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Aerosol black carbon radiative forcing at an industrial city in northern India
Author(s) -
Tripathi S. N.,
Dey Sagnik,
Tare V.,
Satheesh S. K.
Publication year - 2005
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2005gl022515
Subject(s) - radiative forcing , aerosol , atmospheric sciences , environmental science , albedo (alchemy) , single scattering albedo , climatology , atmosphere (unit) , forcing (mathematics) , planetary boundary layer , diurnal temperature variation , carbon black , meteorology , geography , geology , chemistry , art , natural rubber , organic chemistry , performance art , turbulence , art history
During a comprehensive aerosol field campaign as part of ISRO‐GBP, extensive measurements of aerosol black carbon were made during December 2004, for the first time, at Kanpur, an urban continental location in northern India. BC diurnal variation is associated with changes in boundary layer mixing and anthropogenic activities. BC concentration in Kanpur is comparable to those measured in other mega cities of India but much higher than in similar locations of Europe, USA and Asia. High BC concentration is found both in absolute terms (6–20 μg m −3 ) and mass fraction (∼10%) yielding very low single scattering albedo (0.76). The estimated surface forcing is as high as −62 ± 23 W m −2 and top of the atmosphere (TOA) forcing is +9 ± 3 W m −2 , which means the atmospheric absorption is +71 W m −2 . The short wave atmospheric absorption translates to a lower atmospheric heating of ∼1.8°K/day. Large surface cooling and lower atmospheric heating may have impacts to regional climate.
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