Observations and Parameterizations of Particle Size Distributions in Deep Tropical Cirrus and Stratiform Precipitating Clouds: Results from In Situ Observations in TRMM Field Campaigns

Abstract This study reports on the evolution of particle size distributions (PSDs) and habits as measured during slow, Lagrangian-type spiral descents through deep subtropical and tropical cloud layers in Florida, Brazil, and Kwajalein, Marshall Islands, most of which were precipitating. The objective of the flight patterns was to learn more about how the PSDs evolved in the vertical and to obtain information of the vertical structure of microphysical properties. New instrumentation yielding better information on the concentrations of particles in the size (D) range between 0.2 and 2 cm, as well as improved particle imagery, produced more comprehensive observations for tropical stratiform precipitation regions and anvils than have been available previously. Collocated radar observations provided additional information on the vertical structure of the cloud layers sampled. Most of the spirals began at cloud top, with temperatures (T) as low as −50°C, and ended at cloud base or below the melting layer (ML)....

[1]  N. Yoshizawa,et al.  Observation on Microphysical Processes in the Stratiform Precipitations Including Melting Layers at Mt. Fuji , 1985 .

[2]  D. Mitchell Evolution of Snow-Size Spectra in Cyclonic Storms. Part II: Deviations from the Exponential Form , 1991 .

[3]  Paul R. Field,et al.  Aircraft Observations of Ice Crystal Evolution in an Altostratus Cloud , 1999 .

[4]  Greg Michael McFarquhar,et al.  Microphysical Characteristics of Three Anvils Sampled during the Central Equatorial Pacific Experiment , 1996 .

[5]  Andrew J. Heymsfield,et al.  Parameterizations for the cross-sectional area and extinction of cirrus and stratiform ice cloud particles , 2003 .

[6]  Andrew J. Heymsfield,et al.  Precipitation Development in Stratiform Ice Clouds: A Microphysical and Dynamical Study , 1977 .

[7]  A. Heymsfield Ice Particle Evolution in the Anvil of a Severe Thunderstorm during CCOPE , 1986 .

[8]  Andrew J. Heymsfield,et al.  Structure of the Melting Layer in Mesoscale Convective System Stratiform Precipitation , 1989 .

[9]  D. Huffman,et al.  Measurements of the aerosol and ice crystal populations in tropical stratospheric cumulonimbus anvils , 1982 .

[10]  Guifu Zhang,et al.  A method for estimating rain rate and drop size distribution from polarimetric radar measurements , 2001, IEEE Trans. Geosci. Remote. Sens..

[11]  B. Ryan A Bulk Parameterization of the Ice Particle Size Distribution and the Optical Properties in Ice Clouds , 2000 .

[12]  W. Petersen,et al.  Microphysical Observations of Tropical Clouds , 2002 .

[13]  R. C. Srivastava,et al.  Snow Size Spectra and Radar Reflectivity , 1970 .

[14]  D. Parsons,et al.  Size Distributions of Precipitation Particles in Frontal Clouds. , 1979 .

[15]  Monika Hanesch Fall velocity and shape of snowflakes , 1999 .

[16]  Ken-ichiro Muramoto,et al.  A computer database for falling snowflakes , 1993, Annals of Glaciology.

[17]  S. K. Cox,et al.  Infrared Radiative Properties of Tropical Cirrus Clouds Inferred from Aircraft Measurements , 1980 .

[18]  Toshiaki Kozu,et al.  Rainfall Parameter Estimation from Dual-Radar Measurements Combining Reflectivity Profile and Path-integrated Attenuation , 1991 .

[19]  J. Livingston,et al.  Condensed Water in Tropical Cyclone "Oliver", 8 February 1993 , 1995 .

[20]  I. P. Mazin,et al.  An empirical model of the physical structure of upper-layer clouds , 1991 .

[21]  J. Iaquinta,et al.  A general approach for deriving the properties of cirrus and stratiform ice cloud particles , 2002 .

[22]  Paul L. Smith Equivalent Radar Reflectivity Factors for Snow and Ice Particles , 1984 .

[23]  Paul Racette,et al.  The EDOP Radar System on the High-Altitude NASA ER-2 Aircraft , 1996 .

[24]  Andrew J. Heymsfield,et al.  High Albedos of Cirrus in the Tropical Pacific Warm Pool: Microphysical Interpretations from CEPEX and from Kwajalein, Marshall Islands , 1996 .

[25]  Andrew J. Heymsfield,et al.  A Computational Technique for Increasing the Effective Sampling Volume of the PMS Two-Dimensional Particle Size Spectrometer , 1978 .

[26]  W. Rossow,et al.  Advances in understanding clouds from ISCCP , 1999 .

[27]  Tsutomu Takahashi,et al.  Precipitation Mechanisms of Cumulonimbus Clouds at Pohnpei, Micronesia , 1993 .

[28]  W. Collins,et al.  Cloud properties leading to highly reflective tropical cirrus: Interpretations from CEPEX, TOGA COARE, and Kwajalein, Marshall Islands , 1998 .

[29]  Andrew J. Heymsfield,et al.  Parameterization of Tropical Cirrus Ice Crystal Size Distributions and Implications for Radiative Transfer: Results from CEPEX , 1997 .

[30]  Q. Fu An Accurate Parameterization of the Infrared Radiative Properties of Cirrus Clouds for Climate Models , 1996 .

[31]  G. Gordon,et al.  Hydrometeor Evolution in Rainbands over the California Valley , 1986 .

[32]  P. Francis,et al.  Improved Measurements of the Ice Water Content in Cirrus Using a Total-Water Probe , 1995 .

[33]  Robert A. Houze,et al.  Comparison of Radar Data from the TRMM Satellite and Kwajalein Oceanic Validation Site , 2000 .

[34]  K. K. Lo,et al.  The Growth of Snow in Winter Storms:. An Airborne Observational Study , 1982 .

[35]  J. Wilson,et al.  Measurements of high number densities of ice crystals in the tops of tropical cumulonimbus , 1993 .

[36]  Fuk K. Li,et al.  ARMAR: An airborne rain-mapping radar , 1994 .

[37]  D. Mitchell Use of Mass- and Area-Dimensional Power Laws for Determining Precipitation Particle Terminal Velocities , 1996 .