Carbon dioxide (CO2)
is the product obtained when humans burn fossil fuels for energy. CO2 is a greenhouse gas, meaning
that its presence in the atmosphere traps heat produced by incident sunlight, preventing its
release back into space. Although CO2
has been present in the atmosphere for millions of years, the amount added since
the industrial revolution began has been steadily increasing, and continues to
do so even at the present time. This is because the worldwide use offossil fuels has been growing at an ever-increasing rate since the industrial
revolution began.
Climate scientists
over the past several decades have developed climate models to reproduce past
global temperature trends and predict future trends. Models correctly reflect the temperature
increases of recent decades when the additional CO2 from burning
fossil fuels is included, but they fail to show the increases when this CO2
is omitted. With this success at reproducing past
behavior, scientists use climate models to project future developments. These predict increasing extremes of weather
and climate, including generally higher temperatures, and higher likelihoods of
heat waves and droughts, or of intense rainfall and floods, depending on
geographic location on Earth.
Extreme Weather
and Climate Events Have Been Increasing in Recent Years.
Two publications
reviewed here, detailing extreme weather events, avoid reliance on climate models. Rather, these publications analyze actual
weather and climate data, and use rigorous statistical methods to develop their
results and conclusions.
Hansen and
Coworkers Find That Extreme Events are Due to Increased Global Temperatures. James
Hansen is a veteran climate scientist at the National Aeronautics and Space
Administration’s Goddard Institute for Space Studies (GISS). He and his colleagues published “Perceptionof climate change” online in the Proceedings of the [U.S. ] National Academy of Sciences, on August
6, 2012 . (See
Details at the end of this post.)
They divided the Earth’s
surface into a grid and used recorded temperature data for each grid location
from 1951 to 2011. Their results show,
for example, that many grid locations for years in the period 2006-2011 had
average summer temperatures that were 2-3ºC
(3.6-5.4ºF) greater than the temperature that the same grid location had during
1951-1980, which the authors assigned as their base period. (See Details)
Several locations had annual average temperatures that were even higher.
Using rigorous
statistical analysis the authors further showed that, compared to the same base
period, the temperature variation for each of the decades 1981-1990, 1991-2000,
and 2001-2011, shifted successively to higher temperatures. More and more grid locations had decadal
average temperatures that were much higher than would be expected from the
normal variability observed during the base period (see Details).
Hansen and
coworkers call this unprecedented finding “probably the most important change”
from the base period, one characterizing a “new category of ‘extremely hot
summers’”. For example, the authors
state there is a “high degree of confidence that events such as the extreme
summer heat in [Russia ] in 2010 and Texas in 2011 were a consequence of global
warming”. Extreme summer heat can lead in some cases to severe droughts, and in
other cases to excessive rainfall and flooding; these two led to droughts.
The authors point
out that specific weather events that some invoke as leading to global warming,
such as blocking patterns and La Niña events, cannot be considered responsible
for the observed warming trend of the last 3 decades. These patterns have been occurring for a long
time, not just in the recent past. In
contrast, the extreme warming, such as documented in their paper, has arisen
only in conjunction with global warming.
Coumou and
Rahmstorf Find That Extreme Weather Events Are Linked to Human Activity. They
published the Perspective, “A decade of weather extremes”, in Nature Climate
Change, July 2012 (published online: 25 March 2012 | doi: 10.1038/nclimate1452). They reviewed the work of others detailing
extreme weather events occurring between 2000 and 2011 (see Details). Several record-breaking events were singled
out, detailing economic impacts and human costs. While
physical principles can help explain their occurrence, the authors rely on
statistical analysis to identify true outliers among weather events. For past events, this drives home that in the
decade under consideration, extreme events have occurred with unprecedented
frequency. The number of new record hot
days, analyzed on a monthly basis, is now more than three times that expected
if the climate were not undergoing a long-term warming trend. Climate models help substantiate this trend;
they predict higher record temperatures because of “human influence on the
climate”.
Extreme rainfall
events are also increasing in recent years.
This too is understandable on a physical basis; warm air has the
capacity to hold more water vapor than cool air (see this post). This extra moisture is then available for
precipitation should it condense out of the air. The authors also discuss the important role
that climate models play in understanding these events, and in helping
attribute their origins to particular causes.
Importantly, the
authors point out that “attribution is not a ‘yes or no’ issue as the media
might prefer, it is an issue of probability.”
Based on their analyses they conclude “it is very likely that several of
the unprecedented extremes of the past decade would not have occurred without
[man-made] global warming….now…the evidence is strong that [man-made],
unprecedented heat and rainfall extremes are here — and are causing intense
human suffering.”
The U. S. Is
Experiencing Its Hottest Year-To-Date On Record. The
National Climatic Data Center of the U. S. National Oceanic and Atmospheric
Administration reports
(accessed Aug. 10, 2012) that July 2012 was the hottest month on record, since
recordkeeping began in 1895. The July
average temperature was 3.3ºF (1.8ºC) above the average for that month. In addition, the period January-July 2012 was
the hottest year-to-date, and the previous 12 month period was the hottest for
that window on record.
The January-July
2012 period was also the twelfth driest recorded. As of early August 2012 “moderate
to exceptional drought” conditions prevailed over 62.9% of the 48 contiguous
states of the U. S. Current news
accounts relate that the drought conditions are already reducing U. S. agricultural crop yields. It is expected as a result that global food
prices are likely to be several percent higher than usual during this year and
extending into 2013.
While these
phenomena are consistent with expected trends arising from a long-term increase
in the U.
S.
average temperature, it is too early for rigorous analysis to have been made
for the events in 2012.
Analysis
The papers by
Hansen and coworkers, and Coumou and Rahmstorf, examine recent extreme temperature
and precipitation events. Their results
are highly significant, for each separately shows by statistical analysis of past
temperature records that the differences of the observed temperatures from
expected averages are so large that they would be extremely improbable in a
climate that was not warming. Rather,
the occurrence of these extreme events is a hallmark of the warming of the
planet. The authors conclude that it is
very highly probable that these events arise from that warming, perhaps added
to effects of other, more short-term climate patterns (La Niña/El Niño, jet
stream blocking patterns). (These other
effects have always been occurring, including during times that predate the
rise in global average temperature. In
those times extreme events such as are now occurring did not arise.)
These papers
complement two reports over a year ago that for the first time directly linked
extremes of rainfall and flooding to the warming of the average global
temperature as a result of greenhouse gas emissions (see this post). Statistical analyses of rainfall and flooding
were used to correlate observed rainfall patterns or flooding resulting from
heavy rains to the predictions of several climate models.
Most CO2,
and certain other greenhouse gases, persist in the atmosphere for hundreds, or
even a thousand years. For this reason,
within the 1-3 decade time frame under discussion for abating long-term warming
of the planet, their concentration in the atmosphere can never be significantly
reduced, but at best can only be held constant at today’s level or the higher
level reached at some time in the future.
Even if all emissions were to cease right away, the CO2
concentration would remain constant. That is why the European Union’s Roadmap,
to lower emissions by 80-95% by 2050, is so significant and praiseworthy. Even so, however, new emissions from those
nations will continue to accumulate, at lower and lower annual rates, so that
concentrations by 2050 will still be higher than now because of continued emission
during the intervening years.
The use of fossil
fuels for energy around the world is projected to increase, not to level off or
decrease, in the foreseeable future. The
U. S. Energy Information Agency projects worldwide energy usage from 2008 through
2035 will increase, reaching 53% higher in 2035 than in 2008. Much of that increase will arise in China , India and other developing countries. 80% of the energy needs will still be
furnished by burning fossil fuels. Thus
the annual rate of emitting CO2 worldwide will be increasing
significantly in coming decades, and the corresponding accumulated level of
atmospheric CO2 will be considerably higher than it is today.
This means that the
occurrence of extreme weather events such as analyzed here will be more
frequent and/or intense, and damages inflicted on humanity as a result (see the
table in Details and this post, for example) will likewise be more severe.
The economic expenses of responding to weather-inflicted tragedies are
borne by governments and their taxpayers, as well as by private insurers. Any food shortages from droughts or floods will
be felt worldwide as increased food prices.
Dealing with the
worsening increases in global average temperatures can be approximated as a
zero-sum enterprise. On the one hand,
the governments of the world, and private corporations, can undertake
investment as soon as possible to develop energy alternatives that contribute
to lowering the rate of greenhouse gas emissions. Those investments would have the beneficial
effect of contributing to a reduction in extreme weather-related disasters and
their resulting damages. On the other
hand, we can persist in business-as-usual, with the certainty that relief and
restitution expenditures will continue increasing. The choice is ours to make.
Details
Hansen and
coworkers analyzed
world-wide weather data accumulated at GISS.
On a globally based grid they determined average annual temperatures and
standard deviations (SD values, measures of variability) of the annual temperatures
for each grid position.
(Standard deviation
is a measure of variability
observed in repeated measurements for a particular data item such as
temperature; in this case the variability is over the time interval
considered. For a typical “bell shaped”
curve expected for random variations of the data item, 1 SD on either side of
the average value at the top of the “bell” contains 67% of all the measurements;
2 SDs on either side contains 97% of all the measurements; and 3 SDs contain
99.8% of all the measurements.)
Hansen and
coworkers evaluated data sets covering 1951 to 2011. They used the period 1951-1980 to establish
baseline values for the averages and the SDs for each grid position against
which differences that have arisen in more recent years were determined.
Examples for one
year from the base period, 1965, and the recent year 2010 are shown below.
Global grids in the
years 1965 and 2010. The maps show
temperature differences from average values for each location determined over
1951-1980 in ºC for the months June through August. Each grid location is color coded for the
difference from the average for that location according to the color scale at
the bottom (gray indicates locations with no data).
Source: Proceedings
of the [U.S. ] National Academy of Sciences; www.pnas.org/cgi/doi/10.1073/pnas.1205276109
The map display for
1965, within the base period, shows that globally, temperature differences from
local averages were both negative (cooler) and positive (warmer) compared to
the averages. The magnitudes of the
differences, using the color scale for temperature in ºC, were relatively
small. On the other hand, many grid
locations for years in the period 2006-2011 had average annual temperatures
that were 2-3ºC (3.6-5.4ºF) greater than the temperature that the same grid
location had in the base period of 1951-1980; and indeed several locations had
annual average temperatures that were even more than 3ºC higher than those in
the base period. The global display for
2010, above, shows that extreme hot weather prevailed over a large part of
Eurasian Russia, and relatively hot areas in portions of China and the southeastern U. S. The corresponding map for 2011 (not shown
here) clearly shows the extreme heat differences (greater than 3ºC) experienced
in the south central portion of the U. S. in that year. (In the 2006-2011 interval, there were
relatively very few grid locations with temperatures below those of the base
period in a given year, and the extent of the negative difference was much less
than the positive differences just specified.)
The authors
continued with a rigorous statistical analysis of the data they collated, shown
below.
Frequency
distributions for each value of the variability (SD) found for successive
ten-year global average temperatures.
These curves may be considered as highly compressed histograms showing
the fractional occurrence for each value of SD.
(All curves sum to 1.000.) The
curve for a set of numbers that would be found from fully random valuations
about the average (“bell-shaped curve”) is shown in black. Any deviation from the bell-shaped curve
shows the existence of a bias in the distribution of the values. Decades in the base period are: crimson, 1951-1961; yellow,
1961-1971; and green, 1971-1981. Decades showing warming are aqua, 1981-1991; dark
blue, 1991-2001; and magenta,
2001-2011.
Source: Proceedings
of the [U.S. ] National Academy of Sciences; www.pnas.org/cgi/doi/10.1073/pnas.1205276109
Using the base
period 1951-1981, they showed that ten-year distributions for the measure of
variability, the standard deviation, closely followed the “bell-shaped curve” (black
curve in the figure) expected for random, unbiased data sets for the three
decades of the base period (as is expected).
But for each of the decades 1981-1991, 1991-2001, and 2001-2011, the variability
distribution shifts more and more to higher (i.e. positive) standard deviation
values as time passes. This indicates
that more and more grid locations had decadal average temperatures that were
much higher than would be expected from the normal variability of the base
period. Whereas the base period had
essentially no grid locations with temperatures that were 3 standard deviations
above the average (the unbiased bell curve would have only 1 in 769 data points
at that position), by the time of the most recent decade, about 10% (1 in 10
data points for land-based grid locations) had temperatures 3 standard
deviations above the average, and many data points whose temperatures gave even
4 and 5 standard deviations above the averages of the base period (see the
figure).
Coumou and
Rahmstorf reviewed extreme
weather events during the decade of 2000 to 2011. These included both high temperature events
and heavy rainfall events, and their consequences. Examples they chose for mention are shown in
the following table.
Year
|
Region
|
Meteorological
record-breaking event
|
Impact, costs
|
2000
|
Wettest autumn on record83
since 1766.
|
£1.3 billion (ref. 27).
|
|
2002
|
Highest daily rainfall
record in Germany42 since
at least 1901.
|
Flooding of
|
|
2003
|
Hottest summer in at least
500 years30.
|
Death toll exceeding 70,000
(ref. 31).
|
|
2004
|
First hurricane in the
|
Three deaths, US$425 million
damage85.
|
|
2005
|
Record number of tropical
storms, hurricanes and category 5 hurricanes52 since 1970.
|
Costliest
|
|
2007
|
Strongest tropical cyclone
in the Arabian Sea53 since 1970.
|
Biggest natural disaster in
the history of Oman53.
|
|
May–July wettest since
records began in 1766 (ref. 43).
|
Major flooding causing ~£3
billion damage.
|
||
Hottest summer on record in
Greece33
since 1891.
|
Devastating wildfires.
|
||
2009
|
Heatwave breaking many
station temperature records (32–154 years of data)34
|
Worst bushfires on record,
173 deaths, 3,500 houses destroyed34.
|
|
2010
|
Hottest summer since 1500
(ref. 69).
|
500 wildfires around
|
|
Rainfall records44.
|
Worst flooding in
|
||
Eastern Australia
|
Highest December rainfall recorded since 1900
(ref. 45).
|
Brisbane flooding in January 2011, costing 23
lives and an estimated US$2.55 billion86
|
|
2011
|
Most active tornado month on
record (April)3 since 1950.
|
Tornado hit
|
|
January–October wettest on
record1 since 1880.
|
Severe floods when Hurricane
Irene hit.
|
||
Most extreme July heat and
drought since 18802.
|
Wildfires burning 3 million
acres (preliminary impact of US$6–8 billion).
|
||
Hottest and driest spring on
record in France1 since
1880.
|
French grain harvest down by
12%.
|
||
Wettest summer on record
(The Netherlands,
|
Not yet documented.
|
||
72-hour rainfall record (Nara Prefecture)1.
|
73 deaths, 20 missing, severe damage.
|
||
Wettest summer on record1
since 1908.
|
Flooding of
|
© 2012 Macmillan
Publishers Limited
The causes of
extreme weather events can be difficult to pin down. Climate models are useful in projecting
long-term and large scale trends across broad regions of the planet. They are less adept at correlating local or
regional weather events such as these with
large scale trends. For this reason, the
authors note, rigorous statistical analysis is helpful to identify that a
particular event actually falls outside the realm of what would be expected if
the climate were not changing due, for example, to the man-made greenhouse
effect.
Statistical
evaluation of extreme heat events shows that, considered globally, the number
of monthly average temperature records occurring at present is as high as three
times what would be expected if the climate were not changing to higher
temperatures. This is shown in the
graphic below.
© 2012 Macmillan
Publishers Limited
Source: Nature
Climate Science doi: 10.1038/nclimate1452
It is seen that the
ratio of the observed number of monthly average records to that expected in an
unchanging climate begins to grow higher than the value of 1 as early as about
1920. The ratio has grown to values in
the range of 3.0 to 3.5 by 1990.
The table above
also includes many extreme rainfall events and the floods that ensued from
them.
Extremes will
result not simply from the long-term trend of increasing average global
temperatures. Coumou and Rahmstorf point
out, as do Hansen and coworkers, that the Pacific Ocean pattern of La Niña/El Niño/Southern Oscillation,
as well as blocked jet stream patterns, affect shorter term climate and weather
events. They conclude that statistical
analysis of past weather data, modeling of climate events, and reasoning based
on physical principles all have a place in assessing the progress of global
warming. They find that heatwaves and
precipitation extremes have already greatly increased and will continue to do
so as the climate warms further.
Coumou and Rahmstorf include a
graphic that originally appeared in a paper by Barriopedro, D. et al. (Science
332, 220–224 (2011)) dealing with the temperature
extreme in Russia in 2010 (see the table) . It shows that, over the 500 year period from
1500 to 2010, extremes of 10-year average temperatures exceeding the 95th
percentile expected from only random variability occurred only after 2000. The extreme heat waves in Europe in 2003 and
2010 (see the table above), they write, are likely due partly to the long-term
trend of increasing global temperatures (from the man-made greenhouse effect),
and partly to “atmospheric dynamical processes” such as unusual weather pattern
blocking effects. They believe that such
causes have to be considered additive, and not mutually exclusive, in
understanding the causes of these extreme events.
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