On the dynamics of the East African jet. III: Arabian Sea branch.

P. R. Bannon

doi:10.1175/1520-0469(1982)039<2267:OTDOTE>2.0.CO;2

On the dynamics of the East African jet. III: Arabian Sea branch.

P. R. Bannon

Meteorology and Atmospheric Science

Research output: Contribution to journal › Article › peer-review

13 Scopus citations

Abstract

Barotropic simulations of the East African jet are extended to include the Arabian Sea branch of the flow and to allow for flow over the mountains of Africa. Large-scale mass source-sink forcing, present to the east of the model orography, drives the low-level circulation. Many features of the southeast trades, cross- equatorial flow and southwest monsoon are simulated. -from Author

Original language	English (US)
Pages (from-to)	2267-2278
Number of pages	12
Journal	Journal of the Atmospheric Sciences
Volume	39
Issue number	10
DOIs	https://doi.org/10.1175/1520-0469(1982)039<2267:OTDOTE>2.0.CO;2
State	Published - 1982

All Science Journal Classification (ASJC) codes

Atmospheric Science

Access to Document

10.1175/1520-0469(1982)039<2267:OTDOTE>2.0.CO;2

Cite this

@article{e5754164895e4aa3951e42a0bbd51c8d,

title = "On the dynamics of the East African jet. III: Arabian Sea branch.",

abstract = "Barotropic simulations of the East African jet are extended to include the Arabian Sea branch of the flow and to allow for flow over the mountains of Africa. Large-scale mass source-sink forcing, present to the east of the model orography, drives the low-level circulation. Many features of the southeast trades, cross- equatorial flow and southwest monsoon are simulated. -from Author",

author = "Bannon, {P. R.}",

year = "1982",

doi = "10.1175/1520-0469(1982)039<2267:OTDOTE>2.0.CO;2",

language = "English (US)",

volume = "39",

pages = "2267--2278",

journal = "Journal of the Atmospheric Sciences",

issn = "0022-4928",

publisher = "American Meteorological Society",

number = "10",

}

TY - JOUR

T1 - On the dynamics of the East African jet. III

T2 - Arabian Sea branch.

AU - Bannon, P. R.

PY - 1982

Y1 - 1982

N2 - Barotropic simulations of the East African jet are extended to include the Arabian Sea branch of the flow and to allow for flow over the mountains of Africa. Large-scale mass source-sink forcing, present to the east of the model orography, drives the low-level circulation. Many features of the southeast trades, cross- equatorial flow and southwest monsoon are simulated. -from Author

AB - Barotropic simulations of the East African jet are extended to include the Arabian Sea branch of the flow and to allow for flow over the mountains of Africa. Large-scale mass source-sink forcing, present to the east of the model orography, drives the low-level circulation. Many features of the southeast trades, cross- equatorial flow and southwest monsoon are simulated. -from Author

UR - http://www.scopus.com/inward/record.url?scp=0020332361&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=0020332361&partnerID=8YFLogxK

U2 - 10.1175/1520-0469(1982)039<2267:OTDOTE>2.0.CO;2

DO - 10.1175/1520-0469(1982)039<2267:OTDOTE>2.0.CO;2

M3 - Article

AN - SCOPUS:0020332361

SN - 0022-4928

VL - 39

SP - 2267

EP - 2278

JO - Journal of the Atmospheric Sciences

JF - Journal of the Atmospheric Sciences

IS - 10

ER -

On the dynamics of the East African jet. III: Arabian Sea branch.

Abstract

All Science Journal Classification (ASJC) codes

Access to Document

Other files and links

Fingerprint

Cite this