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Title: Analysis of Neptune’s 2017 bright equatorial storm

Journal Article · · Icarus
 [1]; ORCiD logo [1];  [2];  [3];  [1];  [4]; ORCiD logo [3];  [1]; ORCiD logo [1];  [5];  [5]; ORCiD logo [6];  [4]; ORCiD logo [7]; ORCiD logo [8];  [8];  [9];  [1];  [10];  [11] more »;  [1]; ORCiD logo [12];  [4]; ORCiD logo [13];  [14] « less
  1. Univ. of California, Berkeley, CA (United States)
  2. Columbia Univ., New York, NY (United States); American Museum of Natural History,New York, NY (United States)
  3. Uiversidad del País Vasco (Spain)
  4. W. M. Keck Observatory, Kamuela HI (United States)
  5. Univ. of Wisconsin, Madison, WI (United States)
  6. Société Astronomique de France (France)
  7. California Inst. of Technology (CalTech), Pasadena, CA (United States)
  8. Lick Observatory, Mount Hamilton, CA (United States)
  9. Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
  10. Univ. of California, Berkeley, CA (United States); Univ. Grenoble Alpes/CNRS, (France)
  11. Univ. of California, Santa Cruz, CA (United States)
  12. Univ. of Hawaii, Honolulu, HI (United States)
  13. Univ. of California, Los Angeles, CA (United States)
  14. Univ. of California, Santa Barbara, CA (United States)

Herein we report the discovery of a large (~8500 km diameter) infrared-bright storm at Neptune’s equator in June 2017. We tracked the storm over a period of 7 months with high-cadence infrared snapshot imaging, carried out on 14 nights at the 10 m Keck II telescope and 17 nights at the Shane 120 inch reflector at Lick Observatory. The cloud feature was larger and more persistent than any equatorial clouds seen before on Neptune, remaining intermittently active from at least 10 June to 31 December 2017. Our Keck and Lick observations were augmented by very high-cadence images from the amateur community, which permitted the determination of accurate drift rates for the cloud feature. Its zonal drift speed was variable from 10 June to at least 25 July, but remained a constant 237.4 ± 0.2 m s 1 from 30 September until at least 15 November. The pressure of the cloud top was determined from radiative transfer calculations to be 0.3-0.6 bar; this value remained constant over the course of the observations. Multiple cloud break-up events, in which a bright cloud band wrapped around Neptune’s equator, were observed over the course of our observations. No “dark spot” vortices were seen near the equator in HST imaging on 6 and 7 October. The size and pressure of the storm are consistent with moist convection or a planetary-scale wave as the energy source of convective upwelling, but more modeling is required to determine the driver of this equatorial disturbance as well as the triggers for and dynamics of the observed cloud break-up events.

Research Organization:
Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States)
Sponsoring Organization:
Federación Española de Enfermedades Raras (FEDER); Google; Keck Visiting Scholar Program; Ministry of Economy and Competitiveness (MINECO); National Aeronautic and Space Administration (NASA); National Science Foundation (NSF); USDOE National Nuclear Security Administration (NNSA); W. M. Keck Foundation
Grant/Contract Number:
AC52-07NA27344
OSTI ID:
1643764
Report Number(s):
LLNL-JRNL--804297; 1007286
Journal Information:
Icarus, Journal Name: Icarus Vol. 321; ISSN 0019-1035
Publisher:
ElsevierCopyright Statement
Country of Publication:
United States
Language:
English

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Cited By (7)

Ice Giant Circulation Patterns: Implications for Atmospheric Probes journal February 2020
Atmospheric Dynamics and Vertical Structure of Uranus and Neptune’s Weather Layers journal November 2019
Formation of a New Great Dark Spot on Neptune in 2018 journal March 2019
Lifetimes and Occurrence Rates of Dark Vortices on Neptune from 25 Years of Hubble Space Telescope Images journal March 2019
Neptune's Latitudinal Variations as Viewed with ALMA journal June 2019
First ALMA Millimeter-wavelength Maps of Jupiter, with a Multiwavelength Study of Convection journal September 2019
Neptune's Latitudinal Variations as Viewed with ALMA text January 2019

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