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5. More Frequent <strong>and</strong> Severe Storms<br />

www.co2science.org<br />

P a g e | 50<br />

The claim: Among <strong>the</strong> many highly-publicized catastrophic consequences that climate alarmists<br />

contend will attend <strong>the</strong> ongoing rise in <strong>the</strong> air’s CO2 content are predicted increases in <strong>the</strong><br />

frequency <strong>and</strong> severity of a variety of different types of storms.<br />

In an effort to determine if this contention has any validity, many scientists have examined<br />

historical <strong>and</strong> proxy storm records in an attempt to determine how temperature changes of <strong>the</strong><br />

past millennium may have impacted <strong>the</strong> storminess of earth’s climate. Noting that <strong>the</strong> planet's<br />

mean temperature had risen by about 0.6 °C over <strong>the</strong> 20th century, for example, Easterling et<br />

al. (2000) looked for possible impacts of this warming on extreme wea<strong>the</strong>r events that <strong>the</strong>y<br />

said “would add to <strong>the</strong> body of evidence that <strong>the</strong>re is a discernable human affect on <strong>the</strong><br />

climate.” In doing so, however, <strong>the</strong>y found few changes of significance, <strong>and</strong> -- as might have<br />

been expected -- that “in some areas of <strong>the</strong> world increases in extreme events are apparent,<br />

while in o<strong>the</strong>rs <strong>the</strong>re appears to be a decline,” so that <strong>the</strong> overall global response was pretty<br />

much of a wash.<br />

In ano<strong>the</strong>r study of multiple severe wea<strong>the</strong>r phenomena, Kh<strong>and</strong>ekar (2003) briefly reviewed<br />

what he had learned about extreme wea<strong>the</strong>r events in Canada in <strong>the</strong> course of conducting a<br />

study of <strong>the</strong> subject for <strong>the</strong> government of Alberta. This review revealed that “extreme<br />

wea<strong>the</strong>r events such as heat waves, rain storms, tornadoes, winter blizzards, etc., [were] not<br />

increasing anywhere in Canada at [that] time,” while noting that a contemporary special issue<br />

of Natural Hazards (Vol. 29, No. 2, June 2003) concluded much <strong>the</strong> same thing about o<strong>the</strong>r<br />

parts of <strong>the</strong> world, citing in this context a survey article by Balling <strong>and</strong> Cerveny (2003) that<br />

concluded “<strong>the</strong>re is no significant increase in overall severe storm activity (hurricanes,<br />

thunderstorms/tornadoes, winter blizzards) across <strong>the</strong> conterminous United States,” as well as<br />

an article by Changnon (2003a), which concluded that “increasing economic loss due to<br />

wea<strong>the</strong>r extremes in <strong>the</strong> conterminous United States is a result of societal change <strong>and</strong> not<br />

global warming.”<br />

More specifically, Changnon determined that various U.S. wea<strong>the</strong>r extremes over <strong>the</strong> last 50<br />

years of <strong>the</strong> 20th century were mixed, reporting that “one trend is upwards (heavy rainsfloods),<br />

o<strong>the</strong>rs are downward (hail, hurricanes, tornadoes, <strong>and</strong> severe thunderstorms), <strong>and</strong><br />

o<strong>the</strong>rs are unchanging flat trends (winter storms <strong>and</strong> wind storms).” It should be added,<br />

however, that had <strong>the</strong> analysis of heavy rains-floods been extended back to <strong>the</strong> beginning of<br />

<strong>the</strong> 20th century, <strong>the</strong> longer-term behavior of this phenomenon would have been found to<br />

have been indicative of no net change over <strong>the</strong> past hundred years, as demonstrated by Kunkel<br />

(2003).<br />

Down in New Zeal<strong>and</strong>, De Lange <strong>and</strong> Gibb (2000) analyzed trends in sea level derived from<br />

several tide gauges located within Tauranga Harbor over <strong>the</strong> period 1960-1998. And in an<br />

examination of seasonal, interannual <strong>and</strong> decadal distributions of storm surge data, <strong>the</strong>y<br />

discovered a considerable decline in <strong>the</strong>ir annual numbers in <strong>the</strong> latter half of <strong>the</strong> record, while<br />

a similar trend was observed in <strong>the</strong> magnitude of storm surges.<br />

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