SPINOR

More documents

Recommendations

Info

Stokes sepctrum diagn nostics CFs and RFs A. Lagg - Abisko Winter School 8
Contribution Functions (1) The contribution function (CF) describes how different atmospheric layers y contribute to the observed spectrum. Mathematical definition: CF ≡ integrand of formal sol sol. of RTE (here isotropic case, no B field): line core: highest formation wings: lowest formation Intuitively: profile shape indicates atmospheric opacity. Medium is more transparent (less heavily absorbed) in wings. �� one can see „deeper deeper“ into the atmosphere at the wings. A. Lagg - Abisko Winter School 9
Page 1 and 2: SPINOR Inversions based on RFs A. L
Page 3 and 4: Asymmetric profiles and ME (2) ) MH
Page 5 and 6: Example: SIR inversion + • Spatia
Page 7: SPINOR core: the synthesis RTE has
Page 11 and 12: Response Functions A. Lagg - Abisko
Page 13 and 14: Response functions Linearization: s
Page 15 and 16: RFs - Example: Fe 6302.5 model on t
Page 17 and 18: The even more complex case: A. Lagg
Page 19 and 20: The complex fluxtube case: A. Lagg
Page 21 and 22: Penumbral Flux Tubes � SPINOR app
Page 23 and 24: SPINOR & HINODE inv_070214.051204_h
Page 25 and 26: Penumbral Flux Tubes �� confirm
Page 27 and 28: 2-comp comp model Sunspot + molec c
Page 29 and 30: Penumbral Oscillations oscillations
Page 31 and 32: Penumbral Oscillations oscillations
Page 33 and 34: Analysis of Umbral Dots (1) Analysi
Page 35 and 36: Analysis of Umbral Dots (3) atmosph
Page 37 and 38: Analysis of Umbral Dots (5) Conclus
Page 39 and 40: Pore simulation: brightening nea ar
Page 41 and 42: SPINOR: Installation and first us s

SPINOR

Create successful ePaper yourself

Delete template?

Save as template?