Table Of Content

Atmospheric Research, 31 (1994) 359 359 Elsevier Science B.V., Amsterdam Contents Volume 31, 1994 Editorial I asSigesd nine canaive ntodeeeinighehaianddsideieiensebitebees A molecular model for homogeneous nucleation A a dhe eslamhninicarpe bab binegtmediipiabieenehe On the variation of cloud condensation nuclei in association with cloud systems at a mountain-top location Fe ee as Sih seshn sdiablav cccciesdiat aceientetecidpeecibnsadba napus tuepibipaabcebpnnatenieseyuinivnusarvineens Cloud-active particles from African savanna combustion experiments Pham-Van-Dinh, J.-P. Lacaux and R. Serpolay................ccceeesssseececceececeeeeessseeeceeeeeeeeeseeeeeeeeeeees The temperature of an evaporating water droplet with a monolayer coating: comparison of experiment and theory A I i andl aiebia co aiaienligoeselialinienacaainna kines The role of clouds in the enhancement of cloud condensation nuclei concentrations Fe ee HO bcs isiccersicccneniccteseilasdoanancivsenvsonsnneniniiibanteosaneitedersescobntignatenasavees Varying the condensable water vapor content in an expansion cloud chamber aii, UI ai aicokanclaitahdscdenentceicghbiinrbnelaounibciiiesedibininrdineisioinns Efficacy test of a haze chamber with the CCN produced by the burning of savannah grasses EELS ESE ISS BE SEATS oe ORE rE EET EPC SRE CC Ton NE PEO TERY F ane ST Ce IT Ice-producing processes in a North Dakota cumulus cloud A.G. Detwiler, P.L. Smith, J.L. Stith and D.A. Burrow,.....................ccccccssscccssscccesesccesscccsesssces Potential role of nuclei in cloud element formation at high altitudes D.E. Hagen, J. Podzimek, A.J. Heymsfield, M.B. Trueblood and C.K. Lutrus.................... Increasing of the solubility of the AgI nuclei in rain drops induced by the complex formation with dominant ions T.V. Reutova, L.Z. Zhinzhakova and M.M. Chernyak ....................cccceceeeceeeeeeeseeeeeeeeeeseeeseeeeeens On the Terminology of ‘““Thermal Diffusion Chamber” a dale boneeiniene lilacs hale daccanehewrominneseiols Mixtures of nitrate and sulfate in individual particles in acidic fogs ashebeb eeline in cbioalea esi besnuipiaweveetalake Initial cloud droplet number concentrations in clean and polluted areas: Simulation by a condensation model and comparison with measurements | ARSENE SRI RBG We a et eatse aten eR UN Stet Sab ON eee ee MPEEEE NS MRE eae NNT ERR MCERE PDS HAIN On the description of aerosol particle size distribution pgDy ERR SERRE TSE at WP ATER Re es CT a NPN CCI AA TN Oe cS a SOR Mixed aerosol particles as effective ice nucleating systems SRE ESS SSS a Ce WRT TSN we UORRE OS Ree! cS Ree CO aT aF We een erm New microphysics sensor for aircraft use Fe I i ciicsacsitivecanninnsesasiilsmacanaderbensabinnldibcsencaasbesvennetascds The continental carbon cycle during the last glacial maximum I asa ieapie aed reek eosnsnun eka eamiaevan ar inneiialinet Introduction Rt OL LE RIE SF AOL RTT eo oP REY ONT VET NT ERT NTE TOOT TEE RINT Light scattering by nonspherical particles: Remote sensing and climatic implications Se NN a as sasineaiadamehenaianddsnsseubenetainaneeineiniebenenn ~~ Radiative-convective disequilibrium Sa, Se i Fe iva sc nsscoepnanieveinndsbasecnmnantnnusinispeedinioaenesin Planned EOS observations of the land, ocean and atmosphere EEE EN RNR EEE SAAR NORD aE TE SO PRR aero 2 OUI ene oe Oe eT