model is not able to predict the storm's impact.
From this figure it is seen that the COSMIC electron density on the storm day is found to increase compared to the quiet mean value, up to altitudes greater than 300 km.
The IRI model electron density on the storm day is found to be the same as the quiet mean value at all altitudes (Figure 6b), which is also similar to those predicted by the IRI-TEC results (Figure 5c).
Fig. 7. (a) Variations with the dip angle of the mean (5 quiet days) value of ΔH for June 2000 for the stations in the western Pacific region at selected hours and (b) Variations with the dip angle of ΔH on 18 June 2000 at the stations in the western Pacific region at selected hours.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com