pleasing to the eye or mind as through beauty or charm
The electrical discharge takes place when the attractive tension between a region of negatively charged particles and a region of positively charged particles becomes so great that the charged particles suddenly rush together.
The electrical discharge takes place when the attractive tension between a region of negatively charged particles and a region of positively charged particles becomes so great that the charged particles suddenly rush together.
The electrical discharge takes place when the attractive tension between a region of negatively charged particles and a region of positively charged particles becomes so great that the charged particles suddenly rush together.
The electrical discharge takes place when the attractive tension between a region of negatively charged particles and a region of positively charged particles becomes so great that the charged particles suddenly rush together.
The electrical discharge takes place when the attractive tension between a region of negatively charged particles and a region of positively charged particles becomes so great that the charged particles suddenly rush together.
make ineffective by counterbalancing the effect of
The coming together of the oppositely charged particles neutralizes the electrical tension and releases a tremendous amount of energy, which we see as lightning.
The coming together of the oppositely charged particles neutralizes the electrical tension and releases a tremendous amount of energy, which we see as lightning.
extraordinarily large in extent or amount or power
The coming together of the oppositely charged particles neutralizes the electrical tension and releases a tremendous amount of energy, which we see as lightning.
The coming together of the oppositely charged particles neutralizes the electrical tension and releases a tremendous amount of energy, which we see as lightning.
of the immediate past or just previous to the present time
Recent measurements made in the field together with laboratory simulations offer a promising explanation of how this structure of charged particles forms.
assigning numbers to phenomena according to a rule
Recent measurements made in the field together with laboratory simulations offer a promising explanation of how this structure of charged particles forms.
a workplace for the conduct of scientific research
Recent measurements made in the field together with laboratory simulations offer a promising explanation of how this structure of charged particles forms.
the act of imitating the behavior of some situation
Recent measurements made in the field together with laboratory simulations offer a promising explanation of how this structure of charged particles forms.
a verbal commitment agreeing to do something in the future
Recent measurements made in the field together with laboratory simulations offer a promising explanation of how this structure of charged particles forms.
Recent measurements made in the field together with laboratory simulations offer a promising explanation of how this structure of charged particles forms.
an accident resulting from violent impact of a moving object
At such temperatures, the collision between the ice pellets and the ice crystals causes electrical charges to shift so that the ice pellets acquire a negative charge and the ice crystals become positively charged.
At such temperatures, the collision between the ice pellets and the ice crystals causes electrical charges to shift so that the ice pellets acquire a negative charge and the ice crystals become positively charged.
come into the possession of something concrete or abstract
At such temperatures, the collision between the ice pellets and the ice crystals causes electrical charges to shift so that the ice pellets acquire a negative charge and the ice crystals become positively charged.
characterized by denial or opposition or resistance
At such temperatures, the collision between the ice pellets and the ice crystals causes electrical charges to shift so that the ice pellets acquire a negative charge and the ice crystals become positively charged.
Below this large, cold, negatively charged region, the cloud is warmer than -15℃, and at these temperatures, collisions between ice crystals and falling ice pellets produce positively charged ice pellets that then populate a small region at the base of the cloud.
having a good chance of being the case or of coming about
Lightning that strikes the ground is the most likely to be destructive, so even though it represents only 20 percent of all lightning, it has received a lot of scientific attention.
Lightning that strikes the ground is the most likely to be destructive, so even though it represents only 20 percent of all lightning, it has received a lot of scientific attention.
Lightning that strikes the ground is the most likely to be destructive, so even though it represents only 20 percent of all lightning, it has received a lot of scientific attention.
Lightning that strikes the ground is the most likely to be destructive, so even though it represents only 20 percent of all lightning, it has received a lot of scientific attention.
Lightning that strikes the ground is the most likely to be destructive, so even though it represents only 20 percent of all lightning, it has received a lot of scientific attention.
consistent with systematic study of the physical world
Lightning that strikes the ground is the most likely to be destructive, so even though it represents only 20 percent of all lightning, it has received a lot of scientific attention.
Lightning that strikes the ground is the most likely to be destructive, so even though it represents only 20 percent of all lightning, it has received a lot of scientific attention.
Then a strong current of electrons follows that path from the cloud to the ground, and it is that current that illuminates the channel as the lightning we see.
Then a strong current of electrons follows that path from the cloud to the ground, and it is that current that illuminates the channel as the lightning we see.
a natural body of water flowing on or under the earth
When a stream of these negatively charged electrons comes within 100 meters of the ground it is met by a stream of positively charged particles that comes up from the ground.
The channel is only a few centimeters in diameter, but that is wide enough for electrons to follow the channel to the ground in the visible form of a flash of lightning.
characterized by or displaying affirmation or acceptance
The stream of positive particles that meets the surge of electrons from the cloud often arises from a tall pointed structure such as a metal flagpole or a tower.
The stream of positive particles that meets the surge of electrons from the cloud often arises from a tall pointed structure such as a metal flagpole or a tower.
The stream of positive particles that meets the surge of electrons from the cloud often arises from a tall pointed structure such as a metal flagpole or a tower.
Once a channel has been formed, it is usually used by several lightning discharges, each of them consisting of a stream of electrons from the cloud meeting a stream of positive particles along the established path.
Once a channel has been formed, it is usually used by several lightning discharges, each of them consisting of a stream of electrons from the cloud meeting a stream of positive particles along the established path.
According to paragraph 1, all of the following take place in the development of a flash of lightening except great tension between two oppositely charged regions an increase in negatively charged particles over positively charged particles oppositely charged particles coming together the release of electrical energy in the form of visible light 2.
According to paragraph 1, all of the following take place in the development of a flash of lightening except great tension between two oppositely charged regions an increase in negatively charged particles over positively charged particles oppositely charged particles coming together the release of electrical energy in the form of visible light 2.
a process of becoming larger or longer or more numerous
According to paragraph 1, all of the following take place in the development of a flash of lightening except great tension between two oppositely charged regions an increase in negatively charged particles over positively charged particles oppositely charged particles coming together the release of electrical energy in the form of visible light 2.
The author remarks that “Lightning that strikes the ground is the most likely to be destructive” in order to explain why this form of lightning has been investigated so much this form of lightning is not as common as lightning within a cloud scientific understanding of this form of lightning is important the buildup of positive charge on the ground beneath a storm cloud can have serious consequences
The author remarks that “Lightning that strikes the ground is the most likely to be destructive” in order to explain why this form of lightning has been investigated so much this form of lightning is not as common as lightning within a cloud scientific understanding of this form of lightning is important the buildup of positive charge on the ground beneath a storm cloud can have serious consequences
The author remarks that “Lightning that strikes the ground is the most likely to be destructive” in order to explain why this form of lightning has been investigated so much this form of lightning is not as common as lightning within a cloud scientific understanding of this form of lightning is important the buildup of positive charge on the ground beneath a storm cloud can have serious consequences
the condition of someone who knows and comprehends
The author remarks that “Lightning that strikes the ground is the most likely to be destructive” in order to explain why this form of lightning has been investigated so much this form of lightning is not as common as lightning within a cloud scientific understanding of this form of lightning is important the buildup of positive charge on the ground beneath a storm cloud can have serious consequences
The author remarks that “Lightning that strikes the ground is the most likely to be destructive” in order to explain why this form of lightning has been investigated so much this form of lightning is not as common as lightning within a cloud scientific understanding of this form of lightning is important the buildup of positive charge on the ground beneath a storm cloud can have serious consequences
a phenomenon that is caused by some previous phenomenon
The author remarks that “Lightning that strikes the ground is the most likely to be destructive” in order to explain why this form of lightning has been investigated so much this form of lightning is not as common as lightning within a cloud scientific understanding of this form of lightning is important the buildup of positive charge on the ground beneath a storm cloud can have serious consequences
It can be inferred from paragraph 2 that part of the reason that the top of a storm cloud becomes positively charged is that the top of the cloud is warmer than the middle of the cloud the middle of the cloud is already occupied by positively charged particles the negatively charged ice pellets are too heavy to be carried by the updrafts that move ice crystals collisions between ice pellets in the top of the cloud produce mainly positively charged particles 12.
A storm cloud first develops a positively charged layer at the top, then a negatively charged middle layer, and finally, a positively charged layer at the bottom.
Once a channel has been formed, it is usually used by several successive electrical discharges that illuminate the channel as flashes of lightning. 参考答案: 1. B 2. C 3. A 4. B 5. D 6. D 7. A 8. C 9. B 10. C 11. C 12. A 13. C 14. A separation of …
Created on Sat Feb 16 21:07:38 EST 2013
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