examination of three empirical atmospheric models · 2 overview motivation for empirical models...
TRANSCRIPT
Examination of ThreeEmpirical Atmospheric Models
A PresentationGiven to
The Department of Physics Utah State UniversityIn Partial Fulfillment
of the Requirements for the DegreeDoctor of Philosophy
byDavid B. Hansen4 February 2010
Space Weather Center Technical Report TR2010-001
2
Overview
● Motivation for empirical models● Models to be discussed
∘ IRI
∘MSIS
∘HWM● Items to consider for each model
∘Model input and output parameters
∘Valid domains within the model
∘Model formulation
∘Examples of model output
3
Why Create anAnalytic Empirical Model?
● Provides a model based on observation● More useful than data tables● Theoretical models
∘Initialization (background atmosphere)
∘Verification of results● Satellites
∘Design
∘Instrument data verification
6
IRI Description
● Empirical model● ISO/TS 16457 (ISO Standard)
● Input● Default: year, time of year, time of day, altitude,
location● Output
● Electron number density● Ion number densities
∘H+, He+, N+, O+, NO+, O2
+
● Electron, ion, and neutral temperatures
7
Valid IRI Domains
● Year
∘1958-Present● Time of year and time of day: no constraints● Altitude
∘Electron density: 65-1000 km
∘Ion densities: 100-1000 km
∘Temperatures: 120-3000 km● Coordinates: global
∘Best at mid-latitudes
8
IRI Data Sources
● Ground:
∘ Ionosonde: ne altitude profile
∘ Incoherent scatter radar: Te, ne, Ti, ni, mi, ui
● Satellite:
∘ Ionosonde: ne inverse altitude profile
∘ In-situ measurements along satellite trajectory● Rocket:
∘ In-situ measurements along rocket trajectory● Empirical Models:
∘MSIS-86: Tn
∘ IGRF: geomagnetic field
11
IRI Data Fitting
● Altitude profile
° Epstein transition function● Day of year
° Linear interpolation● Latitude vs. longitude
° Spherical harmonics● Time of day
° Epstein step function● Magnetic and solar activity
° Linear interpolation
13
Profile Parameters
● hmF2: height of F2 peak
● foF2: plasma frequency at F2 peak
● NmF2: plasma density at F2 peak
● ymF2: half thickness
26
MSIS Description
● Empirical Model● Input
∘Day of year, time of day, altitude, location, solar activity, magnetic activity
● Output
∘Number densities of neutral species
°H, He, N, O, N2, O
2, Ar
∘Total mass density
∘Temperature of neutral atmosphere
27
Valid MSIS Domains
● Day of year and time of day: no constraints● Altitude
° He, N2, O
2, and Ar densities: ground to exosphere
∘O, H, and N densities: 72.5 km to exosphere
∘Temperature: ground to exosphere
● Coordinates: global● Solar and magnetic activity
∘Above 80 km: user input
° Below 80 km: f10.7
= 150.0, Ap = 4.0 (recommended)
28
MSIS Data Sources
● Incoherent scatter radar: neutral temperature, N2 density
● Satellite
∘Mass spectrometer: neutral composition
°UV absorption: O2 density
∘Accelerometer: total neutral mass density
∘Drag: total neutral mass density● Rocket
∘Mass spectrometer: neutral composition
°UV absorption: O2 density
∘Falling sphere: total neutral mass density
∘Grenade: total neutral mass density
∘Pressure gauge: total neutral mass density● Handbook for MAP (Middle Atmosphere Program)
∘Neutral temperature
∘Total neutral mass density
29
MSIS Data Fitting
● Altitude profile
∘Bates profile (low altitude)
∘Inverse polynomial (high altitude)● Latitude vs. longitude
∘Spherical harmonics● Solar and magnetic activity
∘Polynomials● Time variations (day of year, time of day)
∘Fourier series
37
HWM Description
● Empirical model● Input
∘Day of year, time of day, altitude, geographic location, geomagnetic activity
● Output
∘Northern wind speed
∘Eastern wind speed
38
Valid HWM Domains
● Day of year and time of day: no constraints● Altitude: 0-500 km● Coordinates: global
∘Best at low and mid-latitudes● Low solar activity
39
HWM Data Sources
● Ground
● Fabry-Perot interferometer● Incoherent scatter radar● Medium-frequency radar● LIDAR
● Rocket
● Falling sphere● Rocketsonde● Trimethyl aluminum release
● Satellite
● In-situ measurements along satellite trajectory● Fabry-Perot interferometer
● Numerical
● TIME-GCM● NOAA GFS Analysis● NASA GEOS4 Analysis
40
HWM Data Fitting
● Altitude profile
∘Cubic spline (low altitude)
∘Bates-Walker function (high altitude)● Latitude vs. longitude
∘Vector spherical harmonics● Time variations
∘Fourier series● Magnetic activity
∘Polynomial
47
References
● AIAA PR G-003C-2010: Guide to Reference and Standard Atmosphere Models. American Institude of Aeronautics and Astronautics, Reston, VA. <www.spacewx.com/Docs/AIAA_PR_G_003C_2010.pdf>.
● Anderson, D. N., and R. G. Roble, Neutral wind effects on the equatorial F-region ionosphere, J. Atmos. Terr. Phys., 43, 835, 1981.
● Bilitza, D., and B. Reinisch, International Reference Ionosphere 2007: Improvements and new parameters, Advances in Space Research, 42, 4, 599-609, 2008.
● Bradley, P. A., and J. R. Dudeney, A simple model of the vertical distribution of the electron concentration in the ionosphere, J. Atmos. Terr. Phys., 35, 2131, 1973.
● Drob, D. P., et al., An empirical model of the Earth's horizontal wind fields: HWM07, Journal of Geophysical Research, 113, A12304, 2008.
● ISO/TS 16457:2009: Space systems - Space environment (natural and artificial) - The Earth's ionosphere model: international reference ionosphere (IRI) model and extensions to the plasmasphere. International Organization for Standardization, Geneva, Switzerland. <www.spacewx.com/Docs/ISO_TS_16457_2009_E.pdf>.
48
References (continued)
● Picone, J. M., A. E. Hedin, D. P. Drob, and A. C. Aikin, NRLMSISE-00 empirical model of the atmosphere: Statistical comparisons and scientific issues, Journal of Geophysical Research, 107, A12, 1468, 2002.
● National Research Council, Solar-Terrestrial Research for the 1980's, National Academy Press, Washington, D.C., 1981.
● Roble, R. G., The calculated and observed diurnal variation of the ionosphere over Millstone Hill on March 23-24, 1970, Planet. Space Sci., 23, 1017, 1975.
● Schunk, R. W., and Nagy, A. F., Ionospheres: Physics, Plasma Physics, and Chemistry, Cambridge University Press, Cambridge, UK, 2000: 2nd Ed., 2009.
● Richard Stamper. “Ionospheric Stations-The World.” 6 May 2009. UK Solar System Data Center. 1 Feb. 2010 <http://www.ukssdc.ac.uk/wdcc1/ionosondes/world.html>.
● “URSI Incoherent Scatter Working Group: Incoherent Scatter Radars.” MIT Haystack Observatory. 1Feb. 2010 <http://www.haystack.mit.edu/atm/mho/iswg/index.html>.z