30 April 2009 Space Weather Workshop 2009 The Challenge of Predicting the Ionosphere: Recent results from CISM. W. Jeffrey Hughes Center for Integrated.

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30 April 2009 Space Weather Workshop 2009 The Challenge of Predicting the Ionosphere: Recent results from CISM. W. Jeffrey Hughes Center for Integrated Space Weather Modeling, and Boston University

30 April 2009 Space Weather Workshop 2009 Overview The ionosphere – maintaining a delicate balance. Factors affecting the ionosphere – why is it a challenge to predict? Recent results from CISM: –Solar protons –Geomagnetic storms

30 April 2009 Space Weather Workshop 2009 The ionosphere – maintaining a delicate balance Only a tiny fraction of the upper atmosphere is ionized – varying from in the E-region to in the F-region

30 April 2009 Space Weather Workshop 2009 The life time of an individual free electron is short – seconds to tens of minutes depending on altitude A steady ionosphere is maintained by a dynamic equilibrium between production, loss, and transport of ionization. Changes in factors affecting these processes rapidly change the ionosphere. The ionosphere – maintaining a delicate balance Production – Loss – Transport

30 April 2009 Space Weather Workshop 2009 Production is caused by ionizing radiation – solar EUV, X-rays, solar energetic particles, auroral electrons – acting on the neutrals. Loss is very sensitive to the neutral atmosphere (thermosphere) density, largely driven by temperature. Transport is caused by winds often forced from below and by magnetospheric flows imposed from above. Factors affecting the ionosphere – why is it a challenge to predict?

30 April 2009 Space Weather Workshop 2009 The CISM model suite

30 April 2009 Space Weather Workshop 2009 Solar Energetic Particle (SEP) Modeling led by Janet Luhmann, UC Berkeley CISM is modeling the SEP’s created at the shock waves generated by Interplanetary Coronal Mass Ejections (ICME) in the heliosphere. CISM’s SEP modeling relies on a sufficiently accurate description of the underlying solar wind and ICME shock structure. This is needed to determine: –Shock source strength and attributes –Shock connectivity to an observer Both of which are time dependent In this example the Interplanetary ICME is simulated using the Cone Model (D. Odstrcil )

30 April 2009 Space Weather Workshop 2009 May 1997 ICME cone model results A snapshot of solar wind density in the equatorial and meridional planes. Cone model results (red) and Observations (black) at L1 superposed.

30 April 2009 Space Weather Workshop 2009 Snapshots of the magnetic field line connecting the L1 point to the Sun. This illustrates the challenges faced by the evolution of complex field line shapes in the structured interplanetary medium.

30 April 2009 Space Weather Workshop 2009 Predicted SEP fluxes at five locations for the May 97 case L1 +60 o +30 o -30 o -60 o

30 April 2009 Space Weather Workshop 2009 Comparison of model SEP fluxes with observations for three ICME events: May 1997; Nov 1997; Dec 2006.

30 April 2009 Space Weather Workshop 2009 Magnetosphere-Ionosphere Coupling Led by Stan Solomon, NCAR/HAO CISM models magnetosphere-ionosphere coupling with CMIT – the LFM global magnetospheric MHD model coupled with the global thermosphere-ionosphere TIEGCM model. During geomagnetic storms, strong magnetospheric forcing of the ionosphere/thermosphere occurs causing significant changes to the ionosphere. Comparisons of results from both CMIT and TIEGCM alone with observations confirm the importance of magnetospheric coupling.

30 April 2009 Space Weather Workshop 2009 The 2006 “AGU Storm”

30 April 2009 Space Weather Workshop 2009  TEC from TIE-GCM  TEC from CMIT  TEC from GPS network The December 2006 “AGU Storm”

30 April 2009 Space Weather Workshop 2009 Comparison of CMIT model with Millstone Hill Incoherent Scatter Radar observations. December 2006 Storm

30 April 2009 Space Weather Workshop 2009 Processes Driving Storm-Time Changes in Electron Density

30 April 2009 Space Weather Workshop 2009 April 2004 Storm

30 April 2009 Space Weather Workshop 2009 November 2004 Storm

30 April 2009 Space Weather Workshop 2009 Ionospheric Response to Different Storm Onset Times

30 April 2009 Space Weather Workshop 2009

30 April 2009 Space Weather Workshop 2009 Conclusions Predicting the ionosphere is challenging as the electron density depends sensitively on a number of disparate parameters. Ionospheric memory is short (several hours), data assimilation doesn’t help for more than a few hours. The ionosphere can change abruptly in response to solar flares and other sudden transients. Models can provide guidance to probabilistic forecasts. Currently Geospace models are best for short-term (1- hour) forecasts and nowcasts. For a 1-day forecast, current observational/modeling capabilities suggest most is to be gained from a time dependent heliospheric model with CME propagation.

30 April 2009 Space Weather Workshop 2009 The CISM Space Weather Summer School This year: July , 2009 Students and faculty working at the CISM Summer School – a two-week school held each year.