09:30 〜 09:45
[PCG18-03] A belt-like distribution of gaseous hydrogen cyanide on Neptune's equatorial stratosphere detected by ALMA
キーワード：アルマ、海王星、大気化学
We present a spatially resolved map of integrated- intensity and abundance of Neptune's stratospheric hydrogen cyanide (HCN).
The analyzed data were obtained from the archived 2016 observation of the Atacama Large Millimeter/submillimeter Array.
A 0.42 x 0.39 arcsec synthesized beam, which is equivalent to a latitudinal resolution of ~20 degrees at the disk center, was fine enough to resolve Neptune's 2.24 arcsec diameter disk.
After correcting the effect of different optical path lengths, a spatial distribution of HCN emissions is derived over Neptune's disk, and it clearly shows a band-like HCN enhancement at the equator.
Radiative transfer analysis indicates that the HCN volume mixing ratio measured at the equator was 1.92 ppb above the 10-3 bar pressure level, which is 40% higher than that measured at the southern middle and high latitudes.
The spatial distribution of HCN can be interpreted as either the effect of the transportation of N2 from the troposphere by meridional atmospheric circulation, or an external supply such as cometary collisions (or both of these reasons).
From the meridional circulation point of view, the observed HCN enhancement on both the equator and the pole can be explained by the production and accumulation of HCN at the downward branches of the previously suggested two-cell meridional circulation models.
However, the HCN-depleted latitude of 60 degrees south does not match with the location of the upward branch of the two-cell circulation models.
The analyzed data were obtained from the archived 2016 observation of the Atacama Large Millimeter/submillimeter Array.
A 0.42 x 0.39 arcsec synthesized beam, which is equivalent to a latitudinal resolution of ~20 degrees at the disk center, was fine enough to resolve Neptune's 2.24 arcsec diameter disk.
After correcting the effect of different optical path lengths, a spatial distribution of HCN emissions is derived over Neptune's disk, and it clearly shows a band-like HCN enhancement at the equator.
Radiative transfer analysis indicates that the HCN volume mixing ratio measured at the equator was 1.92 ppb above the 10-3 bar pressure level, which is 40% higher than that measured at the southern middle and high latitudes.
The spatial distribution of HCN can be interpreted as either the effect of the transportation of N2 from the troposphere by meridional atmospheric circulation, or an external supply such as cometary collisions (or both of these reasons).
From the meridional circulation point of view, the observed HCN enhancement on both the equator and the pole can be explained by the production and accumulation of HCN at the downward branches of the previously suggested two-cell meridional circulation models.
However, the HCN-depleted latitude of 60 degrees south does not match with the location of the upward branch of the two-cell circulation models.