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the explorers journal the climate change issue - The Explorers Club

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exploring <strong>climate</strong> <strong>change</strong> No. 1<br />

Venturing<br />

Of <strong>the</strong><br />

to <strong>the</strong> Ends<br />

Earth<br />

exploring our planet’s polar regions:<br />

chroniclers of <strong>the</strong> past and portents of <strong>the</strong> future<br />

by Paul Andrew Mayewski<br />

It has been 50 years since <strong>the</strong> first International<br />

Geophysical Year (IGY) invited <strong>the</strong> best minds in<br />

science from around <strong>the</strong> globe to join forces in tackling<br />

<strong>issue</strong>s such as understanding Earth’s oceans<br />

and atmosphere and <strong>the</strong> delicate relationship<br />

between <strong>the</strong>m. Since <strong>the</strong>n, many advances have<br />

been made in this area, among <strong>the</strong> most important,<br />

<strong>the</strong> understanding of <strong>the</strong> role of greenhouse<br />

gases such as carbon dioxide (CO 2<br />

) in determining<br />

Earth’s <strong>climate</strong>. In more recent years, a realization<br />

that gases such as CO 2<br />

are on <strong>the</strong> rise has led to an<br />

interest in determining and documenting past levels<br />

of greenhouse gases. Ga<strong>the</strong>ring such information,<br />

however, entails journeying literally to <strong>the</strong> ends of<br />

<strong>the</strong> Earth. For <strong>the</strong>re, locked in thousands of meters<br />

of ice, are records of our planet’s changing chemical<br />

and physical <strong>climate</strong> that stretch back nearly a<br />

million years.<br />

When I began my <strong>climate</strong> research nearly 40<br />

years ago, few in <strong>the</strong> scientific community regarded<br />

Earth’s polar regions as important to <strong>the</strong><br />

vast majority of civilization. At that time, Antarctica<br />

was viewed as not only a frozen continent but also<br />

a continent frozen in time. This view seemed to<br />

be amply supported by <strong>the</strong> ice-free valleys of <strong>the</strong><br />

Victoria Land Coast in East Antarctica, where<br />

rocks had been exposed to millions of years of<br />

wind erosion, creating timeless landscapes. <strong>The</strong><br />

vast interior of <strong>the</strong> polar plateau also appeared to<br />

be <strong>change</strong>less to <strong>the</strong> few limited expeditions that<br />

passed but once across <strong>the</strong> surface.<br />

Increased access to <strong>the</strong> most remote portions<br />

of Antarctica and <strong>the</strong> Arctic—afforded by aircraft<br />

and ship in recent years—complemented by our<br />

ability to mount lighter, faster, and more efficient<br />

expeditions and establish well-equipped field stations,<br />

has resulted in <strong>the</strong> acquisition of an abundance<br />

of information that is dramatically changing<br />

our understanding of <strong>the</strong> critical role polar regions<br />

play in Earth’s complex ecosystem.<br />

Remarkably, <strong>the</strong>se regions have now emerged<br />

as “first responders” for monitoring current <strong>climate</strong><br />

because <strong>the</strong>y are so sensitive to warming;<br />

<strong>the</strong> vast ice-trapped environmental libraries <strong>the</strong>y<br />

host chronicle hundreds of thousands of years of<br />

Earth’s <strong>climate</strong> history. <strong>The</strong> ice cores we extract<br />

from <strong>the</strong> polar regions contain highly robust records<br />

of past <strong>climate</strong>. <strong>The</strong>se ancient records not<br />

only allow us to better understand <strong>the</strong> long-term<br />

cyclical <strong>change</strong>s in <strong>climate</strong> caused by natural phenomena<br />

such as <strong>the</strong> 26,000-year precession of<br />

<strong>the</strong> equinoxes, which is in part responsible for <strong>the</strong><br />

ice ages; volcanic eruptions; and solar activity, but<br />

to separate <strong>the</strong>se factors from variations in <strong>climate</strong><br />

22 <strong>the</strong> <strong>explorers</strong> <strong>journal</strong>

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