Uncertainty parameter

The uncertainty parameter U is a parameter introduced by the Minor Planet Center (MPC) to quantify concisely the uncertainty of a perturbed orbital solution for a minor planet.[1][2] The parameter is a logarithmic scale from 0 to 9 that measures the anticipated longitudinal uncertainty[3] in the minor planet's mean anomaly after 10 years.[1][2][4] The uncertainty parameter is also known as condition code in JPL's Small-Body Database Browser.[2][4][5] The U value should not be used as a predictor for the uncertainty in the future motion of near-Earth objects.[1]

Orbital uncertainty

Classical Kuiper belt objects 40–50 AU from the Sun
Object JPL SBDB
Uncertainty
parameter
Horizons
January 2018
Uncertainty in
distance from the Sun
2013 BL76 1 close to none
20000 Varuna2±140 thousand km
19521 Chaos3±840 thousand km
(15807) 1994 GV94±1.4 million km
(160256) 2002 PD1495±8.2 million km
1999 DH86±70 million km
1999 CQ1537±190 million km
1995 KJ19±590 million km
1995 GJ9±160 trillion km

Orbital uncertainty is related to several parameters used in the orbit determination process including the number of observations (measurements), the time spanned by those observations (observation arc), the quality of the observations (e.g. radar vs. optical), and the geometry of the observations. Of these parameters, the time spanned by the observations generally has the greatest effect on the orbital uncertainty.[6]

Objects such as 1995 SN55 with a condition code (Uncertainty Parameter U) of E where the eccentricity is assumed[7] are considered lost. 2010 GZ60 has an Uncertainty Parameter of 9, and could be an Earth threatening asteroid or may always remain beyond the asteroid belt.

Calculation

The U parameter is calculated as follows:[1][8]

First the in-orbit longitude runoff in seconds of arc per decade is calculated

with

uncertainty in the perihelion time in days
eccentricity of the determined orbit
orbital period in years
uncertainty in the orbital period in days
, Gaussian gravitational constant, converted to degrees

In-orbit longitude runoff is then converted to the "uncertainty parameter" U, which is an integer between 0 and 9. The calculated number can be less than 0 or more than 9, but in those cases either 0 or 9 is used instead. For instance: As of 10 September 2016, Ceres technically has an uncertainty of around 2.6, but is instead displayed as the minimal 0. The formula for cutting off the calculated value of U is

648000 is the number of arc seconds in a half circle, so a value greater than 9 would mean that we would have basically no idea where the object will be in 10 years.

U Runoff
Longitude runoff per decade
0 < 1.0 arc second
1 1.04.4 arc seconds
2 4.419.6 arc seconds
3 19.6 arc seconds 1.4 arc minutes
4 1.46.4 arc minutes
5 6.428 arc minutes
6 28 arc minutes 2.1°
7 2.1°9.2°
8 9.2°41°
9 > 41°

References

  1. 1 2 3 4 "Uncertainty Parameter U". Minor Planet Center. Retrieved 2011-11-15.
  2. 1 2 3 "Mission Design Center Trajectory Browser: Trajectory Browser User Guide". Ames Research Center. Retrieved 2016-03-03.
  3. "Editorial Notice" (PDF). The Minor Planet Circulars/minor Planets and Comets (MPC 24597–24780): 24597. 1995-02-15. Retrieved 3 March 2016.
  4. 1 2 Drake, Bret G. (2011-01-01). "Strategic Implications of Human Exploration of Near-Earth Asteroids". NASA Technical Reports Server (NTRS). Retrieved 2016-03-03.
  5. "Definition/Description for SBDB Parameter/Field: condition code". JPL Solar System Dynamics. Retrieved 2011-11-15.
  6. "Near Earth Objects Close-Approach Uncertainties". NASA/JPL Near-Earth Object Program Office. 31 Aug 2005. Retrieved 2011-11-15.
  7. "Export Format for Minor-Planet Orbits". Minor Planet Center. Retrieved 2016-03-03.
  8. Desmars, Josselin; Bancelin, David; Hestroffer, Daniel; Thuillot, William (Jun 2011). Alecian, G.; Belkacem, K.; Samadi, R.; Valls-Gabaud, D., eds. "Statistical Analysis on The Uncertainty of Asteroid Ephemerides". SF2A 2011: Annual meeting of the French Society of Astronomy and Astrophysics. Paris, France: 639–642. Retrieved 3 March 2016.
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