2013
DOI: 10.1016/j.dsr.2012.12.004
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High salinity events in the northern Arabian Sea and Sea of Oman

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Cited by 29 publications
(21 citation statements)
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“…The lower salt tolerance threshold of Prochlorococcus SS120 could reflect the characteristics of its native environment, namely that the average salt concentration is between 3.5 and 3.8%. In contrast, Prochlorococcus AS9601 is an isolate from the Arabian Sea (Shalapyonok et al, 1998), and the average salt concentration in the water is reported to exceed 4.0% (Wang et al, 2013). Therefore, we suspect that the AS9601 strain is adapted to survive in seawater containing higher salt concentrations when compared to Prochlorococcus isolates from other parts of the world's oceans.…”
Section: Salt Acclimated Cells Exhibit Slower Growth Ratesmentioning
confidence: 82%
“…The lower salt tolerance threshold of Prochlorococcus SS120 could reflect the characteristics of its native environment, namely that the average salt concentration is between 3.5 and 3.8%. In contrast, Prochlorococcus AS9601 is an isolate from the Arabian Sea (Shalapyonok et al, 1998), and the average salt concentration in the water is reported to exceed 4.0% (Wang et al, 2013). Therefore, we suspect that the AS9601 strain is adapted to survive in seawater containing higher salt concentrations when compared to Prochlorococcus isolates from other parts of the world's oceans.…”
Section: Salt Acclimated Cells Exhibit Slower Growth Ratesmentioning
confidence: 82%
“…These ejections were related to the presence of mesoscale eddies in the Sea of Oman, and especially to the presence of a dipole in spring; different offshore ejection mechanisms were identified. PGW ejection was also identified in response to tropical atmospheric cyclones (in particular cyclone Gonu; Wang et al, 2012Wang et al, , 2013.…”
Section: Introductionmentioning
confidence: 99%
“…Indeed, in October-November 1999, during the fall intermonsoon, the GOGP99 1 experiment at sea sampled the PGW outflow and identified it as a coastal flow, extending to the southern coast of Oman (see Pous et al, 2004). During other seasons, the path of the PGW in the Gulf of Oman is less regular, as shown by observations and by numerical modeling; also, PGW can exit in the form of short pulses (see Banse, 1997;Senjyu et al, 1998;Bower et al, 2000;Prasad et al, 2001;Thoppil and Hogan, 2009;Wang et al, 2012;Wang et al, 2013). Recently, ARGO floats (see Carton et al, 2012;L'Hégaret et al, 2013) and HYCOM numerical simulations (see L'Hégaret et al, 2015) confirmed that during other seasons, PGW can be expelled from the coast into the Sea of Oman.…”
Section: Introductionmentioning
confidence: 99%
“…Evidence has been shown of seasonal or higher-frequency variability of the surface circulation in the Sea of Oman, which has been related to atmospheric forcing (seasonal wind stress or the effect of atmospheric cyclones) or to Rossby waves emitted from the eastern boundary (Pakistan and India; see Schott et al, 2009). In particular, mesoscale oceanic dipoles (cyclone + anticyclone), as well as isolated eddies, have been observed in the vicinity of Ra's al Hamra (see L'Hegaret et al, 2013) and off Ra's al Hadd (see Wang et al, 2013).…”
Section: Introductionmentioning
confidence: 99%