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NoRH%20Observations%20of%20Prominence%20Eruption

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Title: NoRH%20Observations%20of%20Prominence%20Eruption


1
NoRH Observations of Prominence Eruption
  • Masumi Shimojo
  • Nobeyama Solar Radio Observatory
  • NAOJ/NINS

2004/10/28 Nobeyama Symposium 2004 _at_ SeiSenRyo
2
Todays Topic
  • Introduction
  • What are advantages of prominence eruption
    observations using Nobeyama Radioheliograph?
  • 12 years NoRH Observations of Prominence
    Activities
  • Automatic Detection of Prominence Activities
  • Solar Cycle and Prominence Activities

3
Introduction
  • NoRH observes the thermal microwave (17/34GHz)
    emission from prominences.
  • The typical brightness temperature of a
    prominence before the eruption is about 10,000K.
  • The prominence is usually optically thick plasma.
    Hence, the filament is also the dark feature in
    radio images.

4
Advantages of NoRH Observation 1
  • The influence of the weather is small.
  • NoRH can observe the Sun on cloudy and rainy days
    !!
  • Ex. The transit of Venus
  • But, snow and heavy rain influence the image
    quality.

5
Advantages of NoRH Observation 2
  • Large Field of View
  • 1 Rsun
  • High Time Resolution
  • Flare Observation 100 msec
  • Normal Observation 1 sec

Courtesy of Y. Hanaoka
6
Advantages of NoRH Observation 3
  • The effect of the Doppler shift is very small for
    NoRH Observations, since NoRH observe the thermal
    microwave emission.
  • The brightness temperature of prominence is
    depend only temperature and emission measure of
    prominence plasma.
  • NoRH can observe the high-speed prominence
    eruption.

7
Disadvantages of NoRH Observation
  • It is difficult to resolve the fine structures in
    the prominence.
  • Usually, we can find moving features in the
    prominence. But, the features are made from the
    side-lobes.

8
Advantages of NoRH Observation
ltltSummarygtgt
  • The influence of the weather is small.
  • Large Field of View
  • High time resolution
  • The effect from Doppler shift is small.

We try to develop the automatic detection
system for the prominence eruption.
9
Todays Topic
  • Introduction
  • What are advantages of prominence eruption
    observations using Nobeyama Radioheliograph?
  • 12 years NoRH Observations of Prominence
    Activities
  • Automatic Detection of Prominence Activities
  • Solar Cycle and Prominence Activities

10
Automatic Detection Method Step 1
  • NoRH makes 44 17GHz images, everyday.
  • The time resolution of the images is 10mins.
  • The images are made in quasi real-time.
  • The automatic detection program runs after the
    daily observation.

28 Aug, 2000 004626 UT Original Image
11
Automatic Detection Method Step 2
  • Erase faint features and disk.
  • Tb of faint features is smaller than 2000K.
  • Tb of faint features is smaller than 1/100 of the
    maximum Tb in each image.
  • We delete the major side-lobe effect on the
    method through the process.

After deleted faint features and disk
Original Image
12
Automatic Detection Method Step 3
  • Make a daily average image.
  • We use all 17GHz images on the day.
  • Before calculate the average, we delete disk.

average
daily average image
44 images
13
Automatic Detection Method Step 4
  • Find enhanced pixels in each image.
  • The criterion of enhancements is 6 times larger
    than the daily average image at each pixel.



After deleted faint features
Daily average image
gt 6
14
Automatic Detection Method Step 5
  • If there are the enhance pixels in the images,
    the center of gravity of enhanced pixels is
    calculated from each images.

15
Automatic Detection Method Step 6
  • Define the structure as the limb events, if the
    structure satisfies the following criterions.
  • The center of gravity of enhanced pixels is not
    in the disk
  • The lifetime of the structure in the NoRH's FoV
    is over 30 min.
  • The number of enhance pixels is larger than 400.

16
The method catches these phenomena
  • Prominence activities
  • Eruptive Prominence
  • Disappearance of Prominence (not Eruption)
  • Morphology changing of Prominence
  • Limb flare
  • Flare Loop on the Limb

17
The undetectable events using the method
  • Very fast eruptive events (v gt 300km/s)
  • Because we use 10 min resolution
  • Very long duration events
  • Because we use the daily average as the quiet
    state.
  • Simultaneous eruptive events.
  • Because we use the center of gravity for the
    identification.
  • Weak brightness event
  • The NoRH dynamic range is 1/100.

18
The results of the Automatic Detection
System
  • Survey period 1992/07/01 2004/10/12
  • Over one Solar Cycle
  • Observation time 0800 1530 (JST)
  • The number of detected events 389
  • The percentage of limb flares is less than 5 .
  • You can see the list on our web.
  • http//solar.nro.nao.ac.jp/norh/html/prominence
    /

19
Solar Cycle and Prominence Activities1Number
Variation during One Solar Cycle
  • The number variation of prominence activities is
    similar to that of sunspots.
  • The raise phase of prominence activities is
    shorter than that of sunspot.

Cross Prominence Activities Red line Sun
spot Number
20
Solar Cycle and Prominence Activities2The
distribution of prominence activities of Cycle
21/22
Background KP Magnetogram limb event Size
of Size of Activities 1992 1999
1993 2000 1994 2001 1995 2002
1996 2003 1997 2004 1998
21
Solar Cycle and Prominence Activities3Filament
bands and Prominence Activities
Contour Standard deviation of coronal green
line Thick Line the migration trajectories of
neutral filament bands for cycle 20 (Makarov
and Sivaraman, 1989 Solar Phys. 123, 367)
  • The distribution of the activities is similar to
    the neutral filament bands.

22
Solar Cycle and Prominence Activities4The
distribution of filaments and prominence
activities
Background The distribution of neutral lines
The distribution of filaments of Cycle 21 and
22 Aa Active Region Filaments, Aq Quiescent
Filaments Ap Polar Filaments (Mouradian and
Soru-Escaut, 1994, AA, 290, 279)
  • Prominence activities occurred on the neutral
    filament bands.

23
Solar Cycle and Prominence Activities5When a
polar-crown prominence erupt? 1
  • The polar crown prominences erupted, when the
    polarity of the polar magnetic field reverse.
  • (Gopalswamy, et al.,
  • 2003, ApJ. 598, L63)

24
Solar Cycle and Prominence Activities5 When a
polar-crown prominence erupt? 2
  • The polar-crown prominences erupted when some
    magnetic poles appeared near the polar-crown
    neutral line.
  • Prominence/filament eruptions need magnetic
    activities, like an emerging flux (Feynman and
    Martin, 1995, JGR, 100, A3,3355) , the intrusion
    of opposite polarity magnetic fields.

25
Solar Cycle and Prominence Activities 6 Size of
Active Prominences
  • The frequency distribution of size of active
    prominences show the power-law (like)
    distribution.
  • The correlation between the latitude and size is
    weak.

26
Solar Cycle and Prominence Activities 7 Size of
Active Prominence and Solar Cycle
Neutral lines at Solar Minimum
Neutral lines at Solar Maximum
The scatter plot of date and size of prominence
eruption The diamond marks indicate the average
prominence size of the year.
  • The variation of average active prominence size
    similar to the solar cycle.
  • The size of active prominence seems to relate the
    complexity of the neutral line on photosphere.

27
Summary 1
  • We developed the automatic detection system for
    limb events, mainly prominence activities.
  • The system found 398 events from July, 1992 to
    Oct, 2004.
  • The number variation during solar cycle of
    prominence activities is similar to that of
    sunspots.

28
Summary 2
  • Prominence activities occurred on the neutral
    filament bands.
  • The frequency distribution of size of active
    prominences show the power-law (like)
    distribution.
  • The size of active prominence seems to relate the
    complexity of the neutral line on photosphere.

29
The undetectable events using the method
  • Very fast eruptive events (v gt 300km/s)
  • Because we use 10 min resolution
  • Very long duration events
  • Because we use the daily average as the quiet
    state.
  • Simultaneous eruptive events.
  • Because we use the center of gravity for the
    identification.
  • Weak brightness event
  • The NoRH dynamic range is 1/100.

30
Automatic detection using 3 minuets
time resolution images
Coming soon!!
Using 10 min time resolution images
Using 3min time resolution images
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