Synopsis A cloud climatology describes the time-averaged geographical distribution of cloud properties and their diurnal, seasonal, and interannual variations. Visible and infrared radiation measurements from space are used to obtain cloud top height, cloud optical thickness, and droplet sizes. Visual reports from surface observers on land and sea are used to obtain the frequency of occurrence and the amount of sky covered by each of the various cloud types such as cumulus, stratus, and cirrus. This article summarizes results from both analyses, emphasizing the half-century period of record available from the surface-based climatology.
[1]
Stephen G. Warren,et al.
A Survey of Changes in Cloud Cover and Cloud Types over Land from Surface Observations, 1971–96
,
2007
.
[2]
L. Jenne,et al.
Global distribution of total cloud cover and cloud type amounts over land
,
1986
.
[3]
W. Rossow,et al.
Advances in understanding clouds from ISCCP
,
1999
.
[4]
R. Chervin,et al.
Global distribution of total cloud cover and cloud type amounts over the ocean
,
1988
.
[5]
Stephen G. Warren,et al.
Variations in Cloud Cover and Cloud Types over the Ocean from Surface Observations, 1954-2008
,
2011
.