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Both the distributions of density and temperature of O+ ions have a dawn dusk asymmetry.
The global seasonal/longitudinal (s/l) distributions of density irregularity occurrences observed by ROCSAT-1 from 1999 to 2004 are plotted in the upper panels of each season - March equinox, June solstice, September equinox, and December solstice.
The difference of splitting energies between FM and AFM states of Mn kaolinite is small, and the distributions of density of states are similar except the spin directions are different.
The results indicate that the time required for steady state distributions of density and potential to evolve is determined by the plasma streaming velocity and the axial distance of relevance.
Here, we will carry out a similar study of correlation using a better temporal/spatial resolution in the monthly/latitudinal (m/l) distributions of density irregularity occurrences obtained by ROCSAT and the deep atmospheric convective clouds observed with the outgoing longwave radiation (OLR) measurements in the ITCZ.
Correlation studies carried out between the m/l distributions of density irregularities and the m/l distributions of OLR observations in the ITCZ as the proxy of gravity wave occurrences at seven longitude sectors indicate that good correlations between the irregularities and OLRs only exist in the South American sector and to some extent in the African sector.
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The distributions of densities were compared with ROC (receiver-operating characteristic) curves.
The distribution of density below the seafloor is the next most important influence.
The distribution of density of three subfamilies in two cell types was plotted in Fig. S4.
This may be combined with any distribution of density and axial velocity.
Probability distribution of density is written in terms of the probability distribution of contact points.
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