An improved whitecap timescale for sea spray aerosol production flux modeling using the discrete whitecap method
Abstract
The discrete whitecap method (DWM) to model the sea spray aerosol (SSA) production flux explicitly requires a whitecap timescale, which up to now has only considered a whitecap decay timescale, τdecay. A reevaluation of the DWM suggests that the whitecap timescale should account for the total whitecap lifetime (τwcap), which consists of both the formation timescale (τform) and the decay timescale (timescale definitions are given in the text). Here values of τform for 552 oceanic whitecaps measured at the Martha's Vineyard Coastal Observatory on the east coast of the USA are presented, and added to the corresponding values of τdecay to form 552 whitecap timescales. For the majority of whitecaps, τform makes up about 20–25% of τwcap, but this can be as large as 70% depending on the value of τdecay. Furthermore, an area‐weighted mean whitecap timescale for use in the DWM (τDWM) is defined that encompasses the variable nature of individual whitecap lifetimes within a given time period, and is calculated to be 5.3 s for this entire data set. This value is combined with previously published whitecap coverage parameterizations and estimates of SSA particle production per whitecap area to form a size‐resolved SSA production flux parameterization (dF(r80)/dlog10r80). This parameterization yields integrated sea‐salt mass fluxes that are largely within the range of uncertainty of recent measurements over the size range 0.029 µm r80 < 0.580 µm. Physical factors controlling whitecap lifetime such as bubble plume lifetime and surfactant stabilization are discussed in the context of SSA production from whitecaps.
Document Details
- Document Type
- Pub Defense Publication
- Publication Date
- Sep 09, 2013
- Source ID
- 10.1002/jgrd.50768
Entities
People
- Adrian H. Callaghan
Organizations
- Martin Ryan Institute
- National Science Foundation
- Office of Naval Research
- University of California, San Diego