4.5 Article

WASP-20b and WASP-28b: a hot Saturn and a hot Jupiter in near-aligned orbits around solar-type stars

Journal

ASTRONOMY & ASTROPHYSICS
Volume 575, Issue -, Pages -

Publisher

EDP SCIENCES S A
DOI: 10.1051/0004-6361/201423591

Keywords

planetary systems; stars: individual: WASP-20b; stars: individual: WASP-28b

Funding

  1. UK's Science and Technology Facilities Council
  2. Swiss National Science Foundation [PBGEP2-145594]
  3. STFC [ST/I000666/1, ST/I001719/1, ST/J00152X/1, ST/L000733/1, ST/J001651/1, ST/K006126/1, ST/G001006/1, ST/L00139X/1, PP/D000890/1, ST/M001296/1, PP/F000065/1, ST/J000027/1, PP/F000073/1] Funding Source: UKRI
  4. Science and Technology Facilities Council [ST/J00152X/1, PP/F000065/1, ST/M001296/1, ST/L00139X/1, ST/I000666/1, ST/K006126/1, ST/G001006/1, ST/I001719/1, ST/L000733/1, ST/J000027/1, PP/D000890/1, ST/J001651/1] Funding Source: researchfish
  5. Swiss National Science Foundation (SNF) [PBGEP2_145594] Funding Source: Swiss National Science Foundation (SNF)

Ask authors/readers for more resources

We report the discovery of the planets WASP-20b and WASP-28b along with measurements of their sky-projected orbital obliquities. WASP-20b is an inflated, Saturn-mass planet (0.31 M-Jup; 1.46 R-Jup) in a 4.9-day, near-aligned (lambda = 12.7 +/- 4.2.) orbit around CD-24 102 (V = 10.7; F9). Due to the low density of the planet and the apparent brightness of the host star, WASP-20 is a good target for atmospheric characterisation via transmission spectroscopy. WASP-28b is an inflated, Jupiter-mass planet (0.91 M-Jup; 1.21 R-Jup) in a 3.4-day, near-aligned (lambda = 8 +/- 18 degrees) orbit around a V = 12, F8 star. As intermediate-mass planets in short orbits around aged, cool stars (7(-1)(+2) Gyr and 6000 +/- 100 K for WASP-20; 5(-2)(+3) Gyr and 6100 +/- 150 K for WASP-28), their orbital alignment is consistent with the hypothesis that close-in giant planets are scattered into eccentric orbits with random alignments, which are then circularised and aligned with their stars' spins via tidal dissipation.

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