The isothermal haze chamber with discontinuous flow : a new experimental device for CCN measurements at low supersaturationLEGRAND, C.Atmospheric research. 2000, Vol 54, Num 4, pp 263-277, issn 0169-8095Article

A continuous-flow streamwise thermal-gradient CCN chamber for atmospheric measurementsROBERTS, G. C; NENES, A.Aerosol science and technology. 2005, Vol 39, Num 3, pp 206-221, issn 0278-6826, 16 p.Article

TRANSVERSE MOMENTA FROM AN AIR-SHOWER STUDY.HAZEN WE; HODSON AL; WINTERSTEIN D et al.sdIN: 13TH INT. COSMIC RAY CONF.; DENVER, COLO.; 1973; DENVER, COLO.; UNIV. DENVER; DA. S.D.; VOL. 3; PP. 2124-2125; BIBL. 2 REF.Conference Paper

ANALYSIS OF A CONTINUOUS FLOW PARALLEL PLATE THERMAL DIFFUSION CLOUD CHAMBERBROWN JT JR; SCHOWENGERDT FD.1979; J. AEROSOL SCI.; GBR; DA. 1979; VOL. 10; NO 3; PP. 339-348; BIBL. 13 REF.Article

SEARCH FOR E/3 QUARKS IN COSMIC RAYS WITH THE LEEDS CLOUD CHAMBER.HAZEN WE; HODSON AL; WINTERSTEIN D et al.sdIN: 13TH INT. COSMIC RAY CONF.; DENVER, COLO.; 1973; DENVER, COLO.; UNIV. DENVER; DA. S.D.; VOL. 3; PP. 2087-2089; BIBL. 9 REF.Conference Paper

A THEORETICAL STUDY OF THE EFFECT OF DIFFUSION ON THE POSITIONS OF DROPS IN A LOW-PRESSURE CLOUD CHAMBERHOLT PD.1972; AERE-R-5993; G.B.; DA. 1972; PP. 1-8; BIBL. 12 REF.Report

ON THE LACK OF FRACTIONALLY CHARGED PARTICLES IN COSMIC RADIATION.CLARK AF; ERNST RD; FINN HF et al.sdIN: 13TH INT. COSMIC RAY CONF.; DENVER, COLO.; 1973; DENVER, COLO.; UNIV. DENVER; DA. S.D.; VOL. 3; PP. 2090-2095; BIBL. 5 REF.Conference Paper

VAPOR CHAMBERS FOR AN ATMOSPHERIC CLOUD PHYSICS LABORATORYFLEISCHMAN GL; SCOLLON TR JR; LOOSE JD et al.1981; PROG. ASTRONAUT. AERONAUT.; ISSN 0079-6050; USA; DA. 1981; VOL. 78; PP. 375-401; BIBL. 8 REF.Conference Paper

SUPERSATURATION REGIME WITHIN A SETTLING CLOUD CHAMBER: PRELIMINARY RESULTS.WEICKMANN KM; BARCHET WR.1976; IN: INT. CONF. CLOUD PHYS. PREPR.; BOULDER, COLO.; 1976; BOSTON, MASS.; AM. METEOROL. SOC.; DA. 1976; PP. 602-606; BIBL. 17 REF.Conference Paper

Développement d'un système de mesure des spectres de gouttes en laboratoire = Drop spectrum measuring system for use in a laboratoryPERRIN, Thierry.1984, 133 pThesis

Determination of carbon balances for smog chamber terpene oxidation experiments using a ¹⁴C tracer techniqueHOOKER, C. L; WESTBERG, H. H; SHEPPARD, J. C et al.Journal of atmospheric chemistry. 1985, Vol 2, Num 3, pp 307-320, issn 0167-7764Article

Initial growth forms of snow crystals growing from frozen cloud dropletsYAMAZAKI, G; YAMAZAKI, T.Journal of the Meteorological Society of Japan. 1984, Vol 62, Num 1, pp 190-192, issn 0026-1165Article

Chambre à nuages, de petit volume, munie d'un enregistrement automatique des cristaux de glaceGORBUNOV, B. Z; KAKUTKINA, N. A; KUTSENOGIJ, K. P et al.Izvestiâ Akademii nauk SSSR. Fizika atmosfery i okeana. 1986, Vol 22, Num 3, pp 329-330, issn 0002-3515Article

Morphology of ice crystals grown from the vapour at temperatures between -4 and -1.5°CYAMASHITA, A; ASANO, A.Journal of the Meteorological Society of Japan. 1984, Vol 62, Num 1, pp 140-145, issn 0026-1165Article

ADVANCES IN CLOUD-CHAMBER TECHNIQUES AND MEASUREMENTS OF W VALUE IN A TISSUE-EQUIVALENT GASBUDD T; MARSHALL M; KWOK CS et al.1981; RADIAT. RES.; ISSN 0033-7587; USA; DA. 1981; VOL. 88; NO 2; PP. 228-239; BIBL. 18 REF.Article

EFFET DE LA VISCOSITE SUR LES PROPRIETES DE RESONANCE DES CHAMBRES DE DETENTEEGOR'ICHEV AV; KRAVCHUN PN; CHERNYSHEV KV et al.1978; VEST. MOSKOV. UNIV., 3; SUN; DA. 1978; NO 2; PP. 106-109; BIBL. 2 REF.Article

SPECIFIC IONIZATION OF COSMIC RAY MUONS IN THE MOMENTUM RANGE 3-2000 GEV/C.BASU PS; NANDI BC; SINHA MS et al.sdIN: 13TH INT. COSMIC RAY CONF.; DENVER, COLO.; 1973; DENVER, COLO.; UNIV. DENVER; DA. S.D.; VOL. 3; PP. 2045-2050; BIBL. 6 REF.Conference Paper

A SIMPLE CONTINUOUS ICE CRYSTAL REPLICATOR FOR USE IN LABORATORY CLOUD CHAMBERS.WISHART ER.1977; J. APPL. METEOROL.; U.S.A.; DA. 1977; VOL. 16; NO 3; PP. 317-318; BIBL. 10 REF.Article

LACK OF LOW-DENSITY COSMIC-RAY TRACKS.CLARK AF; FINN HF; HANSEN NE et al.1974; PHYS. REV., D; U.S.A.; DA. 1974; VOL. 10; NO 9; PP. 2721-2734; BIBL. 15 REF.Article

CLOUD CHAMBERS: EXPANSION AND DIFFUSIONSHUTT RP.1979; NUCL. INSTRUM. METHODS; NLD; DA. 1979; VOL. 162; NO 1-3 PART. 2; PP. 379-388; BIBL. 7 REF.Article

THE HYBRID GAS-LIQUID CHAMBER - A NEW COMBINED TRACK DETECTOR.BAKANOV LV; ERMAKOV KN; LEBEDEV VD et al.1977; NUCL. INSTRUM. METHODS; NETHERL.; DA. 1977; VOL. 144; NO 2; PP. 99-101; BIBL. 8 REF.Article

A CONDENSATION NUCLEUS SIJE ANALYZER SUITABLE FOR STUDYING THE KINETICS OF AEROSOL FORMATION.SCHMIDT KH.1975; INTERNATION. J. CHEM. KINET.; U.S.A.; DA. 1975; NO 1; PP. 557-565; BIBL. 2 REF.; (SYMP. CHEM. KINET. DATA UPPER LOWER ATMOS. PROC.; WARRENTON, VA.; 1974)Conference Paper

MEASUREMENTS OF AEROSOL CONCENTRATION UP TO A HEIGHT OF 27 KM.KASELAU KH; FABIAN P; ROHRS H et al.1974; PURE APPL. GEOPHYS.; SWITZ.; DA. 1974; VOL. 112; NO 6; PP. 877-885; BIBL. 6 REF.; (TRACE SUBST. ATMOS. SOURCE SINK. SYMP. Q. PART OF THE 2ND ANNU. MEET. EUR. GEOPHYS. SOC. TRIESTE; 1974)Conference Paper

DEVELOPMENT OF A MIXING TYPE CONDENSATION NUCLEUS COUNTERKOUSAKA Y; NIIDA T; OKUYAMA K et al.1982; J. AEROSOL SCI.; ISSN 0021-8502; GBR; DA. 1982; VOL. 13; NO 3; PP. 231-240; BIBL. 9 REF.Article

FORMES PARTICULIERES DES CRISTAUX DE GLACE FORMES DANS UNE CHAMBRE A NUAGEABURAKAWA H.1982; TEION KAGAKU, BUTSURI-HEN; ISSN 0439-3538; JPN; DA. 1982; VOL. 40; NO 56; PP. 155-157; BIBL. 5 REF.Article