新托福阅读复习材料之美国科学文摘精选(二)
安之若素 2018-02-12     15:30 来源: 来自互联网
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摘要:托福阅读是托福考试中最容易拿高分的一项,但很多同学因为没有找到好的复习方法及材料而与高分失之交臂,今天三立在线教育托福网为大家带来新托福阅读复习材料之美国科学文摘精选(二),希望能帮助到正在托福备考的同学们。

托福阅读是托福考试中最容易拿高分的一项,但很多同学因为没有找到好的复习方法及材料而与高分失之交臂,今天三立在线教育托福网为大家带来新托福阅读复习材料之美国科学文摘精选(二),希望能帮助到正在托福备考的同学们。

新托福阅读复习材料之美国科学文摘精选(二)

The Planet Earth

The 2000 Antarctic Ozone Hole Was Largest Ever

The 2000 Antarctic Ozone Hole was the largest ever observed. Earth's wetter

upper atmosphere may delay global ozone recovery.

NASA researchers have found that an increase in water vapor in the

stratosphere, stemming partially from greenhouse gases, may delay ozone

recovery and increase the rate of climate change.

To check on the long-term stratospheric cooling and ozone depletion, NASA put

data from satellites and other remote sensors into its GISS global climate

model. It was the first study to link greenhouse gases to increased ozone

depletion over populated areas.

Water and ozone. Climate models show cooler stratospheric temperatures happen

when there is more water vapor present. Water vapor also leads to the

breakdown of ozone molecules.

The stratosphere is the dry layer of the atmosphere above the troposphere,

where temperatures increase with height.

According to satellite data, upper atmospheric temperatures around the world -

at altitudes of 20 to 35 miles high -- have cooled between 5.4 and 10.8

degrees Fahrenheit over recent decades.

Driving forces. NASA found two driving forces behind the change in

stratospheric moisture:

Increased emissions of the greenhouse gas methane are transformed into water

in the stratosphere, accounting for about a third of the observed increase

in moisture there.

More water is transported from the lower atmosphere. Warmer air holds more

water vapor than colder air, so the amount of water vapor in the lower

atmosphere increases as it is warmed by the greenhouse effect. Greenhouse

gases, such as carbon dioxide and methane, may enhance the transport of

water into the stratosphere.

The increased transport of water vapor to the stratosphere seems likely to

have been induced by human activities.

Ozone destruction. Rising greenhouse gas emissions account for all or part of

the water vapor increase, which causes stratospheric ozone destruction.

When more water vapor works its way into the stratosphere, the water molecules

can be broken down, releasing reactive molecules that can destroy ozone. If

the trend of increasing stratospheric water vapor continues, it could increase

future global warming and impede ozone stratospheric recovery.

The impact on global warming comes about because both water vapor and ozone

are greenhouse gases, which trap heat leaving the Earth. When they change, the

Earth's energy balance changes too, altering the surface climate.

Warmer ground. Increased water vapor in the stratosphere makes it warmer on

the ground by trapping heat, while the ozone loss makes it colder on the

ground.

Water vapor has a much larger effect, so that overall the changes increase

global warming.

Although ozone depletion cools the Earth's surface, repairing stratospheric

ozone is important to block harmful ultraviolet radiation. Other greenhouse

gas emissions also need to be reduced.

UARS satellite. NASA combined seven years of data from the Upper Atmosphere

Research Satellite (UARS) Halogen Occultation Experiment (HALOE) with data

collected on the ground to paint a complete picture of the upper atmosphere.

NASA's HALOE was aboard the UARS spacecraft when it was launched September 12,

1991 as part of the Earth Science Enterprise Program. The spacecraft's mission

at launch was to improve understanding of stratospheric ozone depletion by

analyzing vertical profiles of ozone, hydrogen chloride, hydrogen fluoride,

methane, water vapor, nitric oxide, nitrogen dioxide, and aerosols.

Fourteen years of lower stratospheric measurements have revealed large

increases in water vapor. Though some older studies conflict with lower

stratospheric observations of water vapor trends, new studies agree with the

increases, showing they have been taking place for more than four decades.

What Is An Ozone Hole?

Ozone molecules are made up of three atoms of oxygen. They comprise a thin

layer of the atmosphere that absorbs harmful ultraviolet radiation from the

Sun.

Most atmospheric ozone is found between approximately six miles and 18 miles

above the Earth's surface.

An ozone "hole" is what scientists call an "ozone depletion area" of in that

region of Earth's atmosphere.

Really big hole. The largest-ever ozone hole was detected on September 6,

2000, by the Total Ozone Mapping Spectrometer (TOMS) aboard a NASA satellite

known as Earth Probe (TOMS-EP).

The Antarctic ozone hole is three times larger than the entire land mass of

the United States, making it the largest such area ever observed.

The hole had expanded to a record size of 11 million square miles. The

previous record was 10.5 million square miles in September 1998.

Scientists were surprised by its enormous size. The lowest readings in the

Antarctic ozone hole usually are observed in late September or early October

each year.

Frail layer. The year 2000 observations reinforced concerns about the frailty

of Earth's ozone layer. Although production of ozone-destroying gases had been

curtailed under international agreements, concentrations of the gases in the

stratosphere have been reaching their peak.

Due to their long persistence in the atmosphere, it will be many decades

before the ozone hole is no longer an annual occurrence.

Antarctic vortex. The year 2000 saw an extremely intense Antarctic vortex --

an upper-altitude stratospheric air current that sweeps around the Antarctic

continent, confining the Antarctic ozone hole.

Variations in the size of the ozone hole and of ozone depletion accompanying

it from one year to the next are not unexpected.

NASA instruments have been measuring Antarctic ozone levels since the early

1970s. Since the discovery of the ozone hole in 1985, TOMS has been a key tool

for monitoring ozone levels above Earth.

TOMS-EP and other ozone-measurement programs are important parts of a global

environmental effort of NASA's Earth Science enterprise, a long-term research

program designed to study Earth's land, oceans, atmosphere, ice and life as a

total integrated system.

To learn more:

Goddard Institute for Space Studies

Upper Atmosphere Research Satellite

Halogen Occultation Experiment

Largest ozone hole detected by TOMS

TOMS ozone data and pictures

NASA Says Wet Upper Atmopsphere Delays Ozone Recovery

NASA Press Release: Wetter Atmopsphere May Delay Ozone Recovery

Inner Planets:MercuryVenusEarthMars

Outer Planets:JupiterSaturnUranusNeptunePluto

Other Bodies:MoonsAsteroidsComets The Voyagers

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