university of colorado/cires – noaa/swpc nadir muri,...

Post on 25-Feb-2016

47 Views

Category:

Documents

0 Downloads

Preview:

Click to see full reader

DESCRIPTION

Numerical Modeling of Neutral Density and Composition for 2005. Mariangel Fedrizzi, Timothy J. Fuller-Rowell, Tomoko Matsuo. University of Colorado/CIRES – NOAA/SWPC. Mihail Codrescu. NOAA/SWPC. - PowerPoint PPT Presentation

TRANSCRIPT

University of Colorado/CIRES – NOAA/SWPC NADIR MURI, Boulder, CO, 21-22 October, 2008

Mariangel Fedrizzi, Timothy J. Fuller-Rowell, Tomoko Matsuo

Numerical Modeling of Neutral Density and Composition for 2005

University of Colorado/CIRES – NOAA/SWPC

Mihail CodrescuNOAA/SWPC

Coupled Thermosphere Ionosphere Plasmasphere Modelwith self-consistent Electrodynamics (CTIPe)

• Global thermosphere 80 - 500 km, solves momentum, energy, composition, etc. Vx, Vy, Vz, Tn, O, O2, N2, ….

• High latitude ionosphere 80 -10,000 km, solves continuity, momentum, energy, etc. O+, H+, O2

+, NO+, N2+, N+, Vi, Ti, ….

• Plasmasphere, and mid and low latitude ionosphere

• Self-consistent electrodynamics

• Forcing: solar UV and EUV, Weimer electric field, TIROS/NOAA auroral precipitation, tidal forcing

University of Colorado/CIRES – NOAA/SWPC NADIR MURI, Boulder, CO, 21-22 October, 2008

University of Colorado/CIRES – NOAA/SWPC NADIR MURI, Boulder, CO, 21-22 October, 2008

Halloween Storm (2003)

University of Colorado/CIRES – NOAA/SWPC NADIR MURI, Boulder, CO, 21-22 October, 2008

Halloween Storm (2003)

Empircal NO model: Marsh et al. 2004• Based on SNOE data• EOFs• Dependent on EUV, season, auroral activity, height, and latitude

University of Colorado/CIRES – NOAA/SWPC NADIR MURI, Boulder, CO, 21-22 October, 2008

Halloween Storm (2003)

Empircal NO model: Marsh et al. 2004• Based on SNOE data• EOFs• Dependent on EUV, season, auroral activity, height, and latitude

Weimer 2005: electric field patterns driven by solar wind data (e.g., IMF, SW vel., SW den.), 1 min. input (database).

University of Colorado/CIRES – NOAA/SWPC NADIR MURI, Boulder, CO, 21-22 October, 2008

Halloween Storm (2003)

Empircal NO model: Marsh et al. 2004• Based on SNOE data• EOFs• Dependent on EUV, season, auroral activity, height, and latitude

Weimer 2005: electric field patterns driven by solar wind data (e.g., IMF, SW vel., SW den), 1 min. input (database).

University of Colorado/CIRES – NOAA/SWPC NADIR MURI, Boulder, CO, 21-22 October, 2008

Neutral Density: Jan-Apr 2005

University of Colorado/CIRES – NOAA/SWPC NADIR MURI, Boulder, CO, 21-22 October, 2008

Lei et al., 2008

CHAMP Neutral Density Periodicities

University of Colorado/CIRES – NOAA/SWPC NADIR MURI, Boulder, CO, 21-22 October, 2008

Lei et al., 2008

CHAMP Neutral Density Periodicities

University of Colorado/CIRES – NOAA/SWPC NADIR MURI, Boulder, CO, 21-22 October, 2008

Lei et al., 2008

CTIPeCHAMP

University of Colorado/CIRES – NOAA/SWPC NADIR MURI, Boulder, CO, 21-22 October, 2008

Crowley et al., 2008 FIGURE 3: (a) raw GUVI ΣO/ N2 ratio as a function of latitude and time for the first 100 days of 2005, with Kp superposed (black line); (b) Residuals 10° latitude bands after bandpass filtering and removal of the of 11-day running mean, expressed as a percentage of the running mean values. Broken line shows Kp after similar bandpass filtering.

GUVI O/N2 Periodicities

University of Colorado/CIRES – NOAA/SWPC NADIR MURI, Boulder, CO, 21-22 October, 2008

Crowley et al., 2008GUVI

CTIPePreliminary Results

University of Colorado/CIRES – NOAA/SWPC NADIR MURI, Boulder, CO, 21-22 October, 2008

University of Colorado/CIRES – NOAA/SWPC NADIR MURI, Boulder, CO, 21-22 October, 2008

Crowley et al., 2008GUVI

Global O/N2 snapshots at 12UTColour scale: 0.2 – 1.0CTIPe

top related