Ocean surface current mapping with bistatic HF radar[P]. United States Patent, 2004, No. 2004/0090363 A1.Barrick D E,Lilleboe P M,Lipa B J. Ocean surface current mapping with bistatic HF radar[P].United States Patent,No,2004/0090363 A1 2004....
The Doppler spectrum of radar return from the sea at HF contains two narrow lines displaced upward and downward from the carrier frequency, resulting from backscatter off ocean surface waves moving toward and away from the radar, respectively. These Bragg lines indicate resonant backscatter which occu...
Ocean surface currents play a key role in the earth's climate. They affect virtually all processes occurring in the ocean and can also directly affect many important socio-economic activities. Himawari-8 meteorological satellite has an international advanced geostationary orbit imager sensor, AHI, with...
The ocean surface currents were reconstructed from the satellite remote sensing data containing altimeter-derived sea surface height and QuikSCAT satellite-derived wind data. Based on the method proposed by Lagerloef, a global weekly 0.5°×0.5° ocean s
Evaluation of turbulent fluxes at the ocean surface using surface renewal theory An internally consistent model is presented that can be used to determine the ocean surface fluxes of heat, moisture, and momentum, given bulk sea surface ... CA Clayson,CW Fairall,JA Curry - 《Journal of ...
How is the SURFACE OCEAN CURRENT(red line)in the image change as it moves through equatorial regions on its path from the Pacific Ocean to the Atlantic Ocean? select all that apply map Group of answer choices it becomes COOLER its salinit...
The OSCAR (ocean surface current analysis real-time), which is a product derived from various satellite observations, has been evaluated in the tropical Indian Ocean (TIO) in two different ways. First, the OSCAR-derived monthly climatology has been compared with available drifter-derived climatology...
SST- Sea Surface Temperature. Temperature of the ocean surface SSTA- Sea Surface Temperature Anomaly. Difference in ocean temperature from daily average during years 1981-2011 HTSGW- Significant Wave Height. Roughly equal to mean wave height as estimated by a "trained observer" ...
least ∼35–45kgm−3, depending on thesalinityand temperature of the ambient ocean water, to be able to plunge (Khan et al., 2005;Mulder and Syvitski, 1995). Hyperpycnal flows can travel significant distances beyond the continental shelf and may be sustained for hours to weeks, hence ...
The ocean can couple with the atmosphere both through the oceanic thermal feedback (e.g.,17,18,19,20,21,22,23,24) and the current feedback (e.g.,25,26,27,28,29,30,31,32,33,34). Both coupling processes strongly involve mesoscale eddies. At the mesoscale, Sea Surface Temperature (...