Title:
WHI Targeted Observation #2: Origin of the slow
solar wind
Authors:
L. Strachan, G. Poletto, L. Abbo, A. Breen, C. Deforest, A.Fludra, Y.-K. Ko, M. Kojima, P.K., S. McIntosh, Manoharan, C. Marque, M.Nishino, M. Tokumaru, K. Reeves, A. Sterling, S. Suess, M. Uzzo, A. Vourlidas,D. Webb
Additional
authors for synergy with WHI
Target of Opportunity #3 Filament cavity campaign: S. Gibson,
T. Kucera, D. Webb, D. Williams
Update History:
18 March 2008
Participating instruments and observatories
Targeted (all have not been confirmed)
Space Based:
SOHO/UVCS – campaign contact Leonard Strachan
SOHO/LASCO – campaign contact Simon Plunkett
SOHO/CDS – campaign contact Terry Kucera
SOHO/EIT -- campaign contact Terry Kucera
Ulysses – campaign contact Steve Suess
TRACE – campaign contact Kathy Reeves
Hinode/XRT – campaign contact Taro Sakao
(ISAS/JAXA), Alphonse Sterling
Hinode/EIS -- campaign contact David Williams,
Alphonse Sterling
Hinode/SOT -- campaign contact Scott McIntosh
SMEI -- campaign contact David Webb
Geotail – contact Masaki Nishino (for analysis)
Ground based:
OOTY Radio Telescope – campaign contact is P.K.Manoharan
EISCAT – campaign contact Andy Breen
NAGOYA –campaign contact Munetoshi Tokumaru
Nancay radioheliograph – campaign contacts
AlainKerdraon, Christophe Marque
Synoptic:
SOHO/LASCO-C2/C3 (higher cadence is desired)
STEREO/SECCHI/EUVI/COR1/COR2/HI
MLSO
ACE (SW composition)
Scientific Objective
Our primary goal is to understand the nature and
origin ofthe slow solar wind and its relation to coronal streamers.
In the event there is a cavity within the streamer, the lower coronal
observations in the core of the streamer will obtain cavity
observations.
Scientific Justification
We require multiple instruments in order to track
the slow wind from its origin in Sun's lower atmosphere, through the
corona, and out to interplanetary space. The slow solar wind, while
often associated with the streamer belt at solar minimum, most likely
originates from more than one type of coronal structure. The various
instruments required have capabilities that are suited for probing the
Sun in different observational regimes. Instruments with the highest
time cadence are best suited for studies of intermittent sources.
Spectroscopic instruments are best suited for time averagedobservations
of steady source regions. The strength of
the spectroscopic observations is that they can tag the wind by
characterizing the kinetic temperatures, outflow speeds, and
abundance composition of the solar wind source regions in the corona.
Operational Considerations
The majority of the coronal observations will be
made off-limb and so the same streamer regions will be observed twice
(1/2 rotationapart) with at least one observation made during the main
campaign period.
In general, observations will be made within the
core of the streamer (and in the cavity if one exists), and in the
streamer flanks, or legs.
Detailed Observing Plans per Instrument (may
need revision later, based on more detailed inputs from instrument
teams).
SOHO/UVCS
The OVI and LYA channels will be used for
measurements of line profiles and intensities of H I Ly-alpha, O VI
1032/1037, and other minor ion lines. FOV
is 40Õ(tangent to limb) x 28Ó (radial) adjustable from
1.7 to 10 solar radii.
SOHO/LASCO
Polarized brightness (pBs) and brightness images
are requested with a higher cadence than the usual synoptics. Full disk
images (C2 and C3) are requested.
OOTY
IPS measurements at 327 MHz will be made over the entire WHI campaign period.
Multiple lines of sight (using ~1000 radio sources) will be used to provide 3D views of the solar wind speed and density turbulence.
NAGOYA
Daily IPS observations between 22h and 7h UT will
be made starting as possible after 1 Apr. 2008. Approximately 30-40
lines-of-sight per day will be used for each scan. Tomographic
reconstructions of solar wind velocity covering the entire range of
heliographic longitude and latitude witha spatial resolution element of
1 deg by 1 deg will be made.
EISCAT
Not yet confirmed. Detailed schedule is TBD. Application for observing time in progress.
NANCAY radioheliograph
Daily observations from ~8:30 UT to 15:30 UT.
Observations will utilize 5 frequencies between 150 and 450 MHz
(additional frequenciesTBD). Spatial resolution about 1 arcmin
(depending on frequency); Time cadence: several images per sec and per
frequency. FOV: full sun images with a 4 Rs FOV.
GEOTAIL
Geotail/MGF (magnetic field), Geotail/LEP (plasma). Exact observingdates are TBD. For approximately 2 days in every 5 days, the Geotail spacecraftstays in the solar wind near the Earth's magnetosphere.
TRACE:
Main wavelength: 171 A
High cadence requested
FOV: 512"x512" -- to include both pointings for
targetted instruments (streamer core and streamer flank)
Available from 10 Apr 2008 onward: eclipses in all
orbits,from 10 to 30 min. duration
Hinode/XRT:
There will be two pointings, streamer core (or cavity center if
present) and streamer flanks.
Hinode/EIS:
Hinode/SOT:
There will be two pointings, streamer core (or cavity center if
present) and streamer flanks.
BFI: Ca II H (3968.5 Ang) full field
(200"x100") of region, 5s cadence
NFI: H I 6562.8 Ang. line core at 5s cadence (200"x100")
For the filtergraph observations, implement in "burst mode," with
observations
at highest reasonable cadence, around ~1 min, for ~10 min, followed by
~50 min
idle time; repeat this four times during the four-hour observing window.
SOHO/EIT:
One 284 A, full resolution, each hour + regular
195 CME watch during WHI observations.
SOHO/CDS:
STRE4W. Two pointings, streamer core (or cavity center if present), streamer flanks. Overall mosaics should overlap with Hinode-EIS spatially and temporally as much as possible. If Hinode time is limited, however, (e.g. to less than than the time needed for two iterations of STRE4W) CDS should ensure sufficient time is spent on each pointing even if exact temporal overlap with EIS is not possible. Preference should be given to overlapping temporally with the core rather than flanks in such a case.
STEREO/SECCHI
No special requests made. STEREO/SECCHI/COR1 and EUVI
synoptic data is desirable.
SMEI
SMEI will try to reserve the time period of campaign observations
(1700-2000 UT minimum, 1650-0230 UT maximum) as "no=cal" during the
campaign.
MLSO
TBD. No special requests made.
ACE
No special requests made.