Geostrophic Balance with a full Coriolis Force: Implications for low Latitude Studies.

Details Geostrophic Balance with a full Coriolis Force: Implications for low Latitude Studies. Geostrophic Balance with a full Coriolis Force: Implications for low Latitude Studies.

May 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002agusm.a42a..06d&link_type=abstract

American Geophysical Union, Spring Meeting 2002, abstract #A42A-06

Physics

3299 General Or Miscellaneous, 3319 General Circulation, 3399 General Or Miscellaneous, 0343 Planetary Atmospheres (5405, 5407, 5409, 5704, 5705, 5707)

Scientific paper

In its standard form, geostrophic balance uses a partial representation of the Coriolis force. The resulting formulation has a singularity at the equator, and violates mass and momentum conservation. When the horizontal projection of the planetary rotation vector is considered, the singularity at the equator disappears, continuity can be preserved, and quasigeostrophy can be formulated at planetary scale. At the same time, the predicted geostrophic winds can differ significantly from the standard approach. Similarities and differences between both approaches to wind diagnostics are shown in an application example.

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