Abstract
Single-scattering albedo (SSA) and absorption Ångström exponent (AAE) are two critical parameters in determining the impact of absorbing aerosol on the Earth's radiative balance. Aerosol emitted by biomass burning represent a significant fraction of absorbing aerosol globally, but it remains difficult to accurately predict SSA and AAE for biomass burning aerosol. Black carbon (BC), brown carbon (BrC), and non-absorbing coatings all make substantial contributions to the absorption coefficient of biomass burning aerosol. SSA and AAE cannot be directly predicted based on fuel type because they depend strongly on burn conditions. It has been suggested that SSA can be effectively parameterized via the modified combustion efficiency (MCE) of a biomass burning event and that this would be useful because emission factors for CO and CO2, from which MCE can be calculated, are available for a large number of fuels. Here we demonstrate, with data from the FLAME-4 experiment, that for a wide variety of globally relevant biomass fuels, over a range of combustion conditions, parameterizations of SSA and AAE based on the elemental carbon (EC) to organic carbon (OC) mass ratio are quantitatively superior to parameterizations based on MCE. We show that the EC/OC ratio and the ratio of EC/(EC + OC) both have significantly better correlations with SSA than MCE. Furthermore, the relationship of EC/(EC + OC) with SSA is linear. These improved parameterizations are significant because, similar to MCE, emission factors for EC (or black carbon) and OC are available for a wide range of biomass fuels. Fitting SSA with MCE yields correlation coefficients (Pearson's r) of ∼0.65 at the visible wavelengths of 405, 532, and 660 nm while fitting SSA with EC/OC or EC/(EC + OC) yields a Pearson's r of 0.94-0.97 at these same wavelengths. The strong correlation coefficient at 405 nm (r = 0.97) suggests that parameterizations based on EC/OC or EC/(EC + OC) have good predictive capabilities even for fuels in which brown carbon absorption is significant. Notably, these parameterizations are effective for emissions from Indonesian peat, which have very little black carbon but significant brown carbon (SSA = 0.990 ± 0.001 at 532 and 660 nm, SSA = 0.937 ± 0.011 at 405 nm). Finally, we demonstrate that our parameterization based on EC/(EC + OC) accurately predicts SSA during the first few hours of plume aging with data from Yokelson et al. (2009) gathered during a biomass burning event in the Yucatán Peninsula of Mexico.
| Original language | English |
|---|---|
| Pages (from-to) | 9549-9561 |
| Number of pages | 13 |
| Journal | Atmospheric Chemistry and Physics |
| Volume | 16 |
| Issue number | 15 |
| DOIs | |
| State | Published - Aug 1 2016 |
Funding
This material is based upon work supported by the National Science Foundation under grant no. 1241479. Chelsea E. Stockwell and Robert J. Yokelson were supported primarily by NSF grant ATM-0936321. Thilina Jayarathne and Elizabeth A. Stone were supported by University of Iowa. FSL operational costs were supported by NASA Earth Science Division Award NNX12AH17G to S. Kreidenweis, P. DeMott, and G. McMeeking, whose collaboration in organizing and executing FLAME-4 is gratefully acknowledged. We thank Ted Christian, Dorothy L. Fibiger, and Shunsuke Nakao for assistance with filter sample collection and sample preparation. We appreciate the contribution of Eric Miller, DavidWeise, Greg Askins, Guenter Engling, Savitri Garivait, Christian L'Orange, Benjamin Legendre, Brian Jenkins, Emily Lincoln, Navashni Govender, Chris Geron, and Kary Peterson for harvesting the fuels for this study. Collection of Indonesian peat by Kevin Ryan and Mark Cochrane was supported by NASA Earth Science Division Award NX13AP46. We also thank Daniel Murphy for valuable suggestions during data collection and manuscript preparation.
| Funders | Funder number |
|---|---|
| 1241479, ATM-0936321 | |
| National Aeronautics and Space Administration | NNX12AH17G |
| University of Iowa | |
| NX13AP46 |