Article of Global Warming
Throughout
its long history, Earth has warmed and cooled time and again. Climate has
changed when the planet received more or less sunlight due to subtle shifts in
its orbit, as the atmosphere or surface changed, or when the Sun’s energy
varied. But in the past century, another force has started to influence Earth’s
climate: humanity
How
does this warming compare to previous changes in Earth’s climate? How can we be
certain that human-released greenhouse gases are causing the warming? How much
more will the Earth warm? How will Earth respond? Answering these
questions is perhaps the most significant scientific challenge of our time.
What is Global Warming?
Global
warming is the unusually rapid increase in Earth’s average surface temperature
over the past century primarily due to the greenhouse gases released as people
burn fossil fuels. The global average surface temperature rose 0.6 to 0.9
degrees Celsius (1.1 to 1.6° F) between 1906 and 2005, and the rate of
temperature increase has nearly doubled in the last 50 years. Temperatures are
certain to go up further.

Despite
ups and downs from year to year, global average surface temperature is rising.
By the beginning of the 21st century, Earth’s temperature was roughly 0.5
degrees Celsius above the long-term (1951–1980) average. (NASA figure adapted
from Goddard Institute for Space Studies Surface Temperature Analysis.)
Earth’s
natural greenhouse effect
Earth’s
temperature begins with the Sun.
Roughly 30 percent of incoming sunlight is reflected back into space by bright
surfaces like clouds and ice. Of the remaining 70 percent, most is absorbed by
the land and ocean, and the rest is absorbed by the atmosphere. The absorbed
solar energy heats our planet.
As
the rocks, the air, and the seas warm, they radiate “heat” energy (thermal
infrared radiation). From the surface, this energy travels into the atmosphere
where much of it is absorbed by water vapor and long-lived greenhouse gases
such as carbon dioxide and methane.
When
they absorb the energy radiating from Earth’s surface, microscopic water or
greenhouse gas molecules turn into tiny heaters— like the bricks in a
fireplace, they radiate heat even after the fire goes out. They radiate in all
directions. The energy that radiates back toward Earth heats both the lower
atmosphere and the surface, enhancing the heating they get from direct
sunlight.
This
absorption and radiation of heat by the atmosphere—the natural greenhouse
effect—is beneficial for life on Earth. If there were no greenhouse effect, the
Earth’s average surface temperature would be a very chilly -18°C (0°F) instead
of the comfortable 15°C (59°F) that it is today.
The
enhanced greenhouse effect
What
has scientists concerned now is that over the past 250 years, humans have
been artificially raising the concentration of greenhouse gases in the
atmosphere at an ever-increasing rate, mostly by burning fossil fuels, but also
from cutting down carbon-absorbing forests. Since the Industrial Revolution
began in about 1750, carbon dioxide levels have increased nearly 38 percent
as of 2009 and methane levels have increased 148 percent.
Discussion
of Sentence :
1.
How
will Earth respond?
This
sentence include to simple future tense, especially in interrogative sentence.
Simple
Future tense : S + Will + V1 ± O
Interrogative sentence : Question
Words + Auxiliary
+ Subject + V1 ± O
How + Will
+ Earth + respond ?
2. Earth’s temperature begins with the
Sun.
This sentence include to simple
present tense.
Simple present expresses daily
habits or usual activities. The simple present also expresses general
statements of fact. This sentence include to general statement of fact.
Simple present tense
: S + V1 ± O
Earth’s
temperature + begins + with the sun
3. Humans have been artificially
raising the concentration of greenhouse gases
This sentence
include to Present Perfect Progressive.
Present Perfect Progressive : Subject (I,You,We,They) / (He,She,It) + Have/Has + Been + V-Ing ± O
Humans +
Have + Been +
artificially raising + the concentration of greenhouse gases.


