The Monterey Area Ship Track Experiment

By P. Durkee, K. Noone, R. Luth. 2000

136 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/a49c46f07b697d7ddb49b0b20a8891c0d9512005

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. G. Feingold
2. H. Xue
3. Bjorn Stevens
4. C. D. Walsh
5. J. Snider
6. C. Twohy
7. M. Petters
8. F. Burnet

In Global and Planetary Change

1. G. Feingold
2. H. Xue
3. Bjorn Stevens
4. C. D. Walsh
5. L. Russell
6. J. Snider
7. C. Twohy
8. M. Petters

Citations in the corpus

• Limits to the Aerosol Indirect Radiative Effect Derived from Observations of Ship Tracks (2002, methodology): “…tracks produced in low-level clouds were extensively studied in the Monterey Area Ship Track (MAST) experiment which was conducted in June 1994 [Durkee et al. (2000) and the other papers in the 15 August 2000 issue of the Journal of the Atmospheric Sciences (Vol. 57, No. 16), which is devoted…”
• Large-Eddy Simulations of Trade Wind Cumuli: Investigation of Aerosol Indirect Effects (2006, methodology): “1996), the Monterey Area Ship Track Experiments (Durkee et al. 2000), the Aerosol Characterization Experiment-II CLOUDY COLUMN experiments (Brenguier et al.”
• Evaluation of the aerosol indirect effect in marine stratocumulus clouds : droplet number, size, liquid water path, and radiative impact (2005, background): “[3] Local enhancements to the atmospheric aerosol through the injections of particles associated with ship exhaust have been associated with ‘‘tracks’’ in clouds, i.e., linear regions of locally higher aerosol particle and cloud droplet concentrations and greater cloud reflectivities [Radke et al., ”
• Large‐eddy simulation of the transient and near‐equilibrium behavior of precipitating shallow convection (2015, unknown): “Observational studies of ship tracks provide another inadvertent experiment within which one could hope to identify lifetime effects [Conover, 1969; Durkee et al., 2000; Hobbs et al., 2000], but in many cases the opposite response of clouds to aerosol perturbations is observed: some observations [Ch”