Heliophysics Events Knowledgebase Coverage Registry (HCR)
Observation Details
Overview Where Groups: Mode, FOV, # spectra in map Data Links
2019-02-28 07:45:04-08:50:15
HOP364 (plumes w/IRIS)
Observing magnetic field by Hinode(SOT/SP) in plume and non-plume regions seen by IRIS and AIA
x,y:-17",-159"
Max FOV:121"x122"
Target:Quiet Sun, Coronal Hole
Nearby Events
6302A Continuum Intensity121"x122"767 spectra
6302A Longitudinal Flux Density121"x122"767 spectra
6302A Transverse Flux Density121"x122"767 spectra
6302A Velocity 6301.5A121"x122"767 spectra

Level 1 Summary
Level 2 Summary
Level 1 Monthly
Level 2 Monthly
SP Cubes 19 MB
SOTSP: HOP364 (plumes w/IRIS)
2019-02-28T07:45:04 to 2019-02-28T08:50:15
Science Goal: Observing magnetic field by Hinode(SOT/SP) in plume and non-plume regions seen by IRIS and AIA
Program: HOP 364 Normal Map, 123"x123", 1-side, Q75
Target: Quiet Sun, Coronal Hole
xcen=-17 ycen=-159
Instrument: SOTSP
HOP/JOP: 364
Description: On-disk solar coronal plumes, best seen in EUV -- AIA 171 A -- form/decay as a result of flux convergence/divergence at their base (Wang et al. 2016
Avallone et al. 2018). It is proposed that flux cancellation, leading to small-scale jets at plume base, is the primary mechanism for plume formation (Raouafi and Stenborg 2014). Avallone et al. (2018) found that plumes are dominantly unipolar in HMI magnetograms, and have similar lifetimes, peak luminosities, base magnetic fluxes in quiet regions and coronal holes. They also found locations of flux convergence forming no plumes in AIA 171, thus suggesting that a critical magnetic field is necessary but not sufficient to form a plume. Moreover, this summer we found hardly any differences between bases of plume and non-plume regions using IRIS MgII and Si IV SJ and spectral data. We propose to repeatedly scan a large FOV of a coronal hole or quiet region by IRIS and SOT/SP, for more than a couple of days, to catch a few plumes, and similarly behaving non-plume areas, and investigate any differences between plume and non-plume regions -- this includes finding out if there is mixed-polarity flux present at plume/non-plume base in SP data.

On-disk solar coronal plumes, best seen in EUV -- AIA 171 A -- form/decay as a result of flux convergence/divergence at their base (Wang et al. 2016
Avallone et al. 2018). It is proposed that flux cancellation, leading to small-scale jets at plume base, is the primary mechanism for plume formation (Raouafi and Stenborg 2014). Avallone et al. (2018) found that plumes are dominantly unipolar in HMI magnetograms, and have similar lifetimes, peak luminosities, base magnetic fluxes in quiet regions and coronal holes. They also found locations of flux convergence forming no plumes in AIA 171, thus suggesting that a critical magnetic field is necessary but not sufficient to form a plume. Moreover, this summer we found hardly any differences between bases of plume and non-plume regions using IRIS MgII and Si IV SJ and spectral data. We propose to repeatedly scan a large FOV of a coronal hole or quiet region by IRIS and SOT/SP, for more than a couple of days, to catch a few plumes, and similarly behaving non-plume areas, and investigate any differences between plume and non-plume regions -- this includes finding out if there is mixed-polarity flux present at plume/non-plume base in SP data.

Annotations:
Hits: 38
Chief Observer
DeRosa (RCO)
Related Links
Cites: HOP364 (plumes w/IRIS)     
Timeline: gif use
See also
Datasets
Get All Data
saaIntervals hiIntervals

wavelength: 6302A Continuum Intensity cadence: -1 min fov: 121,122 images: 767 JavaScript Landing Page
wavelength: 6302A Velocity 6301.5A cadence: -1 min fov: 121,122 images: 767 JavaScript Landing Page
wavelength: 6302A Transverse Flux Density cadence: -1 min fov: 121,122 images: 767 JavaScript Landing Page
wavelength: 6302A Longitudinal Flux Density cadence: -1 min fov: 121,122 images: 767 JavaScript Landing Page
Time Series (SP Datacubes)