Baroclinic modification of midlatitude marine surface wind vectors observed by the NASA scatterometer
- 1 December 1999
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Atmospheres
- Vol. 104 (D24) , 31225-31237
- https://doi.org/10.1029/1999jd900945
Abstract
No abstract availableKeywords
This publication has 24 references indexed in Scilit:
- A model function for the ocean‐normalized radar cross section at 14 GHz derived from NSCAT observationsJournal of Geophysical Research: Oceans, 1999
- Geophysical validation of NSCAT winds using atmospheric data and analysesJournal of Geophysical Research: Oceans, 1999
- The accuracy of the NSCAT 1 vector winds: Comparisons with National Data Buoy Center buoysJournal of Geophysical Research: Oceans, 1999
- Wind observations from new satellite and research vessels agreeEos, 1997
- Estimating Convective Atmospheric Boundary Layer Depth from Microwave Radar Imagery of the Sea SurfaceJournal of Applied Meteorology and Climatology, 1997
- Viewing a cold air outbreak using satellite‐based synthetic aperture radar and advanced very high resolution radiometer imageryJournal of Geophysical Research: Oceans, 1996
- Design of a Nonsingular Level 2.5 Second-Order Closure Model for the Prediction of Atmospheric TurbulenceJournal of the Atmospheric Sciences, 1988
- Development of a turbulence closure model for geophysical fluid problemsReviews of Geophysics, 1982
- An Operational Large-Scale Marine Planetary Boundary Layer ModelJournal of Applied Meteorology, 1982
- Planetary Boundary Layer Winds in Baroclinic ConditionsJournal of the Atmospheric Sciences, 1974