Publications and Papers

Clarke, R. H., and G. D. Hess, 1975: On the relation between surface wind and pressure gradient, especially in lower latitudes.

http://www.springerlink.com/content/g5v8103235450065/

Crombie, D. D., K. Hasselmann, and W. Sell, 1978: High-frequency radar observations of sea waves travelling in opposition to th

http://www.springerlink.com/content/l9515760n2np164k/

Davidson, K. L., 1974: Observational results on the influence of stability and wind-wave coupling on momentum transfer and turb

http://www.springerlink.com/content/jl00w617g97584n4/

Davis, P. A., 1971: Applications of an Airborne Ruby Lidar During a BOMEX Program of Cirrus Observations. J. Appl. Meteor., 10,

http://journals.ametsoc.org/doi/abs/10.1175/1520-0450%281971%29010%3C1314%3AAOAARL%3E2.0.CO%3B2

Dawe, J. T., and P. H. Austin, 2011: Statistical analysis of a LES shallow cumulus cloud ensemble using a cloud tracking algori

http://www.atmos-chem-phys-discuss.net/11/23231/2011/acpd-11-23231-2011.html

Deacon, E. L., 1981: Sea-air gas transfer: The wind speed dependence. Boundary-Layer Meteorology, Volume 21, Number 1, 31-37, d

http://www.springerlink.com/content/h68l715j5j02rn8q/

Delnore, Victor E., 1972: Diurnal Variation of Temperature and Energy Budget for the Oceanic Mixed Layer During BOMEX. J. Phys.

http://journals.ametsoc.org/doi/abs/10.1175/1520-0485%281972%29002%3C0239%3ADVOTAE%3E2.0.CO%3B2

de Roode, Stephan R., Christopher S. Bretherton, 2003: Mass-Flux Budgets of Shallow Cumulus Clouds. J. Atmos. Sci., 60, 137-151

http://journals.ametsoc.org/doi/abs/10.1175/1520-0469%282003%29060%3C0137%3AMFBOSC%3E2.0.CO%3B2

Drummond, A. J., and G. D. Robinson, 1974: "Some Measurements of the Attenuation of Solar Radiation During BOMEX," Appl. Opt. 1

http://www.opticsinfobase.org/abstract.cfm?URI=ao-13-3-487

Elliott, Garry W., 1974: Precipitation Signatures in Sea-Surface-Layer Conditions During BOMEX. J. Phys. Oceanogr., 4, 498-501,

http://journals.ametsoc.org/doi/abs/10.1175/1520-0485%281974%29004%3C0498%3APSISSL%3E2.0.CO%3B2