<--- Back to Details
First PageDocument Content
Oceanography / Atmospheric dynamics / Fluid dynamics / Ocean currents / Rossby wave / Boundary current / Vorticity / Sverdrup balance / Irminger Sea / Atmospheric sciences / Meteorology / Physical oceanography
Date: 2003-11-06 10:00:28
Oceanography
Atmospheric dynamics
Fluid dynamics
Ocean currents
Rossby wave
Boundary current
Vorticity
Sverdrup balance
Irminger Sea
Atmospheric sciences
Meteorology
Physical oceanography

AUGUSTSPALL AND PICKART 1829

Add to Reading List

Source URL: www.whoi.edu

Download Document from Source Website

File Size: 1,03 MB

Share Document on Facebook

Similar Documents

Modification of Long Equatorial Rossby Wave Phase Speeds by Zonal Currents Theodore S. Durland ∗

DocID: 1tpGT - View Document

Meteorology / Atmospheric dynamics / Physical geography / Atmosphere of Earth / Polar vortex / Rossby wave / General circulation model / Stratosphere / Wind

Microsoft Word - JAS_D140191_Figure- f1

DocID: 1rtUd - View Document

Fluid dynamics / Physical oceanography / Oceanography / Physical geography / Physics / Eddy / Antarctic Circumpolar Current / Ekman transport / Rossby wave / Turbulence / Thermohaline circulation / Baroclinity

Phil. Trans. R. Soc. A, 4529–4541 doi:rstaPublished online 25 September 2008 The atmospheric ocean: eddies and jets in the Antarctic Circumpolar Current

DocID: 1rbtz - View Document

Meteorology / Physical geography / Atmospheric dynamics / Jet stream / Rossby wave / Carl-Gustaf Rossby / General circulation model / European Centre for Medium-Range Weather Forecasts / Low-pressure area / Weather forecasting / Climate

Explaining Timescales Associated with Jet Stream Variability Lead Supervisor: John Methven, University of Reading, Department of Meteorology Email: Co-supervisors: Tom Frame, University of Reading

DocID: 1rb1n - View Document

Oceanography / Physical oceanography / Photosynthetic pigments / Tetrapyrroles / Physical geography / Atmospheric dynamics / Physics / Rossby wave / Chlorophyll / Coherence / Baroclinity / SeaWiFS

letters to nature D…f† ˆ DV 2 td . We approximate the behaviour of the decay time with td ˆ y=2:5DV, and use the measured functional form for y, and the expression for DV in equation (2), thereby obtaining a new anal

DocID: 1qZS0 - View Document