Correction to: Venus Evolution Through Time: Key Science Questions, Selected Mission Concepts and Future Investigations

• DOI: 10.1007/s11214-023-01022-5
• Publication Date: 2023-10-31T10:02:24Z
• Authors: Thomas Widemann; Suzanne E. Smrekar; James B. Garvin; Anne Grete Straum...; Adriana C. Ocampo; Mitchell D. Schulte; Thomas Voirin; Scott Hensley; M. Darby Dyar; Jennifer L. Whitten; Daniel C. Nunes; Stephanie A. Getty; Giada N. Arney; Natasha M. Johnson; Erika Kohler; Tilman Spohn; Joseph G. O’Rourke; Colin F. Wilson; Michael J. Way; Colby Ostberg; Frances Westall; Dennis Höning; Seth Jacobson; Arnaud Salvador; Guillaume Avice; Doris Breuer; Lynn Carter; Martha S. Gilmore; Richard Ghail; Jörn Helbert; Paul Byrne; Alison R. Santos; Robert R. Herrick; Noam Izenberg; Emmanuel Marcq; Tobias Rolf; Matt Weller; Cedric Gillmann; Oleg Korablev; Lev Zelenyi; Ludmila Zasova; Dmitry Gorinov; Gaurav Seth; C. V. Narasimha Rao; Nilesh Desai
• Keywords: Planetary science

In the original publication, there has been a discrepancy between values mentioned in the text of Sect. 4.3.3 and in Table 1. The corrected version is provided here: Wrong: The gravity field harmonic coefficients up to an average degree strength of 130 (∼145 km) are generated together with corrections to the spin rate and to the pole right ascension and declination. Correct: The gravity field harmonic coefficients up to an average degree strength of 200 (∼105 km, see Table 1) are generated together with corrections to the spin rate and to the pole right ascension and declination.