Emanuele Böhm

TL;DR: In this paper, a mechanism for the entrainment of cold upwelled waters into plumes is hypothesized, and validated by observational data, and it is proposed that the location of the plume is primarily governed by the sea level structure away from the coast and that coastally upwelling water is passively advected offshore through regions of low sea level.

TL;DR: In this article, satellite-derived sea-surface temperature, TOPEX/POSEIDON (T/P) sea-level anomalies, model wind data, and hydrographic data are used to characterize the upwelling along the Oman coast during the US Joint Global Ocean Flux Study (US JGOFS) Arabian Sea Process Study (ASPS) in 1995 as well as to look at interannual variability in the Upwelling over the period 1993-1995.

TL;DR: In this article, the authors used time and frequency domain analyses to relate coastal meteorological data with 7 years of daily surface temperature and salinity collected at three coastal light stations; offshore of the mouth of Chesapeake Bay, Virginia, on Diamond Shoals, at Cape Hatteras, North Carolina and on Frying Pan Shoals, off Cape Fear.

TL;DR: The existence of a surface barotropic front-jet system at the confluence region off the eastern tip of Oman (Ras Al Hadd or RAH) is documented for 1994-1995 through advanced very high resolution radiometer (AVHRR) and acoustic Doppler current profiler (ADCP) observations as mentioned in this paper.

TL;DR: In this article, a methode simple for estiming the vitesse quand le courant contourne un promontoire prononce was presented, in which le parterre de la vorticite potentielle was calculated.