AN ANALYSIS OF WALL EFFECTS IN THE MODIFIED WIELAND-TWOMEY, THERMAL DIFFUSION CLOUD NUCLEI COUNTER OF GAGIN AND TERLIUCGOROCH A; CARSTENS J.1972; J. RECH. ATMOSPH.; FR.; DA. 1972; VOL. 6; NO 4; PP. 669-672; ABS. FR.; BIBL. 4REF.Serial Issue

STABILITY EFFECTS ON AEROSOL SIZE AND HEIGHT DISTRIBUTIONSGOROCH A; BURK S; DAVIDSON KL et al.1980; TELLUS; SWE; DA. 1980; VOL. 32; NO 3; PP. 245-250; ABS. RUS; BIBL. 6 REF.Article

Observations of strong surface radar ducts over the Persian GulfBROOKS, I. M; GOROCH, A. K; ROGERS, D. P et al.Journal of applied meteorology (1988). 1999, Vol 38, Num 9, pp 1293-1310, issn 0894-8763Article

A comparison of wind speed measured by the Special Sensor Microwave Imager (SSM/I) and the Geosat altimeterNYSTUEN, J. A; LILLY, J. E; GOROCH, A. K et al.International journal of remote sensing (Print). 1993, Vol 14, Num 4, pp 745-756, issn 0143-1161Article

Oceanic precipitation rate climatologyJARRETT, T; GOROCH, A. K; VANDERHILL, M. J et al.IEE proceedings. Part F. Radar and signal processing. 1990, Vol 137, Num 2, pp 125-132, issn 0956-375XArticle

Near earth propagation studyWERT, R; GOROCH, A; TREMPER, D et al.Proceedings of SPIE, the International Society for Optical Engineering. 2005, pp 110-118, issn 0277-786X, isbn 0-8194-5805-8, 1Vol, 9 p.Conference Paper