w.k. peterson 1 , j.m. fontenla 1 , t.n. woods 1 ,
DESCRIPTION
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 PresentationTRANSCRIPT
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
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
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
Photoelectron Observations
FAST observations available from January 1, 1997 to April 30, 2009
ePOP observations available in late 2011
Peterson, MURI, October 2003
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
Transformation to Equivalent Wavelength
Use a constant15 eV ionization potentialPeterson, MURI, October 2003
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
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
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
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
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
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
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
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