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IPCC The Physical Science Basis
Chapter 3; Observations: Surface and Atmospheric Climate Change
http://www.ipcc.ch/pdf/assessment-report/ar4/wg1/ar4-wg1-chapter3.pdf
Page 275-277 Section 3.4.3 Clouds
Chapter 3; Observations: Surface and Atmospheric Climate Change
http://www.ipcc.ch/pdf/assessment-report/ar4/wg1/ar4-wg1-chapter3.pdf
Page 275-277 Section 3.4.3 Clouds
As noted in the TAR and extended with more recent studies,
surface observations suggest increased total cloud cover since
the middle of the last century over many continental regions
including the USA (Sun, 2003; Groisman et al., 2004; Dai et
al., 2006), the former USSR (Sun and Groisman, 2000; Sun et
al., 2001), Western Europe, mid-latitude Canada, and Australia
(Henderson-Sellers, 1992). This increasing cloudiness since
1950 is consistent with an increase in precipitation and a
reduction in DTR (Dai et al., 2006). However, decreasing
cloudiness over this period has been reported over China
(Kaiser, 1998), Italy (Maugeri et al., 2001) and over central
Europe (Auer et al.,2007). If the analyses are restricted to after
about 1971, changes in continental cloud cover become less
coherent. For example, using a worldwide analysis of cloud
data (Hahn and Warren, 2003; Minnis et al., 2004) regional
reductions were found since the early 1970s over western Asia
and Europe but increases over the USA.
In summary, while there is some consistency between
ISCCP, ERBS, SAGE II and surface observations of a reduction
in high cloud cover during the 1990s relative to the 1980s, there
are substantial uncertainties in decadal trends in all data sets
and at present there is no clear consensus on changes in total
cloudiness over decadal time scales.