2D视频雨滴谱仪(2D-VIDEO-DISTROMETER,2DVD)由奥地利JOANNEUM RESEARCH 公司与欧洲太空局 / 欧洲空间技术中心（European Space Agency / European Space and Technology Centre）等机构开发，系统是通过两个摄像头对高速运动物体进行线形扫描，以定性定量记录降水过程、监测降雨详细情况的精密仪器，可测定降水总量、大小、强度、雨滴运动速度、雨滴大小、形状及雨滴分布等。它是目前测量降水与雨滴的最佳产品。  

1. 2D VIDEO DISDROMETER: A STUDY OF DIFFERENT CLIMATIC REGIMES 

YARITZA MEJIAS-ROLON,Undergraduate Student ,University of Puerto Rico at Mayagűez 

Mayagűez, Puerto Rico ,DR. V.N. BRINGI ,Professor,Colorado State University ,Fort Collins, Colorado 

2. Measurements of Precipitation Characteristics by a New Distrometer

M.Schönhuber1), H.E.Urban1), J.P.V.Poiares Baptista2), W.L.Randeu3) and W.Riedler 3)

1) Institute for Applied Systems Technology, JOANNEUM RESEARCH, Graz/Austria

2) ESA/ESTEC (XEP), Noordwijk, The Netherlands

3) Institute of Communications and Wave Propagation, Technical University Graz/Austria

3.An example of computational approach used for aerodynamic design of a rain Disdrometer Un exemple de méthode de calcul utilisée pour le dessin aérodynamique d’un disdromètre de pluie

EMAD HABIB, Graduate Research Assistant, Iowa Institute of Hydraulic Research, The University of Iowa, Iowa City, IA, 52242 USA

WITOLD F. KRAJEWSKI, Professor, Iowa Institute of Hydraulic Research, The University of Iowa, Iowa City, IA, 52242 USA

4. WEATHER RADAR VERSUS 2D-VIDEO-DISTROMETER DATA

M. Schönhuber1), H.E. Urban1), J.P.V. Poiares Baptista2), W.L. Randeu3) and W. Riedler3)

1) Institute for Applied Systems Technology, JOANNEUM RESEARCH, Graz/Austria

2) ESA/ESTEC (XEP), Noordwijk, The Netherlands

3) Institute of Communications and Wave Propagation, Technical University Graz/Austria

5.OBSERVATIONS OF WINTER STORMS WITH 2-D VIDEO DISDROMETER AND POLARIMETRIC RADAR

Kyoko Ikeda*, Edward A. Brandes, and Guifu Zhang

National Center for Atmospheric Research, Boulder, Colorado

Real-time measurements and analyses of precipitation micro-structure and dynamics W. L. Randeu1,2, M. Sch¨onhuber1, and G. Lammer1

1Institute of Applied Systems Technology, Joanneum Research GmbH, Graz/Austria

2Institute of Communications and Wave Propagation, Technical University Graz, Austria

6. DROP SIZE DISTRIBUTIONS IN OKINAWA, JAPAN, FROM 2D-VIDEO DISTROMETER AND C-BAND POLARIMETRIC RADAR

V.N. Bringi (1), K. Nakagawa (2), M. Thurai (1,2), H. Hanado (2), T. Iguchi (2)

Colorado State University, (2) Communications Research Laboratory, Japan

7.Investigation of rainfall microstructure and variability using vertically pointing radar and disdrometer M. Diederich1, S. Crewell1, C. Simmer1, and R. Uijlenhoet2

1Meteorological Institute University of Bonn

2Department of Environmental Sciences Wageningen University

8.Z-R (Radar Reflectivity-Rain rate) relationships derived from Czech Distrometer data

Fiˇser

Institute of Atmospheric Physics, AS CR, Bocni II, 1401, 141 31 Prague, Czech Republic

9. A Method For Estimating Rain Rate And Drop Size Distribution From Polarimetric Radar Measurements

Guifu Zhang, J. Vivekanandan, and Edward Brandes

National Center for Atmospheric Research

Research Application Program

P. O. Box 3000, Boulder, Colorado 80307

Tel: 303-497-8402, Fax: 303-497-8401

10.Sensitivity of 5-cm Wavelength Polarimetric Radar Variables to Raindrop Axial Ratio and Drop Size Distribution

T. D. KEENAN Bureau of Meteorology Research Centre, Melbourne, Victoria, Australia

L. D. CAREY  Colorado State University, Fort Collins, Colorado

D. S. ZRNIC´  NOAA/National Severe Storms Laboratory, Norman, Oklahoma

P. T. MAY  Bureau of Meteorology Research Centre, Melbourne, Victoria, Australia

11. Spurious power-law relations among rainfall and radar parameters By A. R. JAMESON1¤ and A. B. KOSTINSKI2

1RJH Scienti. c, Inc., USA

2Michigan Technological University, USA

13. EXPERIMENTAL AND NUMERICAL STUDIES OF SMALL-SCALE RAINFALL MEASUREMENTS AND VARIABILITY

W. F. Krajewski, A. Kruger and V. Nespor

Iowa Institute of Hydraulic Research, The University of Iowa, Iowa City, Iowa 52242, USA

14. NOTES AND CORRESPONDENCE When is Rain Steady?

R. JAMESON  RJH Scientific, Inc., El Cajon, California

B. KOSTINSKI   Department of Physics, Michigan Technological University, Houghton, Michigan