Laboratory simulations and parameterization of the primary marine aerosol production
By E. Mårtensson, E. D. Nilsson, G. Leeuw, L. Cohen, H. Hansson. 2003
546 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/0d6c1aae63c99798d9808a6e61e73174464a5afa
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In Atmospheric Science
- L. Harris
- Robert Hallberg
- S. Griffies
- Shian‐Jiann Lin
- I. Held
- Andrew T. Wittenberg
- V. Ramaswamy
- Alistair Adcroft
In Global and Planetary Change
- Shian‐Jiann Lin
- L. Harris
- S. Griffies
- Robert Hallberg
- M. Andreae
- Alistair Adcroft
- P. Phillipps
- Yi Ming
Citations in the corpus
- Marine aerosol production: a review of the current knowledge (2007, methodology): “Mårtensson et al. (2003) conducted experiments using artificial seawater (using aquarium-grade sea salt) for four different water temperatures and three different salinities.”
- The GFDL Global Atmosphere and Land Model AM4.0/LM4.0: 2. Model Description, Sensitivity Studies, and Tuning Strategies (2018, methodology): “For sea salt emission, the particles larger than 1.4 lm are parameterized following Monahan et al. (1986) while smaller particles are parameterized according to Martensson et al. (2003), with a 1.33 global scaling factor for both parameterizations.”
- Surfactants and submicron sea spray generation (2006, result): “A temperature dependence of the marine aerosol flux has also been observed in laboratory experiments [Monahan and O’Muircheartaigh, 1986; Mårtensson et al., 2003].”
- Biogenically driven organic contribution to marine aerosol (2004, background): “Thus, the combined aerosol physicochemical characteristics indicate a significant primary aerosol source in which bubble-bursting produces submicrometre particle”
- The composition of fragments of bubbles bursting at the ocean surface (2008, methodology): “ Maurtensson et al. [2003] found size distributions from bubble bursting under various conditions that peaked (dn/dlogr) between 50 and 100 nm diameter, with concentrations at 20 nm only about a factor of two less.”
- The comprehensive model system COSMO-ART – Radiative impact of aerosol on the state of the atmosphere on the regional scale (2009, unknown): “The parameter-isation of M˚artensson et al. (2003) is chosen for particles with a dry particle diameter of 0.02 µ m < D p < 1 µ m. are This is illustrated in Fig.”
- The GFDL Earth System Model Version 4.1 (GFDL‐ESM 4.1): Overall Coupled Model Description and Simulation Characteristics (2020, methodology): “0 using the temperature dependence of Mårtensson et al. (2003), was revised to the stronger temperature‐dependent function of Jaeglé et al. (2011), which takes into account newer constraints from in situ and remotely sensed observations and improves comparison against surface observations in the…”
- Aerosol cloud precipitation interactions. Part 1. The nature and sources of cloud-active aerosols (2008, background): “In contrast, the recent SSA flux study by Nilsson et al. (2007) suggests better agreement with the Mårtensson et al. (2003) parameterization scheme.”