izpis_h1_title_alt

Decomposition of the horizontal wind divergence associated with the Rossby, mixed Rossby-gravity, inertia-gravity, and Kelvin waves on the sphere
ID Neduhal, Valentino (Author), ID Žagar, Nedjeljka (Author), ID Lunkeit, Frank (Author), ID Polichtchouk, Inna (Author), ID Zaplotnik, Žiga (Author)

.pdfPDF - Presentation file, Download (23,18 MB)
MD5: 67F6F2DBEC22490309C9E7519F1B2A06
URLURL - Source URL, Visit https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2023JD040427 This link opens in a new window

Abstract
The paper presents a new method for the decomposition of the horizontal wind divergence among linear waves on the sphere: inertia-gravity (IG), mixed Rossby-gravity (MRG), Kelvin and Rossby waves. The work is motivated by the need to quantify the vertical velocity and momentum fluxes in the tropics where the distinction between the Rossby and gravity regime, present in the extratropics, becomes obliterated. The method leads to divergence power spectra as a function of latitude and pressure. The spectra follow the same power laws as the vertical kinetic energy spectra for different wave types. The key novel aspect of the work is the coexistence of wave types at the same zonal wavenumbers. Applied to ERA5 data in August 2018, the new method reveals that the zonally-integrated Kelvin wave divergence makes up about 19% of the upper-troposphere divergence within 10°S–10°N. The MRG wave divergence has four times smaller magnitude. The relative roles of the two waves vary with scale. Overall small roles of the Kelvin and MRG waves in the tropical divergence is explained by decomposing their kinetic energies into rotational and divergent parts. The beta effects produces less then 5% of the tropospheric divergence associated with Rossby waves. The majority of divergence belongs to IG modes and is nearly equipartitioned between the eastward- and westward-propagating IG modes in the upper troposphere, whereas stratospheric partitioning depends on the background flow.

Language:English
Keywords:meteorology
Work type:Article
Typology:1.01 - Original Scientific Article
Organization:FMF - Faculty of Mathematics and Physics
Publication version:Version of Record
Publication date:29.04.2024
Year:2024
Number of pages:20 str.
Numbering:Vol. 129, iss. 9, art. no. e2023JD040427
PID:20.500.12556/RUL-156065 This link opens in a new window
UDC:551.5
ISSN on article:2169-897X
DOI:10.1029/2023JD040427 This link opens in a new window
COBISS.SI-ID:194571779 This link opens in a new window
Publication date in RUL:07.05.2024
Views:332
Downloads:57
Metadata:XML DC-XML DC-RDF
:
Copy citation
Share:Bookmark and Share

Record is a part of a journal

Title:Journal of geophysical research : Atmospheres
Shortened title:J. geophys. res., Atmos.
Publisher:John Wiley & Sons
ISSN:2169-897X
COBISS.SI-ID:311465 This link opens in a new window

Licences

License:CC BY 4.0, Creative Commons Attribution 4.0 International
Link:http://creativecommons.org/licenses/by/4.0/
Description:This is the standard Creative Commons license that gives others maximum freedom to do what they want with the work as long as they credit the author.

Secondary language

Language:Slovenian
Keywords:meteorologija

Projects

Funder:ARIS - Slovenian Research and Innovation Agency
Project number:J1-9431
Name:Prispevek Rossbyevih in inercijsko-težnostnih valov k vertikalni hitrosti in pretoku gibalne količine v ozračju

Similar documents

Similar works from RUL:
Similar works from other Slovenian collections:

Back