4.7 Article

Contribution of ammonium nitrate to aerosol optical depth and direct radiative forcing by aerosols over East Asia

Journal

ATMOSPHERIC CHEMISTRY AND PHYSICS
Volume 14, Issue 4, Pages 2185-2201

Publisher

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/acp-14-2185-2014

Keywords

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Funding

  1. Ministry of Environment, Republic of Korea in Korea [411-113-013]
  2. Ministry of Environment, Republic of Korea
  3. KEITI [2012000160004]
  4. Korea Meteorological Administration Research and Development Program [CATER 2012-7110]
  5. GIST
  6. Korea Environmental Industry & Technology Institute (KEITI) [411-113-013] Funding Source: Korea Institute of Science & Technology Information (KISTI), National Science & Technology Information Service (NTIS)
  7. Korea Meteorological Administration [CATER-2012-7110] Funding Source: Korea Institute of Science & Technology Information (KISTI), National Science & Technology Information Service (NTIS)
  8. Ministry of Science, ICT & Future Planning, Republic of Korea [GIST-14-12] Funding Source: Korea Institute of Science & Technology Information (KISTI), National Science & Technology Information Service (NTIS)

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This study focused on the contribution of ammonium nitrate (NH4NO3) to aerosol optical depth (AOD) and direct radiative forcing (DRF) by aerosols over an East Asian domain. In order to evaluate the contribution, chemistry-transport model (CTM)-estimated AOD was combined with satellite-retrieved AOD, utilizing a data assimilation technique, over East Asia for the entire year of 2006. Using the assimilated AOD and CTM-estimated aerosol optical properties, the DRF by aerosols was estimated over East Asia via a radiative transfer model (RTM). Both assimilated AOD and estimated DRF values showed relatively good agreements with AOD and DRF by aerosols from AERONET. Based on these results, the contributions of NH4NO3 to AOD and DRF by aerosols (Phi(AOD) and Phi(DRF)) were estimated for the four seasons of 2006 over East Asia. Both Phi(AOD) and Phi(DRF) showed seasonal variations over East Asia within the ranges between 4.7% (summer) and 31.3% (winter) and between 4.7% (summer) and 30.7% (winter), respectively, under clear-sky conditions, showing annual average contributions of 15.6% and 15.3 %. Under all-sky conditions, Phi(DRF) varied between 3.6% (summer) and 24.5% (winter), showing annual average contribution of 12.1% over East Asia. These annual average contributions of NH4NO3 to AOD and DRF are almost comparable to the annual average mass fractions of NH4NO3 in PM2.5 and PM10 (17.0% and 14.0 %, respectively). Phi(AOD) and Phi(DRF) were even larger in the locations where NH3 and NOx emission rates are strong, such as the central East China (CEC) region and Sichuan Basin. For example, under clear-sky conditions, both Phi(AOD) and Phi(DRF) over the CEC region range between 6.9% (summer) and 47.9%(winter) and between 6.7%(summer) and 47.5% (winter), respectively. Based on this analysis, it was concluded that both Phi(AOD) and Phi(DRF) cannot be ignored in East Asian air quality and radiative forcing studies, particularly during winter.

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