IIA Institutional Repository

High altitude (∼4520 m amsl) measurements of black carbon aerosols over Western trans-Himalayas: seasonal heterogeneity and source apportionment

Show simple item record

dc.contributor.author Babu, S. S
dc.contributor.author Chaubey, Jai Prakash
dc.contributor.author Krishna Moorthy, K
dc.contributor.author Gogoi, M. M
dc.contributor.author Kompalli, S. K
dc.contributor.author Sreekanth, V
dc.contributor.author Bagare, S. P
dc.contributor.author Bhatt, B. C
dc.contributor.author Gaur, V. K
dc.contributor.author Prabhu, T. P
dc.contributor.author Shantikumar, N. S
dc.date.accessioned 2012-01-27T14:39:54Z
dc.date.available 2012-01-27T14:39:54Z
dc.date.issued 2011-12
dc.identifier.citation Journal of Geophysical Research D, Vol. 116, D24201 en
dc.identifier.uri http://hdl.handle.net/2248/5681
dc.description Open Access en
dc.description.abstract The first ever, year-round measurements of aerosol black carbon (BC) over the western part of trans- Himalayas are reported from Hanle (∼4520 m above mean sea level). The daily mean BC concentrations varied from as low as 7 ng m−3 to as high as 296 ng m−3 with an annual average of 77 ± 64 ng m−3, indicating significant BC burden even at free- tropospheric altitudes. Variation with in the day as well as from day to day were highly subdued during winter season (December to February) while they used to be the highest in Spring (March to May). In general, the less frequently occurring high BC values contributed more to the annual and seasonal means, while 64% of the values were below the annual mean. Seasonally, highest BC concentration (109 ± 78 ng m−3) occurred during Spring and lowest (66 ± 42/66 ± 62 ng m3) during Summer/Winter season(June to August/December to February). Diurnal variations in general were very weak, except during Spring and Summer when the effects of convective boundary layer dynamics is discernible. Back trajectory clustering and concentration weighted trajectory (CWT) analyses indicated that, most time of the year the sampling location is influenced by the advection from West and Southwest Asia, while the contribution from the Indo-Gangetic Plains (IGP) remained very low during Spring and Summer. The seasonal and annual mean BC at Hanle are significantly lower than the corresponding values reported for other Himalayan stations, while they were quite higher than those reported from the South Pole and pristine Antarctic environments. en
dc.language.iso en en
dc.publisher American Geophysical Union en
dc.relation.uri http://dx.doi.org/10.1029/2011JD016722 en
dc.rights © American Geophysical Union en
dc.title High altitude (∼4520 m amsl) measurements of black carbon aerosols over Western trans-Himalayas: seasonal heterogeneity and source apportionment en
dc.type Article en


Files in this item

This item appears in the following Collection(s)

Show simple item record

Search DSpace


Browse

My Account