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Xnn
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I will not comment about earthquakes and tsumani's.
However, there has been an increase in extreme precipitation
events due to global warming/greenhouse gases.
Basically, greenhouse gases have increased the ability
of the atmosphere to hold water vapor. It is not that
there are more storms than in the past, instead they are more intense.
http://www.ipcc.ch/pdf/assessment-report/ar4/wg1/ar4-wg1-chapter3.pdf
However, there has been an increase in extreme precipitation
events due to global warming/greenhouse gases.
Basically, greenhouse gases have increased the ability
of the atmosphere to hold water vapor. It is not that
there are more storms than in the past, instead they are more intense.
http://www.ipcc.ch/pdf/assessment-report/ar4/wg1/ar4-wg1-chapter3.pdf
Tropical cyclones making landfall in China are
a small fraction of the total storms, and no obvious long-term
trend can be discerned (He et al., 2003; Liu and Chan, 2003;
Chan and Liu, 2004). However, Emanuel (2005a) and Webster
et al. (2005, 2006) indicated that the typhoons have become
more intense in this region, with almost a doubling of PDI values
since the 1950s and an increase of about 30% in the number of
category 4 and 5 storms from 1990 to 2004 compared with 1975
to 1989.
Substantial increases are found in heavy precipitation
events. It is likely that there have been increases in the number
of heavy precipitation events (e.g., 95th percentile) within many
land regions, even in those where there has been a reduction in
total precipitation amount, consistent with a warming climate
and observed significant increasing amounts of water vapour
in the atmosphere. Increases have also been reported for rarer
precipitation events (1 in 50 year return period), but only a few
regions have sufficient data to assess such trends reliably.
Precipitation has generally increased over land north of
30°N over the period 1900 to 2005 but downward trends
dominate the tropics since the 1970s. From 10°N to 30°N,
precipitation increased markedly from 1900 to the 1950s, but
declined after about 1970. Downward trends are present in the
deep tropics from 10°N to 10°S, especially after 1976/1977.
Tropical values dominate the global mean. It has become
significantly wetter in eastern parts of North and South America,
northern Europe, and northern and central Asia, but drier in the
Sahel, the Mediterranean, southern Africa and parts of southern
Asia. Patterns of precipitation change are more spatially
and seasonally variable than temperature change, but where
signifi can't precipitation changes do occur they are consistent
with measured changes in stream flow.
Droughts have become more common, especially in the
tropics and subtropics, since the 1970s. Observed marked
increases in drought in the past three decades arise from more
intense and longer droughts over wider areas, as a critical
threshold for delineating drought is exceeded over increasingly
widespread areas. Decreased land precipitation and increased
temperatures that enhance evapotranspiration and drying
are important factors that have contributed to more regions
experiencing droughts, as measured by the Palmer Drought
Severity Index. The regions where droughts have occurred
seem to be determined largely by changes in SSTs, especially
in the tropics, through associated changes in the atmospheric
circulation and precipitation. In the western USA, diminishing
snow pack and subsequent reductions in soil moisture also
appear to be factors. In Australia and Europe, direct links to
global warming have been inferred through the extreme nature
of high temperatures and heat waves accompanying recent
droughts.
Tropospheric water vapour is increasing. Surface specific
humidity has generally increased after 1976 in close association
with higher temperatures over both land and ocean. Total
column water vapour has increased over the global oceans by
1.2 ± 0.3% per decade from 1988 to 2004, consistent in pattern
and amount with changes in SST and a fairly constant relative
humidity. Strong correlations with SST suggest that total
column water vapour has increased by 4% since 1970. Similar
upward trends in upper-tropospheric specific humidity, which
considerably enhance the greenhouse effect, have also been
detected from 1982 to 2004.