In the transportation field which is not from the application of solar cell?
A、Traffic light
B、Highway wireless telephone
C、The engines of buses
D、--
A、Traffic light
B、Highway wireless telephone
C、The engines of buses
D、--
第1题
A、Microwave relay station
B、Optical cable maintenance
C、Wired telephone
D、--
第2题
A、Oil drilling platform power supply.
B、Marine testing equipment.
C、A and B.
D、--
第3题
b.But since the Sun has no solid surface, it is hard to tell where the atmosphere ends and the main body of the Sun begins.
c.Starting at the outside and going down into the Sun, the zones are the corona, chromosphere, photosphere, convection zone, and finally the core.
d.Solar astronomers know that the Sun is divided into five layers or zones.
e.The first three zones are regarded as the Sun’s atmosphere.
The following sentences are from a paragraph, but they are in the wrong order.Choose the correct order from A, B, C, and D.______
A、c-d-e-b-a
B、d-b-a-c-e
C、c-e-d-b-a
D、d-c-e-b-a
第4题
A.The movement of water from freshwater bodies into the oceans
B.Solar energy in the atmosphere that produces rain over land and oceans
C.Water resources from oceans and freshwater sources inland
D.Transportation of water from oceans into the atmosphere and onto the land
第5题
its location, altitude and strength-is critical to modern-day weather
forecasting, as well as to more specific applications such as the routing of
Line aircraft. By way of definition, a jet in fluid dynamics is simply a core of fluid
(5) moving at a higher velocity than the surrounding fluid, and although
complicated to describe mathematically, the jet streams in the atmosphere are a
straightforward, natural result of the meridional (equator-to-pole) temperature
gradient in the earth' s atmosphere. Analogous flows exist on other planets with
substantial atmospheres having similar temperature gradients.
(10) The temperature gradient derives from the differential solar heating of the
spherical surface of a planet: the surface is generally warmest at the equator
and grows progressively cooler as one moves poleward. The centrifugal effects
of the earth's rotation, often called the Coriolis force, deflect the north-south
transport of heat from the equator to the poles into the predominantly east-west
(15) motion of the jet stream. The relative strength, or velocity, of the jet stream is
proportional to the intensity of this thermal gradient. During the winter
months, when the equator-to-pole temperature disparity is at its greatest, the
jet stream reaches its maximum velocity, while during the summer months,
when the temperature gradient between the equator and the pole is considerably
(20) less, the jet stream reaches its minimum velocity.
The jet stream does not maintain a straight, zonal flow from west to east
but rather takes on a more serpentine look, often with dramatic dips to the
south or rises to the north. There are two major reasons for these nonzonal
motions: the temperature gradient between the equator and the poles and the
(25) presence of land masses on the earth's surface. The meridional temperature
gradient between the equator and poles that gives rise to the jet stream also
produces secondary atmospheric circulations, or eddies which, referred to by
meteorologists as baroclinic waves, have a complex interaction with the jet
stream, one that is intriguingly two-sided. The eddies modify the distribution of
(30) temperature and kinetic energy within the atmosphere, a process that has a
pronounced effect on the location and movement of the jet stream, which itself
interacts with these waves, acting not only as a transport or steering
mechanism but transferring momentum and energy back to the waves.
The presence of land masses on the earth's otherwise watery surface also
(35) modifies the distribution of temperature, because continents heat and cool at a
dramatically slower rate than do the oceans. The topography of the land also
influences the jet stream's location-mountain ranges and plains on large
continents, for example, significantly imbalance the distribution of atmospheric
temperature, narrowing the jet stream. And since the jet stream is a thermally
(40) driven phenomenon, the more complicated the three-dimensional temperature
structure of the earth's atmosphere, the more "wand
A.interpret data
B.explain research methodology
C.evaluate a conclusion
D.suggest a new technique
E.describe a phenomenon
第6题
A.They are more reliable.
B.They have initial advantage.
C.They dont break down from time to time.
D.They are more economical over time.
第7题
The atmosphere is not just a protector but also a great transporter. The transport of water vapor in the atmosphere is an important mechanism by which heat energy is redistributed poleward. Heat energy absorbed at the equator is deposited at the poles and the temperature gradient between these regions is reduced. The circulation of the atmosphere and the weather it generates is but one example of the many complex, interdependent events of nature. The web of life depends on the proper functioning of these natural mechanisms for its continued existence.
Some argue that climate change is too complicated to be attributed only to human activity. For example, fossil studies of radiolaria, a group of one-celled animals characterized by silicon-containing shells, have given scientists a fairly accurate account of climatic conditions in the distant past. Geologists found these 450,000-year-old microorganisms pre served in cores of sediment taken beneath the floor of the Indian Ocean. They provide a re cord of cycles of climatic changes, determined by the alternating layers of species of warm and cold-preferring radiolaria. We now have confirmation that changes in the earth's orbital geometry caused the ice ages.
This does not let us off the hook because although we can hardly alter the basic forces at work that alter climate, even small contributions by humans can have dramatic effects. Given nature's interconnectedness, it is possible that the most serious threats have yet to be recognized.
The first paragraph of the text deals mainly with the earth atmosphere's.
A.sheltering effect
B.reviving effect
C.invigorating effect
D.cleansing effect
第8题
The atmosphere is not just a protector but also a great transporter. The transport of water vapor in the atmosphere is an important mechanism by which heat energy is redistributed poleward. Heat energy absorbed at the equator is deposited at the poles and the temperature gradient between these regions is reduced. The circulation of the atmosphere and the weather it generates is but one example of the many complex, interdependent events of nature. The web of life depends on the proper functioning of these natural mechanisms for its continued existence.
Some argue that climate change is too complicated to be attributed only to human activity. For example, fossil studies of radiolaria, a group of one-celled animals characterized by silicon-containing shells, have given scientists a fairly accurate account of climatic conditions in the distant past. Geologists found these 450, 000-year-old microorganisms preserved in cores of sediment taken beneath the floor of the Indian Ocean. They provide a record of cycles of climatic changes, determined by the alternating layers of species of warm and cold-preferring radiolaria. We now have confirmation that changes in the earth's orbital geometry caused the ice ages.
This does not let us off the hook because although we can hardly alter the basic forces at work that alter climate, even small contributions by humans can have dramatic effects. Given nature's interconnectedness, it is possible that the most serious threats have yet to be recognized.
The first paragraph of the text deals mainly with the earth atmosphere's ______.
A.sheltering effect
B.reviving effect
C.invigorating effect
D.cleansing effect
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