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Solar astrometry with planetary transits

Published online by Cambridge University Press:  24 September 2020

Marcelo Emilio
Affiliation:
Universidade Estadual de Ponta Grossa, 84030-900 Ponta Grossa, PR, Brazil Observatório Nacional, MCTIC, 20921-400 Rio de Janeiro, RJ, Brazil email: memilio@uepg.br Institute for Astronomy, University of Hawaii, Maui, HI 96768, USA emails: kuhn@ifa.hawaii.edu, ifscholl@hawaii.edu
Rock Bush
Affiliation:
Stanford University, Stanford, CA, 94305, USA email: rock@sun.stanford.edu
Jeff Kuhn
Affiliation:
Institute for Astronomy, University of Hawaii, Maui, HI 96768, USA emails: kuhn@ifa.hawaii.edu, ifscholl@hawaii.edu
Isabelle Scholl
Affiliation:
Institute for Astronomy, University of Hawaii, Maui, HI 96768, USA emails: kuhn@ifa.hawaii.edu, ifscholl@hawaii.edu
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Abstract

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Planetary transits are used to measure the solar radius since the beginning of the 18th century and are the most accurate direct method to measure potentially long-term variation in the solar size. Historical measures present a range of values dominated by systematic errors from different instruments and observers. Atmospheric seeing and black drop effect contribute as error sources for the precise timing of the planetary transit ground observations. Both Solar and Heliospheric Observatory (SOHO) and Solar Dynamics Observatory (SDO) made observations of planetary transits from space to derive the solar radius. The International Astronomical Union approved the resolution B3 in 2015, defining a nominal solar radius of precisely 695,700 km. In this work, we show that this value is off by more than 300 km, which is one order of magnitude higher than the error of the most recent solar radius observations.

Type
Contributed Papers
Copyright
© International Astronomical Union 2020

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