Human Emissions Fuel Extreme Weather, Flooding That Harm Humans and the Environment

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    Two seminal Nature papers join growing body

    of evidence that human emissions fuel

    extreme weather, flooding that harm humans

    and the environment

    ByJoe Rommon Feb 16, 2011 at 5:12 pm

    Here we show that human-induced increases in greenhouse gases

    have contributed to the observed intensification of heavy

    precipitation events found over approximately two-thirds ofdata-covered parts of Northern Hemisphere land areas. These

    results are based on a comparison of observed and multi-model

    simulated changes in extreme precipitation over the latter half of the

    twentieth century analysed with an optimal fingerprinting technique.

    Changes in extreme precipitation projected by models, and thus the

    impacts of future changes in extreme precipitation, may be

    underestimated because models seem to underestimate the

    observed increase in heavy precipitation with warmingThats from the first of two seminal studies in Nature, Human

    contribution to more-intense precipitation extremes (subs. reqd). The

    second looked at Anthropogenic greenhouse gas contribution to flood

    risk in England and Wales in autumn 2000 (subs. reqd):

    Occurring during the wettest autumn in England and Wales since

    records began in 1766 these floods damaged nearly 10,000 properties

    across that region, disrupted services severely, and caused insuredlosses estimated at 1.3billion.

    Here we present a multi-step, physically based probabilistic event

    attribution framework showing thatit is very likely that global

    anthropogenic greenhouse gas emissions substantially

    http://thinkprogress.org/climate/2011/02/16/207545/two-nature-paper-join-growing-body-of-evidence-that-human-emissions-fuel-extreme-weather-flooding-that-harm-humans-and-the-environment/http://thinkprogress.org/climate/2011/02/16/207545/two-nature-paper-join-growing-body-of-evidence-that-human-emissions-fuel-extreme-weather-flooding-that-harm-humans-and-the-environment/http://thinkprogress.org/climate/2011/02/16/207545/two-nature-paper-join-growing-body-of-evidence-that-human-emissions-fuel-extreme-weather-flooding-that-harm-humans-and-the-environment/http://thinkprogress.org/climate/2011/02/16/207545/two-nature-paper-join-growing-body-of-evidence-that-human-emissions-fuel-extreme-weather-flooding-that-harm-humans-and-the-environment/http://thinkprogress.org/climate/2011/02/16/207545/two-nature-paper-join-growing-body-of-evidence-that-human-emissions-fuel-extreme-weather-flooding-that-harm-humans-and-the-environment/http://thinkprogress.org/climate/2011/02/16/207545/two-nature-paper-join-growing-body-of-evidence-that-human-emissions-fuel-extreme-weather-flooding-that-harm-humans-and-the-environment/http://thinkprogress.org/author/joe/http://thinkprogress.org/author/joe/http://thinkprogress.org/author/joe/http://www.nature.com/nature/journal/v470/n7334/full/nature09763.htmlhttp://www.nature.com/nature/journal/v470/n7334/full/nature09763.htmlhttp://www.nature.com/nature/journal/v470/n7334/full/nature09763.htmlhttp://www.nature.com/nature/journal/v470/n7334/full/nature09762.htmlhttp://www.nature.com/nature/journal/v470/n7334/full/nature09762.htmlhttp://www.nature.com/nature/journal/v470/n7334/full/nature09762.htmlhttp://www.nature.com/nature/journal/v470/n7334/full/nature09762.htmlhttp://www.nature.com/nature/journal/v470/n7334/full/nature09762.htmlhttp://www.nature.com/nature/journal/v470/n7334/full/nature09763.htmlhttp://www.nature.com/nature/journal/v470/n7334/full/nature09763.htmlhttp://thinkprogress.org/author/joe/http://thinkprogress.org/climate/2011/02/16/207545/two-nature-paper-join-growing-body-of-evidence-that-human-emissions-fuel-extreme-weather-flooding-that-harm-humans-and-the-environment/http://thinkprogress.org/climate/2011/02/16/207545/two-nature-paper-join-growing-body-of-evidence-that-human-emissions-fuel-extreme-weather-flooding-that-harm-humans-and-the-environment/http://thinkprogress.org/climate/2011/02/16/207545/two-nature-paper-join-growing-body-of-evidence-that-human-emissions-fuel-extreme-weather-flooding-that-harm-humans-and-the-environment/http://thinkprogress.org/climate/2011/02/16/207545/two-nature-paper-join-growing-body-of-evidence-that-human-emissions-fuel-extreme-weather-flooding-that-harm-humans-and-the-environment/
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    increased the risk of flood occurrence in England and Wales in

    autumn 2000.

    in nine out of ten cases our model results indicate that

    twentieth-century anthropogenic greenhouse gas emissions

    increased the risk of floods occurring in England and Wales in

    autumn 2000 by more than 20%, and in two out of three cases by

    more than 90%.

    Scientists have predicted for decades that human-caused global

    warming would increased extreme weather events that cause severe

    harm to humans, property, and the environment. These two studies are

    but the latest in a growing body of scientific literature demonstrating

    that these predictions are coming true now.

    They should help lay to rest the myth that human-caused global

    warming will contribute to grievous harm only in some far-off future.

    They also strongly support the view that the human-induced increases

    in greenhouse gases have contributed to the devastating extreme events

    that hit Australia and other parts of the world in the past several

    months, helping to drive up food prices (seehow extreme weather,

    climate change drive record food prices).

    The NYThas a great headline on this story, Research Links Heavy

    Rains and Snow to Humans. It is all heavy precipitation that humans

    are intensifying.

    Of course, many of our top climate scientists have been documenting

    and explaining these types of conclusions for a while. Ill list a bunch of

    the papers below. Kevin Trenberth, head of NCARs Climate Analysis

    Section, has a new paper out, Changes in precipitation with climate

    change that is well worth reading. So I asked him for a comment on

    these two studies. He told me:

    These studies are very reasonable, and the main mechanism is well

    understood: it relates to the increased moisture in the atmosphere with

    higher temperatures and warmer oceans. However, the studies may

    http://climateprogress.org/2011/01/20/lester-brown-extreme-weather-climate-change-record-food-prices/http://climateprogress.org/2011/01/20/lester-brown-extreme-weather-climate-change-record-food-prices/http://climateprogress.org/2011/01/20/lester-brown-extreme-weather-climate-change-record-food-prices/http://www.nytimes.com/2011/02/17/science/earth/17extreme.html?_r=1&partner=rss&emc=rss&pagewanted=printhttp://www.nytimes.com/2011/02/17/science/earth/17extreme.html?_r=1&partner=rss&emc=rss&pagewanted=printhttp://www.nytimes.com/2011/02/17/science/earth/17extreme.html?_r=1&partner=rss&emc=rss&pagewanted=printhttp://www.cgd.ucar.edu/cas/Trenberth/trenberth.papers/ClimateChangeWaterCycle-rev.pdfhttp://www.cgd.ucar.edu/cas/Trenberth/trenberth.papers/ClimateChangeWaterCycle-rev.pdfhttp://www.cgd.ucar.edu/cas/Trenberth/trenberth.papers/ClimateChangeWaterCycle-rev.pdfhttp://www.cgd.ucar.edu/cas/Trenberth/trenberth.papers/ClimateChangeWaterCycle-rev.pdfhttp://www.cgd.ucar.edu/cas/Trenberth/trenberth.papers/ClimateChangeWaterCycle-rev.pdfhttp://www.nytimes.com/2011/02/17/science/earth/17extreme.html?_r=1&partner=rss&emc=rss&pagewanted=printhttp://www.nytimes.com/2011/02/17/science/earth/17extreme.html?_r=1&partner=rss&emc=rss&pagewanted=printhttp://climateprogress.org/2011/01/20/lester-brown-extreme-weather-climate-change-record-food-prices/http://climateprogress.org/2011/01/20/lester-brown-extreme-weather-climate-change-record-food-prices/
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    well be conservative as the tools available (the climate models), do not

    simulate precipitation and all of its characteristics (intensity, frequency

    etc) as well as we would like to see.

    As the first study makes clear, future changes in extreme precipitation

    are likely to be worse than the models suggest.

    In anextended interviewlast year on the subject, Trenberth explained:

    I find it systematically tends to get underplayed and it often gets

    underplayed by my fellow scientists. Because one of the opening

    statements, which Im sure youve probably heard is Well you

    cant attribute a single event to climate change. But there is a

    systematic influence on all of these weather events now-a-daysbecause of the fact that there is this extra water vapor lurking

    around in the atmosphere than there used to be say 30 years

    ago. Its about a 4% extra amount, it invigorates the storms, it

    provides plenty of moisture for these stormsand its unfortunate

    that the public is not associating these with the fact that this is one

    manifestation of climate change. And the prospects are that these kinds

    of things will only get bigger and worse in the future.

    Lets hope these new studies helped put an end to the underplaying ofthe link between human caused emissions and the extreme weather

    events we are experiencing now.

    The Washington Post has a goodpieceon the two studies, Greenhouse

    gases led to increase in deluges, researchers say, with more quotes:

    Human influence on the climate system has the effect of intensifying

    precipitation extremes, said Francis Zwiers, a climate researcher at

    Environment Canada in Toronto and lead researcher on the first study.

    Zwiers and his team gathered 50 years of rainfall statistics, and

    compared those observations to predictions made by computer

    simulations of the 20th century climate.

    http://climateprogress.org/2010/06/14/ncar-trenberth-global-warming-extreme-weather-rain-deluge/http://climateprogress.org/2010/06/14/ncar-trenberth-global-warming-extreme-weather-rain-deluge/http://climateprogress.org/2010/06/14/ncar-trenberth-global-warming-extreme-weather-rain-deluge/http://voices.washingtonpost.com/post-carbon/2011/02/green_house_gases_led_to_incre.htmlhttp://voices.washingtonpost.com/post-carbon/2011/02/green_house_gases_led_to_incre.htmlhttp://voices.washingtonpost.com/post-carbon/2011/02/green_house_gases_led_to_incre.htmlhttp://voices.washingtonpost.com/post-carbon/2011/02/green_house_gases_led_to_incre.htmlhttp://climateprogress.org/2010/06/14/ncar-trenberth-global-warming-extreme-weather-rain-deluge/
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    Those simulations included the warming impact of the billions of tons of

    carbon dioxide human society has pumped into the atmosphere.

    The study found that observed increase in deluges cannot be explained

    by natural internal fluctuations of the climate system alone, saidZwiers. In other words, only the addition of greenhouse gases to the

    atmosphere explains why the United States and Canada have

    experienced a dramatic increase in heavy downpours.

    Large [rainfall] events are becoming larger, Zwiers said. His work

    found that from 1951 to 1999, the probability of heavy downpours

    becoming even more extreme grew by about 7 percent, a figure he

    characterized as really substantial.

    Richard Allan, a climate scientist at the University of Reading in

    England who was not part of the study, called the method employed by

    Zwiers very rigorous.

    He added, Theres already been quite a bit of evidence showing that

    there has been an intensification of rainfall events across the globe.

    But until now there had not been a study that formally identified thishuman effect on precipitation extremes, Zwiers said. This paper

    provides specific scientific evidence that this is indeed the case.

    Note that these studies do not extend beyond the year 2000, so they

    miss the hottest decade on record and the wettest year on record.

    You can see some of the amazing photos from the 2000 UK floodshere.

    http://www.guardian.co.uk/environment/gallery/2011/feb/16/floods-2000-climate-change-pictures#/?picture=371763964&index=1http://www.guardian.co.uk/environment/gallery/2011/feb/16/floods-2000-climate-change-pictures#/?picture=371763964&index=1http://www.guardian.co.uk/environment/gallery/2011/feb/16/floods-2000-climate-change-pictures#/?picture=371763964&index=1http://www.guardian.co.uk/environment/gallery/2011/feb/16/floods-2000-climate-change-pictures#/?picture=371763964&index=1
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    Heres some more quotes from leading scientists via Seth BorensteinsAPstory:

    Both studies should weaken the argument that climate change is a

    victimless crime, said Myles Allen of the University of Oxford. He co-

    authored the second study, which connected flooding and climate

    change in the United Kingdom. Extreme weather is what actually

    hurts people.

    Jonathan Overpeck, a University of Arizona climate scientist, who

    didnt take part in either study, praised them as sensible and

    particularly relevant given the array of extreme weather that weve

    seen this winter and stretching back over the last few years.

    Put the two papers together and we start to see an emerging

    pattern, said Andrew Weaver of the University of Victoria, who wasnt

    part of either study. We should continue to expect increased flooding

    associated with increased extreme precipitation because of increasingatmospheric greenhouse gas. And we have no one to blame but

    ourselves.

    Lets run through some of the other recent studies that support the

    conclusion that human-caused global warming is making weather more

    extreme:

    http://www.forbes.com/feeds/ap/2011/02/16/science-us-sci-climate-floods_8312043.htmlhttp://www.forbes.com/feeds/ap/2011/02/16/science-us-sci-climate-floods_8312043.htmlhttp://www.forbes.com/feeds/ap/2011/02/16/science-us-sci-climate-floods_8312043.htmlhttp://www.guardian.co.uk/environment/gallery/2011/feb/16/floods-2000-climate-change-pictures?picture=371763973http://www.forbes.com/feeds/ap/2011/02/16/science-us-sci-climate-floods_8312043.html
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    Study: Global warming is driving increased frequency of extreme wet or

    dry summer weather in southeast, so droughts and deluges are likely to

    get worse

    A new study by a Duke University-led team of climate scientistssuggests that global warming is the main cause of a significant

    intensification in the North Atlantic Subtropical High (NASH)

    that in recent decades has more than doubled the frequency of

    abnormally wet or dry summer weather in the southeastern

    United States.

    The modelsknown as Coupled Model Intercomparison Project Phase

    3 (CMIP3) modelspredict the NASH will continue to intensifyand expand as concentrations of carbon dioxide and other

    greenhouse gases increase in Earths atmosphere in coming

    decades.This intensification will further increase the

    likelihood of extreme summer precipitation variability

    periods of drought or deluge in southeastern states in coming

    decades, Li says.

    And one of mycommentersposted this list in response to the

    nonsensical quote by Pielke in the Wall Street Journal, Theres no

    data-driven answer yet to the question of how human activity has

    affected extreme weather. The first three may be the most relevant.

    Some observational, modelling and observational and modelling studies

    concerning the trends in temperature extremes and precipitation

    intensity. I have limited myself to material that has been released since

    2007 (when the last IPCC report was released); this is by no means a

    complete list. Not all of them directly challenge the claim about human

    activities affecting extreme weather, but I included them because theypoint to a coherent picture.

    Zhang et al. (2007):Detection of human influence on twentieth-century

    precipitation trends. (Nature)

    We show that anthropogenic forcing has had a detectable

    http://climateprogress.org/2010/10/28/global-warming-extreme-wet-dry-summer-weather-in-southeast-droughts-and-deluges/http://climateprogress.org/2010/10/28/global-warming-extreme-wet-dry-summer-weather-in-southeast-droughts-and-deluges/http://climateprogress.org/2010/10/28/global-warming-extreme-wet-dry-summer-weather-in-southeast-droughts-and-deluges/http://climateprogress.org/2010/10/28/global-warming-extreme-wet-dry-summer-weather-in-southeast-droughts-and-deluges/http://climateprogress.org/2011/02/11/the-world-bank-droughts-and-voodoo-economics/#comment-324978http://climateprogress.org/2011/02/11/the-world-bank-droughts-and-voodoo-economics/#comment-324978http://climateprogress.org/2011/02/11/the-world-bank-droughts-and-voodoo-economics/#comment-324978http://www.nature.com/nature/journal/v448/n7152/abs/nature06025.htmlhttp://www.nature.com/nature/journal/v448/n7152/abs/nature06025.htmlhttp://www.nature.com/nature/journal/v448/n7152/abs/nature06025.htmlhttp://www.nature.com/nature/journal/v448/n7152/abs/nature06025.htmlhttp://www.nature.com/nature/journal/v448/n7152/abs/nature06025.htmlhttp://www.nature.com/nature/journal/v448/n7152/abs/nature06025.htmlhttp://climateprogress.org/2011/02/11/the-world-bank-droughts-and-voodoo-economics/#comment-324978http://climateprogress.org/2010/10/28/global-warming-extreme-wet-dry-summer-weather-in-southeast-droughts-and-deluges/http://climateprogress.org/2010/10/28/global-warming-extreme-wet-dry-summer-weather-in-southeast-droughts-and-deluges/http://climateprogress.org/2010/10/28/global-warming-extreme-wet-dry-summer-weather-in-southeast-droughts-and-deluges/
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    influence on observed changes in average precipitation within

    latitudinal bands, and that these changes cannot be explained

    by internal climate variability or natural forcing. We estimate

    that anthropogenic forcing contributed significantly to observed

    increases in precipitation in the Northern Hemisphere mid-latitudes,drying in the Northern Hemisphere subtropics and tropics, and

    moistening in the Southern Hemisphere subtropics and deep tropics.

    The observed changes, which are larger than estimated from model

    simulations, may have already had significant effects on ecosystems,

    agriculture and human health in regions that are sensitive to changes

    in precipitation, such as the Sahel.

    Christidis et al. (2011):The role of human activity in the recentwarming of extremely warm daytime temperatures. (J. Climate).

    Our analysis is the first that attempts to partition the observed change

    in warm daytime extremes between its anthropogenic and natural

    components and hence attribute part of the change to possible causes.

    Changes in the extreme temperatures are represented by the temporal

    changes in a parameter of an extreme value distribution. Regional

    distributions of the trend in the parameter are computed with and

    without human influence using constraints from the global optimal

    fingerprinting analysis.Anthropogenic forcings alter the regionaldistributions, indicating that extremely warm days have

    become hotter.

    Zwiers et al. (2010):Anthropogenic Influence on Long Return Period

    Daily Temperature Extremes at Regional Scales.(J. Climate).

    We therefore conclude that the influence of anthropogenic

    forcing has had a detectable influence on extreme temperatures

    that have impacts on human society and natural systems atglobal and regional scales. External influence is estimated to have

    resulted in large changes in the likelihood of extreme annual maximum

    and minimum daily temperatures. Globally, waiting times for extreme

    annual minimum daily minimum and daily maximum temperatures

    events that were expected to recur once every 20 years in the 1960s are

    now estimated to exceed 35 and 30 years respectively. . In contrast,

    http://journals.ametsoc.org/doi/abs/10.1175/2011JCLI4150.1http://journals.ametsoc.org/doi/abs/10.1175/2011JCLI4150.1http://journals.ametsoc.org/doi/abs/10.1175/2011JCLI4150.1http://journals.ametsoc.org/doi/abs/10.1175/2011JCLI4150.1http://journals.ametsoc.org/doi/abs/10.1175/2010JCLI3908.1http://journals.ametsoc.org/doi/abs/10.1175/2010JCLI3908.1http://journals.ametsoc.org/doi/abs/10.1175/2010JCLI3908.1http://journals.ametsoc.org/doi/abs/10.1175/2010JCLI3908.1http://journals.ametsoc.org/doi/abs/10.1175/2010JCLI3908.1http://journals.ametsoc.org/doi/abs/10.1175/2010JCLI3908.1http://journals.ametsoc.org/doi/abs/10.1175/2011JCLI4150.1http://journals.ametsoc.org/doi/abs/10.1175/2011JCLI4150.1
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    waiting times for circa 1960s 20-year extremes of annual maximum

    daily minimum and daily maximum temperatures are estimated to

    have decreased to less than 10 and 15 years respectively.

    Krishnamurthy et al. (2009): Changing Frequency and Intensity ofRainfall Extremes over India from 1951 to 2003. (J. Climate).

    Statistically significant increasing trends in extremes of rainfall are

    identified over many parts of India, consistent with the indications from

    climate change models and the hypothesis that the hydrological cycle

    will intensify as the planet warms. Specifically, for the exceedance of

    the 99th percentile of daily rainfall, all locations where a significant

    increasing trend in frequency of exceedance is identified also exhibit a

    significant trend in rainfall intensity.

    Teixeira and Satyamurty (2011): Trends in the Frequency of Intense

    Precipitation Events in Southern and Southeastern Brazil during 1960-

    2004. (J. Climate).

    In both regions, annual heavy and extreme rainfall event frequencies

    present increasing trends in the 45-year period. However, only in

    Southern Brazil is the trend statistically significant. Although longer

    time series are necessary to ensure the existence of long term trends,

    the positive trends are somewhat alarming since they indicate thatclimate changes, in terms of rainfall regimes, are possibly under way in

    Brazil.

    Ding et al. (2009): Changes in hot days and heat waves in China during

    1961-2007. (Int. J. Clim.)

    Over most of China except northwestern China, the frequency of HDs

    was high during the 1960s-1970s, low in the 1980s, and high

    afterwards, with strong interannual variations. A remarkableincreasing trend of HDs occurred after the 1990s in all regions.

    Rodda et al.(2009): A comparative study of the magnitude, frequency

    and distribution of intense rainfall in the United Kingdom. (Int. J.

    Clim).

    Most noticeably, increases up to 20% have occurred in the north-west

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    of the country and in parts of East Anglia. There have also been

    changes in other areas, including decreases of the same magnitude over

    central England. The implications of these changes are considered.

    Kysel (2009): Recent severe heat waves in central Europe: how to viewthem in a long-term prospect? (Int. J. Clim).

    Owing to an increase in mean summer temperatures, probabilities of

    very long heat waves have already risen by an order of magnitude over

    the recent 25 years, and are likely to increase by another order of

    magnitude by around 2040 under the summer warming rate assumed

    by the mid-scenario. Even the lower bound scenario yields a

    considerable decline of return periods associated with intense heat

    waves. Nevertheless, the most severe recent heat waves appear to betypical rather of a late 21st century than a mid-21st century climate.

    Gallant and Karoly (2010): A Combined Climate Extremes Index for the

    Australian Region (J. Climate)

    Over the whole country, the results show an increase in the extent of

    hot and wet extremes and a decrease in the extent of cold and dry

    extremes annually and during all seasons from 1911 to 2008 at a rate of

    between 1% and 2% decade21. These trends mostly stem from changes

    in tropical regions during summer and spring. There are relationshipsbetween the extent of extreme maximum temperatures, precipitation,

    and soil moisture on interannual and decadal time scales that are

    similar to the relationships exhibited by variations of the means.

    However, the trends from 1911 to 2008 and from 1957 to 2008 are not

    consistent with these relationships, providing evidence that the

    processes causing the interannual variations and those causing the

    longer-term trends are different.

    Romps (2011): Response of Tropical Precipitation to Global Warming.

    (J. Atmos. Sci.)

    There are many properties of convection that can change as the

    atmosphere warms, each of which could produce deviations from CC

    scaling. These properties include the effective water-vapor gradient,

    cloud pressure depth, and cloud velocity. A simple theory is developed

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    that predicts the changes in these properties consistent with CC

    scaling. Convection in the cloud-resolving simulations is found to

    change as predicted by this theory, leading to an ~20% increase in local

    precipitation fluxes when the CO2 concentration is doubled. Overall, an

    increase in CO2 leads to more vigorous convection, composed of cloudsthat are wider, taller, and faster.

    Wentz et al. (2007): How Much More Rain Will Global Warming Bring?

    (Science).

    Climate models and satellite observations both indicate that the total

    amount of water in the atmosphere will increase at a rate of 7% per

    kelvin of surface warming. However, the climate models predict that

    global precipitation will increase at a much slower rate of 1 to 3% perkelvin. A recent analysis of satellite observations does not support this

    prediction of a muted response of precipitation to global warming.

    Rather, the observations suggest that precipitation and total

    atmospheric water have increased at about the same rate over the past

    two decades.

    Allan et al. (2010): Current changes in tropical precipitation.

    (Environmental research letters).

    Analysing changes in extreme precipitation using daily data within thewet regions, an increase in the frequency of the heaviest 6% of events

    with warming for the SSM/I observations and model ensemble mean is

    identified. The SSM/I data indicate an increased frequency of the

    heaviest events with warming, several times larger than the expected

    Clausius-Clapeyron scaling and at the upper limit of the substantial

    range in responses in the model simulations.

    Allan and sodden (2008): Atmospheric Warming and the Amplificationof Precipitation Extremes. (Science).

    We used satellite observations and model simulations to examine the

    response of tropical precipitation events to naturally driven changes in

    surface temperature and atmospheric moisture content. These

    observations reveal a distinct link between rainfall extremes and

    temperature, with heavy rain events increasing during warm periods

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    and decreasing during cold periods. Furthermore, the observed

    amplification of rainfall extremes is found to be larger than that

    predicted by models, implying that projections of future changes in

    rainfall extremes in response to anthropogenic global warming may be

    underestimated.

    Lenderink and Meijgaard (2008) Increase in hourly precipitation

    extremes beyond expectations from temperature changes. (Nature).

    Indeed, changes in daily precipitation extremes in global climate

    models seem to be consistent with the 7% increase per degree of

    warming given by the Clausius-Clapeyron relation3, 4, but it is

    uncertain how general this scaling behaviour is across timescales. Here,

    we analyse a 99-year record of hourly precipitation observations fromDe Bilt, the Netherlands, and find that one-hour precipitation extremes

    increase twice as fast with rising temperatures as expected from the

    Clausius-Clapeyron relation when daily mean temperatures exceed

    12C. In addition, simulations with a high-resolution regional

    climate model show that one-hour precipitation extremes increase at a

    rate close to 14% per degree of warming in large parts of Europe. Our

    results demonstrate that changes in short-duration precipitation

    extremes may well exceed expectations from the Clausius-Clapeyron

    relation.

    Of course, dont missTable 3.8in the IPCCs Fourth Assessment,

    Working Group I: The Physical Science Basis.

    Finally, we have one of my favorites,Record high temperatures far

    outpace record lows across U.S.:

    http://www.ipcc.ch/publications_and_data/ar4/wg1/en/ch3s3-8-5.html#table-3-8http://www.ipcc.ch/publications_and_data/ar4/wg1/en/ch3s3-8-5.html#table-3-8http://www.ipcc.ch/publications_and_data/ar4/wg1/en/ch3s3-8-5.html#table-3-8http://climateprogress.org/2010/02/11/science-meehl-ncar-record-high-temperatures-record-lows/http://climateprogress.org/2010/02/11/science-meehl-ncar-record-high-temperatures-record-lows/http://climateprogress.org/2010/02/11/science-meehl-ncar-record-high-temperatures-record-lows/http://climateprogress.org/2010/02/11/science-meehl-ncar-record-high-temperatures-record-lows/http://climateprogress.org/2010/02/11/science-meehl-ncar-record-high-temperatures-record-lows/http://climateprogress.org/2010/02/11/science-meehl-ncar-record-high-temperatures-record-lows/http://www.ipcc.ch/publications_and_data/ar4/wg1/en/ch3s3-8-5.html#table-3-8
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    Spurred by a warming climate, daily record high temperatures occurred

    twice as often as record lows over the last decade across the continental

    United States, new research shows. The ratio of record highs to lows is

    likely to increase dramatically in coming decades if emissions of

    greenhouse gases continue to climb.

    So yes, key weather events are becoming more extremeespecially

    deluges, heat waves, and droughtsas climate scientists have long

    predicted they would if atmospheric concentrations of greenhouse gases

    kept rising. And now we have solid attribution of that increase in

    extreme weather to human emissions in multiple independent studies.

    So lets move on from that debate and focus on how we best minimize

    the damage from future warmingaggressive greenhouse gas

    mitigation plus adaptation.

    http://www.ucar.edu/news/releases/2009/maxmin.jsphttp://www.ucar.edu/news/releases/2009/maxmin.jsphttp://www.ucar.edu/news/releases/2009/maxmin.jsphttp://www.ucar.edu/news/releases/2009/maxmin.jsphttp://www.ucar.edu/news/releases/2009/maxmin.jsphttp://www.ucar.edu/news/releases/2009/maxmin.jsphttp://www.ucar.edu/news/releases/2009/images/temps_2.jpghttp://www.ucar.edu/news/releases/2009/maxmin.jsphttp://www.ucar.edu/news/releases/2009/maxmin.jsphttp://www.ucar.edu/news/releases/2009/maxmin.jsphttp://www.ucar.edu/news/releases/2009/maxmin.jsphttp://www.ucar.edu/news/releases/2009/maxmin.jsp
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    Related Posts:

    The year of living dangerously. Masters: The stunning extremeswe witnessed gives me concern that our climate is showing the

    early signs of instability; Munich Re: The only plausibleexplanation for the rise in weather-related catastrophes is

    climate change

    Hansen: Would recent extreme events have occurred ifatmospheric carbon dioxide had remained at its pre-industrial

    level of 280 ppm? The appropriate answer is almost certainly

    not.

    http://climateprogress.org/2010/12/23/the-year-of-living-dangerously-masters-weather-extremes-climate-change/http://climateprogress.org/2010/12/23/the-year-of-living-dangerously-masters-weather-extremes-climate-change/http://climateprogress.org/2010/12/23/the-year-of-living-dangerously-masters-weather-extremes-climate-change/http://climateprogress.org/2010/12/23/the-year-of-living-dangerously-masters-weather-extremes-climate-change/http://climateprogress.org/2010/12/23/the-year-of-living-dangerously-masters-weather-extremes-climate-change/http://climateprogress.org/2010/12/23/the-year-of-living-dangerously-masters-weather-extremes-climate-change/http://climateprogress.org/2010/10/01/hansen-extreme-events-2010-2012-record-high-global-temperature/http://climateprogress.org/2010/10/01/hansen-extreme-events-2010-2012-record-high-global-temperature/http://climateprogress.org/2010/10/01/hansen-extreme-events-2010-2012-record-high-global-temperature/http://climateprogress.org/2010/10/01/hansen-extreme-events-2010-2012-record-high-global-temperature/http://climateprogress.org/2010/10/01/hansen-extreme-events-2010-2012-record-high-global-temperature/http://climateprogress.org/2010/10/01/hansen-extreme-events-2010-2012-record-high-global-temperature/http://climateprogress.org/2010/10/01/hansen-extreme-events-2010-2012-record-high-global-temperature/http://climateprogress.org/2010/10/01/hansen-extreme-events-2010-2012-record-high-global-temperature/http://climateprogress.org/2010/10/01/hansen-extreme-events-2010-2012-record-high-global-temperature/http://climateprogress.org/2010/12/23/the-year-of-living-dangerously-masters-weather-extremes-climate-change/http://climateprogress.org/2010/12/23/the-year-of-living-dangerously-masters-weather-extremes-climate-change/http://climateprogress.org/2010/12/23/the-year-of-living-dangerously-masters-weather-extremes-climate-change/