Large-Scale Gravity Waves in Daytime ICON-MIGHTI Data from 2020

被引:3
|
作者
Triplett, Colin C. [1 ]
Harding, Brian J. [1 ]
Wu, Yen-Jung J. [1 ]
England, Scott [2 ]
Englert, Christoph R. [3 ]
Makela, Jonathan J. [4 ]
Stevens, Michael H. [3 ]
Immel, Thomas [1 ]
机构
[1] Univ Calif Berkeley, Space Sci Lab, Berkeley, CA 94720 USA
[2] Virginia Polytech Inst & State Univ, Aerosp & Ocean Engn Dept, Blacksburg, VA 24061 USA
[3] US Naval Res Lab, Space Sci Div, Washington, DC 20375 USA
[4] Univ Illinois, Dept Elect & Comp Engn, Urbana, IL 61801 USA
关键词
Large-scale gravity waves; ICON; Thermosphere; Neutral winds; Temperature; O(S-1) DAYGLOW EMISSION; MICHELSON INTERFEROMETER; THERMOSPHERE; CLIMATOLOGY; PARAMETERS; DESIGN;
D O I
10.1007/s11214-022-00944-w
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The Michelson Interferometer for Global High-resolution Thermospheric Imaging (MIGHTI) onboard the NASA Ionospheric Connection Explorer (ICON) has retrieved profiles of thermospheric wind and temperature in the 90-300 km range for over two years. As part of these limb-viewing measurements, MIGHTI also retrieves a relative volume emission rate (VER) of two atomic oxygen (OI) emissions in the same altitude range. Generally, the VER data do not vary in concert with the retrieved winds or temperatures. However, there are periods of observations where the VER measurements clearly vary together with the wind and temperature measurements, in unexpectedly prominent, large-scale structures. These large-scale variations are smaller than the tidal structures that are investigated as part of ICON's main mission. In this study, we present these large-scale variations as they appear together in the MIGHTI VER, zonal wind, and temperature products. We present a method to extract wave parameters from these structures and show their properties over the entire year of 2020. These large-scale waves consistently have vertical-to-horizontal slopes of 0.01 km/km, an upper-limit of similar to 3000 km for horizontal wavelengths and of similar to 35 km for vertical wavelengths. We interpret these waves as inertia gravity waves. While observational evidence for such waves is not new, it was not expected to observe their signatures with ICON data. Thus, this new global data set opens up a new and unique data source to explore this wave-type.
引用
收藏
页数:11
相关论文
共 50 条
  • [31] Large-scale flow response to short gravity waves breaking in a rotating shear flow
    Lott, F
    10TH CONFERENCE ON MOUNTAIN METEOROLOGY, 2002, : 429 - 432
  • [32] LARGE-SCALE NEUTRAL COMPOSITION GRAVITY-WAVES IN THERMOSPHERE OBSERVED BY ESRO 4
    TRINKS, H
    MAYR, HG
    TRANSACTIONS-AMERICAN GEOPHYSICAL UNION, 1976, 57 (08): : 601 - 601
  • [33] Impulsive Joule heating of the auroral thermosphere as a source of generation of large-scale gravity waves
    Ignat'ev, V. M.
    GEOMAGNETISM AND AERONOMY, 2009, 49 (02) : 227 - 231
  • [34] LARGE-SCALE MODULATIONS OF EDGE WAVES
    AKYLAS, TR
    JOURNAL OF FLUID MECHANICS, 1983, 132 (JUL) : 197 - 208
  • [35] Large-scale focusing joint inversion of gravity and magnetic data with Gramian constraint
    Vatankhah, Saeed
    Renaut, Rosemary A.
    Huang, Xingguo
    Mickus, Kevin
    Gharloghi, Mostafa
    GEOPHYSICAL JOURNAL INTERNATIONAL, 2022, 230 (03) : 1585 - 1611
  • [36] Signatures of quantum gravity in the large-scale universe
    Grishchuk, LP
    CURRENT TOPICS IN ASTROFUNDAMENTAL PHYSICS: PRIMORDIAL COSMOLOGY, 1998, 511 : 539 - 558
  • [37] Gravity and large-scale structure: Observational evidence
    Fry, JN
    LONG-RANGE CORRELATIONS IN ASTROPHYSICAL SYSTEMS, 1998, 848 : 62 - 74
  • [38] Large-scale structure in mimetic Horndeski gravity
    Arroja, Frederico
    Okumura, Teppei
    Bartolo, Nicola
    Karmakar, Purnendu
    Matarrese, Sabino
    JOURNAL OF COSMOLOGY AND ASTROPARTICLE PHYSICS, 2018, (05):
  • [39] SOME PROBLEMS OF LARGE-SCALE GRAVITY INTERPRETATION
    GROTEN, E
    JOURNAL OF GEOPHYSICS-ZEITSCHRIFT FUR GEOPHYSIK, 1975, 41 (06): : 659 - 679
  • [40] Large-scale structure in f(T) gravity
    Li, Baojiu
    Sotiriou, Thomas P.
    Barrow, John D.
    PHYSICAL REVIEW D, 2011, 83 (10):