|
measurement of the He + content of CIR energetic ions for some selected intervals. The comparison of the CIR observations by

SOHO, WIND and Ulysses (spacecraft at different locations) will provide spatial gradient information that will tightly constrain

theories of shock acceleration and injection mechanisms. The results should help establish the origin of the ions as predomi-

nantly solar wind ions or interstellar pickup ions, the difference in the efficiency of shock acceleration at the forward and

reverse shocks, and whether the spatial gradients and energy spectra are related as required by current theory.

Planetary Science: Venus Tail Rays In 1996 June, Venus passed through a very close inferior conjunction with the Sun. At that

time CELIAS/CTOF was measuring heavy ions in the solar wind ~4.5x107 km downstream of Venus. During the passage of

SOHO through the Venus wake, three encounters were made with unusual fluxes of O + and C + ions. Their energy distributions

resembled those of the tail rays known to originate in the Venus nightside ionosphere. The C + abundance was ~10% of O +. The

observed O+ speed was very close to the simultaneous solar wind speed and the O+ temperature was a cool 5600 K/amu. The

flux densities for the three events were (2.1-4.4)x103 cm - 2 s - 1.
The Sun-Earth Connection
|
 |
|
An ISTP case study: The 1997 April 7-11 event On 1997 April 1, and again on 1997 April 7, SOHO-EIT was able to observe

supersonic blast waves propagating outward from the site of a modest flare, across nearly the entire surface of the Sun in 1.5 MK

coronal plasma. SOHO-MDI has been able to observe changes in the longitudinal field at the footpoints of these events. The

soft x-ray signature of the flare was observed by SOHO-SEM and by GOES-8,9. The WIND-WAVESinstrument detected Type

III emissions at 13:59 UT on April 7, consistent with the SOHO observations of the flare. The April 7 event apparently led to

two CME's: one directed away from the Sun-earth line, and a halo event. Since launch, SOHO-LASCO has observed several

halo CMEs. These are CMEs that appear as a halo around the entire occulting disk, indicating that the event is directed either

toward or away from Earth. As the April 7 event left the LASCO field of view, WAVESbegan tracking the progress of the event

using TypeII radio emissions. This type II emission, associated with the CME shock, was tracked from a fraction of a solar radii

to ~10-12 solar radii and represents the first occassion that WAVES and LASCO/EIT have been able to make simultaneous

observations.

The flare produced a solar energetic particle event (SEP) that was observed in situ by SOHO/ERNE beginning on April 7. The

interplanetary shock observed by SOHO-CELIAS/PM at ~13 UT on April 10 is associated with a small peak in the ERNE

particle intensity (1.6-3.2 MeV), and a large increase in the SOHO-CELIAS/STOF suprathermal helium flux (85-540 keV). The

STOF composition indicates that interstellar pick up ions (He +) are one of the important seed populations for the particles being

locally accelerated at the shock, in fact a remarkable He +/He+2 ratio of ~1 is observed!

On April 11, the most intense auroral event (K of 8) since the launch of SOHO or POLAR occurred. Throughout its four-day

evolution, the ISTP observatory effectively remained in observational contact with the eruption, collaborating with ground-

based and geosynchronous satellites to capture the origin, propagation, geospace impact, and dissipation of the event. We

believe that we have now, for the first time and by combining observations in near realtime from SOHO, WIND, and POLAR,

observed a solar-terrestrial storm from its inception in the lower corona to its impact on the magnetosphere. While the initial

news media coverage of this event was out of proportion to the probable seriousness of its terrestrial effects, the enormous

response from both media and private citizens to the media coverage indicate that there is widespread interest in solar-terrestrial

physics.

Coordination and dissemination of data sets for Sun Earth Connection Events are being done through ISTP workshops and the
World Wide Web (which allows greater access to a wider user group). The event of 1997 April 7-11 is described at:
http://www-spof.gsfc.nasa.gov/istp/event_apr97/ and http://sohowww.nascom.nasa.gov/gallery/current/ .
|
 |