Evolution of Solar Subsurface Meridional Flows in the Declining Phase of Cycle 23

Astronomy and Astrophysics – Astronomy

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

18

Sun: Activity, Sun: Helioseismology, Sun: Interior, Sun: Sunspots

Scientific paper

We study the evolution of meridional flows in the solar convection zone extending to a depth of 0.793 Rsolar in the period 2000-2003 with helioseismic data taken with the Taiwan Oscillation Network (TON) using the technique of time-distance helioseismology. The meridional flows of each hemisphere formed a single-cell pattern in the convection zone at the solar minimum. An additional divergent flow was created at active latitudes in both hemispheres as the activity developed. The amplitude of this divergent flow correlates with the sunspot number: it increased from solar minimum to maximum (from 1996 to 2000), and then decreased from 2000 to 2003 with the sunspot number. The amplitude of the divergent flow increases with depth from 0.987 Rsolar to a depth of about 0.9 Rsolar, and then decreases with depth at least down to 0.793 Rsolar.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Evolution of Solar Subsurface Meridional Flows in the Declining Phase of Cycle 23 does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Evolution of Solar Subsurface Meridional Flows in the Declining Phase of Cycle 23, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Evolution of Solar Subsurface Meridional Flows in the Declining Phase of Cycle 23 will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1301002

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.