Abstract
Currents on the inner shelf respond to a combination of forcing by intrusions of oceans fronts, eddies and internal waves as well as winds, surface gravity waves and topographic rectifications. To quantify the effect that the interaction of these processes has on inner shelf flows, a shore-based, 25.4 MHZ (High Frequency) Ocean Surface Current Radar (OSCR) was deployed to measure the surface current vector field at high spatial and temporal, resolution over the inner and mid shelf. Surface currents were mapped in near-real time. The surface current maps revealed numerous surface current features.
| Original language | English (US) |
|---|---|
| Title of host publication | Oceans Conference Record (IEEE) |
| Editors | Anon |
| Publisher | IEEE |
| Pages | 1032-1037 |
| Number of pages | 6 |
| Volume | 2 |
| State | Published - 1996 |
| Event | Proceedings of 1996 MTS/IEEE Oceans Conference. Part Suppl - Fort Lauderdale, FL, USA Duration: Sep 23 1996 → Sep 26 1996 |
Other
| Other | Proceedings of 1996 MTS/IEEE Oceans Conference. Part Suppl |
|---|---|
| City | Fort Lauderdale, FL, USA |
| Period | 9/23/96 → 9/26/96 |
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ASJC Scopus subject areas
- Oceanography
Cite this
Observations of a coastal buoyant jet with HF Doppler radar. / Haus, Brian K; Graber, Hans C; Shay, Lynn K.
Oceans Conference Record (IEEE). ed. / Anon. Vol. 2 IEEE, 1996. p. 1032-1037.Research output: Chapter in Book/Report/Conference proceeding › Conference contribution
}
TY - GEN
T1 - Observations of a coastal buoyant jet with HF Doppler radar
AU - Haus, Brian K
AU - Graber, Hans C
AU - Shay, Lynn K
PY - 1996
Y1 - 1996
N2 - Currents on the inner shelf respond to a combination of forcing by intrusions of oceans fronts, eddies and internal waves as well as winds, surface gravity waves and topographic rectifications. To quantify the effect that the interaction of these processes has on inner shelf flows, a shore-based, 25.4 MHZ (High Frequency) Ocean Surface Current Radar (OSCR) was deployed to measure the surface current vector field at high spatial and temporal, resolution over the inner and mid shelf. Surface currents were mapped in near-real time. The surface current maps revealed numerous surface current features.
AB - Currents on the inner shelf respond to a combination of forcing by intrusions of oceans fronts, eddies and internal waves as well as winds, surface gravity waves and topographic rectifications. To quantify the effect that the interaction of these processes has on inner shelf flows, a shore-based, 25.4 MHZ (High Frequency) Ocean Surface Current Radar (OSCR) was deployed to measure the surface current vector field at high spatial and temporal, resolution over the inner and mid shelf. Surface currents were mapped in near-real time. The surface current maps revealed numerous surface current features.
UR - http://www.scopus.com/inward/record.url?scp=0030412184&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=0030412184&partnerID=8YFLogxK
M3 - Conference contribution
VL - 2
SP - 1032
EP - 1037
BT - Oceans Conference Record (IEEE)
A2 - Anon, null
PB - IEEE
ER -