A meteoroid stream survey using the Canadian Meteor Orbit Radar
Autor: | Robert Weryk, Peter Brown, J. Jones, D. K. Wong |
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Rok vydání: | 2010 |
Předmět: |
Leonids
Orbital elements Meteor (satellite) education.field_of_study Meteoroid Comet Population Astronomy Wavelet transform Astronomy and Astrophysics law.invention Wavelet Space and Planetary Science Asteroid law Perseids Orbit (dynamics) Radar education Orbit determination Longitude Geology Remote sensing |
Zdroj: | Icarus. 207:66-81 |
ISSN: | 0019-1035 |
DOI: | 10.1016/j.icarus.2009.11.015 |
Popis: | A 7 year survey using the Canadian Meteor Orbit Radar (CMOR), a specular backscattering orbital radar, has produced three million individually measured meteoroid orbits for particles with mean mass near 10−7 kg. We apply a 3D wavelet transform to our measured velocity vectors, partitioning them into 1° solar longitude bins while stacking all 7 years of data into a single “virtual” year to search for showers which show annual activity and last for at least 3 days. Our automated stream search algorithm has identified 117 meteor showers. We have recovered 42 of the 45 previously described streams from our first reconnaissance survey (Brown, P., Weryk, R.J., Wong, D.K., Jones, J. [2008]. Icarus 195, 317–339). Removing possible duplicate showers from the automated results leaves 109 total streams. These include 42 identified in survey I and at least 62 newly identified streams. Our large data sample and the enhanced sensitivity of the 3D wavelet search compared to our earlier survey have allowed us to extend the period of activity for several major showers. This includes detection of the Geminid shower from early November to late December and the Quadrantids from early November to mid-January. Among our newly identified streams are the Theta Serpentids which appears to be derived from 2008 KP and the Canum Venaticids which have a similar orbit to C/1975 X1 (Sato). We also find evidence that nearly 60% of all our streams are part of seven major stream complexes, linked via secular invariants. |
Databáze: | OpenAIRE |
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