Table Of Content

ATMOSPHERIC Ete, RESEARCH Atmospheric Research 36 (1995) 347-348 Contents Volume 36, 1995 Torrential precipitations on the Spanish east coast: The role of the Mediterranean sea surface temperature ny Seen: Far, IC: SN i ss Sask destin otven rie eeneeteae eine ias deine nak Cc | Some characteristics of the precipitation formed within winter storms over eastern Newfoundland ee nNOS Ne I ics els chinn k ohb vu nton eu Dun aanenedwalCh shud obey REaeE NE wees eRAL ki 17 A parameterization of cloud droplet nucleation. Part II: multiple aerosol types oJ. Guan, C.C. Chmeme, B.C. Baste and 3.0. FORGO oo oi oes ciccccccccsccccesscccecsncsevevecesoegiaseveses 39 Wind-produced submicron particles in the marine atmosphere pes I ec ME a IN oo oc cins ens ds da env agny Sas) ped snnvnqavenadVse scutkdsdnensesn hc at 55 Theory of the water vapor continuum and validations I a a Lt acs aia naga vb end Ran GWEN WARROCK aaa Dew EN Cue baeSuie meas 69 Ice-forming nuclei over the East China Sea Fe Pty MasF s PI RII RE No iio ive sti cevcdnebineacnducdepersasciensecadenervaresetiees 95 Simulation of hydrometeor size spectra evolution by water—water, ice—water and ice-ice interactions St eI MO si pc oa anaes Nida h che nndecne ee Mpuss an cadiin saxwsbus SeAouY shes yeeneon e+e 107 An environmental experiment over Athens urban area under sea breeze conditions eer ~S N, Fi: Pe OO TD. I aa cn sv seed cccn swede csncessovesncenetarepoubirendesessveness 139 Air mass characteristics as related to tropical wave precipitation over Lesser Antilles archipelago re ee UNI cog oh ov bo Ga knee O Aa EX Re aig ee Ode REE ean be oaneaneneee 157 Letter Section A new concept for assessing silver iodide cloud-seeding effects in snow by physical and chemical methods Delt POU Tics TN I FI oi esoi e vic wenger bhi cided es ceqensncuaenacsdscepasnsseebeniaumauers 171 FRIST ANAL ES OT SE RPG oo CME TESTS SPIEL SERN EN RTI NY LAY ABS NIF T 7 AS RO 177 a ee a oa Se ela ages Oe cig eu Wl puck abe aE Ea ue eae baseue iret 181 aie aire tabu fun bb Peat beh ac unde amine bade Ses wog ied sei cuales Cubed SN TeEE PLS MaE NEST ELAN 183 Climatic mapping of ice loads based on airport weather observations I I 0 go ss ras ya auld epee Le brs cna PRD EID na odd MRR aoa emeNbeRe 185 Spatial variation of extreme values for freezing rain SRE EE BRE ee ONS EM ey eR, be OSE Ad DRE ee oR ROMER PO Te MRED EE PETC Tee ewe 195 A comparison of selected models for estimating cable icing Sa: 2 I au oc salah W sian bob 401 veh caus Kshnbeautuned eee ckasus vent 207 Estimating icing amounts caused by freezing precipitation in Canada MN ere hate Rani cae te a fe ee acl a ap wailia eee Nk aba uninkn wee EERE wees 221 2-D and 3-D modelling of low density ice accretion on rotating wires with variable surface irregularities a SR 2 2 our a babe diaade soe bean sian ante nt eehee Te henetiseei Gs 348 Contents Volume 36 / Atmospheric Research 36 (1995) 347-348 Simulation of icicle growth using a three-dimensional random walk model REA tL RIN Meee faeg h tL SOREN PMN eyro 35 een Dae ae eRe eT. PES The effect of aerodynamic torque on the rotation of an overhead line conductor during snow accretion Nee eee nnn enn eeeee Clive v e eem abe poanecdue Correlation of ice load with large-scale and local meteorological conditions in Hungary J. Mika, T. Szentimrey, M. Csomor, Z. Kévér, C. Nemes and P. Domonkos ....................0000005 Use and calibration of Rosemount ice detectors for meteorological research eg er I I og oS dice evnccucsspelssdand venehcdteeeseyecussccssbespercess Wind tunnel evaluation of a rime metering device using a magnetostrictive sensor es ee, es sc ebawh doe unearned dee vavaxceucdkekerirvevacss A method to estimate icing loads on overhead lines ge i i rE url le dir ea le Gao a pb Rade bw eaNeENEs er ie> Hungarian icing activity survey IRS IEEE I aA PURER A CNSR a TER ON RENO ee ODN ot MEE ng tea Oe ayer eee tT ae Superstructure spray and ice accretion on a large U.S. Coast Guard cutter I Ira saat MB Dae uN ded iaddbbasdannedepaueleoey Aircraft icing in visual meterological conditions below low stratus clouds ee a Fi ears eee aS Ra as Vids thenewneatcdieestedd