Aerosol loading in coastal and marine environments in the Indian Ocean region during winter season

Citation
K. Parameswaran et al., Aerosol loading in coastal and marine environments in the Indian Ocean region during winter season, CURRENT SCI, 76(7), 1999, pp. 947-955
Citations number
8
Categorie Soggetti
Multidisciplinary,Multidisciplinary
Journal title
CURRENT SCIENCE
ISSN journal
00113891 → ACNP
Volume
76
Issue
7
Year of publication
1999
Pages
947 - 955
Database
ISI
SICI code
0011-3891(19990410)76:7<947:ALICAM>2.0.ZU;2-7
Abstract
The mass loading of aerosols in the coastal and marine environments is stud ied using a high volume sampler (HVS) and a low pressure impactor (LPI) dur ing the first field phase of the Indian Ocean Experiment (INDOEX), These st udies show that aerosol loading at Thiruvananthapuram is in the range 20-13 0 mu g/m(3) depending on the wind direction. During the sea breeze period, the concentration is low, and during the land breeze period, it is rather h igh. The mean size distribution obtained using the LPI, in general, shows a trimodal distribution. The measurements conducted on the cruise show that the mass loading over the ocean, near to the Thiruvananthapuram coast, is s imilar to 25-40 mu g/m(3) which is comparable to that observed on the coast during the day. At Male a significant reduction in aerosol loading is obse rved when the prevailing flow pattern from north changed to south. This ind icates an increased concentration of aerosols in the northern hemispheric a ir, A sharp decrease in aerosol loading is observed at the Inter-Tropical C onvergence Zone (ITCZ), similar to 15 degrees S during the southward voyage of the ship. South of ITCZ, aerosol loading is less than that in the north . A significant reduction in aerosol concentration is observed during the r eturn voyage in the latitude region 12 degrees S to the equator. An enhance ment in aerosol loading is observed in the central Arabian Sea (lat, 10-15 degrees N), which is higher than near the Indian coast, The cruise data als o showed a significant positive correlation between the columnar aerosol op tical depth (at 0.5 mu m wavelength) and the surface mass loading.