Scientists have discovered that for the last 160,000 years, at least, there has U" P1 }: m4 I \) c3 v( ~. _
been a consistent relationship between the amount of carbon dioxide in the air and
+ C; Z9 e _1 T& Y0 u( V7 fthe average temperature of the planet. The importance of carbon dioxide in
+ K3 |: w1 V, u( tregulating the Earth's temperature was confirmed by scientists working in eastern 3 K. ]0 q7 g, _
(5) Antarctica. Drilling down into a glacier, they extracted a mile-long cylinder of ice ! g/ v- u. A" w( X
from the hole. The glacier had formed as layer upon layer of snow accumulated year
" V( _* }, r* V `" Hafter year. Thus drilling into the ice was tantamount to drilling back through time.
9 M6 f( _1 N" bThe deepest sections of the core are composed of water that fell as snow ' G# e% q) @" l
160,000 years ago. Scientists in Grenoble, France, fractured portions of the core and 8 ^5 v' d5 d" _. W- Z: j7 c
(10)measured the composition of ancient air released from bubbles in the ice.
% j6 z: ^/ t) @4 q' O3 n+ tInstruments were used to measure the ratio of certain isotopes in the frozen water to " R6 u3 |& L3 h: r5 x8 p( n
get an idea of the prevailing atmospheric temperature at the time when that
( m* X2 L+ Z7 Q( x0 jparticular bit of water became locked in the glacier. + M- S- x" a+ z5 i B2 V, i
The result is a remarkable unbroken record of temperature and of atmospheric
: ^& q( ]% H& b; Y* J1 S; j* V2 y. `(15)levels of carbon dioxide. Almost every time the chill of an ice age descended on the 1 D, i; v8 I9 H0 O: Q
planet, carbon dioxide levels dropped. When the global temperature dropped 9°F (5 °C),
# R3 K |% Z4 A% M3 \0 G# j* Vcarbon dioxide levels dropped to 190 parts per million or so. Generally, as each
% T% `: H2 Z& v# ~ice age ended and the Earth basked in a warm interglacial period, carbon dioxide ; f3 n4 x$ a$ L3 t" Z* Z9 \
levels were around 280 parts per million. Through the 160,000 years of that ice
9 Q2 y; G5 @; _7 g(20)record, the level of carbon dioxide in the atmosphere fluctuated between 190 and
# @- P- W/ [* G280 parts per million, but never rose much higher-until the Industrial Revolution 3 @4 B& j7 W8 q9 C' Y! g
beginning in the eighteenth century and continuing today.
6 w; Q, s1 h; Z" c$ dThere is indirect evidence that the link between carbon dioxide levels and
4 Z( e9 V9 I) @' e$ h9 Hglobal temperature change goes back much further than the glacial record. Carbon & h/ U# v: s. B5 ^% K* B
(25) dioxide levels may have been much greater than the current concentration during the5 F5 f5 J- Q* ^( |/ f
Carboniferous period, 360 to 285 million years ago. The period was named for a
2 B: M+ Y) f9 e8 Nprofusion of plant life whose buried remains produced a large fraction of the coal
- [6 X% A4 d9 U0 ^0 i) bdeposits that are being brought to the surface and burned today. |