Detailed knowledge of each of the jet streams of the earth's hemispheres-
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3题
活塞环在工作中产生“跳环”现象是指________。
A.环紧压环槽上平面
B.环紧压环槽下平面
C.环悬浮在环槽中
D.环交替紧压环槽上下平面
第4题
活塞环在环槽中产生扭转与弯曲,其形成的原因是()。
A.环搭口间隙大
B.环平口磨损大
C.环弹力不足
D.环槽过度磨损
第5题
环槽端面磨损使______增大,使活塞环的密封性下降,产生漏气和降低压缩压力等问题。
A.活塞与气缸间隙
B.平面间隙
C.搭口间隙
D.环槽高度
第6题
活塞环在工作中较易产生“跳环”现象的运行工况是________。
A.低速、低负荷
B.低速、高负荷
C.高速、低负荷
D.高速、高负荷
第7题
环槽端面磨损使_______增大,使活塞环的密封性下降,产生漏气和降低压缩压力、爆发压力等问题
A.活塞与气缸间隙
B.平面间隙
C.搭口间隙
D.环槽高度
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