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DOI | 10.1029/2018JD028321 |
Differences in Ice Cloud Optical Depth From CALIPSO and Ground-Based Raman Lidar at the ARM SGP and TWP Sites | |
Balmes, K. A.1; Fu, Q.1; Thorsen, T. J.2 | |
2019-02-16 | |
发表期刊 | JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES |
ISSN | 2169-897X |
EISSN | 2169-8996 |
出版年 | 2019 |
卷号 | 124期号:3页码:1755-1778 |
文章类型 | Article |
语种 | 英语 |
国家 | USA |
英文摘要 | Ice cloud column optical depths from the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) satellite and ground-based Raman lidars (RLs) at the Atmospheric Radiation Measurement (ARM) Southern Great Plains (SGP) and Tropical Western Pacific (TWP) sites are compared for 8 and 4years, respectively. The cloudy mean ice cloud column optical depths from CALIPSO Version 4 data product with a horizontal resolution of 5km are 78% (63%) larger than those from the RLs with a resolution of 10min/30 m at SGP (TWP) for collocated transparent profiles. The main difference at SGP is caused by the lidar ratio that for CALIPSO is related to its treatment of the multiple scattering factor. The main difference at TWP is caused by the averaging resolution. Large differences in the optical depth distribution between the CALIPSO and RL are found for small optical depths at both sites, which are due to optically very thin clouds only detectable by the RLs. The differences in ice cloud column optical depth distributions and their mean values between the CALIPSO and RL can largely be reconciled over both sites after accounting for the averaging resolutions, lidar ratios along with the CALIPSO multiple scattering factor treatment, sensitivity to optically very thin ice clouds, and definition of transparent profiles. This work also examines in detail the lidar ratios that are directly observed by the RLs, which does not support the temperature-dependent parameterizations of ice cloud lidar ratio and multiple scattering factor used in CALIPSO's Version 4 data product. |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000459377000033 |
WOS关键词 | CIRRUS CLOUDS ; RADIATIVE PROPERTIES ; WATER-VAPOR ; SATELLITE-OBSERVATIONS ; AUTOMATED RETRIEVAL ; AEROSOL PROPERTIES ; TROPICAL CIRRUS ; PART I ; EXTINCTION ; CLIMATE |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/32319 |
专题 | 气候变化 |
作者单位 | 1.Univ Washington, Dept Atmospher Sci, Seattle, WA 98195 USA; 2.NASA, Langley Res Ctr, Hampton, VA 23665 USA |
推荐引用方式 GB/T 7714 | Balmes, K. A.,Fu, Q.,Thorsen, T. J.. Differences in Ice Cloud Optical Depth From CALIPSO and Ground-Based Raman Lidar at the ARM SGP and TWP Sites[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2019,124(3):1755-1778. |
APA | Balmes, K. A.,Fu, Q.,&Thorsen, T. J..(2019).Differences in Ice Cloud Optical Depth From CALIPSO and Ground-Based Raman Lidar at the ARM SGP and TWP Sites.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,124(3),1755-1778. |
MLA | Balmes, K. A.,et al."Differences in Ice Cloud Optical Depth From CALIPSO and Ground-Based Raman Lidar at the ARM SGP and TWP Sites".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 124.3(2019):1755-1778. |
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