Significant changes between the ISCCP C and D cloud climatologies

被引:30
作者
Doutriaux-Boucher, M [1 ]
Seze, G
机构
[1] Univ Lille 1, UFR Phys, Opt Atmospher Lab, F-59655 Villeneuve Dascq, France
[2] Univ Paris 06, CNRS, Meteorol Dynam Lab, F-75252 Paris 05, France
关键词
D O I
10.1029/1998GL900081
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
We analyse one year of cloud data from the ISCCP C and D datasets. The two datasets differ by their retrieval algorithms and their definitions of the cloud types defined from the cloud top pressure and cloud optical depth. The differences between the two datasets are first described in terms of the total cloud cover, as well as its repartition in low, middle, and high level cloudiness. We also project the ISCCP C cloud classes into the ISCCP D cloud types to circumvent the problem of different cloud type definitions in the two datasets. The differences between the two datasets are then also investigated in terms of the most frequent cloud type.
引用
收藏
页码:4193 / 4196
页数:4
相关论文
共 20 条
[1]  
Brest CL, 1997, J ATMOS OCEAN TECH, V14, P1091, DOI 10.1175/1520-0426(1997)014<1091:UORCFI>2.0.CO
[2]  
2
[3]  
DOUTRIAUXBOUCHE.M, 1997, THESIS U P M CURIE
[4]  
HAN QY, 1994, J CLIMATE, V7, P465, DOI 10.1175/1520-0442(1994)007<0465:NGSOED>2.0.CO
[5]  
2
[6]   SPURIOUS CHANGES IN THE ISCCP DATASET [J].
KLEIN, SA ;
HARTMANN, DL .
GEOPHYSICAL RESEARCH LETTERS, 1993, 20 (06) :455-458
[7]   DIURNAL-VARIATION OF THE ISCCP CLOUDINESS [J].
KONDRAGUNTA, CR ;
GRUBER, A .
GEOPHYSICAL RESEARCH LETTERS, 1994, 21 (18) :2015-2018
[8]  
LAU NC, 1995, MON WEATHER REV, V123, P1984, DOI 10.1175/1520-0493(1995)123<1984:ASVOTS>2.0.CO
[9]  
2
[10]   COMPARISON BETWEEN SAGE-II AND ISCCP HIGH-LEVEL CLOUDS .1. GLOBAL AND ZONAL MEAN CLOUD AMOUNTS [J].
LIAO, XH ;
ROSSOW, WB ;
RIND, D .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1995, 100 (D1) :1121-1135