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Polar Region Ac.vity Masumi SHIMOJO Nobeyama Solar Radio Observatory NAOJ/NINS SOLARC Science Defini.on Mee.ng 2 nd @ ISAS 2010/3/11

Polar&Region&Ac.vity&...Magne.c&Field&in&the&Polar&Region& by& Hinode’Observaons • The&polar&region&is&doced&with&small&(~4000km)&and&strong& (~1000&gauss)&magne.c&patches&(kG@patches

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Page 1: Polar&Region&Ac.vity&...Magne.c&Field&in&the&Polar&Region& by& Hinode’Observaons • The&polar&region&is&doced&with&small&(~4000km)&and&strong& (~1000&gauss)&magne.c&patches&(kG@patches

Polar  Region  Ac.vity  

Masumi  SHIMOJO  Nobeyama  Solar  Radio  Observatory  

NAOJ/NINS

SOLAR-­‐C  Science  Defini.on  Mee.ng  2nd  @  ISAS  2010/3/11

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Outline

•  Introducing  the  results  obtained  by  Hinode.  – Magne.c  field  in  the  polar  region  

– Coronal  Ac.vity  in  the  polar  region.  • What  is  the  next  step  of  the  study  of  polar  region.  

•  Polar  region  studies  by  SOLAR-­‐C  mission

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The  Strong  Magne.c  Patch  (kG-­‐Patch)  in  the  Polar  Region  (Tsuneta  et  al.  2008)

3

South    Pole  

85°  

80°  

75°  

70°  

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4

Photosphere

kG  patch

Field  line

Fanning  magne.c  field  lines  of  kG-­‐patches

(Ito  et  al.  2010,  Shiota  et  al.  2010)

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Magne.c  Field  Distribu.on    in  the  Polar  Region  and  near  the  Equator  

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PDF

KG-­‐Patch

There  is  no  difference  about    Horizontal  Magne.c  field  

Magne.c  Field  Strength  (Gauss)

Ito  et  al.  2010

Red:  North  Polar  Region  Blue:  Quiet  region  near  Equator  Solid:  Ver.cal  field  Dashed:  Horizontal  Field

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Magne.c  Field  in  the  Polar  Region    by  Hinode  Observa.ons  

•  The  polar  region  is  doced  with  small  (~4000km)  and  strong  (~1000  gauss)  magne.c  patches  (kG-­‐patches).  

•  The  kG-­‐patches  in  the  polar  region  larger  and  stronger  than  the  network  magne.c  field  in  the  quiet  region  of  low  la.tude.  

•  The  KG-­‐patches  in  a  polar  region  have  one  polarity.  There  is  no  patch  that  has  the  other  polarity.  

•  The  magne.c  field  lines  from  the  kG-­‐patches  extend  to  the  interplanetary  space,  and  contracts  the  fan-­‐like  structures.    

•  Although  the  ver.cal  magne.c  field  in  the  polar  region  is  differ  from  that  in  the  quiet  region,  there  is  no  difference    the  horizontal  magne.c  field  around  the  pole  and  the  equator.

(Tsuneta  et  al.  2008  and  Ito  et  al.  2010)

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X-­‐ray  jets  frequently  occur  in  the  polar  region

•  The  number  of  X-­‐ray  jets  in  the  polar  coronal  hole  is  about  60  jets/day.  (Savcheva  et  al.  2007)  

•  Cirtain  et  al.  2007  found  the  two  velocity  components.  –  One  is  sound  speed,  the  other  one  is  alfven  speed

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The  occurrence  rates  and  frequency  distribu.ons  of  of  X-­‐ray  jets

•  The  QR  near  the  pole  is  more  produc.ve  than  the  polar  CH.  •  The  power-­‐law  index  of  the  frequency  distribu.ons  of  the  footpoint  

flare  of  polar  X-­‐ray  jets  in  CH  and  QR  is  1.8.  It  is  steeper  than  that  of  the  previous  study.  (Shimojo  et  al.  1996  :  1.2  mainly  near  AR.)

(Sako  and  Shimojo,  2010)

Occurrence  rates  in  CH  and  QR  near  the  pole The  frequency  distribu.on  of  the  footpoint  flare  of  the  polar  X-­‐ray  jets  in  CH  and  QR  near  the  pole

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The  rela.on  between    kG-­‐patches  and  Coronal  Ac.vi.es

SOT-SP Fe I Stokes-Q 10-Sep-2007 17:00 - 21:26UT Transverse Magnetic Field (White: East/West, Black: North/South) Saturates at the degree of polarization 0.2%

850

900

950

1000

Y (a

rcse

cs)

SOT-FG Na I Stokes-V 10-Sep-2007 21:01:19UT Line-of-sight Magnetic Field Saturates at the degree of polarizaton 1%

XRT Al_poly 10-Sep-2007 21:00:46UT

-50 0 50 100 150X (arcsecs)

850

900

950

1000

Y (a

rcse

cs)

EIT 195A 10-Sep-2007 21:12:42UT

-50 0 50 100 150X (arcsecs)

(Shimojo  and  Tsuneta,  2009)

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The  coronal  ac.vi.es  occur  on  the  kG-­‐pathes  with  “small  emerging  fluxes”.  

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Yellow:  XRT  images  (>  1MK  plasma)  B/W:  Stoke-­‐V  of  Na  I  line

(Shimojo  and  Tsuneta,  2009)

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The  Polar  X-­‐ray  Jet  with  the  EFR

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The  coronal  ac.vity  in  the  polar  region

•  X-­‐ray  jets  frequently  occur  in  the  polar  region.  •  The  power-­‐law  index  of  the  frequency  distribu.on  as  a  func.on  of  the  X-­‐ray  intensity  of  footpoint  flare  of  jets  is  1.8.  It  is  steeper  than  that  of  X-­‐ray  jets  around  ARs.  

•  Most  of  kG-­‐patches  are  not  associated  with  coronal  structures.  

•  The  coronal  ac.vi.es  occur  on  the  kG-­‐patches  with  small  EFRs.  

(Savcheva  et  al.  2007,  Shimojo  &  Tsuneta  2009,  Sako  &  Shimojo  2010)

The  X-­‐ray  jets  in  the  polar  region  can  be  used  as  the  proxy    of  the  magne.c  ac.vity  (EFR)  in  the  polar  region.

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The  next  step  of  the  polar  ac.vity  study  “We  need  long  term  (>5  years)  monitoring  obs.”

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What  happen  ?

We  are  here,  now

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Polar  Ac.vity  study  by  SOLAR-­‐C •  Magne.c  field  in  the  polar  region  

–  Targets  for  Plan-­‐A  •  The  global  surface  flow  and  magne.c  pacern  in  the  polar  region  and  their  

.me  evolu.on.  •  The  long  .me  evolu.on  of  the  ver.cal  (poloidal)  magne.c  field.  (Plan-­‐A  can  

not  measure  weak  horizontal  field.)  –  Targets  for  Plan-­‐B  

•  The  long  .me  evolu.on  of  total  magne.c  field.  •  The  height  varia.on  of  magne.c  fields  from  photosphere  to  corona  •  Small  Emerging  flux,  Horizontal  magne.c  field  in  the  polar  region.    

•  Coronal  Ac.vi.es  in  the  polar  region  –  Target  for  Plan-­‐A:  

•  The  coronal  hole  boundary  varia.on  and  transient  events  (brightening,  jets)  obtained  by  X-­‐ray  Imager  

•  Velocity  field  in  the  corona  hole  obtained  by  UV/EUV  spectrograph  –  Target  for  Plan-­‐B  

•  The  velocity  field  above  the  polar  region  (It  is  realized  by  the  low-­‐scacer  light  spectrograph)  

•  Magne.c  reconnec.on  in  Chromosphere  and  Corona  with  spectrograph