Differences between collection 4 and 5 MODIS ice cloud optical/microphysical products and their impact on radiative forcing simulations

被引:54
|
作者
Yang, Ping [1 ]
Zhang, Lei
Hong, Gang
Nasiri, Shaima L.
Baum, Bryan A.
Huang, Hung-Lung
King, Michael D.
Platnick, Steven
机构
[1] Texas A&M Univ, Dept Atmospher Sci, College Stn, TX 77843 USA
[2] Lanzhou Univ, Coll Atmospher Sci, Lanzhou 730000, Peoples R China
[3] Univ Wisconsin, Ctr Space Sci & Engn, Madison, WI 53706 USA
[4] NASA, Goddard Space Flight Ctr, Div Earth Sci, Greenbelt, MD 20771 USA
来源
基金
美国国家航空航天局; 美国国家科学基金会;
关键词
Aqua; clouds; Moderate Resolution Imaging Spectroradiometer (MODIS); radiative forcing; remote sensing; static libraries;
D O I
10.1109/TGRS.2007.898276
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
This paper reports on the comparison of two latest versions (collections 4 and 5) of ice cloud products derived from the Moderate Resolution Imaging Spectroradiometer (MODIS) measurements. The differences between the bulk optical properties of ice clouds used in collections 4 and 5 and the relevant impact on simulating the correlation of the bidirectional reflection functions at two MODIS bands centered at 0.65 (or 0.86) and 2.13 mu m are investigated. The level-3 MODIS ice cloud properties (specifically, ice cloud fraction, optical thickness, and effective particle size in this paper) from the collection 4 and 5 datasets; are compared for a tropical belt of 30 degrees S-30 degrees N. Furthermore, the impact of the differences between the MODIS collection 4 and 5 ice cloud products on the simulation of the radiative forcing of these clouds is investigated. Over the tropics, the averaged ice cloud fraction from collection 5 is 1. 1% more than the collection 4 counterpart, the averaged optical thickness from collection 5 is 1.2 larger than the collection 4 counterpart, and the averaged effective particle radius from collection 5 is 1.8 mu m smaller than the collection 4 counterpart. Moreover, the magnitude of the differences between collection 5 and 4 ice cloud properties also depends on the surface characteristics, i.e., over land or over ocean. The differences of these two datasets (collections 4 and 5) of cloud properties can have a significant impact on the simulation of the radiative forcing of ice clouds. In terms of total (longwave plus shortwave) cloud radiative forcing, the differences between the collection, 5 and 4 results are distributed primarily between -60 and 20 W . m(-2) but peak at 0 W . m(-2).
引用
收藏
页码:2886 / 2899
页数:14
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