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 (Avtor), ID Žagar, Nedjeljka (Avtor), ID Lunkeit, Frank (Avtor), ID Polichtchouk, Inna (Avtor), ID Zaplotnik, Žiga (Avtor)

.pdfPDF - Predstavitvena datoteka, prenos (23,18 MB)
MD5: 67F6F2DBEC22490309C9E7519F1B2A06
URLURL - Izvorni URL, za dostop obiščite https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2023JD040427 Povezava se odpre v novem oknu

Izvleček
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.

Jezik:Angleški jezik
Ključne besede:meteorology
Vrsta gradiva:Članek v reviji
Tipologija:1.01 - Izvirni znanstveni članek
Organizacija:FMF - Fakulteta za matematiko in fiziko
Različica publikacije:Objavljena publikacija
Datum objave:29.04.2024
Leto izida:2024
Št. strani:20 str.
Številčenje:Vol. 129, iss. 9, art. no. e2023JD040427
PID:20.500.12556/RUL-156065 Povezava se odpre v novem oknu
UDK:551.5
ISSN pri članku:2169-897X
DOI:10.1029/2023JD040427 Povezava se odpre v novem oknu
COBISS.SI-ID:194571779 Povezava se odpre v novem oknu
Datum objave v RUL:07.05.2024
Število ogledov:333
Število prenosov:57
Metapodatki:XML DC-XML DC-RDF
:
Kopiraj citat
Objavi na:Bookmark and Share

Gradivo je del revije

Naslov:Journal of geophysical research : Atmospheres
Skrajšan naslov:J. geophys. res., Atmos.
Založnik:John Wiley & Sons
ISSN:2169-897X
COBISS.SI-ID:311465 Povezava se odpre v novem oknu

Licence

Licenca:CC BY 4.0, Creative Commons Priznanje avtorstva 4.0 Mednarodna
Povezava:http://creativecommons.org/licenses/by/4.0/deed.sl
Opis:To je standardna licenca Creative Commons, ki daje uporabnikom največ možnosti za nadaljnjo uporabo dela, pri čemer morajo navesti avtorja.

Sekundarni jezik

Jezik:Slovenski jezik
Ključne besede:meteorologija

Projekti

Financer:ARIS - Javna agencija za znanstvenoraziskovalno in inovacijsko dejavnost Republike Slovenije
Številka projekta:J1-9431
Naslov:Prispevek Rossbyevih in inercijsko-težnostnih valov k vertikalni hitrosti in pretoku gibalne količine v ozračju

Podobna dela

Podobna dela v RUL:
Podobna dela v drugih slovenskih zbirkah:

Nazaj