E. Kyrola et al., PRELIMINARY RETRIEVAL OF SOLAR-WIND LATITUDE DISTRIBUTION FROM SOLAR-WIND ANISOTROPIES SOHO OBSERVATIONS/, J GEO R-S P, 103(A7), 1998, pp. 14523-14538
The Solar Wind Anisotropies (SWAN) instrument on board the SOHO spacec
raft measures Lyman alpha radiation emanating mainly from neutral hydr
ogen gas in the solar neighborhood. This gas is part of the local inte
rstellar cloud in which the Sun and the heliosphere are immersed. Meas
urements of Lyman alpha can be used to infer the local cloud character
istics like the velocity and the direction of the flow, gas temperatur
e, and density. The strong interaction between the Sun and the neutral
hydrogen gas also makes possible investigations of solar characterist
ics by Lyman alpha measurements. In this work we will concentrate on d
eriving the latitudinal distribution of solar-induced ionization from
SWAN Lyman alpha maps measured in 1996 at a time of the solar minimum.
From the ionization we derive the distribution of the solar wind mass
flux SWAN Lyman alpha data show that the ionization and the mass flux
are nearly flat for all solar latitudes except the narrow belt from -
20 degrees to 20 degrees around the solar equator. In this region, ion
ization and the solar wind mass flux show a definite increase, which c
an be seen as an intensity depression in the Lyman alpha data from dir
ections near the ecliptic. These results confirm earlier in situ measu
rements by Ulysses during the present minimum and Lyman alpha measurem
ents by Prognoz satellites 20 years ago.