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Published September 1, 2023 | public
Journal Article

Drift rates of major Neptunian features between 2018 and 2021

Abstract

Using near-infrared observations of Neptune from the Keck and Lick Observatories, and the Hubble Space Telescope in combination with amateur datasets, we calculated the drift rates of prominent infrared-bright cloud features on Neptune between 2018 and 2021. These features had lifespans of ~ 1 day to ≥ 1 month and were located at mid-latitudes and near the south pole. Our observations permitted determination of drift rates via feature tracking. These drift rates were compared to three zonal wind profiles describing Neptune's atmosphere determined from features tracked in H band (1.6 µm), K' band (2.1 µm), and Voyager 2 data at visible wavelengths. Features near -70 deg measured in the F845M filter (845 nm) were particularly consistent with the K' wind profile. The southern mid-latitudes hosted multiple features whose lifespans were ≥ 1 month, providing evidence that these latitudes are a region of high stability in Neptune's atmosphere. We also used HST F467M (467 nm) data to analyze a dark, circumpolar wave at -60° latitude observed on Neptune since the Voyager 2 era. Its drift rate in recent years (2019–2021) is 4.866 ± 0.009°/day. This is consistent with previous measurements by Karkoschka (2011), which predict a 4.858 ± 0.022°/day drift rate during these years. It also gained a complementary bright band just to the north.

Additional Information

© 2023 Elsevier Inc. Thank you to the two anonymous referees whose comments helped improve the manuscript tremendously. This work has been supported by the National Science Foundation, NSF Grant AST-1615004 to UC Berkeley. Many of the images were obtained with the W. M. Keck Observatory, which is operated as a scientific partnership among the California Institute of Technology, the University of California and the National Aeronautics and Space Administration. The Observatory was made possible by the generous financial support of the W. M. Keck Foundation, United States. The authors wish to recognize and acknowledge the very significant cultural role and reverence that the summit of Maunakea has always had within the indigenous Hawaiian community. We are most fortunate to have the opportunity to conduct observations from this mountain. We further made use of data obtained with the NASA/ESA Hubble Space Telescope, obtained from the data archive at the Space Telescope Science Institute. This work used data acquired from the NASA/ESA HST Space Telescope, associated with OPAL program (PI: Simon, GO13937), and archived by the Space Telescope Science Institute, which is operated by the Association of Universities for Research in Astronomy, Inc., under NASA contract NAS 5-26555. All maps are available at http://dx.doi.org/10.17909/T9G593 . STScI is operated by the Association of Universities for Research in Astronomy, Inc. under NASA contract NAS 5–26555 Research at Lick Observatory is partially supported by a generous gift from Google. We are grateful to amateur astronomers performing Neptune observations and submitting them to databases such as PVOL. RH, ASL and JFR were supported by been supported by Grant PID2019-109467GB-I00 funded by MCIN/AEI/10.13039/501100011033/ and by Grupos Gobierno Vasco IT1366-19. Hipercam observations were obtained at Gran Telescopio Canarias (GTC), installed at the Spanish Observatorio del Roque de los Muchachos of the Instituto de Astrofísica de Canarias, on the island of La Palma. Planetcam observations were collected at the Centro Astronómico Hispano en Andalucía (CAHA) at Calar Alto, proposal 19B-2.2-015, operated jointly by Junta de Andalucía and Consejo Superior de Investigaciones Científicas (IAA-CSIC). Software: Astropy, astroscrappy, emcee, matplotlib, nirc2_reduce, numpy, pandas, scikit-image, scipy, WinJupos. Declaration of Competing Interest: The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Additional details

Created:
August 22, 2023
Modified:
October 20, 2023