w.k. peterson 1 , j.m. fontenla 1 , t.n. woods 1 ,

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Photoelectrons as a Tool to Evaluate Spectral and Temporal Variations of Solar EUV Irradiance Models W.K. Peterson 1 , J.M. Fontenla 1 , T.N. Woods 1 , P.G. Richards 2 , S.C. Solomon 3 , H.P. Warren 4 , W.K. Tobiska 5 , and P.C. Chamberlin 6 1 LASP/CU, 2 George Mason, 3 NCAR/HAO, 4 NRL, 5 Utah State, 6 NASA/GSFC Peterson, MURI, October 2003

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Photoelectrons as a Tool to Evaluate Spectral and Temporal Variations of Solar EUV Irradiance Models. W.K. Peterson 1 , J.M. Fontenla 1 , T.N. Woods 1 , P.G. Richards 2 , S.C. Solomon 3 , H.P. Warren 4 , W.K. Tobiska 5 , and P.C. Chamberlin 6 1 LASP/CU, 2 George Mason, 3 NCAR/HAO, - PowerPoint PPT Presentation

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Page 1: W.K. Peterson 1 ,  J.M. Fontenla 1 , T.N. Woods 1 ,

Photoelectrons as a Tool to Evaluate Spectral and Temporal Variations of Solar EUV Irradiance Models

W.K. Peterson1, J.M. Fontenla1, T.N. Woods1,

P.G. Richards2, S.C. Solomon3, H.P. Warren4,

W.K. Tobiska5, and P.C. Chamberlin6

1LASP/CU, 2George Mason, 3NCAR/HAO,

4NRL, 5Utah State, 6NASA/GSFC

Peterson, MURI, October 2003

Page 2: W.K. Peterson 1 ,  J.M. Fontenla 1 , T.N. Woods 1 ,

Outline• Our method to compare photoelectron energy

observations and irradiance models • Comparisons of photoelectron energy spectra with those

predicted with two photoelectron production codes driven by the SPRM predictive model, and the FISM, HEUVAC, S2000, and NRL irradiance models

• Conclusions: – Surprisingly the empirical HEUVAC (EUVAC extended to 1 nm)

model produces photoelectron spectra that match the observations on daily and solar rotation period time scales.

– The SRPM prediction model matches the data as well or better than any of the data or index driven models.

– The physics based NRLEUV model does the poorest job of capturing the variation of energetic photoelectrons on a solar rotation time scale.

Peterson, MURI, October 2003

Page 3: W.K. Peterson 1 ,  J.M. Fontenla 1 , T.N. Woods 1 ,

Uncertainties in solar Irradiances create uncertainties in thermospheric models

Altitude-wavelength dependence of energy deposition from solar irradiance in units of Log10(Wm-4)

From Solomon and Qian 2005

Solar minimum conditions

Color Bar: Log10(Wm-4)Peterson, MURI, October 2003

Page 4: W.K. Peterson 1 ,  J.M. Fontenla 1 , T.N. Woods 1 ,

Photoelectron Observations

FAST observations available from January 1, 1997 to April 30, 2009

ePOP observations available in late 2011

Peterson, MURI, October 2003

Page 5: W.K. Peterson 1 ,  J.M. Fontenla 1 , T.N. Woods 1 ,

Model Data Comparison

Average of 56 one-minute average spectra obtained for SZA < 90o

Two PE production codes

Seven Solar irradiance models

Peterson, MURI, October 2003

Page 6: W.K. Peterson 1 ,  J.M. Fontenla 1 , T.N. Woods 1 ,

Transformation to Equivalent Wavelength

Use a constant15 eV ionization potentialPeterson, MURI, October 2003

Page 7: W.K. Peterson 1 ,  J.M. Fontenla 1 , T.N. Woods 1 ,

Relative DifferenceObservation - Model / Model

as a Function of the Wavelength Equivalent of the Photoelectron Energy

S/N inadequate below ~3 nm (> 385 eV)

Above ~16 nm differences are less than +/- 50%

Above ~30 nm slight differences in PE’s predicted from the GLOW and FLIP models.

Both the GLOW and FLIP codes showTIMDED/SEE irradiances systematicallylow below about 15 nm

Peterson, MURI, October 2003

* GLOW/HEUVAC best agrees with observations

Page 8: W.K. Peterson 1 ,  J.M. Fontenla 1 , T.N. Woods 1 ,

FAST Observations from August 31 to September 30 2005

Observed Photoelectron flux vs. Energy (eV)

Vs. Equivalent Wavelength (nm)

F10.7

KP

DST

Each line in the color spectrogram panels shows a daily average photoelectron energy spectra with the flux given by the color bars on the right.

Peterson, MURI, October 2003

F10.7

AP

Page 9: W.K. Peterson 1 ,  J.M. Fontenla 1 , T.N. Woods 1 ,

Differences between Observations and Model PE Energy Spectra over a Solar Rotation

HEUVAC

SPRM-Rome

FISM

S2000

NRLEUV

Photoelectron energy spectra produced using the empirical HEUVAC model agree best with Observations.

The SPRM predictive model does as well as the TIMED/SEE based FISM model

Peterson, MURI, October 2003

SPRM-MLSO

Page 10: W.K. Peterson 1 ,  J.M. Fontenla 1 , T.N. Woods 1 ,

Observation-Model Differences -2

FISM produces good agreement except for underestimating the PE fluxes between 5 and 15 nm

S2000 produces low fluxes below 15 nm and relatively good agreement above 15 nm.

NRLEUV systematically underestimates the photoelectron flux below 15 nm

RED: Model >200% LowGREEN: Model = ObservationsBLACK: No data

Peterson, MURI, October 2003

HEUVAC

SPRM-Rome

FISM

S2000

NRLEUV

SPRM-MLSO

Page 11: W.K. Peterson 1 ,  J.M. Fontenla 1 , T.N. Woods 1 ,

Solar Irradiance Models Differ at Many Wavelengths

HEUVAC Model Color Bar is Irradiance in w/m2

Relative Differences are(Model - HEUVAC) / HEUVAC

HEUVAC

FISM

S2000

NRLEUV

RED: Model >400% than HEUVACGreen: Model = HEUVAC

Irradiance models are qualitatively

different above and below

~27 nm Peterson, MURI, October 2003

SPRM-Rome

SPRM-MLSO

F10.7

Page 12: W.K. Peterson 1 ,  J.M. Fontenla 1 , T.N. Woods 1 ,

Irradiance Power above and below 27 nm

HEUVAC

FISM

S2000

NRLEUV

Lowest: NRLEUVHighest: HEUVAC/S2000

Lowest: HEUVAC/NRLHighest: SPRM

SPRM-Rome

SPRM-MLSO

Peterson, MURI, October 2003

Photoelectron spectra produced using HEUVAC agree best with data

Page 13: W.K. Peterson 1 ,  J.M. Fontenla 1 , T.N. Woods 1 ,

Irradiance Spectral Models

• HEUVAC model has by design has broad spectral structure (~1eV) above 27 nm

• To first order all models agree about the spectral shape below 27 nm

• The most significant differences between irradiance models are in the relative power above and below 27 nm.

HEUVAC

FISM

S2000

NRLEUV

SPRM-Rome

SPRM-MLSO

Peterson, MURI, October 2003

Page 14: W.K. Peterson 1 ,  J.M. Fontenla 1 , T.N. Woods 1 ,

Conclusions• Surprisingly the empirical HEUVAC (EUVAC extended

to 1 nm) model produces photoelectron spectra that best match the observations on daily and solar rotation period time scales.

• Fontenla’s SRPM prediction model matches the photoelectron data as well or better than any of the other data or index driven models investigated.

• The physics based NRLEUV model does the poorest job of capturing the variation of energetic photoelectrons on a solar rotation time scale.

• We need SDO/EVE observations to fully understand We need SDO/EVE observations to fully understand the temporal and spectral variations of solar the temporal and spectral variations of solar irradiance.irradiance.

Peterson, COSPAR, 2010, C12-0018