This paper provides an overview of dust transport pathways and concentrations over the Arabian Sea during 1995. Results indicate that the transport and input of dust to the region is complex, being affected by both temporally and spatially important processes. Highest values of dust were found off the Omani coast and in the entrance to the Gulf of Oman. Dust levels were generally lower in summer than the other seasons, although still relatively high compared to other oceanic regions. The Findlater jet, rather than acting as a source of dust from Africa, appears to block the direct transport of dust to the open Arabian Sea from desert dust source regions in the Middle East and Iran/Pakistan. Dust transport aloft, above the jet, rather than at the surface, may be more important during summer. In an opposite pattern to dust, sea salt levels were exceedingly high during the summer monsoon, presumably due to the sustained strong surface winds. The high sea salt aerosols during the summer months may be impacting on the strong aerosol reflectance and absorbance signals over the Arabian Sea that are detected by satellite each year.
Tindale, Neil (2003): Aerosols, long irradiation neutron activation analysis. United States JGOFS Process Study Data 1989-1998; CD-ROM volume 1, version 2, Woods Hole Oceanographic Institution, USA: U.S. JGOFS Data Management Office
Tindale, Neil (2003): Aerosols, short irradiation neutron activation analysis. United States JGOFS Process Study Data 1989-1998; CD-ROM volume 1, version 2, Woods Hole Oceanographic Institution, USA: U.S. JGOFS Data Management Office
Direitos
CC-BY: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
Fonte
Supplement to: Tindale, Neil; Pease, P (1999): Aerosols over the Arabian Sea: Atmospheric transport pathways and concentrations of dust and sea salt. Deep Sea Research Part II: Topical Studies in Oceanography, 46(8-9), 1577-1596, doi:10.1016/S0967-0645(99)00036-3