| contributor author | Sassen, Kenneth | |
| date accessioned | 2017-06-09T14:40:57Z | |
| date available | 2017-06-09T14:40:57Z | |
| date copyright | 1991/12/01 | |
| date issued | 1991 | |
| identifier issn | 0003-0007 | |
| identifier other | ams-24375.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4161040 | |
| description abstract | The development of the polarization lidar field over the past two decades is reviewed, and the current cloud-research capabilities and limitations are evaluated. Relying on fundamental scattering principles governing the interaction of polarized laser light with distinctly shaped hydrometers, this remote-sensing technique has contributed to our knowledge of the composition and structure of a variety of cloud types. For example, polarization lidar is a key component of current climate-research programs to characterize the properties of cirrus clouds, and is an integral part of multiple remote-sensor studies of mixed-phase cloud systems, such as winter mountain storms. Although unambiguous cloud-phase discrimination and the identification of some ice particle types and orientations are demonstrated capabilities, recent theoretical approaches involving ice crystal ray-tracing and cloud microphysical model simulations are, promising to increase the utility of the technique. New results simulating the single and multiple scattering properties of precipitating mixed-phase clouds are given for illustration of such methods. | |
| publisher | American Meteorological Society | |
| title | The Polarization Lidar Technique for Cloud Research: A Review and Current Assessment | |
| type | Journal Paper | |
| journal volume | 72 | |
| journal issue | 12 | |
| journal title | Bulletin of the American Meteorological Society | |
| identifier doi | 10.1175/1520-0477(1991)072<1848:TPLTFC>2.0.CO;2 | |
| journal fristpage | 1848 | |
| journal lastpage | 1866 | |
| tree | Bulletin of the American Meteorological Society:;1991:;volume( 072 ):;issue: 012 | |
| contenttype | Fulltext | |