z-logo
Premium
Large potential energy of gravity waves over a smooth surface with little convection: Simulation and observation
Author(s) -
Kawatani Yoshio,
Dhaka S. K.,
Takahashi Masaaki,
Tsuda Toshitaka
Publication year - 2003
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2003gl016960
Subject(s) - equator , gravity wave , convection , geology , gravitational wave , climatology , geophysics , atmospheric sciences , altitude (triangle) , equatorial waves , meteorology , environmental science , latitude , geodesy , physics , geometry , mathematics , astrophysics
A numerical experiment is conducted using an Atmospheric General Circulation Model (AGCM) to investigate the presence of the large potential energy over a region of low topography and little convective activity, focusing on the tropical Atlantic region (10°E to 20°W, 0° to 20°S). It is found that gravity waves with a time period of 24 hours are excited near the Equator (∼5°–15°N) in a region of large moist heating extending vertically up to 10–13 km. The gravity waves propagate upward from this region with a bias toward the south and are manifested as large energy fluxes in the cross equatorial region. Enhanced energy fluxes are therefore simulated at 20–30 km altitude over a region with no significant source of gravity waves, and are confirmed using Global Positioning Satellite/Meteorology (GPS/MET) experiment data.

This content is not available in your region!

Continue researching here.

Having issues? You can contact us here
Accelerating Research

Address

John Eccles House
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom